超压
月球土壤
压缩性
地质学
球体
岩土工程
材料科学
矿物学
机械
热力学
物理
天文
作者
Edward Schreiber,Orson L. Anderson,Naohiro Sogat,N. Warren,Christopher A. Scholz
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:1970-01-30
卷期号:167 (3918): 732-734
被引量:29
标识
DOI:10.1126/science.167.3918.732
摘要
Four experiments on lunar materials are reported: (i) resonance on glass spheres from the soil; (ii) compressibility of rock 10017; (iii) sound velocities of rocks 10046 and 10017; (iv) sound velocity of the lunar fines. The data overlap and are mutually consistent. The glass beads and rock 10017 have mechanical properties which correspond to terrestrial materials. Results of (iv) are consistent with low seismic travel times in the lunar maria. Results of analysis of the microbreccia (10046) agreed with the soil during the first pressure cycle, but after overpressure the rock changed, and it then resembled rock 10017. Three models of the lunar surface were constructed giving density and velocity profiles.
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