首页> 美国卫生研究院文献>International Journal of Environmental Research and Public Health >Geospatial Distributions of Groundwater Quality in Gedaref State Using Geographic Information System (GIS) and Drinking Water Quality Index (DWQI)
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Geospatial Distributions of Groundwater Quality in Gedaref State Using Geographic Information System (GIS) and Drinking Water Quality Index (DWQI)

机译:基于地理信息系统(GIS)和饮用水水质指数(DWQI)的格达雷夫州地下水质量的地理空间分布

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摘要

The observation of groundwater quality elements is essential for understanding the classification and distribution of drinking water. Geographic Information System (GIS) and remote sensing (RS), are intensive tools for the performance and analysis of spatial datum associated with groundwater sources control. In this study, groundwater quality parameters were observed in three different aquifers including: sandstone, alluvium and basalt. These aquifers are the primary source of national drinking water and partly for agricultural activity in El Faw, El Raha (Fw-Rh), El Qalabat and El Quresha (Qa-Qu) localities in the southern part of Gedaref State in eastern Sudan. The aquifers have been overworked intensively as the main source of indigenous water supply in the study area. The interpolation methods were used to demonstrate the facies pattern and Drinking Water Quality Index (DWQI) of the groundwater in the research area. The GIS interpolation tool was used to obtain the spatial distribution of groundwater quality parameters and DWQI in the area. Forty samples were assembled and investigated for the analysis of major cations and anions. The groundwater in this research is controlled by sodium and bicarbonate ions that defined the composition of the water type to be Na HCO3. However, from the plots of piper diagram; the samples result revealed (40%) Na-Mg-HCO3 and (35%) Na-HCO3 water types. The outcome of the analysis reveals that several groundwater samples have been found to be suitable for drinking purposes in Fa-Rh and Qa-Qu areas.
机译:观察地下水水质元素对于了解饮用水的分类和分布至关重要。地理信息系统(GIS)和遥感(RS)是用于执行和分析与地下水源控制相关的空间基准的密集工具。在这项研究中,在三个不同的含水层中观测到了地下水质量参数,包括:砂岩,冲​​积层和玄武岩。这些含水层是国家饮用水的主要来源,部分是苏丹东部格达勒夫州南部地区的艾法,拉哈(Fw-Rh),加拉巴特和盖尔沙(Qa-Qu)地区的农业活动。含水层已被过度劳累,成为研究区域本地供水的主要来源。采用插值法对研究区地下水的相貌模式和饮用水水质指数(DWQI)进行了验证。 GIS插值工具用于获取该地区地下水水质参数和DWQI的空间分布。组装了40个样品并进行了研究,以分析主要的阳离子和阴离子。这项研究中的地下水由钠和碳酸氢根离子控制,这些离子将水类型的组成定义为Na HCO3。然而,从吹笛者图的情节;样品结果显示(40%)Na-Mg-HCO3和(35%)Na-HCO3水类型。分析结果表明,在Fa-Rh和Qa-Qu地区发现了一些适合饮用的地下水样品。

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