瓦斯莱特和环木石的电导性过渡区中的水含量
Xiaoge Huang1, Yousheng Xu, Shun-Ichiro Karato
1Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
Nature
|April 9, 2005
概括
地球 地球 地球 地球 地球 地球
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 地质化学 地质化学
背景情况:
- 地球的过渡区 (深度为410660公里) 由于矿泉水的溶解性,可能会作为一个重要的水库.
- 水的含量影响着地球的进化和物质特性.
- 过渡区的确切水量仍然是未知的.
研究的目的:
- 为了确定水和温度对wadsleyite和ringwoodite电导率的影响.
- 为了推断地幔过渡区的水含量.
主要方法:
- 在不同的水和温度条件下,实验确定wadsleyite和ringwoodite的电导率.
- 实验结果与地球物理导电数据的比较.
主要成果:
- 瓦斯莱和环木的电导率对水含量高度敏感,但对温度敏感度较小.
- 太平洋地幔过渡区的推断水含量约为0.10.2 wt%的质量.
- 这种推断的含水量超过了上层地幔部分融化的临界值.
结论:
- 地幔过渡区的水含量因地区而异.
- 在大约410公里深处的部分融化可能发生在太平洋等地区,影响元素分布.
- 水含量,而不是温度,是这些矿物质电导率的主要控制因素.
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