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Effectiveness of groundwater nitrate removal in a river riparian area: the importance of hydrogeological conditions

机译:河流河岸地区地下水硝酸盐去除的有效性:水文地质条件的重要性

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Riparian areas are often considered important ecological ecotones that decrease the nitrate load of groundwater discharging into rivers. In this paper, the effectiveness of nitrogen removal from groundwater in a riparian area has been evaluated. We used a quantitative hydrogeological approach which delimited homogeneous stream tubes based on the water table contour. We constructed water and mass balances and used the results to estimate the mass of nitrogen removed by biological processes. Nitrogen removal effectiveness was calculated as the ratio of nitrogen removed to the total nitrogen mass flowing through the riparian area. This approach requires knowledge of the hydrogeological settings and coverage of an area larger than the study site. The removal we observed was seasonally variable, ranging between 2.2 and 7.6 mg N m(-2) day(-1) and represented up to 95% of the total nitrogen mass entering the riparian area in late summer. Removal effectiveness was only 27-38% in winter, due to the combination of a high nitrogen input and a low plant uptake. Nitrogen removal was highest in spring, but effectiveness was about 60% because the input was as high as in winter. Rainwater infiltrating the riparian area could represent almost the same quantity as groundwater input. Under such conditions, the dilution effect is very important in riparian areas that are not nitrate sources and it is essential to maintain this non-nitrate-emissive use. This study showed that the effectiveness of nitrogen removal in a riparian area is highly dependent on the pathway of water movement through its biologically active layers. (C) 2003 Elsevier Science B.V. All rights reserved. [References: 44]
机译:河岸地区通常被认为是重要的生态过渡带,可以减少流入河流的地下水的硝酸盐负荷。本文评估了河岸地区地下水脱氮的有效性。我们使用了定量水文地质方法,该方法根据地下水位轮廓划定了均质流管。我们构造了水与质量的平衡,并使用结果来估计通过生物过程除去的氮的质量。脱氮效率的计算方法是:脱氮量与流经河岸地区的总氮量之比。这种方法需要了解水文地质环境和覆盖面积大于研究地点的区域。我们观察到的去除量是季节性变化的,介于2.2至7.6 mg N m(-2)天(-1)之间,占夏末进入河岸区的总氮量的95%。由于高氮输入和低植物吸收的结合,冬季的去除效率仅为27-38%。春季的氮去除率最高,但由于输入量与冬季一样高,因此效率约为60%。渗透到河岸地区的雨水数量几乎与地下水输入量相同。在这种情况下,稀释作用在不是硝酸盐来源的河岸地区非常重要,因此必须保持这种非硝酸盐排放用途。这项研究表明,河岸地区脱氮的有效性高度依赖于水通过其生物活性层的流动途径。 (C)2003 Elsevier Science B.V.保留所有权利。 [参考:44]

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