Chandrayaan-3' s predecessor Chandrayaan-1. The team led by researchers from the University of Hawai'i (UH) at Manoa in the US discovered that these electrons in Earth's plasma sheet are contributing to weathering processes -- breaking down or dissolving of rocks and minerals -- on the Moon's surface. The research, published in the journal Nature Astronomy, found that the electrons may have aided the formation of water on the lunar body.
Knowing the concentrations and distributions of water on the Moon is critical to understanding its formation and evolution, and to providing water resources for future human exploration, the researchers said. The new finding may also help explain the origin of the water ice previously discovered in the permanently shaded regions of the Moon, they said. Chandrayaan-1 played a crucial role in the discovery of water molecules on the Moon.
Chandrayaan-1 was launched by the Indian Space Research Organisation (ISRO) in October 2008, and operated until August 2009. The mission included an orbiter and an impactor. The scientists analysed the remote sensing data that were collected by the Moon Mineralogy Mapper instrument, an imaging spectrometer, onboard India's Chandrayaan 1 mission between 2008 and 2009.
Solar wind, which is composed of high energy particles such as protons, bombards the lunar surface and is thought to be one of the primary ways in which water has been formed on the Moon. The team of experts investigated the changes in surface weathering as the Moon passes through Earth's magnetotail, an area that almost completely shields the lunar body from solar wind but not the Sun's light photons. "When the Moon is outside of the magnetotail, the lunar surface is bombarded with solar
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