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检测与2016年熊本地震相关的地下水位变化
Shun Yamamoto1, Katsuaki Koike2, Yosuke Alexandre Yamashiki3
1Graduate School of Advanced Integrated Studies in Human Survivability, Kyoto University, Kyoto, Japan. yamamoto.shun.58r@st.kyoto-u.ac.jp.
Scientific reports
|December 21, 2023
概括
地下水位在2016年熊本地震之前显示出先驱性变化. 分析揭示了水库对主要地震事件造成的地变形的反应.
科学领域:
- 地质物理学 地质物理学
- 水文学的水文学
背景情况:
- 地下水位波动受到各种因素的影响,包括地变形.
- 了解这些关系可以帮助地震预测研究.
研究的目的:
- 为了调查2016年熊本地震之前地下水位的前体变化.
- 为了确定地下水位变化和16年内地变形之间的联系.
主要方法:
- 分析了来自17个地点的地下水位时间序列数据.
- 观测到的地下水位与在多孔水层中建模的水位的比较.
- 地下水变化与大地震造成的地压力的相关性.
主要成果:
- 观察到的地下水水平低于特定多孔层 (托加瓦岩,阿索前火山岩) 的建模水平.
- 观测和建模水平之间的显著差异减少,导致2016年地震.
- 地下水位的变化表明,在2011年东北地震后地的压力放松,在熊本地震之前的压力积累.
结论:
- 地下水位监测可以潜在地检测与地震事件相关的前体变化.
- 在大规模地震的影响下,地变形显著影响地下水的行为.
- 这项研究通过水文分析为地震前体现象提供了宝贵的见解.
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