Water in the Earth's interior
Water in the Earth's interior
复制标题
地球内部的水
DOI：
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发表时间：
2009
期刊：
影响因子：
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通讯作者：
Wang Duo
中科院分区：
文献类型：
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作者：
Wang Duo
水的分布和循环对于认识地球内部的物理化学性质、地球动力学过程和地球演化具有重要作用。本文综述了地球内部水的各种情况，包括地球内部水的探测方法、水的状态、水的储存量、水在地球内部各圈层中的含量、水在高温高压下在矿物中的溶解度以及地球物理观测的一些结果。地球内部的含水量可能比地球表面的含水量大好几倍。微量水对地震波的电导率和速度有显著影响。
Distributions and circulars of water play an important role in understanding the physical and chemical properties of earth interior,geodynamical process,and evolution of earth. This paper reviews the various aspects of water in the earth's interior,including the exploring method,state,storage capacity,content in the different spheres of earth,solubility in minerals at high temperature and pressure,and some results from geophysical observations. The amount of water content in the earth's interior may be several times larger than that at the earth's surface. Trace water can significantly affect the electrical conductivity and velocity of seismic wave.