月球土壤
测量员
登月
凝聚力(化学)
地质学
航天器
平方(代数)
天体生物学
大地测量学
矿物学
物理
天文
数学
几何学
动物
阿波罗
量子力学
生物
作者
E. M. Christensen,R. Choate,L. D. Jaffe,R. L. Spencer,F. B. Sperling,S. A. Batterson,H. E. Benson,R. E. Hutton,Rebecca H. Jones,H.Y. Ko,F. N. Schmidt,Ronald F. Scott,George H. Sutton
出处
期刊:Science
[American Association for the Advancement of Science]
日期:1967-11-03
卷期号:158 (3801): 637-640
被引量:22
标识
DOI:10.1126/science.158.3801.637
摘要
The mechanical properties of the lunar soil at the Surveyor V landing site seem to be generally consistent with values determined for soils at the landing sites of Surveyor I and III. These three maria sites are hundreds of kilometers apart. However, the static bearing capability may be somewhat lower than that at the previous landing sites (2 × 105 to 6 × 105 dynes per square centimeter or 3 to 8 pounds per square inch). The results of the erosion experiment, the spacecraft landing effects, and other observations indicate that the soil has significant amounts of fine-grained material and a measurable cohesion.
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