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iBook The Future of the Universe - 2. It’s a Matter of Time

2. It’s a Matter of Time


The Sun is the lifeblood of humanity. It warms us and gives us light. Although our everyday existence depends upon the Sun, the evolution of life on Earth was only possible because the Sun and the Solar System are partly composed of the embers cast into space by a long line of stellar ancestors. Indeed, the intricate and multitudinous steps that have paved the way to our existence started as soon as the Milky Way galaxy formed some 12 to 13 billion years ago. Step by tiny step our journey has been traced out. We are both ancient and modern, with our bodies being composed of archaic matter forged in the unimaginably intense fires of the primordial moment of creation (the so-called Big Bang) and from matter transformed and fused in the dense and blistering hot cores of massive stars. The calcium that is contained within the bones that animate our all-too-temporary bodies was formed in the violence of star explosions. As pioneer astrophysicist Sir Arthur Eddington once so aptly put it, “We are the journey work of the stars.” Every atom in the universe, other than those atoms of hydrogen and helium,1 was made by the Sun’s distant ancestors, generated piece by piece from the time of the first stars onward. Earth and the life that teems on, above, and through it; the other planets that orbit the Sun; their attendant satellites, and the swarm of comets that surrounds the Solar System, are all made of material produced by long-dead stars. The Sun provides Earth with energy. If it were not for the Sun, we would not be here—it’s as simple as that. It is also because of the Sun, however, that we may not be here forever. Deep within the Sun there is a demon, a lurking monster that will eventually see release and, if nothing is done to tame it, it will destroy all life on Earth. We are in the midst of a horror movie. The twist, however, is that we know the cause from the very outset. Indeed, the only part of the movie that we don’t know is exactly when 23 24 Rejuvenating the Sun and Avoiding Other Global Catastrophes the horror will be perpetrated. We can be fairly sure the demon won’t be released in our lifetime; even our descendants a million generations from now will not necessarily be its victims. Although we live in the midst of this movie, we will never know the final outcome of the saga. It is our distant descendants (perhaps 50 million generations from now) that will face the demon in the Sun—unless, that is, they do something about it, and for the present we can only guess at how well they might fare. Not only will we not know the outcome of this story, there is the open-ended possibility that no destruction will actually be perpetuated. Perhaps our distant descendants will actually survive the onslaught. Time and Transformation What is this demon that lies in the Sun? It is, in fact, the very two-headed demon that led to our existence in the first place: time and transformation. The Sun is converting a staggering (that is, by human standards) 4 billion kilograms of matter (actually hydrogen; see below) into energy every second of the day, day after day after day. Since it formed some 4.56 billion years ago, the Sun has converted about 6 x 1026 kg of matter into energy. That’s equivalent to the mass of the planet Saturn and five Earths. It is a ceaseless process; the Sun is hungry, and it feeds upon itself. And yet, the total amount of matter already transformed into energy is a mere 0.03 percent of the Sun’s current mass—a minuscule diet and one that it can easily afford to consume. In order for the Sun to replenish the energy radiated into space at its surface, and for that matter for the Sun to remain inflated, it has tapped into a seemingly inexhaustible energy source—the hydrogen out of which it is predominantly made. The energy is derived via the conversion of hydrogen into helium through the proton-proton chain (described in Chapter 3) of fusion reactions— a beautiful sequence of chance encounters, interactions, and explosive transformations, described once again in prosaic form by Sir Arthur Eddington as “a jolly crockery-smashing turn of a music-hall.”2 Out of the chaos deep within the Sun’s core, energy is generated, the Sun remains hot and stable, and in consequence It’s a Matter of Time 25 we can live on a gently warmed Earth. Not too hot, not too cold, we occupy the Goldilocks planet of the Solar System. But the demon lurks and grows within the Sun. The Sun contains within its massive girth something like 1.4 x 1030 kg of hydrogen (and about 0.589 x 1030 kg of material other than hydrogen)—a seemingly endless supply of fuel, but for an ever energy hungry Sun it is not enough. It can never be enough. One day the hydrogen within its core will all be gone, transformed into energy and an ‘ash’ of helium. This is deep time, some 5 billion years from now, when the demon will be born: a roaring cuckoo-child that will grow into a bloated red giant. The time that it takes a star to use up the hydrogen supply in its core is called the main-sequence lifetime, or TMS. The details relating to stellar structure, internal energy generation, and stellar evolution will be presented in detail in the next chapter. For the moment let us simply take it as a fact that a fraction q of a star’s total mass M* is available in the form of hydrogen to produce energy. The main-sequence lifetime can now be calculated according to the total amount of energy available to the star divided by the rate at which that energy supply is used up. The total fusion energy available to a star can be determined from an experimental result first established by chemist Francis Aston in 1919. Specifically, Aston, who was working at the Cavendish Laboratory in Cambridge, found that the mass of four protons was smaller than the mass of a helium atom nucleus (composed of two protons and two neutrons) by 0.007 percent of the mass of the protons. From this observation, Eddington realized in 1920 that if nature could coax (somehow) four hydrogen (H) atoms into forming a helium (He) atom, then energy could be made available to a star. Symbolically, 4H ⇒ He + E, where E is the energy liberated per conversion. The energy term, Eddington reasoned, would be related to the mass difference found by Aston—that is, using Einstein’s famous equation linking mass and energy, E = m c2, where c is the speed of light and m = 0.007 MH, and where MH is the mass of the hydrogen atom. In this fashion, the total amount of energy available to a star is Etotal = 0.007 c2 q M* X, where X is the mass fraction of a star that is hydrogen (X = 0.75, for our purposes). Now, the rate at which a star consumes its 26 Rejuvenating the Sun and Avoiding Other Global Catastrophes energy supply is given by its luminosity L*, which accounts for the electromagnetic energy radiated into space per unit time at its surface. Accordingly, we have: TMS ≈ Etotal/L∗ = 0007c2 qM∗ X /L∗ (2.1) For the Sun, detailed numerical models indicate that q ≈ 0.13 and consequently TMS(SUN) ≈ 3 x 1017 seconds ≈ 1010 years. On this basis the Sun is middle-aged with respect to its mainsequence lifetime, and has some 5 to 6 billion years of hydrogen fuel supply left. Time and solar transformation—these are humanity’s deeptime enemies. Time we cannot control, but the transformation and mixing of matter in the Sun we might just be able to influence, and this proactive engineering option – literally the rejuvenation of the Sun – is perhaps the last best hope for providing our distant offspring with a long-term future, and our best hope for saving Planet Earth from total destruction. The Deadly Earth Life is a continuous struggle against the elements and, apparently, there are many more ways of dying than there are of staying alive. It is a narrow path that we have to tread to literally keep life and limb together. Over the timescales of concern in this book, however, it is not the survival of any one individual that is especially important. Rather, it is the long-term survival of humanity and Earth that matters, along with all the incredible diverse species of animals that live upon and in it. The scale of any disaster can be measured in numerous ways— some more impersonal than others. The scale might be measured in lives lost, or in financial infrastructure undermined. It can be measured in irreplaceable historical artifacts destroyed or future growth delayed. But in a typical human lifetime (a measure of, say, 70 years) the sum total of natural disasters that might be witnessed – be they hurricanes, tsunamis, earthquakes, or volcanic eruptions – will be small fry compared to the disasters caused It’s a Matter of Time 27 Figure 2.1. A satellite image of Hurricane Katrina. This one event devastated the city of New Orleans in August 2005. It caused the untimely death of 1,836 people and produced an estimated $81.2 billion in damage and destruction. (Image courtesy of NASA). by extraterrestrial influences that operate on timescales of many thousands of years and longer. Indeed, on the timescale of tens of thousands of years countless numbers of hurricanes (Figure 2.1) will have whipped across the face of Earth, buzzing over the landscape, in accordance with our accelerated time frame, like a carefree fly on a hot summer’s day. Whole segments of continents will have been shaken and shifted by earthquakes, or become covered in ash and blistering lava by volcanic eruptions. But all of 28 Rejuvenating the Sun and Avoiding Other Global Catastrophes these disasters combined will melt into insignificance on the day when a 2-km-diameter asteroid ploughs into Earth’s atmosphere. And here the correct adjective is when, not if. This event will happen—it’s a certainty, unless humanity does something about it. The Deadly Solar System The main belt asteroid region, located between the planetsMars and Jupiter, is a reservoir for planetesimals that failed to be accreted into planets. They are primordial objects formed at the very beginning of Solar System history, and they are the scourge of the inner Solar System. Countless collisions, grazing sideswipes, and smallparticle strafing have ground the initial population of asteroids into a vast swarm of blasted and fragmented shards. There are literally hundreds of thousands of asteroids now orbiting our Sun. The meteorites that occasionally careen through Earth’s atmosphere, in a blaze of light and concussion of sonic booms, are asteroid fragments, and it is by collecting these small fragments that we have learned about the processes by which our Solar System formed. The chances of an individual being struck by a meteorite are (luckily) very slim. Certainly, a few people have been bruised by meteorites throughout recorded history, but as far as reliable sources go, no one has ever been killed by a meteorite strike.3 The main belt asteroids are not a direct threat to Earth. The simple reason for this is because they move along circular orbits located between Mars and Jupiter. There is, however, a small subset of asteroids (admittedly derived from the main belt region) that do, however, pose a collisional threat to Earth. These are the nearEarth asteroids (NEAs). The NEAs have more elliptical orbits than their main belt relatives, and this property can bring them into the region of Earth’s orbit4 where collisions (and close encounters) will eventually occur. The most recent impact of a 10-m-sized asteroid with Earth occurred on September 3, 2004. Military reconnaissance spacecraft recorded this particular event, and the material that survived atmospheric passage (fortunately) ploughed into the Antarctic ice shelf. Unfortunately (for science), the fall location of this particular impact means that no ground investigation took place, and the It’s a Matter of Time 29 Figure 2.2. The Tunguska fireball devastation. At 07:17 local time on June 30, 1908, the sky over central Siberia filled with the light of a massive, detonating fireball. In an instant thousands of trees were felled and scorched by a searing blast wave generated by the catastrophic breakup of the meteoroid just 10 km above the ground. It is still a matter of contention between planetary scientists whether the Tunguska object was a comet (predominantly composed of water ice) or an asteroid (predominantly stony in composition). The photograph reproduced here was taken during the 1927 expedition led by Leonid Kulik to study the impact area. crater and possible fragments are now lost. Historically speaking, the best-studied large impact event occurred in Siberia on June 30,1908. This – the so-called Tunguska event5 devastated some 2,000 square kilometers of forest and produced a series of longwavelength acoustic waves that propagated around the world multiple times (Figure 2.2). The last major event involving a 10- to 15-km-sized impactor occurred some 65 million years ago. It has been argued that it was as a result of this particular impact that the dinosaurs (and indeed, most of the world’s large land animals) became extinct (Figure 2.3), although many researchers also argue that the impact was more of a coup de grace than the principal agent behind the extinction. Many other abrupt extinction events are recorded in the fossil record and only a few of these have been linked to large impact structures.6 The extensive and, indeed, ongoing collisional alteration of the main-belt asteroid population dictates that there are now many more small asteroids than large ones. Earth impact probability increases, therefore, with decreasing asteroid size (or mass). So, for example, Earth experiences a collision with a 50-m-diameter 30 Rejuvenating the Sun and Avoiding Other Global Catastrophes Figure 2.3. The Chicxulub impact crater located on the Yucatan peninsula, Mexico. The actual crater is no longer a distinctive surface structure, and the image shown here is a reconstruction of the crater through surface magnetic and gravitational anomaly measurements. The crater is 170 km across and is dated to the time of the great dinosaur extinction 65 million years ago. (Image courtesy of V. L. Sharpton, LPI). asteroid once every few hundred years; an encounter with a 1-km-sized asteroid occurs every few hundred thousand years, and an impact from a 10- to 15-km-sized asteroid takes place every few tens of millions of years (Figure 2.4). An approximate formula Figure 2.4. The total number of objects N(M) with masses larger than mass M, falling to Earth per year. Extinction event (EE) impacts occur on timescales of several tens of millions of years, whereas Tunguska-like events occur on timescales of a few hundred years. It’s a Matter of Time 31 for the time interval between impacts from asteroids of diameter D-km is: TNEA (yrs) = 10 5+08ln D−km . Dealing with potential Earth-impacting comets and asteroids will presumably be one of the first priorities of future space engineers. The nature of the danger posed by such objects, however, must first be understood. Indeed, we still need to know which objects might impact Earth. To this end a small number of astronomers, working from observatories dotted around the world, are scanning the sky in the search for rogue asteroids, annotating their numbers and determining their orbits. The orbits and nearterm evolution of all asteroids, both main-belt and Earth crossing, with sizes larger than a few kilometers will soon be known, and in principle the times of potential future impacts from these objects will be predictable. Our present knowledge of the asteroid population with sizes less than about 1 km is limited, and the lead-time we might currently expect before the next Tunguskalike impact is perhaps a few seconds. In other words, the first we will know about the event is when it has happened. Although this is far from comforting news, within the next half-century (perhaps) most of the potential Tunguska-like impactors, with diameters of just a few tens of meters, will also be catalogued. In 1999 MIT researcher Richard Binzel developed a 10-point scheme to measure the impact threat posed by an asteroid. Based upon the estimated size, potential impact velocity and impact probability, the so-called Torino scale developed by Binzel assigns a color and a number to any Earth-approaching asteroid. The Torino scheme is described in Table 2.1. At the time of this writing only one object – an asteroid called 2004 VD17 – has a Torino scale designation greater than white 0. This particular asteroid is believed to be some 600 m across, with a mass of about 2.5 x 1011 kg. Having an estimated impact velocity of 21 km/s this asteroid could impart some 14,000 megatons of TNT-equivalent energy upon impacting Earth. The Torino scale designation for 2004 VD17 is Green 1, and while an Earth impact is highly unlikely, a relatively close approach on May 4, 2102, is predicted. It is highly likely that follow-up observations of this particular asteroid, during the next several months and years, will see it downgraded to a Torino scale white 0 object. 32 Rejuvenating the Sun and Avoiding Other Global Catastrophes Table 2.1. The Torino impact scale. Further details can be found at http://neo.jpl.nasa.gov/torino_scale.html. Color Number Comments White 0 No direct impact threat. Or a small object (size less than 50 m) that might possibly produce a meteorite shower. Green 1 Close Earth passage, but very low probability of impact. Yellow 2 An object warranting further attention, but no great impact concern. Yellow 3 An object with a > 1% chance of hitting Earth. Impact would produce local destruction. Object warrants further study. Yellow 4 An object with a > 1% chance of hitting Earth. Impact would produce regional destruction. Object warrants further study. Orange 5 Close encounter posing a serious threat of impact resulting in regional destruction. Impact lead-time less than 10 years. Orange 6 Threat of a global catastrophe. Impact lead-time less than 30 years. Orange 7 Very close encounter by a large object that might hit Earth during the next 100 years. Red 8 A certain impact, resulting in localized devastation. Red 9 A certain impact, resulting in regional devastation. Red 10 A certain collision, resulting in catastrophic global devastation. Knowing when an impact might occur, however, is only part of the story; what to do about the impending impact is something else altogether. A number of proposals concerning asteroid defense tactics have been put forward in recent years, and they range from the “blast ‘em to pieces” type of proposal to the “change their orbit slowly and gently” type. Of course, the action that might be taken is dictated by the size of the asteroid and the potential lead-time before Earth impact is going to occur. If the asteroid is a small one (perhaps a few hundreds of meters across; see Figure 2.5) and the lead-time to an impact is very short (a few years) then blasting it with nuclear weapons is probably the best last-choice action.7 If the asteroid is large (in excess of, say, 500 m or so) and the lead time is many tens to hundreds of years, then attempts to just slightly alter the asteroid’s orbit (for example, by attaching a set of large space sails) would seem to make sense. It’s a Matter of Time 33 Figure 2.5. Asteroid (25143) Itokawa is some 0.535 by 0.294 by 0.209 km in size and weighs in at about 3.5 x 1010 kg. Visited by the Japanese Hayabusa spacecraft in late 2005, it is presently believed that the complex structures observed on its surface are the result of a collisional breakup followed by a reassembly phase. That many (possibly most) asteroids are loosely structured rubble piles has important consequences for any potential collisional avoidance strategies. (Image courtesy of JAXA). The potential impact threat posed by near-Earth asteroids and methods by which such impacts might be avoided are relatively well understood (at least in principle) at the present time. Indeed, the stage is set (literally ready and waiting) for the first attempts to alter the orbit of a ‘safe’ non-impacting asteroid.8 The first (terrestrial) asteroid impact avoidance engineers have already been born. The Deadly Stars The Sun is situated at a distance of 8,000 pc from the galactic center. It travels through space at a speed of 230 km/s and completes one galactic orbit every 200 million years. On its journey around the galactic center, the Sun is accompanied by an ever-moving host of stellar companions. The nearest star to the Sun is currently the faint dwarf star Proxima Centauri. Located just under 1.3 pc away, however, our nearest stellar neighbor is not actually visible to the naked eye. Within the volume encompassed by a sphere of radius 5 pc centered on the Sun, there are 49 star systems. Indeed, the number of stars per unit volume of space in the solar neighborhood is determined to be * ≈ 0.1 stars/pc3. This is a useful number, since it enables us to determine the 34 Rejuvenating the Sun and Avoiding Other Global Catastrophes typical time interval (TCE) for close encounters between the Sun and another star. To determine TCE we need to first set up an impact cross section area: = d2, where d is the encounter distance as measured from the Sun. Given that the Sun has a relative velocity V* (km/s) with respect to its nearest neighbors, then in time T the volume swept out by the Sun will be V = V* T. In the volume of space swept out, however, there will be N* = V * actual stars. Hence, in time T, the number of stars encountered by the Sun within distance d is N* = * V* T. The time interval between individual encounters is, therefore, about TCE =1/ * V*. The question now is, what do we mean by a close encounter? As the approach distance d is increased so the cross sectional area increases and TCE correspondingly decreases, so distant encounters become common. The time interval between stars being as close to the Sun as Proxima Centauri (d ≈ 1.3 pc) is now 74,000 years, given a typical relative velocity of V* = 25 km/s. What about an even closer encounter, say at a distance of 5,000 AU, well inside of the Solar System’s cometary reservoir, the Oort Cloud?9 In this case TCE ≈ 200 million years. How about an approach as close as 5 AU? At this encounter distance the Solar System will almost certainly be destroyed (depending on the mass of the interloping star), with the planets being scattered out of their current orbits and most probably ejected to a cold, dark death in interstellar space. For this situation, TCE = 2 x 1014 years, which is well in excess of the present age of the galaxy (Tgal ≈ 13 x 109 years). Within the main-sequence lifetime of the Sun [TMS(Sun) ≈ 1010 years], no star is likely to pass closer than d ≈ 730 AU. Although a direct collision – or even a very close encounter – between the Sun and another star is a highly unlikely event, encounters at the distance of the Oort Cloud and of a few thousand astronomical units will happen reasonably often, and these encounters can still be deadly to life on Earth. Cometary nuclei in the outer part of the Oort Cloud will have their orbits gravitationally perturbed by passing nearby stars. The smaller the closest approach distance, the more massive and the slower the speed of the perturbing star, the greater the number of cometary nuclei that will have their orbits changed. Many of the cometary nuclei will be ejected from the Solar System, doomed thereafter to It’s a Matter of Time 35 Figure 2.6. Close-up of a cometary nucleus. In this image the surface of periodic comet Wild 2 is revealed by a camera carried aboard the Stardust spacecraft (http://stardust.jpl.nasa.gov/home/index.html). The nucleus is about 5 km across. (Image courtesy of NASA) rove the depths of interstellar space. Other cometary nuclei will have their orbits perturbed in such a fashion that they will swing into the inner Solar System, and while on their journey around the Sun they may potentially hit one of the planets (Figure 2.6). Although Proxima Centauri is currently the closest star to the Sun, we can ask which stars in the solar neighborhood are going to make even closer approaches to the Sun in the future. This question, in fact, was recently answered by Joan Garcia-Sanchez of the University of Barcelona and co-workers.10 Using data gathered by the Hipparcos astrometric satellite, the team found a total of 87 stars that will pass within 5 pc of the Sun during the next 10 million years. Of these, the star Gliese 710 will make the closest approach of all, skimming the edge of the Oort Cloud at a distance of about 0.3 pc (or 70,000 AU) from the Sun (Figure 2.7). The closest approach will occur some 1.4 million years from now. Estimates of the effect of Glies 710 on the Oort Cloud suggest that around 2 million long-period comets will be perturbed into potential Earthcrossing orbits over a time interval lasting perhaps 5 million years. 36 Rejuvenating the Sun and Avoiding Other Global Catastrophes 0 0.5 1 1.5 2 1 1.2 1.4 1.6 1.8 2 Time (millions of years) Distance (pc) Gliese 710 HD33487 HD179939 Oort cloud boundary Figure 2.7. Closest approach distances of some selected nearby stars. The curved solid line shows the distance variation with time of Gliese 710. The stars HD 33487 and HD 158576 will pass as close as 2 and 0.9 pc respectively to the Solar System. After Gliese 710, the star HD 158576 makes the second closest approach to the Solar System during the next 5 million years. As this is a chapter concerned with timescales, we can ask the following: What is the likely time interval TLPC between longperiod comet hits on Earth? The target area of Earth (ignoring gravitational focusing) is E = RE 2, where RE = 6371 km is Earth’s radius. The probability that a single Earth-orbit crossing comet might actually strike Earth is, therefore, Phit = 2 E/(4 DE) 2), where DE = 1 AU = 149.6 million km is Earth’s orbital radius. The factor of 2 accounts for the fact that the cometary orbit cuts through the sphere of radius 1 AU twice, and it is assumed that long-period comets can approach the Sun from any direction (an assumption that is not strictly true for cometary showers). If the number of comets heading into the inner Solar System is fcom comets per year, then the time interval between possible Earth impacts will be of order TLPC = 1/[(RE/DE) 2 fcom/2] ≈ 109 (yr)/fcom. The typical flux of long-period comets approaching to within 1 AU of the Sun is estimated to be fcom ∼100 per year. (This may rise to ∼200 per year during a cometary shower such as that induced by Gliese 710.) These numbers indicate that long-period comet impacts upon Earth are going to be rare, even under cometary shower conditions, with TLPC ∼5 – 10 x 106 years. The situation with long-period comet impacts is actually more complicated than indicated above. Oscillations of the Solar System above and below the galactic plane (with a period of It’s a Matter of Time 37 about 35 million years), gravitational tides resulting from galactic spiral arm encounters, and the close passage of giant molecular clouds can also perturb the orbits of cometary nuclei in the Oort Cloud, causing cometary showers. Mass extinction events deduced from the fossil record (Figure 2.8) and the estimates of terrestrial crater ages suggest that cometary impacts occur in discrete bursts, lasting for perhaps a few million years, separated by intervals corresponding to 25 to 30 million years.11 Long-period comet impacts may well be rare, but they pose a tremendous threat to life on Earth. Their large, kilometric size and high encounter velocities indicate that they can deliver devastatingly large amounts of impact energy. Not only this, the lead time between the detection of a long-period comet and its possible impact with Earth might be just a few months. This is a very different situation to the NEA threat discussed earlier, and there is no obvious engineering option that can easily save Earth from a Chicxulub Wilkes Land % Extinction 100 End Late Ordovician Devonian End Triassic End Permian End Cretaceous 500 50 0 0 100 200 300 400 Time before present (Myr) Figure 2.8. Schematic diagram of marine species extinctions as recorded in the fossil record over the last 550 million years. The so-called ‘big five’ events are labeled. The dinosaurs and the Chicxulub impact crater are dated to the end-Cretacious extinction some 65 million years ago. The greatest mass extinction occurred at the end of the Permian, about 250 million years ago. It has been suggested that the end-Permian extinction coincided with the formation of the 480-km-diameter Wilkes Land impact crater recently found in eastern Antarctica. The ripple effect, with a period of about 25 to 30 million years, is clearly visible in the extinction curve. 38 Rejuvenating the Sun and Avoiding Other Global Catastrophes Figure 2.9. On July 4, 2005, the Deep Impact mission produced a new impact crater on the surface of Comet Tempel 1. The comet is some 14 km x 5 km x 5 km in size and predominantly composed of water ice. The impact was produced through the direct hit of a 1-m-long, 1-mdiameter copper cylinder striking the icy surface at about 10 km/s. The impact crater produced is thought to be about 100 m across. (Image courtesy of NASA) direct hit by a long-period comet. Brute explosive force is perhaps one solution (Figure 2.9), but the multiple fragments produced by such actions may well exacerbate rather than fix the problem. Indeed, one of the most pressing issues related to the long-term survival of humanity is how to quickly (on a time scale of months) alter, albeit very slightly, the orbital track of a directly impacting long-period comet without breaking it apart. Deadly Novae The end phases of some stars are very violent. They literally blow themselves to pieces (Figure 2.10), spraying processed nuclear material into interstellar space at immense speeds and irradiating vast volumes of space with lethal X- and -ray radiation.12 There It’s a Matter of Time 39 Figure 2.10. The Crab Nebula, the icon of a supernova remnant. The ‘New Star’ associated with the production of the Crab Nebula was recorded in numerous Chinese and Korean chronicles, and was first seen in July 1054. The object was visible for many months, and was reportedly visible in broad daylight. At a distance of 2,000 pc, the maximum brightness of the nova would have been about magnitude -6, brighter than the planet Venus but not as bright as a half-illuminated Moon. (Hubble Space Telescope image, courtesy of NASA) is some debate concerning the minimum distance beyond which Earth’s atmosphere might be safe from a nearby supernova event, but it is typically thought to be between 50 and 100 pc. An approximate timescale for nova irradiation can be made as follows. Here we will work in two dimensions only and consider the galactic disc to be a circular band with an inner radius of 1 Kpc and an outer radius of 15 Kpc. The area of this galactic disk is then Agal ≈ 7 x108 pc2. If the critical distance from the Sun for a nova detonation is taken to be Rcrt, then on average the number of nova NNVA that must occur before one is at least within a distance Rcrt from the Sun is NNVA = Agal/( R2 crt) . If we take Rcrt = 60 pc, then 40 Rejuvenating the Sun and Avoiding Other Global Catastrophes NNVA ≈ 6,000. Taking a disk nova rate of SNVA = 0.04 per year, then the typical time interval TNVA between critical nova explosions is going to be TNVA = [Agal/( Rcrt 2 )]/SNVA ≈ 1.5 x 106 years. The next closest Type I supernova-producing system13 to us may have already been identified, and it is the binary star known as IK Pegasus (also designated HR 1820). In this particular case one of the stars in the binary has already formed into a white dwarf, while its companion is presently in a subgiant phase. The two stars are sufficiently close (just 42 R apart, in fact) that the subgiant star is actively adding mass to the white dwarf star. This latter accretion is the critical point. In 1930 Nobel Prize-winning physicist and mathematician Subrahmanyan Chandrasekhar showed that there is a maximum mass limit for a white dwarf to remain stable. The critical mass – the Chandrasekhar limit – beyond which a white dwarf will catastrophically collapse is MCLM ≈1.4 M Once MWD > MCLM then gravitational collapse will ensue, and a Type I supernova will result (Figure 2.11). It is estimated that the white dwarf component in IK Pegasus has a mass of about 1.2 M and this means that once it has accreted an additional 0.2 M of material from its companion a dramatic collapse will occur. If the accretion rate is as high as 10−6 solar masses of material per year, then IK Pegasus will undergo supernova disruption in about 200,000 years from now, at a distance of some 44 pc—well inside the ‘danger zone’ for perturbing Earth’s atmosphere (Figure 2.12). For an accretion rate of 10−7 solar masses per year, supernova disruption will occur about 2 million years from now, when the system is at a distance of 43 pc from us. The rate at which the white dwarf star in IK Pegasus accretes matter from its companion must be less than 5 x 10−8 solar masses of material per year if supernova disruption is to take place at a distance when the system is beyond the safe distance boundary of 60 pc. At the present time astronomers do not know what the accretion rate for the white dwarf in the IK Pegasus system is. The speed with which material is blasted into space by a supernova is typically several thousands of kilometers per second. Clearly if a planet is within a few tens of parsecs of a supernova explosion and chances to encounter such a disruptive blast wave, then its atmosphere would be severally denuded. It’s a Matter of Time 41 Star of mass M2 Star of mass M1 MS star Giant star MS star WD star Giant star WD star Binary star Secondary Primary (1) (2) Ejection (3) SN Figure 2.11. Stages in the production of a Type I supernova. The process begins with the formation of a binary star system in which one star – the primary – has a mass M1 greater than that of its companion – the secondary – of mass M2. Since the primary star is the more massive of the pair it will evolve into a giant star long before the secondary does (Stellar evolution will be discussed in the next chapter). At stage (1) the giant primary star begins to lose mass to the secondary, and the two begin to spiral together within a common envelope. Eventually, the primary giant evolves into a white dwarf star in close orbit about its companion (the now-enhanced mass secondary). Eventually, at stage (2), the secondary star evolves away from the main sequence to become a giant star and mass exchange begins again. At this stage, however, the white dwarf can only accrete so much material before the Chandrasekhar limit is reached. Finally, at stage (3), the white dwarf collapses to produce the Type I supernova and the giant secondary companion is slung outwards at high speed into interstellar space. Not only this, the atmosphere of such a planet would probably have been badly disrupted long before the material blast wave actually arrived. At distances of less than about 50 to 100 pc, the flux of energetic cosmic rays, combined with that of the X-ray and -ray radiation produced by the supernova explosion will probably destroy or at least badly perturb the atmosphere surrounding an Earth-like planet. An intriguing book – The Cycle of Cosmic Catastrophes [Bear and Company, Rochester, Vermont (2006)] by Richard Firestone, Allen West, and Simon WarwickSmith – presents the argument that Earth suffered a triple blow from the supernova responsible for producing the Geminga pulsar and gamma-ray source.14 Based upon radiocarbon data (and a host 42 Rejuvenating the Sun and Avoiding Other Global Catastrophes 35 45 55 65 0 0.5 1 1.5 2 2.5 3 Time (millions of years) )cp(ecnatsiD -6 -7 Minimum safety zone t(min) Figure 2.12. Variation in the distance to IK Pegasus. The system will be at its closest to the Solar System at a time t(min) = 1.14 million years from now. The safe distance beyond which the supernova will have little effect on Earth’s atmosphere is estimated to fall between 50 to 60 pc. The points labeled -6 and -7 correspond to the distances and times at which a supernova will occur when the accretion rate is 10−6 and 10−7 M/yr respectively. of other environmental markers), Firestone and co-authors argue that 41,000 years ago the atmosphere encountered the X- and gamma-ray burst from the Geminga supernova event, then 23,000 years later(18,0000 years ago) Earth encountered the supernova shockwave, followed 5,000 years later (13,0000 years ago) by a slower-moving debris wave. Firestone and his co-authors link the various events to mega-fauna extinctions, massive flooding, and dramatic climate change. The peak energy output per unit time (the luminosity) of a typical Type I supernova is LSN ∼1036 (watts). This is a tremendous amount of energy being radiated into space—indeed, 10 billion times greater than the Sun’s present luminosity—and yet it is by no means the most energetic of celestial cataclysms. The star Eta Carina is the next most likely candidate, among the known stars within a few thousand parsecs of us, to produce a Type II supernova—the result of the catastrophic collapse of a single massive star. Eta Carina is some 5 million times more luminous than the Sun, and it is estimated to be about 120 times larger in size. There is some evidence that Eta Carina is actually a binary system, but it is reasonably clear (whether singular or a binary) that the system contains at least one 50 to 100 M star. For at least the last century and a half it has undergone It’s a Matter of Time 43 Figure 2.13. Eta Carina as photographed by the Hubble Space Telescope in the mid-1990s. The twin lobes of the expanding envelope are clearly visible, and the surrounding trelliswork of twisted veins indicates those locations where carbon grains have formed. The envelope is expanding into space at a speed of about 700 km/s. An equatorial disk can also be seen in this image, which has been reproduced in a negative format to enhance the visible detail. (Image courtesy of NASA) quasi-periodic outbursts in brightness, and since the early 1840s it has lost an estimated2–3 M of material into space. Much of this material resides in a surrounding double-lobed nebula called the Homunculus (Figure 2.13). Various model calculations suggest that Eta Carina will undergo supernova collapse within the next 100,000 years, but since it is situated at a distance some 2,500 pc away from us, the effects of Eta Carina’s destruction will be of little consequence to Earth. Indeed, as seen from Earth, the peak brightness of the Eta Carina supernova will be about magnitude −4, comparable in brightness to the planet Venus.15 In contrast, if IK Pegasus undergoes supernova disruption when it is at its closest point to Earth, it will attain a peak brightness of about magnitude −16, brighter than the full Moon. 44 Rejuvenating the Sun and Avoiding Other Global Catastrophes GRBs and Hypernovae By far the most energetic of explosions within the entire universe are those associated with the hypernovae that are responsible for producing gamma ray burster (GRB) events. The GRB production mechanism is believed to result from the gravitational collapse of a rapidly spinning, massive, magnetic star (sometimes called a collapsar; see Figure 2.14). The rotation and the strong magnetic field combine to produce two exceptionally strong and twisted magnetic columns protruding along the star’s spin axis. Electromagnetic radiation, such as gamma rays, are then directed along these magnetic columns and literally ‘squirted’ into space as two oppositely directed jets.16 Although the details of the GRB production mechanism are still being worked out, it is clear that they can release a staggering 1054 joules worth of energy into space in just a few tenths of seconds. At these energy-release levels a GRB occurring within a few kilo parsecs of Earth could potentially cause biologically significant irradiation. The time interval between GRB events occurring in our galaxy has been estimated to be of order TGRB ∼108 years (but see later), and although the exposure time to the burster radiation is just a few seconds (affecting just one hemisphere of Earth, Figure 2.14. Artist’s image of a collapsar producing a GBR event. The gamma rays are channeled along the oppositely directed, magnetically confined jets. (Image courtesy of NASA) It’s a Matter of Time 45 therefore), the energy flux might nonetheless seriously damage Earth’s upper atmospheric structure. One set of calculations by Brian Thomas and co-workers at the University of Kansas17 finds that even a 10-second exposure to the gamma rays from a GRB 2,000 pc away can severely damage Earth’s ozone layer. Indeed, the effect of the gamma rays is to break apart the molecular nitrogen (N2) in the atmosphere, which then reacts with molecular oxygen (O2) to produce nitric acid (NO). It is the nitric acid that destroys the ozone (O3), further producing nitrogen oxide (NO2). Then, in a feedback loop, the NO2 reacts with O2 to produce more NO, which then destroys more O3. The computer model indicates that it takes at least five years for the atmosphere to recover the ozone lost due to the gamma ray exposure. It is not so much the loss of atmospheric ozone that is the problem for life on Earth, but rather the problem that the Sun’s UV radiation, normally absorbed by the ozone, will be able to penetrate to the ground. Extended exposure to solar UV rays will, for example, result in a dramatic increase in animal and human skin cancers; surface dwelling plankton (the bottom of the aquatic food chain) would also be killed off, probably resulting in numerous ecosystem failures. It has been suggested that the Ordovician mass extinction (see Figure 2.10), in which 60 percent of marine species became extinct some 450 million years ago, was the result of atmospheric disruption caused by a nearby GRB event. The evidence for this, however, is not fully convincing,18 and recent studies suggest that GRBs must occur well within 1,000 pc of Earth before any serious atmospheric damage is likely to occur. In addition, Krzysztof Stanek and co-workers19 have recently argued that GRBs tend to occur mostly in small, irregularly shaped galaxies having low heavy element abundances. (These elements will be discussed in the next chapter.) What this means for us is that the odds of any GRBs occurring in our Milky Way galaxy now and in the future are actually very low indeed, and the interval between events is probably even longer than the 108 years indicated earlier. Can anything be done to protect Earth from GRBs? In principle, perhaps surprisingly, yes. A hypernova precursor star will of necessity be highly luminous, and if situated within the range at which damage to Earth’s atmosphere might result (i.e., less 46 Rejuvenating the Sun and Avoiding Other Global Catastrophes than 1,000 pc), it will be a very obvious astronomical object. In principle, future inhabitants of Earth will at least know which stars to guard against. Further, detailed spectral observations could also determine the direction of the progenitor star’s spin axis, and this would determine if Earth were situated in the direct line of fire. If Earth were actually exposed to a burst of gamma rays from a GRB, then in principle large UV sunscreens could be placed in near-Earth orbit to temporarily protect Earth’s surface-dwelling life forms from direct solar UV exposure (Figure 2.15). The potential importance of hypernovae and GRBs in controlling the emergence of intelligent life has recently been discussed by James Annis.20 Indeed, Annis argues that our Milky Way galaxy has been sterilized of life on numerous occasions in the past. It is generally believed that the GRB rate decreases with time—that is, GRB events were much more common when our galaxy was younger. Annis argues that because of this effect the Sunshield located at L1 1 AU Sun Dia. ~ 20,000 km L1 ~ 0.01 AU Earth Figure 2.15. It has been suggested that Earth’s climate might be manipulated by placing a sunshield at the Sun-Earth L1 point, where gravitational interactions are equal and opposite. Technically, to completely cover the Sun at L1 the sunshield would need to have a diameter of 20,000 km. Clearly a much smaller diameter sunshield is required in practice, since it is not the intention to block out all of Earth-incident sunlight. It’s a Matter of Time 47 galaxy has only recently undergone a phase-transition allowing for the long-term survival of complex life forms (such as us). His argument runs like this: In the early galaxy GRB events were so common that even if life did manage to evolve on some specific planet it would soon thereafter be destroyed. As the GRB rate decreased with time, however, various strongholds of life could develop and undergo advanced evolution, eventually producing (in some cases) intelligent species capable of space exploration. Annis, in fact, argues that this phase transition requirement offers a solution to Fermi’s Paradox. His point is that since intelligent life will not evolve in the galaxy until the GRB rate drops to a level allowing for the phase-transition to occur, the time for the emergence of extraterrestrial civilizations capable of galactic colonization cannot be much different from TUS ∼4.5 billion years. Hence, extraterrestrial civilizations are only just on the verge of beginning galactic colonization, and perhaps they will be here very soon. The Embrace of Andromeda Of order 20 million Sun diameters separate our Sun from Proxima Centauri. In contrast, only about 20 galaxy diameters separate the Milky Way galaxy from its nearest comparable-sized companion M31—the Andromeda Galaxy. It is because of this basic size compared to separation conditions that star collisions are rare, but galaxy interactions are relatively common. It is certain that the Milky Way galaxy has ‘cannibalized’ numerous smaller Local Group21 galaxies in the past with little effect upon its overall structure; the forthcoming interaction with M31, however, will be much more extensive than any of its previous encounters. The Andromeda Galaxy is presently some 730 Kpc away, but it is moving towards us at a speed22 of about 120 km/s. We do not know if a direct collision and interaction with our Milky Way galaxy is actually going to occur, but if it does, then at its current speed M31 will merge with our galaxy in something like TM31∼6 x 109 years (Figure 2.16). 48 Rejuvenating the Sun and Avoiding Other Global Catastrophes Figure 2.16. A snapshot from a computer model simulation of the collision between the Milky Way galaxy (to the upper right) and M31. (Image courtesy of John Dubinski, University of Toronto). The possible consequences for our Solar System as the merger between M31 and our Milky Way galaxy proceeds are difficult to predict. It is clear, however, that star collisions are still highly unlikely to happen; the average separation between stars will continue to remain at many millions of Sun-diameters. This being said, a close stellar encounter is certainly possible, and our Solar System may yet be disrupted in TM31 years from now—intriguingly, a time not far removed from the canonical end of the Sun’s mainsequence phase; our distant descendants may be in for double trouble. Although the star-Sun close-encounter timescale will not be greatly changed by the merger of our galaxy with M31, the time interval TNVA between Type II supernova12 encounters will decrease. This result follows in the wake of the enhanced star formation that will occur during the M31 collision.23 The star formation rate will inevitably increase during the M31 merger because of the compression and interaction of the large gas and dust clouds known to reside in the interstellar media of both galaxies. Our distant descendants will certainly experience a wonderful view as the Andromeda galaxy approaches over the next several billion years. Two Milky Way bands may eventually grace the night sky, and myriad glowing gas clouds, star formation regions and supernovae will sparkle in the heavens. Indeed, a beautiful but potentially deadly vista lies ahead for humanity. It’s a Matter of Time 49 Deep Time Even if Earth physically survives the inevitable future close encounters with wayward stars, nova explosions, and the ravages of an aging Sun, it still has a ‘natural’ winding-down mechanism in the form of inescapable gravity. Indeed, any object orbiting around a fixed center will lose energy due to gravitational radiation. It is certainly a small amount of energy that is lost per orbit, but how long it takes is not the issue at this stage. As Earth loses orbital energy through the generation of gravitational waves it will spiral in towards the Sun. The decay time, TGRV will be of order TGRV ≈ (c/Vorb 5 P, where Vorb is the orbital velocity, c is the speed of light and P is the orbital period. Earth currently has Vorb = 30 km/s and P = 1 year, which dictates a decay time of TGRV ≈ 1020 years. For the planet Mercury the decay time is TGRV ≈ 1016 years. Mercury, however, will be consumed by the expanding Sun in about 6 billion years, long before its TGRV destruction time. Earth, on the other hand, may physically survive the Sun’s red giant phase, and correspondingly, some 8 billion years from now find itself in orbit around a white dwarf star. If it continues to survive against disruption through close stellar encounters, then its eventual demise (in the deep, deep future) will be to spiral into the surface of a zero temperature, zero luminosity black dwarf sphere24 supported by degenerate electron pressure—the cold and dark relic of the Sun. The Doomsday Event The great philosopher and biologist J. B. S. Haldane once remarked that “The universe is not only as queer as we suppose, but queerer than we can suppose.” Haldane is indeed right, and it is entirely possible that there are physical entities within our Milky Way galaxy that might destroy Earth (and the Solar System) in its entirety if encountered just the once. Such entities might include massive black holes, putative strange matter, and of course, the phenomena that Haldane tells us we know nothing about. More will be said about black holes in Chapter 5, but since there is currently no consensus on what the mass distribution of black 50 Rejuvenating the Sun and Avoiding Other Global Catastrophes holes is, we can presently say very little about the chances of Earth or the Solar System encountering one (other than it hasn’t happened in 4.5 billion years). Strange matter is certainly odd stuff, but entirely possible within the context of allowed modern atomic physics. The suggestion is that such matter, made of strange quarks (the fractionally-charged, basic building blocks of matter), might form within the interiors of high-density neutron stars, and it may also be stable (in the form of so-called stranglets) outside of such objects. It has been further speculated that should ordinary matter (such as the stuff Earth is made of) meet a stranglet, then it will become transformed into strange matter. There is currently no proof that strange matter exists, but Haldane’s comment surely resonates on such issues. The fact that Earth formed some 8 or 9 billon years after the universe came into existence (the moment of the Big Bang) and has survived for at least 4.5 billion years tells us that doomsday catastrophes must be rare in our galaxy, but the question is, how rare? If a randomly occurring event (i.e., a stranglet or massive black hole encounter) destroys a planetary system at some constant rate tau, , then the probability that a specific planetary system will survive a time t decreases as e−t/ . That is, the survival probability decreases exponentially with time. If the event causing destruction occurs relatively often, then will be small and the survival probability soon becomes very small. If destruction events are rare, then will be large and the probability of a planetary system surviving for a long time is high. It is not, unfortunately, possible to constrain with any certainty at the present time, other than by making the statement that the continued existence of the Solar System suggests that it is unlikely that tau is less than several billion years. The Long and the Short of It The timescales upon which astronomical disasters are likely to occur are compared in the inequality below. TNEA 1−km << TNVA ≈ TLPC ≈ TGRB < TM31 < TMS << TCE d = 5AU << TGRV It’s a Matter of Time 51 At the far right hand end of the time sequence, if nothing else destroys Earth first, it will meet its ultimate doom by being accreted onto the surface of the Sun, which will have evolved into a black dwarf star. In the near term, however, the most likely astronomical disaster would be that due to an impact by a relatively small (perhaps 100 to 1,000 meters across) asteroid or comet. These are the smaller, more common near-Earth objects (NEOs) that feed into the inner Solar System from the main belt asteroid region and the Jupiter family of comets. The most serious impacts, however, will be those from the long-period comets. On about the same timescale that a cometary shower impacts the Solar System, it is liable to be irradiated by a near-by supernova outburst and possibly by a GRB event. Although Annis20 has argued that GRB events are capable of sterilizing the galaxy, not all researchers agree with this claim. Indeed, it has been pointed out that just a few centimeters of rock, soil, or water would completely protect any life forms on the Earth’s surface from GRB irradiation.25 Perhaps the most important issue with respect to surviving a GRB event is the time required to regenerate atmospheric ozone (destroyed by the incoming -rays). It is the ozone shield that protects life on Earth from the harmful UV solar-background radiation.21 Making the Best of It The first steps toward securing humanity’s long-term survival will probably focus on the means of detecting and then either destroying or diverting potential Earth-impacting asteroids and comets. Methods will also have to be developed for repairing Earth’s atmosphere following the ravages imposed by supernovae and GRB irradiation events. Although each of these catastropheavoiding steps will require great ingenuity, enormous engineering skill, tremendous daring, and total cooperation between the world’s nations, there is in principle no specific or fundamental reason why they cannot be achieved. Time, of course, will tell how well humanity lives up to the task. What is perhaps most important to note at this moment, however, is that there is a 52 Rejuvenating the Sun and Avoiding Other Global Catastrophes straightforward progression in project size and required skill development that takes us from impact avoidance to terraforming, Solar System colonization, and ultimately to solar rejuvenation. Once again, the deep future is not isolated from our present. Before moving on to consider the detailed properties of the Sun and how it might be rejuvenated, let’s briefly review a few of the larger-scale, stepping-stone projects that our descendants may eventually want to undertake. Dyson Spheres The Sun radiates a total of 3.85 x 1026 joules of electromagnetic energy into space per second. At a distance of 1 astronomical unit from the Sun, Earth receives a flux of 1,369 watts/m2 of solar energy at the top of its atmosphere. Multiplied by Earth’s cross sectional area of 1.3x108 km2, this translates to an energy budget of about 1.8 x 1011 watts. Earth, therefore, taps only a minuscule amount of the Sun’s energy output, something like 3.4 x 10−17 percent of the available energy, in fact. Indeed, small fry. In what has become a classic paper, Freeman Dyson in 1960 proposed that the existence of extraterrestrial civilizations might be revealed through the infrared emission from artificially constructed worlds.26 Specifically, Dyson argued that a sufficiently advanced civilization might utilize the material extracted from a Jovian-type planet to engineer a sphere around its parent star. The engineered shell in our Solar System might have a radius of about 1 AU and be several meters thick. In principle this shell could support extended human colonies and large industrial complexes capable of tapping a substantial fraction of the Sun’s energy output. The heat signature of the shell (now commonly called a Dyson sphere) would be that of a blackbody radiator with a temperature of 200 to 300 K. Such structures would likely be bright infrared sources in the 10-micron wavelength region of the electromagnetic spectrum. Interestingly, and unlike the radio surveys that search for intentional beacons or leaked transmissions from extraterrestrial civilizations, Dyson-like spheres would be potentially observable without the specific intent of the originating civilization. It’s a Matter of Time 53 Dyson spheres have indeed been searched for, but no finds have been reported to date.27 The problem, however, with serendipitous detection surveys (just as with the radio search for extraterrestrial signals) is to know when a null result actually indicates that there are no sources. At present we cannot say, one way or the other, whether any galactic civilization has built Dyson sphere-like structures. Clearly, engineering ability aside, there is a cost versus potential payback tradeoff that any civilization has to consider before embarking on the construction of a Dyson sphere. It may, in fact, make more sense to engineer the smaller real estate within a planetary system first. For example, within our Solar System, the terraforming of Mars and Venus might represent the first steps in this direction. Terraforming Vast amounts of literature have been published on terraforming— literally, the engineering of an otherwise barren world into one compatible with biological life. As a basic minimum requirement, however, the process of terraforming should result in the presence of liquid water on the surface of the planet being engineered. Liquid water will only exist on the surface of a planet if the average surface temperature (Figure 2.17) is above 273 K and if the atmosphere provides a surface pressure in excess of 610 Pa (which defines the so-called triple-point condition). In the case of Mars and Venus, the would-be engineer faces a range of problems— problems that, in fact, fall at the two extremes of the terraforming spectrum. Mars is a frozen, geologically inactive world with a tenuous atmosphere, while Venus is (possibly) geologically active, has a massive atmosphere, and a surface temperature in excess of 700 K. For Mars, the atmospheric pressures and temperatures are too low to allow liquid water to remain very long on its surface, while on Venus the surface temperature is far too hot and the atmospheric pressure is 90 times greater than that on Earth. Mars is a relatively small planet, about half the size of Earth, and its interior consequently cooled off rapidly, resulting in the permanent shutdown of the majority of its volcanic networks.28 This latter effect is particularly important with respect to the 54 Rejuvenating the Sun and Avoiding Other Global Catastrophes Orbital eccentricity Greenhouse effect Sun’s luminosity Axial inclination Orbital semimajor axis Atmosphere Geological activity Surface Temperature Stabilization Figure 2.17. Factors determining the surface temperature of a planet. The irradiance by the Sun will depend upon the planet’s orbital characteristics, the planet’s geological activity, and the structure and composition of its atmosphere. The variation in the orbital and axial tilt parameters (dashed line box) are governed by the Croll-Milankovitch cycle in the case of Earth.6 heating of the planet’s surface, since it is the geochemical carbon cycle that normally controls the greenhouse gas content of a planet’s atmosphere. On Earth, for example, chemical weathering and plate tectonic activity control the cycling of carbon between gaseous and mineral phases. The volcanoes formed at the plate subduction zones allow for the release of carbon dioxide (CO2) into the atmosphere, thus increasing the greenhouse heating effect. At the same time the CO2 in the atmosphere is chemically incorporated into rocks such as limestone by the weathering and erosion of silicate rocks, once again trapping the carbon in a solid phase. It is the feedback loop between the temperaturesensitive chemical weathering process (it runs more rapidly at warmer temperatures) and the release of CO2 by volcanic activity that has allowed Earth to maintain a near constant temperature for the past several billions of years (Figure 2.18). On Mars, the CO2 release mechanism via volcanic outgassing no longer works and, consequently, its ancient atmosphere has literally frozen out. The CO2 is now mostly trapped within its constituent rocks. For the surface temperature of Mars to once again rise above 273 K the CO2 content of its present atmosphere would have to be increased by a factor of about 200. This would raise the greenhouse It’s a Matter of Time 55 Atmospheric CO2 Biotic up-take Oceans (T) Silicate rocks Weathering (T) Sedimentation Volcanic activity Human activity Solar heating Figure 2.18. The terrestrial carbon-dioxide cycle. The (T) term in the Oceans and Weathering boxes indicate specific temperature sensitivity. If, for example, the oceans are warm, then carbonate minerals are more rapidly formed, and the rate at which the ocean takes up CO2 increases concomitantly, reducing the atmospheric CO2 concentration. The reduced atmospheric CO2 content then results in global cooling, which eventually checks the ocean-warming effect. Likewise, an increase in atmospheric temperature increases the rate at which silicate rocks can dissolve CO2 to produce carbonate rocks. The hotter the temperature, the faster the ‘weathering’ effect on silicate rocks, and the greater the rate at which carbonates are deposited into the ocean. The CO2 contained in the sedimentary carbonate rocks is eventually returned to the atmosphere through volcanic outgassing. Human activity is presently causing an increase in atmospheric CO2 through, for example, the burning of fossil fuels and the clear-cutting of ancient forests. The atmosphere is directly heated by the Sun, and this heating effect will increase with time, eventually forcing – if left unchecked – the loss of Earth’s oceans and the death of the biosphere. gas content to a level that it could offset the low solar irradiance at the orbit of Mars. Such an increase in the CO2 abundance would also raise the surface pressure well above 610 Pa, allowing liquid water to exist in a stable form at its surface. In principle such a process could be initiated by manipulating (that is, increasing) the brightness of Mars with the aid of space reflectors.29 Although the atmosphere of Mars needs to be warmed up by the terraforming engineer, the atmosphere of Venus needs to be cooled down. This process could in principle be achieved by reducing the amount of CO2 in the Venusian atmosphere, either by physically removing it or by increasing the CO2 uptake by the planet’s crust. Radiation shields or reflectors would also need to be installed in orbit around the planet to reduce the solar irradiance.30 56 Rejuvenating the Sun and Avoiding Other Global Catastrophes Indeed, even if there were no greenhouse heating factor for Venus, its surface temperature would be about 313 K (that is, an uncomfortably high 40°C) based purely upon its orbital proximity to the Sun. Transforming Mars and Venus into habitats suitable for nurturing biological life will only be achieved through the investment of considerable money and through long-term cooperation between all nations on Earth. It would also require the development of the engineering skills needed to perform such large-scale operations. Some of these skills will, with little doubt, first be honed in the engineering of Earth’s atmosphere. Global warming resulting from the generation and release of greenhouse gases, wide-scale industrial pollution, along with poor land use and agricultural management, are all conspiring to destroy the natural feedback systems that have maintained Earth’s relatively steady global temperature over the eons. Professor James Lovelock has introduced the profoundly important Gaia concept to describe the whole-Earth feedback system and, in his recent book The Revenge of Gaia: Why Earth Is Fighting Back—and How We Can Still Save Humanity (Penguin Books, London, 2006), he paints a disturbing picture for our near-term future. Human activity is changing Earth’s atmosphere and there are clear signs that traditional weather patterns have changed and will continue to change for the worse. Stronger and more numerous hurricanes (Figure 2.1) and tropical storms, the melting of Arctic and Antarctic ice fields, the retreat of glaciers around the world—all are being observed.31 Humanity’s short-term (over the next few hundred years) survival may well depend upon the engineering skills that our children develop in order to revitalize Gaia and Earth’s atmosphere. One suggestion that has been made for solving the global warming problem calls for the injection of sulphur dioxide (SO2) into Earth’s atmosphere to increase its albedo, thereby causing more solar energy to be reflected back into space.32 This, in fact, mimics the cooling effects associated with the sulfur plumes emitted by volcanoes.33 Another possible solution is to increase the absorption of atmospheric CO2 in the oceans by seeding surface waters with iron particles.34 Physicist Edward Teller and co-workers35 have further suggested that the global warming effects due to enhanced atmospheric CO2 concentrations could It’s a Matter of Time 57 be counteracted by the deployment of an electrically conducting mesh in Earth’s stratosphere (or in near-Earth orbit) with the aim of reducing the direct solar heating of the atmosphere. Alternatively, Jerome Pearson and co-workers36 have proposed that atmospheric insolation could be increased by engineering an equatorial ring of particles around Earth (similar to Saturn’s rings). Indeed, by making the ring particles out of dismantled near-Earth asteroids (NEAs), this proposal also solves some of the potential impact problems faced by our descendants.37 In an ideal world the drastic manipulation of Earth’s atmosphere would not be required. Gaia currently does it for free. However, given the apparent lack of political leadership on industrial emissions issues, such as those recommended in the Kyoto Accord, it is not at all likely that the basic engineering skills needed to terraform Mars and Venus will be developed on Earth during the next 100 years. Although we already have the ability (by default) to alter planetary atmospheres (that is, terraform) by the careless exploitation of Earth’s resources, what is needed in the future is the ability and skill to control the alterations.38 Lovelock poignantly writes in his latest book, however, “The idea that humans are yet intelligent enough to serve as stewards of Earth is among the most hubristic ever.” Humanity has much to learn and there is much work that needs to be done. Space Structures That our descendants will eventually exploit all of the useful and available real estate within our Solar System seems inevitable. Terraformed Mars and Venus, enclosed Moon and Mercury bases, industrial processing plants located in the main asteroid belt and on the Jovian Moons—all may come about. Part and parcel with this development will be humans adaptating to living in space. Skylab, Mir, and the International Space Station have already supported small (non-reproducing) human colonies, but in the future kilometric-scale space structures, such as those envisioned by physicist Gerard O’Neill, will presumably be engineered.39 Indeed, the space structures considered by O’Neill are truly grand in conception. Composed of 30-km long x 6-km diameter 58 Rejuvenating the Sun and Avoiding Other Global Catastrophes rotating cylinders, the space platforms would have an Earth-like atmosphere (and weather system) and potentially house, feed, and employ 10,000 people. The challenge, as noted by O’Neill,39 “is to bring the goal of space colonization into economic feasibility now, and the key is to treat the region beyond Earth not as a void but as a culture medium, rich in matter and energy.” In addition to building space colonies and terraforming, Paul Birch has suggested that rigid shells might eventually be engineered around all of the planets (and some of their moons) within the Solar System.40 Such supramundane planets would have habitable atmospheres, natural gravity, and be made of material extracted from asteroids, smaller planetary moons, and even the Sun. Perhaps somewhat overly optimistic, Birch suggests that the first supramundane habitats will be built around the planet Venus by 2040! Thinking Long-Term The solution to Fermi’s Paradox that is being followed in this book, as outlined in Chapter 1, is that advanced civilizations do not engage in galactic colonization because they have found no need to. This is not to suggest that stellar exploration won’t ever take place. But a clear distinction between local exploration and galactic colonization is drawn. Perhaps the first stellar voyages will be initiated in order to divert nearby rogue stars that are heading for an uncomfortably close encounter with the Solar System [i.e., on a timescale of TCE (d = 5000 AU) ≈ 200 million years, or TM31 ∼6 billion years]. Indeed, the possibility of controlling the space motion of a star through the induction of mass loss has been discussed by David Criswell41 (an operation described in more detail in Chapter 5). Long-time advocate and researcher into terraforming and space colonization Martyn Fogg42 has further investigated the possibility of star exchange to ensure the longterm habitability of the Solar System. It does not seem unreasonable to assume (or at least adopt as a working hypothesis) that all intelligent life forms that are capable of molding and adapting their environments will expand to live upon and commercially exploit all of the accessible components It’s a Matter of Time 59 of their parent planetary system.43 In addition, it also does not seem unreasonable to assume that all advanced civilization will find some way of avoiding a Malthusian catastrophe44 in which the demands of a population overreach the available food and raw materials supply. Indeed, our descendants will have to solve this problem if they are to have a long-term future. In addition, the longterm survival of a civilization (in, say, a planetary system similar to our own) will require the development of planetary defense programs to shield against asteroid and comet impacts. Such programs will, in fact, probably constitute the first truly global space initiatives, literally (certainly hopefully) uniting humanity through a common goal for survival against otherwise devastating odds. By tackling the NEO impact problem, as a space-based initiative, humanity will begin to develop the skills necessary to tackle even larger-scale projects. Again, as a working hypothesis, it does not seem unreasonable to assume that all advanced extraterrestrial civilizations will undertake terraforming projects, construct colonies and outposts on planetary moons, and engineer O’Neill-style spacecraft to produce their food. All such projects will anchor a civilization to its planetary system. Its financial investments, its sense of self, and indeed all that a civilization might physically require to exist will be infused within its home planetary system. Such an investment of time, lives, and money is hardly something that any civilization will willingly abandon and move away from. Indeed, such a holistic system is worth saving by any and all means that fall within the realms of possible physics and engineering. In terms of timescale the first astronomical danger that our descendants will need to guard against is that from NEO impacts (TNEO ∼105−6 years), then long-period comet impacts and supernova irradiation (TLPC ∼TNVA ∼106−7 years). The next significant timescale – indeed the ultimate timescale of concern in this book – will be the exhaustion of hydrogen in the Sun’s core about 5 billion years from now. If Earth and our descendants are to survive beyond the canonical TMS then two options present themselves: either tame the natural gigantism of the aging Sun by rejuvenating it, or leave the Solar System for good. Our descendants may be the first to reach for the stars in a quest for a new Earth, leaving a devastated and blistered Solar System (as described in Chapter 4) 60 Rejuvenating the Sun and Avoiding Other Global Catastrophes far behind them. But, as shall be explained later in Chapter 5, it is not unreasonable to think of extending the lifetime of the Sun, and thereby the potential life-supporting viability of the Solar System, by a factor of between 10 and 15, to TMS(engineered) ∼1011 years. This engineered lifetime is still three orders of magnitude smaller than the planet scattering encounter timescale by a nearby rogue star [i.e., TCE (d = 5 AU) ∼2 x 1014 years], but it is surely better than doing nothing. Either the Sun becomes a giant some 5 billion years from now and in the process destroys all life within the Solar System, or through the act of rejuvenation our descendants create an additional 95-billion-year time span over which to enjoy the nurturing light and warmth of a tamed Sun. Notes and References 1. Strictly speaking there are small amounts of deuterium and lithium produced during the time of primordial nucleosynthesis. Interestingly, the fusion of deuterium to produce 3He (via the reaction: D + P ⇒ 3He + gamma ray) is of great importance during the early (pre-main sequence) stage of star formation. Some of the consequences of stars undergoing an early deuterium burning phase are discussed in M. Beech and R. Mitalas, The formation of massive stars, Astrophysical Journal Supplement, 95, 517–534 (1994). 2. A. S. Eddington, The Internal Constitution of the Stars, Cambridge University Press, Cambridge (1926). Although the physical arguments presented in this book are now somewhat dated, they remain a brilliant example of lucid science writing. 3. K. Yau, P. Weissmann, and D. Yeomans, Meteorite falls in China and some related human casualty events, Meteoritics, 29, 864–871 (1994) provide a summary of meteorite falls recorded in Chinese chronicles between 700 B.C. to A.D. 1920. They report on one event that occurred in Ch’ing-yang in 1490, where it is claimed that stones fell like rain and many tens of thousands of people were killed. The reported death toll seems very high, but this may possibly describe a Tunguska-like impact (see Note 5 below) event where meteorites actually survived to hit the ground (and people). As shown in the author’s book Meteors and Meteorites: Origins and Observations (Crowood Press, 2006, p. 26), the probability of a person who lives to the ripe old age of 99 years being struck by a 1-gm meteorite is one It’s a Matter of Time 61 chance in 1.5 billion. The other way of saying this is that one person should be hit (not necessarily killed) worldwide every 33 years (or so). 4. Three NEA groups are generally recognized: the so-called Apollo, Amor, and Aten asteroid groups. Both the Apollo and Amor groups have their aphelia (greatest distance from the Sun) within the main belt asteroid region. The Apollo NEA group has perihelia (closest point to the Sun) inside of Earth’s orbit, while the Amors have perihelia just outside of Earth’s orbit. The Aten NEA group have perihelia well inside and aphelia just outside of Earth’s orbit. 5. It has been estimated that the equivalent of some 5 megatons of TNT energy was liberated in the Tunguska explosion. In the comprehensively titled research paper, Earth impact effects program: a web-based computer program for calculating the regional environmental consequences of a meteoroid impact, by Gareth Collins, Jay Melosh and Robert Marcus [Meteoritics and Planetary Sciences, 40 (6), 817–840 (2005)], the equations that describe the environmental effects of an impact (such as crater size, overpressure, thermal radiation, blast wave propagation, and seismic effects, as well as casualty levels) have been gathered together. The web site is accessible at http://www.lpl.arizon.edu/impacteffects. 6. Not every mass-extinction event observable in the fossil record can be associated with an impact. Some are, without a doubt, geological in nature and relate, for example, to variations in sea-level, anoxic ocean events, extensive volcanism, tectonic activity as well as climate change [see the excellent book by Tony Hallam, Catastrophes and Lesser Calamities—The Causes of Mass Extinctions, Oxford University Press, Oxford, 2005]. Impact extinction events can be identified by a significant increase in the iridium abundance in the terrestrial rocks that indicate the extinction boundary. Comets and asteroids are relatively rich in iridium (compared to Earth’s crustal rocks) and, following a large impact event, the constituent iridium is deposited over much of Earth’s surface, forming a thin iridium-rich layer. Perhaps the most famous such iridium rich boundary layer is that which was produced by the impact that resulted in the 180-km diameter Chicxulub crater in the Yucatan peninsula at the end of the Cretaceous Period (65 million years ago). On a smaller scale Jan van Dam of Utrecht University in the Netherlands, and co-workers [Long-period astronomical forcing of mammal turnover. Nature, 443, 687–691 (2006)] have found that there are ‘spikes’ in rodent extinction record spaced at intervals of 2.4 million and 1.2 million years. These intervals, van Dam argues, correspond to variations in Earth’s orbit and shifts in the tilt of Earth’s rotation axis to its orbital plane. The 62 Rejuvenating the Sun and Avoiding Other Global Catastrophes cycles of extinction have apparently been active for at least the past 22 million years. The Croll-Milankovitch cycle, which links long-term climate change to variations in Earth’s orbit, is generally believed to control the timing of Earth’s ice ages; events that invariably lead to many species becoming extinct [for a description of the C-M cycle see, Doug Macdougal, Frozen Earth: The Once and Future Story of Ice Ages. University of California Press, Berkeley (2006), pp. 65–88]. 7. Simply blasting an asteroid with a volley of, say, nuclear missiles may actually increase the impact devastation. Instead of one object hitting Earth, a series of explosions might result in multiple fragments striking Earth over a much larger area than that corresponding to a single-body impact. This is especially a problem given the current understanding that many asteroids are ‘rubble piles’ of loosely bound components. A good general review of the observational status and future spacecraft missions to comets and asteroids can be found in the article by A. C. Levasseur-Regourd, E. Hadamcik, and J. Lasue, Interior structure and surface properties of NEOs: what is known and what should be understood to mitigate potential impacts. Advances in Space Science, 37, 161–168 (2006). 8. A space tractor concept is discussed in some detail by E. Lu and S. Love in their article, Gravitational tractor for towing asteroids, Nature, 438, 177–178 (2005). The European Space Agency (ESA) is currently considering a spacecraft mission (the Don Quijote mission) to study the internal structure of an asteroid (presently unspecified). The mission will also attempt to change the orbit and rotation state of the target asteroid through high-speed surface impacts. An overview of the ESA mission can be found in a 2006 paper presented by Ian Carnelli, Andres Galvez and Dario Izzo, Don Quijote: a NEO deflection precursor mission, to a NASA workshop dedicated to near-Earth object detection, characterization, and threat mitigation— available at: http://www.esa.int/gsp/ACT/doc/ACT-RPR-4200-ICNASANEOWS-DonQuijote.pdf. 9. The Oort Cloud, named after the Dutch astronomer Jan Oort (1900–1992) who first suggested its existence, delineates the outer edge of the Solar System. It is literally the three-dimensional boundary beyond which the Sun’s gravitational influence no longer holds sway over the rest of the galaxy. It is a dynamical boundary that expands and contracts according to the time dependent distribution of matter in the solar neighborhood. Of order 1012 to 1013 cometary nuclei are believed to delineate the Oort Cloud region stretching between ∼10,000 to ∼50,000 AU from the Sun. Cometary nuclei within the Oort Cloud region are continually ejected into It’s a Matter of Time 63 interstellar space and into the inner Solar System as a result of gravitational perturbations from close passing stars, massive molecular clouds embedded within the interstellar medium, and during spiral arm region crossings. 10. J. Garcia-Sanchez et al., Stellar encounters with the Solar System, Astronomy and Astrophysics, 379, 634–659, (2001). In addition, R. A. Matthews [The close approach of stars in the solar neighborhood. Q. J. R. Astr. Soc. 35, 1–9. (1994)] finds that Proxima Centauri will not be at its closest approach to the Sun for another 26,700 years. At that time it will be 0.941 pc away. 11. See, for example, the recent research paper by W. M. Napier, Evidence for cometary bombardment episodes, Monthly Notices of the Royal Astronomical Society, 366, 977–982 (2006). A more general account of cometary impacts is given in the very readable book by Duncan Steel, Target Earth: The Search for Rogue Asteroids and Doomsday Comets That Threaten Our Planet [Readers Digest Association Inc., New York (2000)]. 12. D. H. Clark, W. H., McCrea, and F. R. Stephenson [Frequency of nearby supernovae and climatic and biological catastrophes, Nature, 265, 318–319 (1977)] investigated the possibility of Earth encountering the radiation burst or blast wave associated with a Type II supernova (see Note 13 below) during galactic spiral arm crossings. They concluded that such an ‘encounter’ might take place once every 108 years, assuming a Type II SN rate of one every 100 years. The current, revised SN rate is actually some three to four times higher than that adopted by Clark et al., with one SN occurring every 25 to 30 years. This brings the typical time between close SN passages to a value of order 3 x 107 years. 13. Two main categories of supernova are generally recognized. Type I novae are produced through the accretion-driven collapse of a white dwarf star in a binary system. A Type II supernova is produced, on the other hand, by the collapse of the iron-rich core of a massive (Minitial > 8 M) star. The supernova types are generally distinguished observationally according to their spectra, brightness variations with time, and galactic location – Type II supernova, for example, only occur in spiral arm regions where massive stars are actively forming. 14. A pulsar is a rapidly spinning neutron star, and it is believed that such objects form during the supernova disruption of massive stars (i.e., in Type II SN). Spinning at a rate of 4.2 revolutions per second, the Geminga pulsar is believed to be about 300,000 years old. While Firestone and co-authors have assembled an impressive quantity of data to support their thesis, it should be pointed out that much of 64 Rejuvenating the Sun and Avoiding Other Global Catastrophes what they claim is controversial and almost all their data has multiple possible interpretations not necessarily requiring external (that is astronomical) driving influences. 15. Optical astronomers measure stellar brightness in terms of apparent magnitude. The apparent magnitude of a star is based upon the logarithm of the energy flux received from the star at the surface of Earth. The magnitude scale works in such a way that the brighter an object is, the more negative its magnitude. The faintest star visible to the human eye has an apparent magnitude of about +6, while the Hubble Space Telescope can record stars and galaxies as faint as magnitude +24. In contrast, the full Moon has an apparent magnitude of –12, and the apparent magnitude of the Sun is –27. 16. Collapsars are believed to be the final stage of massive star evolution. The progenitors are the highly distinctive Wolf-Rayet stars, first studied by the French astronomers Charles Wolf and Georges Rayet in the early 1900s. These stars are distinguished by showing emission lines in their spectra (virtually all other stars show only absorption lines) and they undergo extreme mass loss. By way of comparison, the Sun loses mass via a stellar wind at a rate of ∼10−14 M/yr, while a Wolf-Rayet star loses mass at a rate of 10−4 to 10−5 M/yr. The Wolf-Rayet stars are believed to represent the end stages of the evolution of stars with initial masses greater than ∼30 M, and the very final hypernova collapse is believed to produce a black hole rather than a neutron star. Working with Professor Romas Mitalas at the University of Western Ontario, this author studied the effects of mass loss upon massive stars [Effect of mass loss and overshooting on the width of the main sequence of massive stars, The Astrophysical Journal, 352, 291–299 (1990)] and found that the mass loss strongly reduces the observed luminosity but increases the surface temperature—a result that actually proves useful with respect to star-engineering. An alternative model for the cause of hypernova and GRB generation envisions the coalescence of two neutron stars previously orbiting each other in a binary system. Such mergers will again probably result in the formation of a black hole. Michael Shara discusses the possible consequences of star collisions and mergers in When stars collide, Scientific American, 287 (5), 46–51 (2002). 17. Brian Thomas et al., Terrestrial ozone depletion due to a Milky Way Gamma-Ray burst. Astrophysical Journal, 622, L153–L156 (2006). The authors conclude that a 10-second burst of gamma rays results in a globally averaged ozone depletion of order 35 percent (with some latitudes seeing a 55 percent reduction). A 50 percent decrease in It’s a Matter of Time 65 the ozone column translates to a three-fold increase in the UVB flux received at Earth’s surface. 18. J. Scalo and J. C. Wheeler [Astrophysical and astrobiological implications of gamma-ray burst properties. Astrophysical Journal, 566, 723–737 (2002)] have discussed the potential biological consequences of Earth encountering a strong burst of gamma rays. They point out that very little gamma-ray radiation actually reaches Earth’s surface and, indeed, a column of water just a few tens of centimeters thick would fully protect any marine organisms from a dangerous dose of radiation. Shielding by small amounts of rock and soil would protect other organisms. 19. Krzysztof Stanek et al, Protecting the Milky Way: metals keep the GRBs away. Paper submitted to the Astrophysical Journal in April 2006. 20. J. Annis. An astrophysical explanation for the Great Silence. Journal of the British Interplanetary Society. 52, 19–22 (1999). 21. Our Milky Way Galaxy is part of the so-called Local Group (LG) of galaxies. The LG contains at least 36 members within a region that stretches about 1 Mpc across its longest dimension. Most of the LG members are dwarf elliptical and irregular galaxies with masses of between one thousandth to one millionth that of the Milky Way. The Andromeda Galaxy (M31) is comparable in size and mass to our galaxy. Detailed studies of the central region of M31 reveal a double nucleus indicative of a past ‘collision’ and ‘disruption’ of a smaller LG member by Andromeda. 22. In order to determine the true spatial velocity and direction of motion of M31 a measure of both its line-of-sight (radial) velocity as well as its velocity tangential to the line-of-sight is required. Only the radial component is known and, consequently, it is not clear under what circumstances M31 will actually ‘collide’ with the Milky Way. 23. The burst of star formation triggered by the (potential) merger of M31 with the Milky Way will certainly produce large numbers of massive stars (stars with initial masses greater than 8 M). These massive stars have lifetimes of just a few million years (as indicated by Equation 2.1), and they eventually undergo core-collapse as Type II supernovae. Type II supernovae are typically less energetic than Type I supernovae (see Note 13 above), but the starburst conditions should result in a far greater number of such events occurring in our galaxy than observed at the present. 24. A black dwarf is the name given to the cold (near zero degrees Kelvin) remnant of a fully cooled-off white dwarf. Such objects remain stable against collapse due to the electron degeneracy of their interior, the 66 Rejuvenating the Sun and Avoiding Other Global Catastrophes pressure support for such gases being independent of temperature. The cooling time required to produce a black dwarf, however, is longer than the present age of the universe. 25. J. Scalo and J. C. Wheeler (see Note 18) point out that any life forms that might have evolved on Mars, even with its higher density atmosphere of the past, would not have fared so well as terrestrial organisms. They estimate that since the formation of the Solar System some 1,000 biologically significant GRB-related events have possibly occurred, and that surface life on Mars (i.e., eukaryotic bacteria) has probably been ‘sterilized’ many times over. This being said, Professor Alexander Pavlov (University of Arizona) and co-workers have recently argued [Was Earth ever infected by Martian Biota? Clues from radioresistant bacteria. Astrobiology, 6 (6), 911–918 (2006)] that the radiation tolerance of some terrestrial bacteria (e.i., Deinococcus radiodurans) is more likely to have evolved on Mars than Earth. The bacteria, having evolved on early Mars, were later transported to Earth via Martian meteorites. 26. Freeman Dyson, Search for artificial stellar sources of infrared radiation, Science, 131, 1667 (1960). A shell of radius 1 AU has a surface area of order 2 x (4 ) x (1.496 x 108) 2 = 5.6 x 1017 square kilometers. The factor of 2 accounts for both the inner and outer surfaces of the shell. Compared to Earth’s present land area, this corresponds to a 4 billion-fold increase in potential lebensraum. This being said, the shell of a Dyson sphere cannot, for dynamical stability reasons, be solid, but must consist of a ‘swarm’ of moonlets. Richard Carrigan, Jr. [Searching for Dyson spheres with Planck spectrum fits to IRAS, International Astronomical Congress paper: IAC-04-IAA- 1.1.1.06] provides an extensive review of observational searches. In a Phase I study of some 4,400 infrared point sources detected with IRAS (the Infra-Red Astronomical Satellite flown in 1983), Carrigan finds that about 1 in 600 have flux characteristics consistent with the radiation expected from a pure blackbody radiator with a temperature in the range 150 < T(K) < 500 [see, http://home.fnal.gov/∼carrigan/ Infrared_Astronomy/Fermilab_search.htm]. 27. It is not absolutely clear that Mars is volcanically dead. The crystallization ages of a number of Martian basaltic meteorites are as young as 165 million years. This corresponds to about 4 percent of the planet’s age. As pointed out by William Hartmann [A Traveler’s Guide to Mars, Workman Pub. NY (2003)], it is unlikely that Mars has been volcanically active for the past 96 percent of its history and then suddenly, in recent times, all eruptions stopped. It’s a Matter of Time 67 28. Solar reflectors can be used to either enhance the heating of a planet by reflecting additional sunlight into its atmosphere, or they can act as cooling shades by directly blocking the incoming sunlight. It has been proposed that the effects of CO2 global warming on Earth could be offset by placing a 2,000-km diameter parasol between Earth and the Sun [see, for example, Martin Hoffert and co-workers, Advanced technology paths to global climate stability: energy for a greenhouse planet, Science, 298, 981–987 (2002)]. 29. The U.S. National Academy of Sciences published a policy report in 1992 in which it was suggested that the effects of CO2 warming could be counteracted by installing 55,000 mirrors – each of surface area 100 km2 – in random inclination, near-Earth orbits. The effect of the mirrors would be to reduce the amount of solar energy intercepting Earth’s atmosphere. A similar concept could be used to reduce the direct solar heating of Venus. 30. The U.S. Climate Change Science Program (www.climatescience. gov/) released a report in April 2006 concluding that over the past 50 years there is clear and uncontroversial evidence for human activity-induced climate change. Likewise, Gabrielle Walker [The tipping point of the iceberg, Nature, 441, 802–805 (2006)] describes in sobering detail the distinct climate changes being recorded in Earth’s polar regions. It is perhaps a little ironic that some of the effects of human-induced global warming have been masked by anthropogenic aerosol production, which tends to actually cool the planet [see, for example, Jim Coakley’s commentary article, Reflections on aerosol cooling. Nature, 438, 1091–1092, 2005]. The irony of this situation is that as some (indeed a sad, small few) nations begin to curb and set new limits on the industrial emission of aerosols, the cooling effect that the aerosols cause will be lost—a process that will actually enhance global warming. 31. F. J. Dyson and G. Marland, Technical fixes for the climatic effects of CO2. Workshop on the global effects of carbon dioxide from fossil fuels. DOE report CONF-770385 (1979). 32. The 1991 eruption of Mt. Pinatubo induced a global mean temperature cooling of ∼0.5 K as a result of the release of sunlight-scattering SO2-based particles. The dispersal of SO2 into the atmosphere would, in principle, increase Earth’s insolation by increasing the amount of solar radiation that is reflected back into space [see, for example, the atmospheric model described by K. Taylor and J. Pinner, Response of the climate system to atmospheric aerosols and greenhouse gases, Nature, 369, 734–737 (1994)]. 68 Rejuvenating the Sun and Avoiding Other Global Catastrophes 33. J. H. Martin and co-workers [Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean, Nature, 371, 123–129 (1994)] seeded a 64-square-km area of the open Pacific with 15,600 liters of iron solution, and found a dramatic increase in the biomass of phytoplankton. It is the increased photosynthetic activity of the enhanced biomass that absorbs the atmospheric CO2. 34. E. Teller, L. Wood, and R. Hyde [Global warming and ice ages: I Prospects for physics-based modulation of global change. 22nd International Seminar on planetary emergencies, Erice (Sicily), Italy (1997)] argue that the predicted increase in global warming due to the enhanced CO2 abundance can be offset by a 1 percent reduction in the amount of solar radiation reaching Earth. They also argue that the onset of ice ages could be canceled by the appropriate manipulation of atmospheric CO2 concentrations and the amount of solar energy reaching Earth. 35. James Peason and co-workers [Earth rings for planetary environment control, 53rd International Astronautical Congress, 2002 (IAF-02- U.1.01)] modeled various ring systems extending out to distances between 1.2 and 1.8 Earth radii. The ring system casts a variable width and location shadow upon Earth’s surface, and it is this shading effect that results in atmospheric cooling. 36. O’Leary and co-workers [Retrieval of Asteroidal Materials, Space Resources and Space Settlements, NASA SP-428, 173–189 (1979)] studied the methods by which material from the Moon and Earthapproaching asteroids might be mined for chemical processing and the fabrication of large space structures. Indeed, O’Leary et al., conclude in their report that “immediate studies on asteroidalretrieval mission opportunities” be initiated, with “technology readiness for asteroid retrieval by the mid-1980s”. Twenty years late perhaps, in 2005, the first direct sampling of an asteroid surface was completed (hopefully) by the Japanese Space Agency’s Hyabusa spacecraft. The term ‘hopefully’ is employed since it is currently unclear if material was actually collected. We will only know for sure when the spacecraft returns to Earth in June 2010. 37. David Keith [Geoengineering, Nature, 409, 420 (2001)] discusses how the damaging side effects of pollution, derived from human industrial activity, might be redressed by planetary scale environmental engineering. He concludes: “I judge it likely that this century will see serious debate about—and perhaps implementation of—deliberate planetary-scale engineering.” 38. O’Neill outlines his plans in The Colonization of Space [Physics Today, September (1974)]. His study concludes that, given the It’s a Matter of Time 69 appropriate funding and political commitment, space colonies could be constructed “without robbing or harming anyone and without polluting anything.” He also argues that virtually all industry could be moved away from Earth and into space within 100 years. Writing these notes 32 years from the time of O’Neill’s original publication, it is clear that his ideas have not, as of yet, found the required imagination, funding and political will for action from either industry or national governments. 39. P. Birch, Supramundane planets, J. Brit. Interplan. Soc. 44, 169–182 (1991). The name supramundane is derived from the Latin supra (above) and mundus (world). The shell of a supramundane planet is not physically anchored to the surface of its central body and, consequently, the Jovian planets could be utilized as regions of colonization. A suprajupiter shell would have a surface area some 316 times that of Earth and potentially house, feed, and support up to 300 billion people. 40. D. R. Criswell [Solar system industrialization: implications for interstellar migrations, Interstellar Migration and the Human Experience, R. Finney and E. Jones (eds.) University of California Press, Berkeley (1985). pp. 50–87] has described human industrial development in terms of a triangular pyramid. The base of the pyramid is labeled according to ‘skill,’ ‘matter,’ and ‘energy.’ As human civilization has learned to control and use these three ‘bases,’ so it has produced the tip of the pyramid that Criswell calls “cumulative controlled connectives,” or CCCs. It is the future growth of CCCs that will determine human destiny and, increasingly, the ‘matter’ and ‘energy’ bases markers of the industrial growth pyramid that will ‘demand’ the extraction and exploitation of the raw materials residing within the greater Solar System beyond Earth. 41. M. J. Fogg [Solar exchange as a measure of ensuring the long term habitability of Earth, Speculations in Science and Technology. 12 (2), 153–157 (1988)] builds upon the idea of star lifting described by Criswell (see Note 40 above and the detailed discussion in Chapter 5). 42. Philosopher Nick Boston [Astronomical waste: The opportunity cost of delayed technological development. Utilitas, 15, 308–318 (2003)] takes this argument even further and argues that we (indeed, any galactic civilization) should strive to embrace and utilize the entire gamut of resources available within the Milky Way galaxy (and the Virgo super cluster beyond). That is, he argues humanity should strive to become a Kardashev Type III civilization (see Chapter 1, and especially Note 18 in that chapter). Indeed, he opens his paper in the following way: “As I write these words, suns are illuminating 70 Rejuvenating the Sun and Avoiding Other Global Catastrophes and heating empty rooms, unused energy is being flushed down black holes, and our great common endowment of negentropy is being irreversibly degraded into entropy on a cosmic scale. These are resources that an advanced civilization could have used to create value structures, such as sentient beings living worthwhile lives.” 43. The idea of a dynamic relationship between human population levels and the land carrying capacity was first articulated by Thomas Malthus (1766–1834) in 1798. The Malthusian catastrophe is often presented in the form that it is only such factors as epidemics and wars that hold human population levels in check. That is, if left unchecked the population level would simply increase to a point whereby the demand for food would outstrip all possible supply. Presumably (or at least hopefully) our descendants will solve the problem of epidemics and become more peaceful. If one follows the arguments presented by Criswell (Reference 40), then a Malthusian meltdown can be avoided by taking agriculture into space, indeed by adopting, for example, the space colonization strategies suggested by O’Neill (see Note 38).

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