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Oozing of water in parts of Andhra Pradesh, India.

机译:在印度安得拉邦部分地区渗水。

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Oozing of water and rise in water level were reported by villagers and media during the third week of January 2005, in parts of Rangareddy, Nalgonda and Mahboobnagar districts of Andhra Pradesh, India. The event also coincided with the aftermath of the 9.3 magnitude earthquake in Sumatra, Indonesia and the tsunami in the Indian Ocean. The villagers and State and Central agencies were baffled by the unusual phenomenon. After a general reconnaissance, an integrated study comprising water level monitoring, water quality analyses, topography survey, isotopic analyses, mise-a-la-masse survey and electrical resistivity imaging (ERI) was carried out at two sites near Mukindapur and Devanur of Yalal mandal in Ranga Reddy district, where the phenomenon of water-oozing was observed. The integrated study revealed that the oozing of water at the studied location is purely hydrological/hydrogeological and a shallow phenomenon. Scientific data could not attribute any strong connection to the deeper tectonics nor to the impact of the Sumatra earthquake and aftershocks. However, investigations form a prelude to any such geogenic activity in the region, suggesting monitoring of water level and further studies during the current hydrological year for any definite conclusion..
机译:2005年1月第三周,印度安得拉邦Rangareddy,Nalgonda和Mahboobnagar部分地区的村民和媒体报道渗水和水位上升。该事件还与印度尼西亚苏门答腊9.3级地震和印度洋海啸的后果相吻合。村民以及国家和中央机构对这种异常现象感到困惑。进行全面侦察后,在Mukindapur和Yalal的Devanur附近的两个地点进行了综合研究,包括水位监测,水质分析,地形调查,同位素分析,muse-a-la-Masse调查和电阻率成像(ERI)。朗加雷迪(Ranga Reddy)地区的曼达尔(mandal),观察到渗水现象。综合研究表明,研究地点的渗水纯粹是水文/水文地质现象,是一种浅水现象。科学数据既不能归因于深部构造,也不能归因于苏门答腊地震和余震的影响。但是,调查是该地区任何此类地质活动的序幕,建议监测水位并在当前水文学年期间进行进一步研究以得出明确结论。

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