【摘要】 人们关注地球深部水对地球介质的力学和物理性质影响．以往实验研究大都用气体设备在几百MPa的低压力下进行的．为实现深部高压条件，本文用固体传压技术在1000-1300℃；1．0～2．0GPa（相当上地幔）温压条件进行橄榄石晶体内水溶解度实验研究．实验表明，固体传压技术用于晶体“含水”实验研究是一种有效方法；研究证实，与低压实验一样，高压下水赋存在橄榄石晶体中仍以H离子作为“杂质”进入晶体缺陷为主要形式，并发现水的溶解度与实验压力相关，更多还原

【Abstract】 In the past, experiment reasench about hydrogen solubility in olivine crystal have been done under low pressure of several hundueds MPa woth gus equipment mostly. Tohave condition of high pressure as in the upper mantle, we have done experiment reaserchunder the temperature of 1000～1300℃ and pressure of 1.0～ 2.0GPa (correspond to the upper mantle) by solid conduction pressure technology. The so1id conduction method that have been used "water in crystal" experiment reaserch. We have found the re1ativily of water solubility with experimental pressure.更多还原