对透性和粘土矿物质的实验研究在高温下对石的分阶段变化
Jingjie Wu1, Can Cao2, Bo Xiong3
1School of Energy Resources, China University of Geosciences (Beijing), 29 College Road, Haidian District, Beijing 100083, China.
ACS omega
|March 24, 2025
概括
这项研究模拟了高达1400°C的泥石透性,揭示了由粘土矿物驱动的三个阶段的变化. 高温处理显著改变岩石特性,影响地下工程适用性.
科学领域:
- 地质地质地质地质地质地
- 材料科学 材料科学 材料科学
- 地质技术工程 地质技术工程
背景情况:
- 目前关于泥石透性的研究仅限于低于800°C的温度.
- 这种差距阻碍了在更高温度下运行的地下工程项目的指导.
研究的目的:
- 在高达1400°C的模拟温度下调查岩的透性和矿物质变化.
- 了解温度诱导的矿物变化与岩石透性之间的关系.
主要方法:
- 进行了高达1400°C的一般热模拟.
- 在不同温度下分析了石灰岩的透性和矿物成分变化.
主要成果:
- 石灰岩的透性和孔隙结构的变化发生在三个不同的阶段,与粘土矿物转化相关.
- 脱氧化在第二阶段增加了透性;再结晶后的液相冷却在第三阶段引起了复杂的变化.
- 含有Mg的石灰岩在1000°C以上表现出更强的温度反应,这是由于高液相含量和矿石的形成.
结论:
- 粘土矿物质的变化是岩在高温下的透性演变的关键驱动因素.
- 在高温下含有Mg的砂岩的行为需要在地下工程应用中仔细考虑.
- 了解这些高温效应对于深度地下项目的安全有效设计至关重要.
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