概括
地球 地球 地球 地球 地球 地球
科学领域:
- 地质化学 地质化学
- 矿物学是一门学科.
- 石化学 石化学是一门学科.
背景情况:
- 地球的上层地幔含有,主要是矿物中的基 (OH).
- 氧化的度因矿物种而异,并反映了地质形成条件.
- 名义上无水矿物质是地幔的重要储量库.
研究的目的:
- 在主要的上层地幔矿物中量化氧化 (OH) 度.
- 评估名义上无水矿物质在地幔的水预算和地化学中的作用.
- 通过这些矿物质,调查水回收到深层地幔的潜力.
主要方法:
- 在素,石榴石和橄中分析氧化物 (OH) 含量.
- 基于重量的H(2) O度测量.
- 地质化学建模地幔中的储库.
主要成果:
- 铁素是主要地幔矿物中含水量最多的矿物质 (200500 ppm H(2) O).
- 石榴和橄含有显著较少的水 (150 ppm H(2) O).
- 表面上无水矿物质可能会把所有水都储存在枯竭的地幔中.
结论:
- 无水矿物质,特别是氧化物,对于地幔水的储存至关重要.
- 这些矿物质在上层地幔的地化学中发挥着关键作用.
- 它们提供了一种可信的机制,可以将地表水回收到地球深层.
相关概念视频
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