在高压实验中合抗变形和脱水
Lisa Eberhard1, Mattia Luca Mazzucchelli2, Stefan Markus Schmalholz2
1Department of Earth Sciences, Utrecht University, Utrecht, The Netherlands.
而不是温度或组成, 触发了反岩脱水. 应变度局部增加了反岩的内部能量,使其能够释放液体并影响地化学和地物理过程.
科学领域:
- 地质化学
- 地质学
- 矿物物理
背景情况:
- 反岩脱水是潜水区的关键反应,影响地质化学和地质物理过程.
- 了解反岩脱水的驱动因素对于模拟潜水区动态至关重要.
研究的目的:
- 调查抗原体脱水的发生.
- 确定驱动抗原石释放液体的化学和物理参数.
- 确定变形在抗酸脱水中的作用.
主要方法:
- 水静电和同轴的格里格斯对抗石蛇形石的实验.
- 高压和高温试验 (1.5 GPa,620670°C).
- 运行产品的分析和数值模拟 合反应动力学和机械工作速度.
主要成果:
- 抗酸脱水仅限于变形的样本.
- 在曲脱水带中形成的纳米大小的橄和正氧化物.
- 与变形相关的脱水得到了数字模拟的支持.
- 应变度局部增加了抗原体的内部能量,使其脱水.
结论:
- 变形,而不是矿物学或化学异质或温度梯度,是抗原体脱水的主要驱动因素.
- 结合的机械和化学过程对于理解抗酸脱水至关重要.
- 这项研究提供了在俯冲区因变形而引起的抗高脱水的机制框架.
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