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首页> 外文期刊>Acta Geophysica >Recognition of district-wise groundwater stress zones using the GLDAS-2 catchment land surface model during lean season in the Indian state of West Bengal
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Recognition of district-wise groundwater stress zones using the GLDAS-2 catchment land surface model during lean season in the Indian state of West Bengal

机译:在西孟加拉邦印度贫民区贫民季节期间,在贫民窟季节陆地表面模型的认识

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Water is essential for irrigation, drinking and industrial purposes from global to the regional scale. The groundwater considered a significant water resource specifically in regions where the surface water is not sufficient. Therefore, the research problem is focused on district-wise sustainable groundwater management due to urbanization. The number of impervious surface areas like roofing on built-up areas, concrete and asphalt road surface were increased due to the level of urban development. Thus, these surface areas can inhibit infiltration and surface retention by the impact of urbanization because vegetation/forest areas are decreased. The present research examines the district-wise spatiotemporal groundwater storage (GWS) changes under terrestrial water storage using the global land data assimilation system-2 (GLDAS-2) catchment land surface model (CLSM) from 2000 to 2014 in West Bengal, India. The objective of the research is mainly focused on the delineation of groundwater stress zones (GWSZs) based on ten biophysical and hydrological factors according to the deficiency of groundwater storage using the analytic hierarchy process by the GIS platform. Additionally, the spatiotemporal soil moisture (surface soil moisture, root zone soil moisture, and profile soil moisture) changes for the identification of water stress areas using CLSM were studied. Finally, generated results were validated by the observed groundwater level and groundwater recharge data. The sensitivity analysis has been performed for GWSZs mapping due to the deficit of groundwater storage. Three correlation coefficient methods (Kendall, Pearson and Spearman) are applied for the interrelationship between the most significant parameters for the generation of GWSZ from sensitivity analysis. The results show that the northeastern (max: 1097.35 mm) and the southern (max: 993.22 mm) parts have high groundwater storage due to higher amount of soil moisture and forest cover compared to other parts of the state. The results also show that the maximum and minimum total annual groundwater recharge shown in Paschim Medinipore [(361,148.51 hectare-meter (ham)] and Howrah (31,510.46 ham) from 2012 to 2013. The generated outcome can create the best sustainable groundwater management practices based upon the human attitude toward risk.
机译:水对全球范围为区域规模的灌溉,饮酒和工业用途至关重要。地下水被认为是在地表水不充分的区域中专门的显着水资源。因此,研究问题集中在城市化导致的地区可持续地下水管理。由于城市发展水平,由于城市发展水平,屋顶,混凝土和沥青路面上的屋顶等不透水表面区域的数量增加。因此,由于植被/森林区域减少,这些表面区域可以通过城市化的影响来抑制渗透和表面保持。本研究在印度西孟加拉邦2000年至2014年,使用全球土地数据同化系统-2(GLDAS-2)集水区面积模型(CLSM)在地面储水下的地下水位地下水储存(GWS)变化。该研究的目的主要专注于根据GIS平台的分析层次过程的地下水储存缺陷的十个生物物理和水文因素来划定地下水应力区域(GWSZ)。另外,研究了使用CLSM的水分应力区域的鉴定的时空土壤水分(表面土壤水分,根部区域土壤水分和剖面土壤水分)。最后,由观察到的地下水位和地下水补给数据验证了产生的结果。由于地下水储存的缺陷,已经对GWSZ映射进行了灵敏度分析。三种相关系数方法(KENDALL,PEARSON和SPEARMAN)应用于从敏感性分析产生GWSZ的最重要参数之间的相互关系。结果表明,东北(最大:1097.35毫米)和南方(最多993.22毫米)零件具有高层地下水储存,与国家的其他部分相比,土壤水分和森林覆盖量高。结果还表明,2012年至2013年,Paschim Medinipore中显示的最大和最低总年度地下水补给[(361,148.51公顷)和Howrah(31,510.46 Ham)。生成的结果可以创造最佳可持续地下水管理实践对人类对风险的态度。

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