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Impact of human activities on groundwater vulnerability in hombolo catchment: Dodoma, Tanzania

机译:人类活动对汉博洛流域地下水脆弱性的影响:坦桑尼亚多多马

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Groundwater is an important freshwater resource in Tanzania. However, rapid urbanization, informal/unplanned settlements and agricultural intensification in major basins threaten its sustainability. Most groundwater aquifers in the country are not monitored or managed, thus exposing them to potential contamination and overexploitation. This paper is based on a research conducted in the months of February and March, 2014, to assess how hydrogeological parameters and human activities impact on groundwater resources in Hombolo catchment. Thirty water samples collected from boreholes and shallow wells in the catchment were found to have high nitrate concentrations of 51.35 and 37.91 mg/L, respectively. Nitrate concentration varied by land use types with agricultural areas being the largest contributor (exceeding 154 mg/L) while wells in residential areas had relatively low concentrations (about 2.97 mg/L). However, the nitrate results do not represent the whole year; it is limited to two (2) months of field study. Using DRASTIC overlay and index method, 37.5 and 6.6% of the catchment were classifed as moderate and high vulnerability, respectively. However, when DRASTIC governing equation was explicitly integrated with human activities rating, areas with high vulnerability increased from 6.6 to 17.5%. Increased human activities, changed groundwater vulnerability over time and moderate areas in 1987 had changed to high vulnerability by 2014. Integrating human activities in the methodology is more suitable for groundwater vulnerability assessment.
机译:地下水是坦桑尼亚重要的淡水资源。但是,快速的城市化,非正式/计划外的定居点以及主要流域的农业集约化威胁到其可持续性。该国大多数地下水含水层没有得到监测或管理,因此使它们暴露于潜在的污染和过度开发中。本文基于2014年2月和3月进行的一项研究,以评估水文地质参数和人类活动如何影响Hombolo流域的地下水资源。从该流域的钻孔和浅井中收集的30个水样的硝酸盐浓度分别为51.35和37.91 mg / L。硝酸盐浓度随土地用途类型而异,其中农业地区是最大的贡献者(超过154 mg / L),而住宅区的水井中硝酸盐浓度相对较低(约2.97 mg / L)。但是,硝酸盐结果并不代表全年。它仅限于两(2)个月的实地研究。使用DRASTIC覆盖和指数法,分别将流域的37.5和6.6%分为中度和高度脆弱性。但是,当DRASTIC控制方程式与人类活动评分明确集成时,高度脆弱区域从6.6增加到17.5%。人类活动的增加,随着时间的流逝改变了地下水的脆弱性并在1987年变为温和地区,到2014年已转变为高度脆弱性。将人类活动纳入该方法更适合于地下水脆弱性评估。

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