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A CASE OF HYDROCHEMICAL CHARACTERIZATION OF AN ALLUVIAL AQUIFER INFLUENCED BY HUMAN ACTIVITIES

机译:人类活动对冲积含水层水化学特性的影响

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2l physico--chemical parameters have been determined in 47 groundwater sarnples col- lected in October l994 from the alluvial aquifer of the Pisuerga river, located at the north-east of Valladolid (north--western Spain). Conventional hydrochemical methods and multivariate statistical analysis have been used to discriminate natural phenomena and pollution processes in the area. It has been demonstrated the existence of a heterogeneity in groundwater mineral contents related to anthropic actions such as irrigation, source of irrigation water and location of polluting sources. This study demonstrates the existence of two sub-units in the alluvial aquifer (left and right river banks) with different hydrochemical characteristics, and identifies three different singular areas in the left bank. Groundwater from this bank showed higher levels of dissolved ions caused by concen- tration processes derived from the predominant use of groundwater for crop irrigation, whilst in the right bank of the aquifer less saline water from canals is used. Degradation of groundwater quality has been observed in some areas of the left aquifer sub-unit (north, Santovenia and south-central sites) where anomalous high concentrations of sulphate, sodium, chloride and nitrate were measured, and can be related to the presence of potentially polluting sources such as leachates from industrial waste disposals, sewage effluents and use of organic and inorganic fertilizers.
机译:在1994年10月从位于巴利亚多利德(西班牙西北部)东北的Pisuerga河冲积含水层收集的47个地下水尖峰中,确定了2l的理化参数。常规的水化学方法和多元统计分析已被用来区分该地区的自然现象和污染过程。已经证明,与诸如灌溉,灌溉水源和污染源位置等人类活动有关的地下水矿物质含量存在异质性。这项研究证明了冲积含水层(左右河岸)中两个具有不同水化学特征的亚单元的存在,并确定了左岸三个不同的奇异区域。来自该河岸的地下水显示出浓度较高的溶解离子,这是由于主要用于灌溉农作物而产生的浓缩过程引起的,而在含水层的右岸,运河中使用的盐水较少。在左含水层亚单元的某些区域(北部,圣托维尼亚和中南部站点)已观察到地下水质量下降,这些区域测量到异常高浓度的硫酸盐,钠,氯化物和硝酸盐,这可能与地下水的存在有关。潜在的污染源,例如来自工业废物处理的渗滤液,污水,有机和无机肥料的使用。

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