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Investigating nitrate transport in a thick sandstone unsaturated zone based on integrated modelling – the Eden Valley, UK

机译:基于综合模型研究厚砂岩非饱和带中的硝酸盐迁移 - 英国伊甸园谷

摘要

Pollution of water by nitrate is not only an environmental issue but also an economic one and a threat to human health. In the Eden Valley (EV), groundwater nitrate concentrations are very variable distributed and have a rising trend, with some groundwater exceeding the limit of 50mg NO3 l-1 demanded by the EU Nitrate and Water Framework Directive. This study was undertaken to investigate the lag time between nitrate loading and entering groundwater, and explore the linkage between the nitrate in groundwater and its historic surface application. This involved the application of integrated nitrate transport modelling in the unsaturated zone (USZ) of Permo-Triassic sandstones (PT-SS). Three process-based models were integrated in the study. A map of the USZ thickness of the PT-SS was derived from a groundwater flow model using GIS-Groundwater – a GIS groundwater flow model; the historic and future arrival time of nitrate at the water table were modelled using a GIS nitrate transport model in the USZ; and a GIS model for nitrate dilution in the saturated zone was developed to validate the results.udThe modelled thickness of the PT-SS USZ in the Eden Valley varies from 0 – 183m and hence this imposes a large range of nitrate transport time (lag time) in the USZ (up to c. 60 years). The variable USZ thickness is one of the major reasons for the observed variable distribution of nitrate groundwater concentrations in the EV. The peak nitrate loading at around 1983 has affected most of the study area, and will arrive at the water table in the areas with thicker USZ within the next 35 years. The results of this study, especially the lag time between nitrate surface loading and entering the groundwater, are significant in supporting decision making. The integrated model developed in this study is readily-transferable to other regions or countries for any diffuse conservative pollutant, and can be used for studying the impact of climate and landuse changes on groundwater nitrate pollution.
机译:硝酸盐对水的污染不仅是环境问题,而且是经济问题,也是对人类健康的威胁。在伊甸谷(EV)中,地下水硝酸盐浓度的分布变化很大,并且呈上升趋势,有些地下水超过了《欧盟硝酸盐和水框架指令》所要求的50mg NO3 l-1的限值。这项研究旨在调查硝酸盐负荷与进入地下水之间的滞后时间,并探讨地下水中硝酸盐与其历史地表应用之间的联系。这涉及在二叠系-三叠纪砂岩(PT-SS)的非饱和带(USZ)中应用综合硝酸盐运移模型。在研究中集成了三个基于过程的模型。 PT-SS的USZ厚度图是使用GIS-地下水(一种GIS地下水流模型)从地下水流模型得出的;使用USZ中的GIS硝酸盐迁移模型对地下水中硝酸盐的历史和未来到达时间进行建模。 ud伊甸谷地区PT-SS USZ的模拟厚度在0 – 183m之间变化,因此,硝酸盐的运输时间范围很大(滞后)。时间(最长约60年)。 USZ厚度的变化是在电动汽车中观察到硝酸盐地下水浓度变化的主要原因之一。 1983年左右的硝酸盐峰值负荷已影响了整个研究区域,并将在未来35年内到达USZ较厚区域的地下水位。这项研究的结果,特别是硝酸盐表面负荷与进入地下水之间的滞后时间,对于支持决策具有重要意义。本研究开发的综合模型可以很容易地将任何弥散的保守污染物转移到其他地区或国家,并且可以用于研究气候和土地利用变化对地下水硝酸盐污染的影响。

著录项

  • 作者

    Wang Lei; Butcher Andrew;

  • 作者单位
  • 年度 2011
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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