在城市环境中识别地下空洞
Boualem Bouyahiaoui1, Abdeslam Abtout2, Yasser Bayou2
1Center of Astronomy, Astrophysics and Geophysics Research, Route de l'Observatoire, Bouzaréah, Alger, 16340, Algeria. b.bouyahiaoui@yahoo.com.
Scientific reports
|January 17, 2025
概括
重力测量调查显示,阿尔及利亚的地下空洞与钻井活动不同. 这些洞很可能是由天然的水循环引起的,而不是阿尔比安钻井现场.
科学领域:
- 地质物理学 地质物理学
- 环境地质 环境地质学
背景情况:
- 在阿尔及利亚M'Rara地区封闭的阿尔比安钻井现场附近观察到土地沉降,崩和裂.
- 假设936米深的盐层内的潜在空洞与这些现象有关.
研究的目的:
- 调查阿尔比安钻井现场周围观察到的地质现象的原因.
- 为了确定地下空洞的存在和起源,特别是在盐层内.
主要方法:
- 进行了一项新的重力测量调查,以绘制地下密度变化的地图.
- 数据处理包括多项式拟合,梯度分析和3D反转来识别异常区域.
主要成果:
- 重力测量数据显示了与液压钻井操作无直接关系的异常.
- 有证据表明,这些空洞不是钻井活动的结果.
结论:
- 观察到的地质现象很可能是由来自雷特姆山谷的地下水循环引起的.
- 重力测量是一种有效的地质物理方法,用于检测复杂环境中的空洞.
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