关于水和对岩石气排气率的影响的研究
Pengfei Li1, Qiang Sun2, Lin Cong3
1College of Geology and Environment, Xi'an University of Science and Technology, Xi'an, Shaanxi 710054, China.
The Science of the total environment
|June 24, 2024
概括
岩石水和度显著影响了气的呼出. 该研究发现,的呼出率随着和而增加,然后随着和而减少,在0.7和0.8水和 (Sw) 之间达到峰值.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 岩石物理 岩石物理
背景情况:
- (Rn) 是一种放射性气体,对于追踪地质过程至关重要.
- 岩石的特性,包括的呼气,对水含量变化很敏感.
- 了解这些变化对于预测地质活动至关重要.
研究的目的:
- 调查不同水和水平如何影响岩石中的出气率.
- 为了确定岩石水和和气呼气特征之间的关系.
- 为了确定子沉的最佳水和范围.
主要方法:
- 用离心试验来实现可控的岩石水和.
- 进行了测量试验,以量化呼气速率.
- 室内实验设置被用于精确的分析.
主要成果:
- 拉登呼气率最初随着岩石水和度的增加而上升.
- 在较高和水平下,观察到子呼气率的随后下降.
- 峰降水率发生在约0.7到0.8的水和度 (Sw).
- 高水和度表明对出气的抑制作用.
结论:
- 岩石中的水和是影响子呼气动态的一个关键因素.
- 这些发现为和岩石环境中的子行为提供了洞察力.
- 这项研究有助于预测受岩石水相互作用影响的地质过程.
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