The Institute of Geology and Geophysics of the Chinese Academy of Sciences, in conjunction with the University of Science and Technology of China and the Chang'e-7 volatile payload team, carried out systematic rare gas isotope analysis using the Chang'e-6 lunar soil samples provided by the National Space Administration. The study found that there are systemic differences in the solar wind received from the front and back of the moon, and the Earth's magnetosphere plays the role of a “speed regulator” in it. The relevant research was published online in “Nature - Earth Science” on July 15.
Zhitongcaijing · 2d ago
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The Institute of Geology and Geophysics of the Chinese Academy of Sciences, in conjunction with the University of Science and Technology of China and the Chang'e-7 volatile payload team, carried out systematic rare gas isotope analysis using the Chang'e-6 lunar soil samples provided by the National Space Administration. The study found that there are systemic differences in the solar wind received from the front and back of the moon, and the Earth's magnetosphere plays the role of a “speed regulator” in it. The relevant research was published online in “Nature - Earth Science” on July 15.
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