地球下层地幔中的水
Motohiko Murakami1, Kei Hirose, Hisayoshi Yurimoto
1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan. mmurakam@geo.titech.ac.jp
概括
地球的下层地幔矿物可以储存大量的气,矿和矿含有大量的水. 这一发现表明,下层地幔可能比地球海洋含水量多5倍.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 地球科学 地球科学 地球科学
背景情况:
- 地球的下层地幔是理解行星组成和演变的关键区域.
- 下层地幔的水含量受到很小的约束,影响了地幔动态和挥发性循环的模型.
研究的目的:
- 量化地球下地幔主要矿物质中 (H2O) 溶解度.
- 为了评估地球深处的水储存潜力.
主要方法:
- 合成了具有代表性的下地幔矿物质 (MgSiO3-perovskite,CaSiO3-perovskite,magnesiowüstite) 在自然的矿石组成中.
- 利用二次离子质谱 (SIMS) 来测量的度.
- 使用红外显微光谱来确认基 (OH) 基的存在.
主要成果:
- 富含MgSiO3的矿和矿溶解大约0.2重量%的H2O.
- 富含CaSiO3的矿溶解了大约0.4重量%的H2O.
- 红外光谱学证实了Mg-perovskite和magnesiowüstite中的OH吸收带.
结论:
- 地球主要的下地幔矿物质表现出显著的溶性.
- 下层地幔可能会储存多达地球所有海洋的5倍的H2O.
- 这些发现对地球深层的挥发性循环和地幔动态有着深刻的影响.
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