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Spatial and Temporal Characteristics of Carbon Tetrachloride Pollution in a Karst Aquifer

机译:岩溶含水层中四氯化碳污染的时空特征

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摘要

The karst aquifer in a northern city of China was polluted by carbon tetrachloride (CCl4). The pollution characteristics was studied by four years' monitoring CCl4 concentration of the karst groundwater in 15 typical wells and analysis of the CCl4 content in 206 soil samples from 17 boreholes in polluted source area. The CCl4 pollution plume is distributed as a belt-dumbbell form. Two polluted centers are located at the southern pollution source sub-area and the northern artificial discharge sub-area respectively. 95.4% polluted wells are laid in Ordovician limestone aquifer. In general, CCl4 concentration of groundwater in all wells decreased in recent years and inside year the CT concentration during the period of August to October was much higher. The CCl4 polluted the karst aquifer by directly seeping of wastewater in the pesticide plant area, flowing into the aquifer through bare section of limestone in effluent ditch, and leaking under ditch by soil. The heterogeneity of water-bearing media and artificial exploitation control the CCl4 diffusion and the CCl4 plume is similar with the groundwater flow field.
机译:中国北方城市的岩溶含水层被四氯化碳(CCl4)污染。通过四年监测15个典型井中的喀斯特地下水CCl4浓度并分析污染源地区17个钻孔的206个土壤样品中CCl4含量,研究了污染特征。 CCl4污染羽流以皮带哑铃形式分布。两个污染中心分别位于南部污染源子区域和北部人工排放子区域。 95.4%的污染井位于奥陶系石灰岩含水层中。总体而言,近年来所有井中的地下水CCl4浓度均下降,而在8月至10月的一年中,CT浓度则高得多。四氯化碳通过直接渗入农药厂区的废水,通过废水沟中的石灰石裸露部分流入含水层,并在沟渠下被土壤泄漏而污染了喀斯特含水层。含水介质的非均质性和人工开采控制着CCl4的扩散,CCl4的羽状流与地下水流场相似。

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