月球永久阴影坑中月壤的物理状态
The Physical State of Lunar Soil in the Permanently Shadowed Craters of the Moon
AI总结：
通过实验研究月球永久阴影坑月壤的物理状态，发现其因缺乏热循环而压实程度较低，且压实度随土壤深度变化，为相关工程设计与能量预算提供依据。
摘要：
月球永久阴影坑中月壤的物理状态通过实验研究得以推断。永久阴影坑不会经历月球其他区域所经历的热循环，因此其压实程度可能略低。这项研究具有重要意义，因为挖掘、巡视和着陆相互作用，以及相关技术的能量预算和部署计划，都需要进行适当的规模调整和设计。结果表明，由热循环引起的压实程度是土壤柱中深度的函数。
英文摘要：
The physical state of the lunar soil in the permanently shadowed craters of the moon is inferred from experimental investigation. The permanently shadowed craters do not undergo the same thermal cycling experienced by other parts of the moon and therefore could be slightly less compacted. This study is significant because excavating, roving, and landing interactions, along with the energy budgets and deployment schedules for associated technology, need to be scaled and designed properly. Results indicate that the degree of compaction due to thermal cycling is a function of the depth in the soil column.
机构、总结、中文摘要均由AI分析而来，可能存在错误，请以论文正文为准。
