在性地中,连贯的层状交织生长
E Petrishcheva1, D Heuser1, R Abart1
1Department of Lithospheric Research, University of Vienna, 1090 Vienna, Austria.
概括
这项研究提出了地溶解的新热力学模型,揭示了连贯的相互生长取决于前体成分,而不仅仅是温度和压力. 这影响了对矿物阶段行为的理解.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 材料科学 材料科学 材料科学
背景情况:
- 地溶解包括分离富含 (阿尔比特) 和富含 (奥托克拉斯) 的阶段.
- 之前的模型假设接口处的应变为零,从而限制了它们的适用性.
- 了解连贯的相互生长对于解释地质过程至关重要.
研究的目的:
- 开发一种更一般的热力学模型,用于性地石中连贯的板状杂交生长.
- 调查前体成分对弹性能量和溶液行为的影响.
- 为了比较模型预测与实验观察状方位的模型预测.
主要方法:
- 弹性应力和应变的热力学分析.
- 在叶片微结构中最大限度地减少整体弹性能量.
- 根据体积比例和前体成分计算弹性能量的计算.
主要成果:
- 弹性能量取决于富含Na和富含K的地板的体积比例.
- 一致的溶解曲线因同质前体相的组成而有所不同.
- 预测的叶片方向与实验观测一致,在尽量减少应变能量时.
结论:
- 该模型提供了一个更准确的热力学框架,用于地溶解.
- 前体的组成是决定连贯的杂交生长和solvus特征的关键因素.
- 这项研究完善了我们对地质条件下的矿物相变化的理解.
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