中国长江六号发现月球远方有76 ppm的水, 是长江五号站点的两倍, China's Chang’e-6 finds Moon's far side has 76 ppm water, twice as much as Chang’e-5 site, aiding future missions.

中国的长江6号飞行任务揭示了月球远方水的新细节,发现由于太阳风和撞击过程,浅石质中平均有76 ppm,略低于表面平均值。 China’s Chang’e-6 mission has revealed new details about water on the Moon’s far side, finding an average of 76 ppm in shallow regolith—slightly less than the surface average—due to solar wind and impact processes. 根据一天的时间,水位有所不同,受着 regolith 组成和着陆器下降的干扰的影响. Water levels vary by time of day and are influenced by regolith composition and disturbances from the lander’s descent. 该地点的储水量大约是长江5号降落区的两倍。 The site holds about twice as much water as the Chang’e-5 landing zone. 这些洞察力突出表明,精细的表面材料是未来特派团的潜在资源。 These insights highlight fine-grained surface material as a potential resource for future missions. 中国计划在2026年和2029年前后发射长江-7和长江-8,以进一步探索月球南极,支持开发一个国际月球研究站,到2035年建立基本模型。 China plans to launch Chang’e-7 in 2026 and Chang’e-8 around 2029 to further explore the lunar south pole, supporting development of an International Lunar Research Station, with a basic model by 2035.