摘要
本文简要阐述地幔矿物中水溶解度的研究方法及过程,探讨晶体结构、化学组成、水逸度、温度、压力、氧逸度、硅活度等对溶解度的影响,结合橄榄石、辉石、石榴石、瓦兹利石、林伍德石等主要造岩矿物的研究成果,分析了地幔的储水能力,并指出存在的问题及今后的研究方向.
In this paper,we briefly elucidate the methods and process to research the water solubility of mantle minerals at high temperature and high pressure.Some potential influence factors on the water solubility of mantle minerals,such as crystal structure, chemical components, water fugacity,temperature,pressure,oxygen fugacity and silicate activity are discussed.The water solubility for the main rock-forming minerals in the upper mantle and transition zone e.g.olivine,pyroxene,garnet, wadsleyite,ringwoodite are reviewed.Furthermore,the capacity of water storage at different depth of the mantle is compared.Finally,we elaborate the existing problems of experimental research,and view the next-step work.
出处
《地球物理学进展》
CSCD
北大核心
2015年第5期2055-2063,共9页
Progress in Geophysics
基金
中国科学院地球化学研究所"135"项目
中国科学院百人计划项目
国家自然科学基金项目(41474078
4130406和41174079)联合资助
关键词
地幔矿物
水溶解度
方法及过程
影响因素
储水能力
mantle minerals
water solubility
methods and progress
influence factors
storage capacity