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Understanding nitrate contamination based on the relationship between changes in groundwater levels and changes in water quality with precipitation fluctuations

机译:根据地下水位变化与降水波动引起的水质变化之间的关系了解硝酸盐污染

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There are growing concerns about nitrate contamination in Kumamoto City, where 700,000 people completely depend on groundwater as a source of drinking water. We found that some groundwater samples showed considerably different nitrate concentrations although their sampling locations were close to one another, and we speculated that this phenomenon was due to the differences in subsurface geological properties. In order to verify this hypothesis, we carried out temporally intensive long-term monitoring of the groundwater levels and water qualities at three of the closely related sampling wells, and the results revealed that the changes in water level and water quality were different at each well. The water level at well T1, where nitrate concentrations ranged from 12 to 26 mg N/L, showed a significantly sensitive and unique response to heavy rain, which indicated that the subsurface at this site might be highly permeable; this would have allowed for the influent water to easily reach the groundwater aquifer over a short period. However, wells T2 and T3, which were located within 0.6 and 1.9 km from well T1, respectively, had nitrate concentrations that were lower than that in well T1 (45-8.0 mg N/L) and showed only gradual responses to heavy rain. These observations suggest that the highly permeable subsurface properties in the vicinity of well T1 contributed to the more serious nitrate contamination in well T1 than those at wells T2 and T3. This study demonstrates the importance of temporally intensive, long-term monitoring for capturing changes in groundwater level and water quality with precipitation fluctuations, and we showed how this approach can lead to a better understanding of the nitrate contamination situation. (C) 2018 Elsevier B.V. All rights reserved.
机译:在熊本市,硝酸盐污染日益引起人们的关注,那里有70万人完全依靠地下水作为饮用水源。我们发现一些地下水样品虽然采样位置彼此接近,但硝酸盐浓度却有很大不同,我们推测这种现象是由于地下地质特性的差异所致。为了验证该假设,我们对三个紧密相关的采样井进行了时间密集的长期监测,以监测地下水位和水质,结果表明,每口井的水位和水质变化都不同。 T1井的水位(硝酸盐浓度范围为12至26 mg N / L)对大雨表现出明显的敏感和独特的响应,这表明该地点的地下可能具有高渗透性。这样一来,流入水就可以在短时间内轻松到达地下水含水层。然而,分别位于距T1井0.6公里和1.9公里处的T2和T3井的硝酸盐浓度低于T1井(45-8.0 mg N / L),且仅显示出对大雨的逐渐响应。这些观察结果表明,与T2和T3井相比,T1井附近的高渗透性地下特性导致了T1井中更严重的硝酸盐污染。这项研究表明,为了捕捉地下水水位和水质随降水的变化而进行的时间密集的长期监测的重要性,并且我们展示了这种方法如何能够更好地理解硝酸盐污染状况。 (C)2018 Elsevier B.V.保留所有权利。

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