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Modeling effects of nitrate from non-point sources on groundwater quality in an agricultural watershed in Prince Edward Island, Canada

机译:非点源硝酸盐对加拿大爱德华王子岛农业流域地下水质量的模拟作用

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Intensification of potato farming has contaminated groundwater with nitrate in many cases in Prince Edward Island, Canada, which raises concerns for drinking water quality and associated ecosystem protection. Numerical models were developed to simulate nitrate-N transport in groundwater and enhance understanding of the impacts of farming on water quality in the Wilmot River watershed. Nitrate is assumed non-reactive based on δ15N and δ18O in nitrate and geochemical information. The source functions were reconstructed from tile drain measurements, N budget and historical land-use information. The transport model was calibrated to long-term nitrate-N observations in the Wilmot River and verified against nitrate-N measurements in two rivers from watersheds with similar physical conditions. Simulations show groundwater flow is stratified and vertical flux decreases exponentially with depth. While it would take several years to reduce the nitrate-N in the shallow portion of the aquifer, it would take several decades or even longer to restore water quality in the deeper portions of the aquifer. Elevated nitrate-N concentrations in base flow are positively correlated with potato cropping intensity and significant reductions in nitrate- N loading are required if the nitrate level of surface water is to recover to the standard in the Canadian Water Quality Guidelines.
机译:在加拿大的爱德华王子岛,马铃薯耕作的集约化在许多情况下已经用硝酸盐污染了地下水,这引起了人们对饮用水水质和相关生态系统保护的关注。建立了数值模型来模拟地下水中硝态氮的运移,并增强对威尔莫特河流域农业对水质影响的理解。根据硝酸盐和地球化学信息中的δ15N和δ18O,假定硝酸盐为非反应性。源功能是根据瓷砖排水量测量,N个预算和历史土地使用信息重建的。该运输模型已根据威尔莫特河中的长期硝酸盐氮观测值进行了校准,并针对物理条件相似的分水岭的两条河流中的硝酸盐氮含量进行了验证。模拟表明,地下水流分层,垂直通量随深度呈指数下降。减少含水层浅层中的硝酸盐氮需要数年时间,而恢复含水层较深部分中的水质则需要数十年甚至更长的时间。基流中硝酸盐氮含量的升高与马铃薯的种植强度呈正相关,如果地表水的硝酸盐水平要恢复到《加拿大水质指南》的标准,则需要大量减少硝酸盐氮的含量。

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