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Groundwater response analysis to multiple earthquakes on Jeju volcanic island

机译:济州火山岛的多次地震地下水响应分析

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Earthquakes have been known to induce a groundwater response. This study statistically analyzed the relationship between the changes in groundwater level (oscillation) and seismic waves, as well as the relationship between the changes in groundwater level and earthquakes of various magnitudes and epicenters more than 1,000 km distance from Jeju Island. The analysis showed that the groundwater level in Jeju Island is changed mostly by earthquakes larger than M = 7.0 within a 3,000 km from the epicenter. A positive relationship appeared between the earthquake magnitude and groundwater level change. A similar positive trend was observed between the maximum groundwater level and the seismic amplitude of the earthquakes. Geologically and spatially, the northern area of the island showed the highest response to earthquakes, the southern area showed an intermediate response, and the western and eastern areas showed the lowest response. The highest groundwater response in the northern area might be linked to its permeable structures and geological layers.
机译:已知地震会引起地下水响应。本研究对距济州岛1000多公里以外的各种震级和震级的地下水位(振荡)与地震波之间的关系以及地下水位的变化与地震之间的关系进行了统计分析。分析表明,在距震中3000公里以内,大于M = 7.0的地震改变了济州岛的地下水位。地震烈度与地下水位变化之间存在正相关关系。在最大地下水位和地震的地震幅度之间也观察到类似的积极趋势。在地质和空间上,该岛的北部地区对地震的响应最高,南部地区的响应中等,西部和东部地区的响应最低。北部地区最高的地下水响应可能与其渗透结构和地质层有关。

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