在极端条件下水的热导率
Cunzhi Zhang1, Marcello Puligheddu1,2, Linfeng Zhang3
1Pritzker School of Molecular Engineering, University of Chicago, Chicago, Illinois 60637, United States.
The journal of physical chemistry. B
|July 31, 2023
概括
在极端的地幔条件下预测水的导热率 (κ) 是很困难的. 这项研究使用分子动力学和人工智能来显示 κ 与压力增加,在实验具有挑战性的情况下提供了可靠的估计.
科学领域:
- 地质物理学 地质物理学
- 物理化学 物理化学
- 计算材料科学科学 计算材料科学
背景情况:
- 在极端条件下对水的导热率 (κ) 的实验测量,例如在地球地幔中发现的,在实验上具有挑战性.
- 对于高温 (1,0002,000 K) 和高压 (22 GPa) 的水的 κ 存在有限的数据.
研究的目的:
- 为了预测高温和高压水的导热性,与地球地幔条件相关.
- 为了在极端条件下确定水的导热率,压力和声速之间的关系.
主要方法:
- 利用接近平衡的分子动力学模拟.
- 在密度函数理论数据上训练有素的深度神经网络潜力.
- 计算了状态方程,并应用了热导电性的简化模型.
主要成果:
- 导热率 (κ) 显示温度依赖性较弱,和单调,大约平方根增加与压力.
- 在高压下 κ 的上升与声音速度的增加有关.
- 开发了一种可靠的估计方法,用于在T和P的广泛范围内测量水的导热率.
结论:
- 这些发现为了解行星内部的热传输提供了关键数据.
- 已建立的关系提供了一种可靠的方法,用于估计水的导热率在实验无法访问的制度.
- 这项工作弥合了理论预测和需要准确的地质物理数据之间的差距.
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