...
首页> 外文期刊>Sustainable Water Resources Management >Quantitative assessment of groundwater resource potential in a coalfield of Damodar River Basin India
【24h】

Quantitative assessment of groundwater resource potential in a coalfield of Damodar River Basin India

机译:印度Damodar河流域某煤田地下水资源潜力定量评价。

获取原文
获取原文并翻译 | 示例

摘要

The present study was carried out for the quantitative assessment of groundwater resource potentials in East Bokaro Coalfield of Damodar River Basin. The rise and fall of groundwater table is closely related to the hydro-meteorological conditions, water level, landform, geology and morphological factors. Average annual rainfall for the entire period of 35 years is 1366 mm in which annual maximum rainfall was 2544 mm in the year 2001 and minimum was 733 mm in the year 2004. The fluctuation of groundwater level ranged between 0.15 and 2.87 mbgl in the study area. Rainfall is the main source to replenish the groundwater by percolation through deep soil zones. Besides rainfall, the mine water discharges from the local mining areas and existing water bodies including water logged in abundant mine quarries. Mine water also contributed to the groundwater recharge as return flow. The study area is highly disturbed and the permeabilities of individual geological units are spatially variable and depend on lithology, fracturing and attenuation with depth. The total annual replenishable recharge was calculated to be 48.5 million m_(3)/year and net annual groundwater availability was estimated to be 13.7 million m_(3)by rainfall infiltration method. The stage of groundwater development was calculated as per GEC-1997 guideline, which falls under the safe category (i.e., 67%). But water resource conservation for sustainable water management is urgently required in the study area.
机译:本研究旨在定量评估达莫达河流域东博卡罗煤田的地下水资源潜力。地下水位的上升和下降与水文气象条件,水位,地貌,地质和形态因素密切相关。整个35年期间的年平均降雨量为1366毫米,其中2001年的年最大降雨量为2544毫米,2004年的年最小降雨量为733毫米。研究区域的地下水水位波动在0.15和2.87mbgl之间。降雨是通过深层土壤渗流补充地下水的主要来源。除降雨外,矿井水还从当地矿区和现有水体中排出,其中包括大量采石场中记录的水。矿井水也作为回流量促进了地下水的补给。研究区域受到严重干扰,单个地质单元的渗透率在空间上是可变的,并且取决于岩性,裂缝和深度衰减。通过降雨入渗法计算出的年度可补充总补给量为4850万立方米(3)/年,估计年净地下水可用量为1370万立方米(3)。地下水开发阶段是根据GEC-1997指南计算的,属于安全类别(即67%)。但是研究区域迫切需要水资源保护以实现可持续的水管理。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号