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Evaluation of the Karst Water Quality Upstream of Junhe River Basin in Shandong Province, China

机译:山东省君河盆地喀斯特水质评价

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Seventy nine karst water samples were used to study the quality of groundwater in upstream of Junhe River. The main hydrochemical types were HCO_3 type, HCO_3·SO_4 type, HCO_3·Cl type and Cl type, and the HCO_3 type occupied 58% of the total evaluation area. The sample points were grouped in the lower-left corner of the Piper picture, showing that the content of alkaline-earth metal ions exceeded that of alkali metal ions and weak acid ions exceeded the strong acid ions. The Schoeller picture demonstrated that the karst water originated from the same recharge source that was precipitation and the connectedness in the area was well. Groundwater comprehensive quality evaluation showed that most samples were at level IV. Karst water pollution in evaluation area was serious, and it was urgent to improve the quality of groundwater.
机译:七十九个喀斯特水样用于研究君河河上游地下水的质量。主要的水化学类型是HCO_3型,HCO_3·SO_4型,HCO_3·CL型和CL型,HCO_3类型占总评估区域的58%。将样品点分组在吹笛器图的左下角,表明碱土金属离子的含量超过了碱金属离子和弱酸离子的含量超过了强酸离子。 Schoeller图片表明,喀斯特水源来自同一补充源,该源是沉淀的,该区域的连接良好。地下水综合质量评价显示,大多数样品在IV级。评估区的喀斯特水污染严重,迫切需要提高地下水的质量。

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