Passive Seismic Monitoring of a Karst Aquifer During Flood Events.

A. Nader, J. Albaric, A. Marchand, M. Gros, M. Steinmann, B. Fores, V. Stefani, B. Pohl, H. Celle‐Jeanton, C. Sue
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Abstract

Summary Karst aquifers are considered challenging sites for monitoring. They endure various behaviors during floods due to their heterogeneous structure and complex recharge mechanisms. This shows that multiple parameters should interfere as well as multiple methods emerging from different disciplines should be used to investigate such environments. This work is held with the objective of identifying the dynamics of superficial and deep water flows in a karst environment. Taking Fourbanne’s aquifer as a case study, we show in the following the ability of seismic noise combined with hydrological data to detect water flows and bedload transport in the vicinity of the underground conduit. This study is a part of the SISMEAUCLIM project that aims to develop a new approach to temporal monitoring of karst aquifers, subject to floods by analyzing jointly seismological, hydrogeological, and atmospheric data.
洪水期间岩溶含水层的被动地震监测。
喀斯特含水层被认为是具有挑战性的监测地点。由于其非均匀的结构和复杂的补给机制,它们在洪水中承受着各种各样的行为。这表明多个参数应该相互干扰,并且应该使用来自不同学科的多种方法来研究这种环境。这项工作的目的是确定喀斯特环境中浅层和深层水流的动力学。以Fourbanne含水层为例,我们在下面展示了地震噪声与水文数据相结合检测地下管道附近水流和层载运移的能力。本研究是SISMEAUCLIM项目的一部分,该项目旨在通过联合分析地震、水文地质和大气数据,开发一种新的方法来监测受洪水影响的喀斯特含水层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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