Numerical simulation of mass and heat transfer for water extraction from icy lunar regolith

IF 2.8 3区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Advances in Space Research Pub Date : 2024-12-01 Epub Date: 2024-05-11 DOI:10.1016/j.asr.2024.05.018
Yang Yang, Qinggong Wang, Junping Gu, Wei Yao
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Abstract

The confirmation of water ice’s existence in the permanent shadow area led to extensive research in the field of water ice mining from icy lunar regolith. A priori numerical simulation of water ice mining is necessary for guiding the development of lunar water ice mining schemes more reasonably. A 2D axisymmetric numerical simulation model capable of simulating the thermal extraction process about mining water ice from icy lunar regolith is constructed, which is executed in the COMSOL Multiphysics. The thermal extraction cases of lunar regolith with different initial water ice content and heating fluxes are simulated. The EER (energy efficiency ratio) is used to evaluate the efficiency of thermal extraction. The results show that the EER is higher as the initial water ice content is increased, which means more power is used to heat water and less power is used to heat the regolith. The icy lunar regolith with initial water ice content higher than 5.0 wt% is found to be more valuable, over which the EER at the end of thermal extraction will not increase much as the initial water ice content increases. However, the higher heating flux leads to the lower EER at the end of thermal extraction. The speed and economics of thermal extraction are suggested to be weighted before the mission’s implementation. The status of thermal diffusion (thermal transpiration) is studied, and the results indicate that thermal diffusion and advection both can be ignored in thermal extraction modeling, unless the average magnitude of temperature gradient and pressure gradient exceed the maximum of 75764 K/m and 11053 Pa/m in our calculation cases, respectively.
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从冰质月球岩石中提取水的传质和传热数值模拟
永久阴影区水冰存在的确认引发了从冰冷的月球碎屑中开采水冰领域的广泛研究。为了更合理地指导月球水冰开采方案的制定,有必要对水冰开采进行先验的数值模拟。本文在 COMSOL Multiphysics 中构建了一个二维轴对称数值模拟模型,该模型能够模拟从冰冷的月球残积岩中开采水冰的热提取过程。模拟了不同初始水冰含量和热通量的月球碎屑热萃取情况。EER(能效比)用于评估热萃取的效率。结果表明,初始水冰含量越高,EER 越高,这意味着用于加热水的功率越大,而用于加热残积岩的功率越小。研究发现,初始水冰含量高于 5.0 wt% 的冰质月球岩石更有价值,在其之上,热萃取结束时的 EER 不会随着初始水冰含量的增加而增加很多。然而,加热通量越高,热萃取结束时的能效比就越低。建议在执行任务前对热提取的速度和经济性进行权衡。研究了热扩散(热蒸腾)的状况,结果表明在热提取建模中可以忽略热扩散和平流,除非温度梯度和压力梯度的平均值分别超过我们计算案例中的最大值 75764 K/m 和 11053 Pa/m。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Advances in Space Research
Advances in Space Research 地学天文-地球科学综合
CiteScore
5.20
自引率
11.50%
发文量
800
审稿时长
5.8 months
期刊介绍: The COSPAR publication Advances in Space Research (ASR) is an open journal covering all areas of space research including: space studies of the Earth''s surface, meteorology, climate, the Earth-Moon system, planets and small bodies of the solar system, upper atmospheres, ionospheres and magnetospheres of the Earth and planets including reference atmospheres, space plasmas in the solar system, astrophysics from space, materials sciences in space, fundamental physics in space, space debris, space weather, Earth observations of space phenomena, etc. NB: Please note that manuscripts related to life sciences as related to space are no more accepted for submission to Advances in Space Research. Such manuscripts should now be submitted to the new COSPAR Journal Life Sciences in Space Research (LSSR). All submissions are reviewed by two scientists in the field. COSPAR is an interdisciplinary scientific organization concerned with the progress of space research on an international scale. Operating under the rules of ICSU, COSPAR ignores political considerations and considers all questions solely from the scientific viewpoint.
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