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Der Saturnmond Titan in Echtfarben

Der Saturnmond Titan ist einer von mehreren Kandidaten für eine mögliche Besiedlung des äußeren Solarsystems. Eine mögliche Motivation ist der Abbau von Kohlenwasserstoff.


Natürliche Rohstoffe[Bearbeiten | Quelltext bearbeiten]

Seen auf Titan

Den Daten der Cassini-Mission zufolge lagert auf Titan ein Kohlenwasserstoffvorkommen, das die Menge natürlicher Gas- und Ölreserven auf der Erde um das hundertfache übersteigt. Der Kohlenwasserstoff regnet vom Himmel und sammelt sich in großflächigen Seen.

[1]

Ralph Lorenz meinte dazu: "Titan is just covered in carbon-bearing material—it’s a giant factory of organic chemicals. [...] This vast carbon inventory is an important window into the geology and climate history of Titan.”[2]

("Titan ist mit kohlenstoffhaltigem Material nur so bedeckt - er ist eine riesige Fabrik für organische Chemikalien. [...] Diese reichhaltigen Kohlenstoffvorkommen geben uns wichtige Einblicke in die Geologie und die Klimageschichte Titans.")



Ein "See" auf Titan im Vergleich mit dem Lake Superior

Radar images obtained on July 21, 2006 appear to show lakes of liquid hydrocarbon (such as methane and ethane) in Titan's northern latitudes. This is the first discovery of currently-existing lakes anywhere besides Earth. The lakes range in size from about a kilometer to one which is one hundred kilometers across.[3]

On March 13, 2007, JPL announced that it found strong evidence of seas of methane and ethane in the northern hemisphere. At least one of these is larger than any of the Great Lakes in North America.[4]

Suitability[Bearbeiten | Quelltext bearbeiten]

The Jovian system is the least likely to be developed for collecting resources from a gas giant, because of its extraordinary radiation belt. The American aerospace engineer and author Robert Zubrin identified Saturn as the most important and most valuable of the three other gas giants, because of its relative proximity, low radiation, and excellent system of moons. He also named Titan as the most important moon on which to establish a base to develop the resources of the Saturn system. [5]

Habitability[Bearbeiten | Quelltext bearbeiten]

Dr. Zubrin has pointed out that Titan possesses an abundance of all the elements necessary to support life, saying "In certain ways, Titan is the most hospitable extraterrestrial world within our solar system for human colonization." [6] The atmosphere contains plentiful nitrogen and methane, and strong evidence indicates that liquid methane is on the surface and, liquid water, and ammonia are present under the surface and are often delivered to the surface by volcanic activity. Water can easily be used to generate breathable oxygen. Nitrogen is ideal to add buffer gas partial pressure to breathable air; indeed, nitrogen forms about 78% of Earth's atmosphere. [7] Nitrogen, methane and ammonia can all be used to produce fertilizer for growing food.

Atmosphere[Bearbeiten | Quelltext bearbeiten]

Additionally, Titan has an atmospheric pressure one and a half times that of Earth -- approximately the same as 5 meters underwater on Earth. This means that the interior air pressure of landing craft and habitats could be set equal or close to the exterior pressure, reducing the difficulty and complexity of structural engineering for landing craft and habitats compared with low or zero pressure environments such as on the Moon, Mars, or the asteroids. The thick atmosphere would also make radiation a non-issue, unlike on the Moon, Mars, or the asteroids. However, Titan's atmosphere contains hydrogen cyanide, and is extremely toxic for humans: even small amounts are enough to cause death.

Gravity[Bearbeiten | Quelltext bearbeiten]

Titan has a surface gravity of 0.14 g, slightly less than that of the Moon. Managing long-term effects of low gravity on human health would therefore be a significant issue for long-term occupation of Titan, more so than on Mars. These effects are still an active field of study. They can include symptoms such as loss of bone density, loss of muscle density, and a weakened immune system. Astronauts in Earth orbit have remained in microgravity for up to a year and more at a time. Effective countermeasures for the negative effects of low gravity are well-established, particularly an aggressive regimen of daily physical exercise. The variation in the negative effects of low gravity as a function of different levels of low gravity are not known, since all research in this area is restricted to humans in zero gravity. The same goes for the potential effects of low gravity on fetal and pediatric development. It has been hypothesized that children born and raised in low gravity such as on Titan would not be well adapted for life under the higher gravity of Earth. [8]

Temperature[Bearbeiten | Quelltext bearbeiten]

The temperature on Titan is about 94 K (-179 °C, or -290.2 °F), so insulation and heat generation and management would be significant concerns. Although the air pressure at the surface is about 1.5 times that of Earth sea level, because of the colder temperature, the density of the air is about 4.5 times that of Earth sea level. This substantial density should moderate shifts in temperature over time and from one locale to another, to a fraction of the types of temperature changes familiar from the day/night cycle, the seasons, and weather on Earth. The corresponding narrow range of temperature variation further reduces the difficulties in structural engineering.

Relative thickness of the atmosphere combined with extreme cold makes additional troubles for human habitation. Unlike vacuum, the high atmospheric density makes thermoinsulation a significant engineering problem.

Flight on Titan[Bearbeiten | Quelltext bearbeiten]

The very high ratio of atmospheric density to surface gravity also greatly reduces the wingspan needed for an aircraft to maintain lift, so much so that a human would be able to strap on wings and easily fly through the atmosphere.[6]

References[Bearbeiten | Quelltext bearbeiten]

{Reflist}

Further reading[Bearbeiten | Quelltext bearbeiten]

  • Stephen L. Gillett, "Titan as the Abode of Life," Analog, Vol. CXII No. 13, pp. 40–55 (1992)

[[Category:Titan]] [[Category:Space colonization]] [[es:Colonización de Titán]] [[fr:Colonisation de Titan]] [[pl:Mozliwosci eksploatacji Tytana]] [[sv:Rymdkolonisering#Titan]]

  1. Titan’s surface organics surpass oil reserves on Earth. 13 February 2008 http://www.esa.int/esaSC/SEMCSUUHJCF_index_0.html
  2. Ergebnisse einer Studie von Ralph Lorenz, Mitglied des Radar-Teams der Cassini-Mission und der Johns Hopkins University, veröffentlicht 29.1.2008 in den Geophysical Research Letters
  3. Cassini-Huygens: News
  4. Cassini-Huygens: News
  5. Robert Zubrin, Entering Space: Creating a Spacefaring Civilization, section: The Persian Gulf of the solar system, pp. 161-163, Tarcher/Putnam, 1999, ISBN 978-1-58542-036-0
  6. a b Robert Zubrin, Entering Space: Creating a Spacefaring Civilization, section: Titan, pp. 163-166, Tarcher/Putnam, 1999, ISBN 978-1-58542-036-0
  7. Robert Zubrin, The Case for Mars: The Plan to Settle the Red Planet and Why We Must, p. 146, Simon & Schuster/Touchstone, 1996, ISBN 978-0-684-83550-1
  8. Robert Zubrin, "Colonizing the Outer Solar System", in Islands in the Sky: Bold New Ideas for Colonizing Space, pp. 85-94, Stanley Schmidt and Robert Zubrin, eds., Wiley, 1996, ISBN 978-0-471-13561-6