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Groundwater Situation at Southwest Coast of India -A Field study, Overview, Opportunities and Challenges

机译:印度西南海岸的地下水形势 - 田野研究,概述,机遇和挑战

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Most of the coastal regions are experiencing water related problems such as acute shortage of water, decline trend in water level and saltwater intrusion. Groundwater resource is becoming scarce, as is evidenced by the increasing demand on water, improper planning, poor agricultural practices, inefficient utilization, groundwater mining, peculiar soil characteristics, and steep slopes. Hence, there is a need to study the overall status of groundwater level fluctuations (gwlf) in a micro watershed located at 13° 0 '00" to 13° 2' 30" North Latitude and 74° 47' 00" to 74° 50' 00" East Longitude south west coast of India. The current study aims to present and evaluates the periodical behavior of gwlf by statistical properties and also, we investigate the effect of meteorological parameters which includes temperature, relative humidity, rainfall, evaporation, land use/cover, stream flow, and soil type on groundwater level fluctuations. Therefore, in order to understand the periodical behavior of groundwater level fluctuations for forty two open wells, weekly and seasonal analysis has been carried out using historical groundwater level data for a period of seven years (2004-2011). It is noticed that groundwater level is peak during the monsoon and declines in summer season for the past seven years. It is also observed that there is increase in water level from 2004 to 2007 and 2008 to 201 land decline tend in the 2008 and 2011 year respectively. Rainfall, temperature, stream flow, soil type are the major influence factors for groundwater level fluctuations in the present study. The results obtained from the current study provide insights on the relevance of taking into account for good agricultural practices, conjunctive use, proper planning and development of groundwater resources in a sustainable manner.
机译:大多数沿海地区正在经历水有关的问题,如急性缺乏水,水平和盐水侵犯的趋势下降。地下水资源正在变得稀缺,正如日益增长的水,规划,农业实践差,利用率低下,利用率,地下水挖掘,特殊土壤特征和陡坡的需求所证明。因此,需要研究位于13°0 '00“至13°2'30”北纬和74°47'00“至74°50的微水流域地下水位波动(GWLF)的整体状态。至74°50 '00“印度的东度南海西海岸。目前的研究旨在通过统计特性展示和评估GWLF的定期行为,以及探讨气象参数的影响,包括温度,相对湿度,降雨,蒸发,土地使用/盖,流流程和土壤类型的地下水水平波动。因此,为了了解地下水位的周期性行为为四十两个开放井的波动,每周和季节性分析使用历史地下水位数据进行了七年(2004 - 2011年)。人们注意到地下水位在季风期间的峰值是峰值,并且过去七年夏季下降。还观察到,从2004年到2007年和2008年到2011年的2011年趋势分别趋于2011年的2008年到2011年的2011年下降。降雨,温度,流流,土壤类型是本研究地下水位波动的主要影响因素。从目前的研究中获得的结果提供了对考虑到良好的农业实践,联合使用,适当规划和地下水资源的相关性的相关性的见解。

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