Controlling soil disturbance of a lunar regolith simulant bed during depressurization in a vacuum chamber

被引:4
|
作者
Go, Gyu-Hyun [1 ]
Lee, Jangguen [2 ]
Chung, Taeil [2 ]
Ryu, Byung Hyun [2 ]
Jin, Hyunwoo [2 ]
Zhuang, Li [2 ]
Shin, Hyu Soung [2 ]
Kim, Jae Hyun [3 ]
Yun, Tae Sup [4 ]
机构
[1] Kumoh Natl Inst Technol, Dept Civil Engn, Gumi, South Korea
[2] Korea Inst Civil Engn & Bldg Technol KICT, Dept Future Technol & Convergence Res, Goyang, South Korea
[3] Kangwon Natl Univ, Dept Civil Engn, Chunchon, South Korea
[4] Yonsei Univ, Sch Civil & Environm Engn, Seoul, South Korea
关键词
CONSOLIDATION; FLUIDIZATION;
D O I
10.1038/s41598-021-81317-1
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A dusty thermal vacuum chamber (DTVC) containing a regolith simulant bed is essential for testing equipment and techniques related to lunar surface exploration. Space agencies have been reluctant to operate a DTVC because of the challenge of controlling soil disturbance of the lunar regolith simulant bed during pumping down or depressurization, which may contaminate or even damage the chamber and vacuum equipment. There appears to be no previously available solution to this problem, or how to avoid it. We investigated the mechanism of soil disturbance during depressurization and established a criterion for evaluating its occurrence. The proposed criterion was validated by extensive experiments and numerical modelling to simulate air evacuation from soil voids. There is a critical pressure difference (CPD) between the top and bottom of the lunar regolith simulant bed that causes soil disturbance during depressurization. We found a simple equation estimating the CPD and further provided guideline on the optimum depressurization rate to avoid soil disturbance before the target vacuum level is achieved under varying soil conditions.
引用
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页数:8
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