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Spatial and temporal variation of salt ions in the surface water of Shule River Valley in Gansu Province, China

机译:甘肃省舒河河谷地表水域盐离子的空间和时间变异

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The objective of the study was to assess the quality of the Shule River water for irrigational purposes. Surface water samples were collected along the course of the river in May and October 2012. The samples were analyzed for pH, electrical conductivity (EC), bicarbonate, chloride, sulphate, sodium, potassium, calcium and magnesium. Surface water was generally alkaline (average pH 8.17) and water pH and total dissolved solids in May were higher than those in October. EC ranged from 0.24 to 2.15 mS cm(-1). Sodium was identified as the dominant cation, sulphate was identified as the dominant anion in May for both samples of river water but, in October, the dominant anions are respectively sulphate, bicarbonate and chloride from the upper region to the lower region. The total dissolved solids, chloride and sodium were found to exceed the permissible limits for irrigation water in the lower region. According to the principal factor analysis results, among water quality parameters measured in this study, chloride is the best indicator for monitoring water quality. The results revealed a deteriorating water quality in the lower region of the river.
机译:该研究的目的是评估Shule River水的质量以进行灌溉目的。沿着5月和2012年10月沿河进程收集地面水样。分析样品以进行pH,电导率(EC),碳酸氢盐,氯化物,硫酸盐,钠,钾,钙和镁。地表水通常是碱性(平均pH8.17),水pH和总溶解固体在10月份均高于10月份。 EC的级别为0.24至2.15 ms(-1)。将钠被鉴定为优势阳离子,硫酸盐被鉴定为5月份河水样品中的显性阴离子,但在10月份,主要阴离子分别从上部区域到下部区域的硫酸盐,碳酸氢盐和氯化物。发现总溶解的固体,氯化钠和钠超过下部区域的灌溉水的允许限制。根据本研究中测量的水质参数的主要因素分析结果,氯化物是监测水质的最佳指标。结果表明,河流下部水质劣化。

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