Titan (moon)

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This article is about the planet Saturn's largest natural satellite. For other uses, see Titan (disambiguation).
Titan
Titan in natural color
Titan seen from the Cassini–Huygens spacecraft.
Discovery
Discovered byChristiaan Huygens
Discovery dateMarch 25 1655
Orbital characteristics[1]
1,221,870 km
Eccentricity0.0288
15.945 days
Inclination0.34854° (to Saturn's equator)
Satellite ofSaturn
Physical characteristics
Mean radius
2576 ± 2.00 km (0.404 Earths) [2]
8.3×107 km²
Mass1.3452 ± 0.0002×1023 kg (0.0225 Earths)[2]
Mean density
1.8798 ± 0.0044 g/cm³[2]
1.352 m/s2 (0.14 g)
2.639 km/s
(synchronous)
zero
Albedo0.22[3]
Temperature93.7 K (−-179.45°C)[4]
Atmosphere
Surface pressure
146.7 kPa
Composition by volume98.4% nitrogen
1.6% methane[5]

Titan (/ˈtaɪ.tən/, from Ancient Greek Τῑτάν) or Saturn VI is the largest moon of Saturn, the only moon known to have a dense atmosphere,[6] and the only object other than Earth for which clear evidence of stable bodies of surface liquid has been found.[7]

Titan is the twentieth-most distant moon of Saturn and sixth-farthest among those large enough to assume a spheroid shape. Frequently described as a satellite with planet-like characteristics, Titan's diameter is roughly 50% larger than Earth's moon and it is 80% more massive. It is the second-largest moon in the Solar System, after Jupiter's moon Ganymede, and it is larger by diameter than the smallest planet, Mercury (although only half as massive). Titan was the first known moon of Saturn, discovered in 1655 by the Dutch astronomer Christiaan Huygens.[8]

Titan is primarily composed of water ice and rocky material. The dense atmosphere prevented understanding of Titan's surface until new information accumulated with the arrival of the Cassini–Huygens mission in 2004, including the discovery of liquid hydrocarbon lakes in the satellite's polar regions. These are the only large, stable bodies of surface liquid known to exist anywhere other than Earth. The surface is geologically young; although mountains and several possible cryovolcanoes have been discovered, it is relatively smooth and few impact craters have been discovered.

The atmosphere of Titan is largely composed of nitrogen and its climate includes methane and ethane clouds. The climate—including wind and rain—creates surface features that are similar to those on Earth, such as sand dunes and shorelines, and like Earth, is dominated by seasonal weather patterns. With its liquids (both surface and subsurface) and robust nitrogen atmosphere, Titan is viewed as analogous to the early Earth, although at much lower temperature. The satellite has thus been cited as a possible host for microbial extraterrestrial life or, at least, as a prebiotic environment rich in complex organic chemistry. Researchers have suggested a possible underground liquid ocean might serve as a biotic environment.[9][10]

Discovery and naming

Christiaan Huygens, discoverer of Titan

Titan was discovered on March 25, 1655, by the Dutch astronomer Christiaan Huygens. Huygens was inspired by Galileo's discovery of Jupiter's four largest moons in 1610 and his improvements on telescope technology.[11] Huygens himself made advances in the technology and his discovery of Titan owed "partly to the quality of his telescope and partly to luck."[12] He named it simply Saturni Luna (or Luna Saturni, Latin for "Saturn's moon"), publishing in the 1655 tract De Saturni Luna Observatio Nova. After Giovanni Domenico Cassini published his discoveries of four more moons of Saturn between 1673 and 1686, astronomers fell into the habit of referring to these and Titan as Saturn I through V (with Titan then in fourth position). Other early epithets for Titan include "Saturn's ordinary satellite".[13] Titan is officially numbered Saturn VI because after the 1789 discoveries the numbering scheme was frozen to avoid causing any more confusion (Titan having borne the numbers II and IV as well as VI). Numerous small moons have been discovered closer to Saturn since then.

The name "Titan," and the names of all seven satellites of Saturn then known, come from John Herschel (son of William Herschel, discoverer of Mimas and Enceladus) in his 1847 publication Results of Astronomical Observations made at the Cape of Good Hope.[14] He suggested the names of the mythological Titans, sisters and brothers of Cronos, the Greek Saturn.

Orbit and rotation

Titan's orbit (highlighted in red) among the other large inner moons of Saturn. The moons outside its orbit are (l-r) Iapetus and Hyperion; those inside are Dione, Tethys, Enceladus and Mimas

Titan orbits Saturn once every 15 days and 22 hours. Like the Earth's moon and many of the other gas giant satellites, its orbital period is identical to its rotational period; Titan is thus tidally locked in synchronous orbit around Saturn. Its orbital eccentricity is 0.0288, and it is inclined 0.348 degrees relative to the Saturnian equator.[1] Viewed from Earth, the moon reaches an angular distance of about 20 Saturn radii (just over 1.2 million kilometers) from Saturn and subtends a disk 0.8 arcseconds in diameter.

Titan is locked in orbital resonance with the small, irregularly-shaped satellite Hyperion; the two bodies orbit in a 3:4 ratio, respectively. A "slow and smooth" evolution of the resonance—in which Hyperion would have migrated from a chaotic orbit—is considered unlikely, based on models. Hyperion likely formed in a stable orbital island, while massive Titan absorbed or ejected bodies that made close approaches.[15]

Bulk characteristics

Titan compared to Earth.
Titan's internal structure.

Titan is 5,150 km across, compared to 4,879 km for the planet Mercury and 3,474 km for Earth's moon. Before the arrival of Voyager 1 in 1980, Titan was thought to be slightly larger than Ganymede (diameter 5,262 km) and thus the largest moon in the Solar System; this was an overestimation caused by Titan's dense, opaque atmosphere, which extends many miles above its surface and increases its apparent diameter.[16] Titan's diameter and mass (and thus its density) are similar to Jovian moons Ganymede and Callisto.[17] Based on its bulk density of 1.88 g/cm³, Titan's bulk composition is half water ice and half rocky material. Though similar in composition to Dione and Enceladus, it is denser due to gravitational compression.

Titan is probably differentiated into several layers with a 3,400 km (2,040 mi) rocky center surrounded by several layers composed of different crystal forms of ice.[18] Its interior may still be hot and there may be a liquid layer consisting of water and ammonia between the ice I crust and deeper ice layers made of high pressure forms of ice. Evidence for such an ocean has recently been uncovered by the Cassini probe in the form of natural extremely low frequency (ELF) radio waves in Titan's atmosphere. Titan's surface is thought to be a poor reflector of ELF waves, so they may instead be reflecting off the liquid-ice boundary of a subsurface ocean.[19]

Atmosphere

True-color image of layers of haze in Titan's atmosphere.

Titan is the only known moon with a fully developed atmosphere that consists of more than just trace gases. Atmosphere thickness has been suggested ranging between 200 km[20] and 880 km.[21] The atmosphere is opaque at many wavelengths and a complete reflectance spectrum of the surface is impossible to acquire from the outside;[22] it was this haziness that led to errors in diameter estimates.

The presence of a significant atmosphere was first discovered by Gerard P. Kuiper in 1944 using a spectroscopic technique that yielded an estimate of an atmospheric partial pressure of methane of the order of 100 millibars (10 kPa).[23] Observations from the Voyager space probes have shown that the Titanian atmosphere is denser than Earth's, with a surface pressure more than one and a half times that of our planet. It supports opaque haze layers that block most visible light from the Sun and other sources and renders Titan's surface features obscure. The haze that can be seen in the picture to the right contributes to the moon's anti-greenhouse effect and lowers the temperature by reflecting sunlight away from the satellite. The atmosphere is so thick and the gravity so low, that humans could fly through it by flapping "wings" attached to their arms.[24] The Huygens probe was unable to detect the direction of the Sun during its descent, and although it was able to take images from the surface, the Huygens team likened the process to "taking pictures of an asphalt parking lot at dusk".[25]

The atmosphere is 98.4% nitrogen—the only dense nitrogen-rich atmosphere in the solar system aside from the Earth's—with the remaining 1.6% composed of methane and trace amounts of other gases such as hydrocarbons (including ethane, diacetylene, methylacetylene, acetylene, propane), argon, carbon dioxide, carbon monoxide, cyanogen, cyanoacetylene, hydrogen cyanide and helium.[5] The hydrocarbons are thought to form in Titan's upper atmosphere in reactions resulting from the breakup of methane by the Sun's ultraviolet light, producing a thick orange smog. Titan has no magnetic field and sometimes orbits outside Saturn's magnetosphere, directly exposing it to the solar wind. This may ionize and carry away some molecules from the top of the atmosphere.

Energy from the Sun should have converted all traces of methane in Titan's atmosphere into hydrocarbons within 50 million years; a relatively short time compared to the age of the Solar System. This suggests that methane must be somehow replenished by a resevoir on or within Titan itself. That Titan's atmosphere contains more than a thousand times as much methane as carbon monoxide would appear to rule out significant contributions from cometary impacts, since comets are composed of more carbon monoxide than methane. That Titan might have accreted an atmosphere from the early Saturnian nebula at the time of formation also seems unlikely; in such a case, it ought to have atmospheric abundances similar to the solar nebula, including hydrogen and neon.[26] A possible biological origin for the methane has not been discounted (see below).[10]

A graph detailing temperature, pressure, and other aspects of Titan's atmosphere. At the surface, the pressure on Titan is 50% greater than on Earth.

Simulations of global wind patterns based on wind speed data taken by Huygens during its descent have suggested that Titan's atmosphere circulates in a single enormous Hadley cell. Warm air rises in Titan's southern hemisphere—which was experiencing summer during Huygens' descent—and sinks in the northern hemisphere, resulting in high-altitude air flow from south to north and low-altitude airflow from north to south. Such a large Hadley cell is only possible on a slowly rotating world such as Titan.[27] The pole-to-pole wind circulation cell appears to be centered on the stratosphere; simulations suggest it ought to change every twelve years, with a three year transition period, over the course of Titan's year (30 terrestrial years).[28] There is also a pattern of air circulation found flowing in the direction of Titan's rotation, from west to east.[27] Observations by Cassini of the atmosphere made in 2004 also suggest that Titan is a "super rotator," like Venus, with an atmosphere that rotates much faster than its surface.[29]

Titan's ionosphere is also more complex than Earth's, with the main ionosphere at an altitude of 1200 km but with an additional layer of charged particles at 63 km. This splits Titan's atmosphere to some extent into two separate radio resonating chambers. The source of natural ELF waves (see above) on Titan is unclear as there does not appear to be extensive lightning activity.[19]

Climate

A methane cloud imaged in false colour over Titan's north pole

Titan's temperature is about 94 K (−179 °C, or −290.2 °F) at the surface. At this temperature water ice does not sublimate from solid to gas, so the atmosphere is nearly free of water vapor. The clouds on Titan, probably composed of methane, ethane or other simple organics, are scattered and variable, punctuating the overall haze.[16] The orange color as seen from space must be produced by other more complex chemicals in small quantities, possibly tholins, a tar-like organic precipitate.[30] The findings of the Huygens probe indicate that Titan's atmosphere periodically rains liquid methane and other organic compounds onto the moon's surface.[31] It is possible that areas of Titan's surface may be coated in a layer of tholins, but this has not been confirmed.[32]

Ground-based observations show that Titan's climate changes with the seasons. Over the course of Saturn's 30-year orbit, Titan's cloud systems appear to manifest for 25 years, and then fade for four to five years, before reappearing again.[33]

Clouds

In 2006, Cassini imaged cloud cover over Titan's north pole. In September, it imaged a large cloud at a height of 40 km. Although methane is known to condense in Titan's atmosphere, the cloud was more likely to be ethane, as the detected size of the particles was only 1–3 microns and ethane can also freeze at these altitudes. In December, Cassini again observed cloud cover and detected methane, ethane and other organics. The cloud was over 2,400 km in diameter and was still visible during a following flyby a month later. One hypothesis is that it is currently raining (or, if cool enough, snowing) on the north pole; the downdrafts at high northern latitudes are strong enough to drive organic particles towards the surface. These were the strongest evidence yet for the long hypothesised "methanological" cycle (analogous to Earth's hydrological cycle) on Titan.[33]

Clouds have also been found over the south pole. While typically covering 1% of Titan's disk, outburst events have been observed in which the cloud cover rapidly expands to as much as 8%. One hypothesis asserts that the southern clouds are formed when heightened levels of sunlight during the Titanian summer generate uplift in the atmosphere, resulting in convection. This explanation is complicated by the fact that cloud formation has been observed not only post-summer solstice but also at mid-spring. Increased methane humidity at the south pole possibly contributes to the rapid increases in cloud size.[34] It is currently summer in Titan's southern hemisphere and will remain so until 2010, when Saturn's orbit, which governs the moon's motion, will tilt the northern hemisphere towards the Sun.[27] When the seasons switch, ethane will begin to condense over the south pole.[35]

Research models that match well with observations, suggest that clouds on Titan cluster at preferred coordinates and that cloud cover varies by distance from surface on different parts of the satellite. In the polar regions (above 60 degrees latitude), widespread and permanent ethane clouds appear in and above the troposphere; at lower latitudes, mainly methane clouds are found between 15 and 18 km, and are more sporadic and localized. In the summer hemisphere, frequent, thick but sporadic methane clouds seem to cluster around 40°.[28]

Surface features

See also: list of geological features on Titan
Titan in false color showing surface details and atmosphere. "Xanadu" is the bright region at the centre-right

The surface of Titan has been described as "complex, fluid-processed, [and] geologically young."[36] The Cassini spacecraft has used radar altimetry and synthetic aperture radar (SAR) imaging to map portions of Titan during its close fly-bys of the moon. The first images revealed a diverse geology, with both rough and smooth areas. There are features that seem volcanic in origin, which probably disgorge water mixed with ammonia. There are also streaky features, some of them hundreds of kilometers in length, that appear to be caused by windblown particles.[37][38] Examination has also shown the surface to be relatively smooth; the few objects that seem to be impact craters appeared to have been filled in, perhaps by raining hydrocarbons or volcanoes. Radar altimetry suggests height variation is low, typically no more than 150 meters. Occasional elevation changes of 500 meters have been discovered and Titan has mountains that sometimes reach several hundred meters to more than 1 kilometer in height.[39]

Titan's surface is marked by broad regions of bright and dark terrain. These include Xanadu, a large, reflective, equatorial area about the size of Australia. It was first identified in infrared images from the Hubble Space Telescope in 1994, and later viewed by the Cassini spacecraft. The convoluted region is filled with hills and cut by valleys and chasms.[40] It is criss-crossed in places by dark lineaments—sinuous topographical features resembling ridges or crevices. These may represent tectonic activity, which would indicate that Xanadu is geologically young. Alternatively, the lineaments may by liquid-formed channels, suggesting old terrain that has been cut through by stream systems.[41] There are dark areas of similar size elsewhere on the moon, observed from the ground and by Cassini; it had been speculated that these are methane or ethane seas, but Cassini observations seem to indicate otherwise (see below).

Liquids

File:PIA09102PIA09102 Liquid Lakes on Titan.jpg
Pseudo-colored radar imaging data from a Cassini flyby of northern lattitudes, published in the journal Nature to illustrate the convincing evidence for large bodies of liquid. The false blue coloring indicates low radar reflectivity areas, likely caused by liquid.

Given Hubble and other observational data, the existence of liquid methane had long been suggested on Titan, either in disconnected pockets or on the scale of satellite-wide oceans, similar to water on Earth.[42] The Cassini mission would affirm the former hypothesis, although though not immediately. When the probe arrived in the Saturnian system in 2004, it was hoped that hydrocarbon lakes or oceans might be detectable by reflected sunlight from the surface of any liquid bodies, but no specular reflections were initially observed.[43]

The possibility remained that liquid ethane and methane might be found on Titan's poles, where it was expected to be abundant and stable.[7] At Titan's south pole, an enigmatic dark feature named Ontario Lacus was the first suspected lake identified, possibly created by clouds that are observed to cluster in the area.[44] A possible shoreline was also identified at the pole via radar imagery.[45] Following a flyby on July 22, 2006, in which the Cassini spacecraft's radar imaged the northern latitudes (which are currently in winter), a number of large, smooth (and thus dark to radar) patches were seen dotting the surface near the pole.[46] Based on the observations, scientists announced "definitive evidence of lakes filled with methane on Saturn's moon Titan" in January 2007.[7][47] The Cassini–Huygens team concluded that the imaged features are almost certainly the long sought hydrocarbon lakes, the first stable bodies of liquid found off Earth. Some appear to have channels associated with liquid and lie in topographical depressions.[7]

Repeated coverage of these areas should prove whether they are truly liquid, as any changes that correspond with wind blowing on the surface of the liquid would alter the roughness of the surface and be visible in the radar. The high relative humidity of methane in Titan’s lower atmosphere could be maintained by evaporation from lakes covering only 0.002–0.02% of the whole surface.[4]

File:TitanSeaComparison.jpg
NASA image comparing a body of liquid on Titan with Lake Superior.

During a Cassini flyby in late February 2007, radar and camera observations revealed several large features in the north polar region that may be large expanses of liquid methane and/or ethane, including one sea with an area of over 100,000 square kilometers (larger than Lake Superior), and another (though less definite) region potentially the size of the Caspian Sea.[48]

Image of Titan taken during Huygens' descent, showing hills and topographical features that resemble a shoreline and drainage channels.

The discoveries at the poles contrast with the findings of the Huygens probe, which landed near Titan's equator on January 14 2005. The images taken by the probe during its descent showed no open areas of liquid, but strongly indicated the presence of liquids in the recent past, showing pale hills crisscrossed with dark drainage channels that lead into a wide, flat, darker region. It was initially thought that the dark region might be a lake of a fluid or at least tar-like substance, but it is now clear that Huygens landed on the dark region, and that it is solid without any indication of liquids. A penetrometer studied the composition of the surface as the craft impacted it, and it was initially reported that the surface was similar to wet clay, or perhaps crème brûlée (that is, a hard crust covering a sticky material). Subsequent analysis of the data suggests that this reading was likely caused by Huygens displacing a large pebble as it landed, and that the surface is better described as a 'sand' made of ice grains.[49] The images taken after the probe's landing show a flat plain covered in pebbles. The pebbles may be made of water ice and are somewhat rounded, which may indicate the action of fluids.[50]

Impact craters

Impact crater on Titan's surface

Radar SAR and imaging data from Cassini have revealed a relative paucity of impact craters on Titan's surface, suggesting a youthful surface. The few impact craters discovered include a 440 km wide multi-ring impact basin named Menrva (seen by Cassini's ISS as a bright-dark concentric pattern).[51] A smaller 80 km wide flat-floored crater named Sinlap[52] and a 30 km crater with a central peak and dark floor named Ksa have also been observed.[53] RADAR and Cassini imaging have also revealed a number of "crateriforms", circular features on the surface of Titan that may be impact related, but lack certain features that would make identification certain. For example, a 90 km wide ring of bright, rough material known as Guabonito has been observed by Cassini.[54] This feature is thought to be an impact crater filled-in by dark, windblown sediment. Several other similar features have been observed in the dark Shangri-la and Aaru regions. RADAR observed several circular features that may be craters in the bright region Xanadu during Cassini's April 30, 2006 flyby of Titan.[55]

Pre-Cassini models of impact trajectories and angles suggest that where the impactor strikes the water-ice crust, a small amount of ejecta remains as liquid water within the crater. It may persist as liquid for centuries or longer, sufficient for "the synthesis of simple precursor molecules to the origin of life."[56] While infill from various geological processes is one reason for Titan's relative deficiency of craters, atmospheric shielding also plays a role; it is estimated that Titan's atmosphere reduces the number of craters on its surface by a factor of two.[57]

Cryovolcanism and mountains

See also: Cryovolcano
Near-infrared image of Tortola Facula, thought to be a possible cryovolcano.

Scientists have speculated that conditions on Titan resemble those of early Earth, though at a much lower temperature. Evidence of volcanic activity from the latest Cassini mission suggests that temperatures are probably much higher in hotbeds, enough for liquid water to exist. Argon 40 detection in the atmosphere indicates that volcanoes spew plumes of "lava" composed of water and ammonia.[58] Cassini detected methane emissions from one suspected cryovolcano, and volcanism is now believed to be a significant source of the methane in the atmosphere.[59][60] One of the first features imaged by Cassini, Ganesa Macula, resembles the geographic features called "pancake domes" found on Venus, and is thus believed to be cryovolcanic in origin.[61]

The pressure necessary to drive the cryovolcanoes may be caused by ice "underplating" Titan's outer shell. The low pressure ice, overlaying a liquid layer of ammonium sulfate, ascends buoyantly, and the unstable system can produce dramatic plume events. Titan is resurfaced through the process by grain sized ice and ammonium sulfate ash, which helps produce a wind-shaped landscape and sand dune features.[62]

A mountain range measuring 150 km long, 30 km wide and 1.5 km high was discovered by Cassini in 2006. This range lies in the southern hemisphere and is thought to be composed of icy material and covered in methane snow. The movement of tectonic plates, perhaps influenced by a nearby impact basin, could have opened a gap through which the mountain's material upwelled.[63]

Dark terrain

Sand dunes on Earth (top), compared with dunes on Titan's surface.

In the first images of Titan's surface taken by Earth-based telescopes in the early 2000s, large regions of dark terrain were revealed straddling Titan's equator.[64] Prior to the arrival of Cassini, these regions were thought to be seas of organic matter like tar or seas of liquid hydrocarbons.[65] Radar images captured by the Cassini spacecraft have instead revealed some of these regions to be extensive plains covered in longitudinal sand dunes, up to 330 meters high.[66] The longitudinal (or linear) dunes are believed to be formed by moderataly variable winds that either follow one mean direction or alternate between two different directions. Dunes of this type are always aligned with average wind direction. In the case of Titan, steady zonal (eastward) winds combine with variable tidal winds (approximately 0.5 meter per second).[67] The tidal winds are the result of tidal forces from Saturn on Titan's atmosphere, which are 400 times stronger than the tidal forces of the Moon on Earth and tend to drive wind toward the equator. This wind pattern causes sand dunes to build up in long parallel lines aligned west-to-east. The dunes break up around mountains, where the wind direction shifts.

The sand on Titan might have formed when liquid methane rained and eroded the ice bedrock, possibly in the form of flash floods. Alternatively, the sand could also have come from organic solids produced by photochemical reactions in Titan's atmosphere.[68][66][67]

Observation and exploration

Cassini image of Epimetheus and Titan

Titan is never visible to the naked eye, but can be observed through small telescopes or strong binoculars. Amateur observation is difficult because of the proximity of the satellite to Saturn's brilliant globe and ring system; an occulting bar, covering part of the eyepiece and used to block the bright planet, greatly improves viewing.[69] Titan has a maximum apparent magnitude of +7.9. This compares to +4.6 for the similarly sized Ganymede, in the Jovian system.

Observations of Titan prior to the space age were limited. In 1907 Spanish astronomer Jose Comas Sola suggested that he had observed darkening near the edges of Titan's disk and two round white patches in its center. The deduction of an atmosphere by Kuiper in the 1940s was the next major observational event.[70]

The first probe to visit the Saturnian system was Pioneer 11 in 1979, which determined that Titan was likely too cold to support life.[71] The craft took the first images of the moon (including some of it and Saturn together) but these were of low quality; the first ever close-up of Titan was taken on September 2, 1979.[72]

Titan was examined by both Voyager 1 and Voyager 2 in 1980 and 1981, respectively. Voyager 1's course was diverted specifically to make a closer pass of Titan. Unfortunately, the craft did not possess any instruments that could penetrate Titan's haze, an unforeseen factor. Many years later, intensive digital processing of images taken through Voyager 1''s orange filter did reveal hints of the light and dark features now known as Xanadu and Shangri-la,[73] but by then they had already been observed in the infrared by the Hubble Space Telescope. Voyager 2 took only a cursory look at Titan. The Voyager 2 team had the option of steering the spacecraft to take a detailed look at Titan or to use another trajectory which would allow it to visit Uranus and Neptune. Given the lack of surface features seen by Voyager 1, the latter plan was implemented.

Cassini-Huygens

Main articles: Cassini–Huygens and Huygens probe

Even with the data provided by the Voyagers, Titan remained a body of mystery—a planet-like satellite, which is shrouded in an atmosphere that makes detailed observation difficult. The intrigue that had surrounded Titan since the 17th century observations of Christiaan Huygens and Giovanni Cassini was finally gratified by the spacecraft named in their honor.

The Cassini–Huygens spacecraft reached Saturn on July 1, 2004 and has begun the process of mapping Titan's surface by radar. A joint project of the European Space Agency (ESA) and NASA, Cassini-Huygens has proved a very successful mission. The Cassini probe flew by Titan on October 26 2004 and took the highest-resolution images ever of the moon's surface, at only 1,200 kilometers, discerning patches of light and dark that would be invisible to the human eye from the Earth. Huygens landed on Titan on January 14, 2005, discovering that many of the moon's surface features seem to have been formed by flowing fluids at some point in the past.[74] Present liquid on the surface may be found near the north pole, in the form of many lakes that were recently discovered by Cassini.[46] Titan is the most distant body from Earth that has seen a space probe landing.[75]

Huygens landing site

Huygens image from Titan's surface

The Huygens probe landed just off the easternmost tip of a bright region now called Adiri, where it photographed pale hills with dark 'rivers' running down to a dark plain. Current understanding is that the hills (also referred to as highlands) are composed mainly of water ice. Dark organic compounds, created in the upper atmosphere by the ultraviolet radiation of the Sun, may rain from Titan's atmosphere. They are washed down the hills with the methane rain and are deposited on the plains over geological time scales.[59]

After landing, Huygens photographed a dark plain covered in small rocks and pebbles, which are composed of water ice.[59] The two rocks just below the middle of the image on the right are smaller than they may appear: the left-hand one is 15 centimeters (6 inches) across, and the one in the center is 4 centimeters (about 1.5 inches) across, at a distance of about 85 centimeters (about 33 inches) from Huygens. There is evidence of erosion at the base of the rocks, indicating possible fluvial activity. The surface is darker than originally expected, consisting of a mixture of water and hydrocarbon ice. It is believed that the 'soil' visible in the images is precipitation from the hydrocarbon haze above.

In March of 2007, NASA, ESA, and COSPAR decided to name the Huygens landing site The Hubert Curiel Memorial Station in memory of a president of the ESA.[76]

Prebiotic conditions and possible life

See also: Planetary habitability

Scientists believe that the atmosphere of early Earth was similar in composition to the current atmosphere on Titan. Many hypotheses have developed that attempt to bridge the step from chemical to biological evolution. The Miller-Urey experiment and several following experiments have shown that with an atmosphere similar to that of Titan and the addition of UV radiation, complex molecules and polymer substances like tholins can be generated. The reaction starts with dissociation of nitrogen and methane forming hydrocyan and ethyne. Further reactions have been studied extensively.[77]

All of these experiments have led to the suggestion that enough organic material exists on Titan to start a chemical evolution analogous to what is thought to have started life on Earth. While the analogy assumes the presence of liquid water for longer periods than is currently observable, several theories suggest that liquid water from an impact could be preserved under a frozen isolation layer.[78] It has also been observed that liquid ammonia oceans could exist deep below the surface;[9] one model suggests an ammonia-water solution as much as 200 km deep beneath a water ice crust, conditions that "while extreme by terrestrial standards, are such that life could indeed survive."[10] Heat transfer between the interior and upper layers would be critical in sustaining any sub-surface oceanic life.[9]

Detection of microbial life on Titan would depend on its biogenic effects. That the atmospheric methane and nitrogen are of biological origin has been examined, for example.[10] Hydrogen has been cited as one molecule suitable to test for life on Titan: if methanogenic life is consuming atmospheric hydrogen in sufficient volume it will have a measurable effect on the mixing ratio in the troposphere.[79]

Despite these biological possibilities, there are formidable obstacles to life on Titan and any analogy to Earth is inexact. At a vast distance from the Sun, Titan is frigid (a fact exacerbated by the anti-greenhouse effect of its cloud cover), and its atmosphere lacks CO2. Given these difficulties, the topic of life on Titan may be best described as an experiment for examining theories on conditions necessary prior to flourishing life's on Earth.[80] While life itself may not exist, the prebiotic conditions of the Titanian environment, and the possible presence of organic chemistry, remain of great interest in understanding the early history of the terrestrial biosphere.[81] Using Titan as a prebiotic experiment involves not only observation through spacecraft, but laboratory experiment, and chemical and photochemical modelling on Earth.[77]

An alternate explanation for life's hypothetical existence on Titan has been proposed: if life were to be found on Titan, it would be statistically more likely to have originated from Earth than to have appeared independently, a process known as panspermia. It is theorized that large asteroid and cometary impacts on Earth's surface have caused hundreds of millions of fragments of microbe-laden rock to escape Earth's gravity. Calculations indicate that a number of these would encounter many of the bodies in the solar system, including Titan.[82][83]

While the Cassini–Huygens mission was not equipped to provide evidence for biology or complex organics, it did support the theory of an environment on Titan that is similar, in some ways, to that of the primordial Earth. Future missions are not currently being planned to research the issue, and considering the time required for executing a voyage, further scientific data may be decades away.[81]

See also

References

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Further reading

  • Lorenz, Ralph (May 2002). Lifting Titan's Veil: Exploring the Giant Moon of Saturn. Cambridge University Press. ISBN 0-521-79348-3. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)

External links

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