玄武岩
风化土
月球土壤
月母马
月球地质
地球化学
地质学
土壤水分
火成岩
角砾岩
矿物学
稀土
天体生物学
物理
土壤科学
作者
Chunlai Li,Haisheng Hu,Ming Yang,Zhaoyu Pei,Qin Zhou,Xin Ren,Bin Liu,Dawei Liu,Xingguo Zeng,Guangliang Zhang,Hongbo Zhang,Jianjun Liu,Qiong Wang,Xin Deng,Caijin Xiao,Yonggang Yao,Dingshuai Xue,Wei Zuo,Yan Su,Wu Wen,Ziyuan Ouyang
摘要
Abstract Forty-five years after the Apollo and Luna missions returned lunar samples, China's Chang’E-5 (CE-5) mission collected new samples from the mid-latitude region in the northeastern Oceanus Procellarum of the Moon. Our study shows that 95% of CE-5 lunar soil sizes are found to be within the range of 1.40–9.35 μm, while 95% of the soils by mass are within the size range of 4.84–432.27 μm. The bulk density, true density and specific surface area of CE-5 soils are 1.2387 g/cm3, 3.1952 g/cm3 and 0.56 m2/g, respectively. Fragments from the CE-5 regolith are classified into igneous clasts (mostly basalt), agglutinate and glass. A few breccias were also found. The minerals and compositions of CE-5 soils are consistent with mare basalts and can be classified as low-Ti/low-Al/low-K type with lower rare-earth-element contents than materials rich in potassium, rare earth element and phosphorus. CE-5 soils have high FeO and low Mg index, which could represent a new class of basalt.
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