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TSUNAMI PROTECTION BY NATURAL AND ARTIFICIAL BARRIERS

机译:自然和人工障碍物对海啸的保护

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Tsunami may be defined as a series of long wavelength waves, having period from 30 minutes to a couple of hours, occurring due to displacement of a large volume of water in ocean or a big lake. The various initiating events would include earthquakes, volcanic eruptions, underwater explosions, underwater landslides, and meteorite impact. The 2004 Indian Ocean tsunami exemplified this hazard for the Indian coast, especially the eastern one. The Fukushima incident in 2011 drew fresh attention to tsunami analysis, early detection and tsunami protection among nuclear community. Tsunami protection may be in active form like seawall to resist the incoming wave. Investigators have also brought out the passive resistance offered by coastal features like sand dunes, mangroves, vegetation, coral reefs and artificial structures. The present paper brings together the information regarding passive tsunami protection, available in recent literature.
机译:海啸可定义为一系列长波,周期为30分钟至几个小时,这是由于海洋或大湖中大量水的流失而产生的。各种引发事件包括地震,火山爆发,水下爆炸,水下滑坡和陨石撞击。 2004年印度洋海啸就是印度海岸,尤其是东部沿海地区这种危害的例证。 2011年的福岛事件使人们更加关注海啸分析,核社区中的早期发现和海啸保护。海啸保护可以采取主动形式,例如防波堤,以抵御传入的海浪。调查人员还发现了沙丘,红树林,植被,珊瑚礁和人造结构等沿海地貌所带来的消极抵抗。本文汇集了有关被动海啸保护的信息,这些信息可从最近的文献中获得。

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