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Stress transfer patterns and local seismicity related to reservoir water-level variations. A case study in central Costa Rica

机译:与水库水位变化有关的应力传递模式和局部地震活动。哥斯达黎加中部的案例研究

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摘要

This study main aim was to analyse the spatio-temporal trend in seismicity recorded in the proximity of the Pirrís Reservoir (central Costa Rica), where impoundment for the purposes of filling the reservoir to its total volume (3,6 * 107 m3) started in 2011. We differentiated between the events that occurred before, during and after this filling operation. Using a seismic analysis, we sought to define and understand the effects which such reservoir operations have on seismic activity in the area. To this end, we evaluated the spatio-temporal evolution of Coulomb failure stress (ΔCFS) changes due to surface water load, and its correlation with seismicity. Overall, the results of this study provide a perspective of how the water load in the reservoir can affect the stress state in the close area. In our study case, we have detected: an increase in b-value after impoundment, an increment of rate for shallowest events (h ≤ 10 km), an increasing trend of higher magnitude events and a possible trigger effect on local faults. All these aspects could be useful to control the reservoir operations and to help in decision making in order to guarantee the safety of these critical emplacements.
机译:这项研究的主要目的是分析在皮里斯水库(哥斯达黎加中部)附近记录的地震活动的时空趋势,在该水库中蓄水以将水库填满至其总体积(3,6 * 107 m 3 )始于2011年。我们对填充操作之前,之中和之后发生的事件进行了区分。通过地震分析,我们试图定义和理解此类储层作业对该地区地震活动的影响。为此,我们评估了由于地表水负荷引起的库仑破坏应力(ΔCFS)变化的时空演变及其与地震活动的相关性。总的来说,这项研究的结果为水库中的水负荷如何影响封闭区域的应力状态提供了一个视角。在我们的研究案例中,我们发现:蓄水后b值增加,最浅事件(h≤10 km)的速率增加,高强度事件的趋势增加以及对局部断层的可能触发作用。所有这些方面对于控制储层的运行并有助于做出决策以确保这些关键位置的安全都是有用的。

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