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A catchment-scale approach to understand the nitrate legacy issues in Permo–Triassic sandstones in the Eden Valley, UK

机译:一种流域规模的方法来了解英国伊甸园谷的二叠纪 - 三叠纪砂岩中的硝酸盐遗留问题

摘要

Nitrate water pollution, which is mainly caused by agricultural activities, remains an international problem. It has been identified as a major threat to the implementation of the EU Water Framework Directive. It could take decades for nitrate leached from the soil to discharge into freshwaters due to nitrate long time-lag in the groundwater system. Nevertheless, this nitrate legacy issue has generally been ignored in the environmental water management. Efforts have been made to tackle the agricultural diffuse groundwater pollution in the Eden Valley, UK. However, it is necessary to investigate the impacts of historical nitrate loading from agricultural land on the trend in nitrate concentrations in the Permo–Triassic sandstones, which form the major aquifers in the study area. For this purpose, this paper presents an approach to representing nitrate transport in the groundwater system at the catchment scale but in simplified ways. This method considers the spatio-temporal nitrate loading from agricultural land, the impact of low-permeability superficial deposits on nitrate movement, the nitrate transport via both the intergranular matrix and fractures in the unsaturated zones, and nitrate transport and dilution in the saturated zones. It requires modelled recharge values, together with published aquifer properties and local geological information. Monte Carlo simulations were undertaken to analyse the sensitivity of parameters, and to calibrate the model using nitrate monitoring data. Time series of annual nitrate concentrations from 1925 to 2150 were generated for four aquifer zones in the Eden Valley, i.e. ‘St Bees Sandstones’, ‘Silicified Penrith Sandstones’, ‘Non-silicified Penrith Sandstones’ and ‘interbedded Brockram Penrith Sandstones’. The results show that the nitrate concentrations in the first three aquifer zones keep rising until their peak values are reached at their turning-point years, while the last aquifer zone has a declining trend in nitrate concentration. These results can help policy makers understand how the historical nitrate loading from agricultural land affect the evolution of the quality of groundwater and groundwater-dependent surface waters. The model developed in this study requires relatively modest parameterisation but provides a framework for informing the long-term impact and timescale of different scenarios introduced to deliver water-quality compliance.
机译:主要由农业活动引起的硝酸盐水污染仍然是一个国际问题。它已被确认为对欧盟水框架指令实施的主要威胁。由于硝态氮在地下水系统中的长时间滞后,硝酸盐从土壤中沥出并排放到淡水中可能需要数十年的时间。然而,这种硝酸盐遗留问题在环境水管理中通常被忽略。已做出努力来解决英国伊甸园谷地区的农业地下水扩散问题。但是,有必要调查农业土地上的历史硝酸盐负荷对Permo-Triassic砂岩中硝酸盐浓度趋势的影响,这些砂岩是研究区的主要含水层。为此,本文提出了一种以流域尺度来表示地下水系统中硝酸盐迁移的方法,但是方法很简单。该方法考虑了农田中硝酸盐的时空分布,低渗透性表层沉积物对硝酸盐运动的影响,硝酸盐通过晶间基质和不饱和区裂缝的硝酸盐迁移以及饱和区的硝酸盐迁移和稀释。它需要建模的补给值,以及已发布的含水层特性和当地地质信息。进行了蒙特卡洛模拟,以分析参数的敏感性,并使用硝酸盐监测数据对模型进行校准。伊甸谷的四个含水层带产生了从1925年到2150年的年硝酸盐浓度的时间序列,即“圣蜜蜂砂岩”,“硅化彭里斯砂岩”,“非硅化彭里斯砂岩”和“互穿的布罗克兰姆彭里斯砂岩”。结果表明,前三个含水层区的硝酸盐浓度一直保持上升,直到在其转折点年达到峰值为止,而最后一个含水层区的硝酸盐浓度呈下降趋势。这些结果可以帮助决策者了解农业土地上的历史硝酸盐含量如何影响地下水和依赖地下水的地表水水质的演变。本研究中开发的模型需要相对适度的参数设置,但提供了一个框架,用于告知为实现水质合规而引入的不同方案的长期影响和时间表。

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    Wang Lei;

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  • 年度 2015
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