破裂砂岩在深水和采矿引发的压力下深水和高限制水下的透特性
Hongsheng Tu1, Runze Wu2, Sheng Jia2
1School of Mines, China University of Mining and Technology, Xuzhou, 221116, China.
Scientific reports
|March 1, 2026
概括
深度采矿的泄漏是复杂的. 较高的水压会增加流量,而限制的压力会导致三阶段的演变,稳定透性. 断裂粗度和孔径是理解这种行为的关键.
科学领域:
- 地质技术工程 地质技术工程
- 水文地质学 水文地质学
- 岩石机械 岩石机械
背景情况:
- 深度采矿面临着高限制压力和水压的挑战.
- 在这些条件下,破碎的岩石质量表现出复杂的透演变.
- 了解压力-漏合对于安全的采矿操作至关重要.
研究的目的:
- 调查封闭压力,水压,断裂粗度 (JRC) 和孔径对断裂砂岩中透的结合效应.
- 制定一个统一的压力透框架,用于深水,高度封闭的水环境.
- 建立稳定透性的定量关系.
主要方法:
- 在单一断裂的砂岩上进行了三轴透实验.
- 限制压力,水压,JRC和光圈的系统变化.
- 对漏流量,有效应力和断裂变形的分析.
主要成果:
- 漏流量随着水压线性增加,随着限制压力非线性减少.
- 观察到一个三个阶段的透演变 (弹性,弹性-塑性,紧缩平衡) 与一个稳定值.
- 升高的水压降低了有效的正常应力,削弱了断裂关闭,特别是在粗的断裂中,增强了透性.
- 断裂粗度和孔径共同控制透率的大小,减弱率和稳定性.
结论:
- 确定了稳定透度和断裂参数之间的定量关系.
- 断裂粗度和孔径对于在高压力下控制漏行为至关重要.
- 结果为预测漏演变和减轻深度采矿中的水冲入风险提供了洞察力.
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