December 7, 2022

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How karst caves can be used as a terrestrial simulation platform to test and design human bases in lunar lava tubes

Karst cave simulation platform. Credit: Space: Science & Technology (2022). DOI: 10.34133/2022/9875780
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Karst cave simulation platform. Credit: Space: Science & Technology (2022). DOI: 10.34133/2022/9875780

If human beings want to survive on the other planets for a long time, they must first find or set up a safe, stable, and long-term shelter. Lunar lava tubes are geological structures on the moon discovered in recent years. They take the form of hollow pipe-shaped caves formed on the surface of the planet by volcanic activity.

Because a lunar tube has a hard basalt roof, its internal environmental factors such as temperature changes, radiation doses, and the probability of being hit by meteorites are relatively limited. As such, it offers in theory an ideal human lunar habitat. Until now, more than 300 potential cave entrances have been identified on the moon. The "skylights" they display are the result of a kind of pit caused by the active lava tube collapsing.

In a new article published in Space: Science & Technology, the research team led by Gengxin Xie and Linli Guo has discussed the feasibility of using lunar for human habitation, proposed the idea of using the Earth's caves to simulate extraterrestrial lava tubes, selected caves in Chongqing as the simulation site, and demonstrated the feasibility in terms of both structural and environmental aspects. They hope to promote the development of related research on extraterrestrial bases through simulation experiments.

The rationality of using a lunar lava tube to establish a lunar base

The external energy required by the closed system involved in the operation of a human lunar base mainly consists of three parts: human respiration, plant photosynthesis, and internal temperature control.

The researchers showed that the minimum energy consumption for maintaining a lunar base hosting 8 astronauts deep inside a lava tube cave is about 145.5 kW in a semicircular tunnel cave with an area of about 8,000 square meters and a height of 50 meters. At this stage, a lava tube is the best choice for establishing a lunar base.

Compared with the lunar surface, lunar lava tubes have the advantages of small radiation and less extreme conditions, more suitable for a human lunar base.

There is a variation in depth of radiation intensity of different particles in the lunar soil. This intensity at 6 m below the lunar surface is almost zero. Even at a depth of less than 1 m, and solar particle events (SPE) do not affect the interior of the lava tube.

A suitable tube should not be broken down by meteorites. This means that the possible influence radius of the meteorite must be smaller than the tube's burial depth. According to experimental and simulation studies, the safest condition the scientist have now calculated is the ratio of target thickness-to-crater diameter. That is, if it is smaller than 0.87 then a "skylight" (crater) will appear.

There is very little moon dust inside lunar lava tubes. Moon dust is the charged dust formed by small debris on the lunar surface under the action of the solar wind. Being charged, they can be adsorbed on equipment. In addition, moon dust is abrasive, and very harmful to people and machines. But the interior of lava tubes is a permanent shadow zone, generally inaccessible to the solar wind, where charged moon dust is hardly produced.

The moonquakes observed by the lunar seismic network between 1969 to 1977 varied in where, how often and how severely they shook the moon. The fact that the lunar lava tubes has survived on the moon for so many years suggests that its structure is stable enough to withstand the effects of moonquakes. This is a natural advantage over bases built on the moon's surface.

Intensity changes of various particles with depth. The figure shows the total particle mass, protons, neutrons, and other particles including electrons, positrons, protons, mesons, muons, k-mesons, and deuterons. Credit: Space: Science & Technology (2022). DOI: 10.34133/2022/9875780
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Intensity changes of various particles with depth. The figure shows the total particle mass, protons, neutrons, and other particles including electrons, positrons, protons, mesons, muons, k-mesons, and deuterons. Credit: Space: Science & Technology (2022). DOI: 10.34133/2022/9875780

Using a karst cave to simulate lunar lava tubes

Karst caves refer to the underground space formed by the dissolution, invasion, and collapse of soluble limestone under certain conditions. Taking karst caves in Chongqing as an example, the researchers show that Earth karst caves can be considered as good analogs of lunar lava tubes under three aspects: structure, environment, and insulation.

The researchers intend to use karst caves to simulate the internal environment of extraterrestrial caves and isolate them from the external environment by sealing the caves. The cave experiment is divided into two parts. The first part involves automatic construction technology in the and in situ utilization technology.

The other part is the artificial ecosystem experiment. Regarding energy supply and light, they plan to use light pipes to introduce sunlight into the ecological laboratory and provide it for crop growth and develop a set of automatic control energy control systems.

More information: Jinghang Ding et al, Karst Cave as Terrestrial Simulation Platform to Test and Design Human Base in Lunar Lava Tube, Space: Science & Technology (2022). DOI: 10.34133/2022/9875780

Provided by Beijing Institute of Technology Press

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