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“Shock event”, an impact phenomenon observed in water wells around the Arabian Gulf coastal city Dammam, Saudi Arabia: possible relationship with Sumatra tsunami event of December 26, 2004

机译:“冲击事件”,在沙特阿拉伯阿拉伯湾沿海城市达曼附近的水井中观察到的一种冲击现象:与2004年12月26日苏门答腊海啸事件的可能关系

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摘要

A sudden disturbance in water level was recorded by hydrographs monitoring wells in the coastal city Dammam, Saudi Arabia on December 26, 2004. The water level was being recorded from the shallow (1–3 M deep) coastal aquifer at that time. In two wells, this disturbance was observed ~12 h after the Sumatra earthquake/tsunami event of December 26, 2004. The timing of this event is synchronous in two wells near the coast, but an inland well away from the coast line did not show any such disturbance. It is hypothesized that this disturbance, we call it the “shock event”, is resulted by sudden impact of tsunamis traveling in the Arabian Gulf from southeast toward northwest. As the tsunamis propagated, they suddenly impacted the coastal shallow groundwater aquifer resulting in the “shock event”.
机译:2004年12月26日,沙特阿拉伯沿海城市达曼(Dammam)的水位计监测井记录了水位的突然扰动。当时,该水位是从沿海浅水层(深1-3 M)记录的。在2004年12月26日的苏门答腊地震/海啸事件发生后约12小时,在两口井中观察到了这种扰动。在沿海附近的两口井中,此事件的发生时间是同步的,但未显示出远离海岸线的内陆井任何此类干扰。据推测,这种扰动,我们称之为“休克事件”,是由海啸从东南向西北传播到阿拉伯湾的突然影响造成的。随着海啸的蔓延,它们突然冲击了沿海浅层地下水含水层,导致了“休克事件”。

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