火山的透度缩放关系从核心到现场尺度测量
Dolan D Lucero1, S Michelle Bourret2, John P Ortiz2
1Los Alamos National Laboratory, Los Alamos, USA. dolanlucero@lanl.gov.
Scientific reports
|April 15, 2025
概括
爆炸气体迁移信号是区分化学物质和核事件的关键. 这项研究表明,岩石透性测量与尺寸有很大差异,影响了地下流量预测.
科学领域:
- 地质物理学 地质物理学
- 水文地质学 水文地质学
- 爆炸物工程 爆炸物工程
背景情况:
- 了解爆炸的地下信号传播对于区分化学和核事件至关重要.
- 气体迁移是一个关键的差异化因素,受到岩石透性的强烈影响.
- 准确的场尺度透性测定是具有挑战性的,因为尺度依赖的变化.
研究的目的:
- 为了估计化学爆炸试验周围的地质单元的爆炸前透性.
- 为了研究测量尺度对火山岩中液压性质表征的影响.
- 评估局部级透性测量的可靠性,以预测现场规模的运输.
主要方法:
- 透性测量是在三个尺度上进行的:核心样本 (厘米),钻孔打包器测试 (米) 和腔压测试 (几十米).
- 在内华达国家安全站点的P道测试周围,分析了10个不同的图夫单元.
- 来自不同尺度的数据进行了比较,以确定透度的尺度依赖变化.
主要成果:
- 来自核心样本和钻孔包装器测试的透率估计显示出最小的差异.
- 洞穴加压测试给出了对大多数岩石单位的透率估计,比较小规模的测量高出两个数量级.
- 在火山岩的液压性质表征中观察到显著的尺度依赖.
结论:
- 测量尺度对火山岩中液压性能的表征产生了深远的影响.
- 局部级的透度测量 (小于10米) 可能无法充分捕捉准确的场级流量和质量运输预测所需的异质性.
- 更大规模的测试对于对爆炸监测相关的地下液压特性可靠的表征至关重要.
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