Nitrate contamination of groundwater in the western Po Plain (Italy): the effects of groundwater and surface water interactions
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  • 作者:Manuela Lasagna ; Domenico Antonio De Luca ; Elisa Franchino
  • 关键词:GW–SW interactions ; Nitrates ; Losing and gaining streams ; Denitrification ; Hyporheic zone ; Riparian zone ; Po River
  • 刊名:Environmental Earth Sciences
  • 出版年:2016
  • 出版时间:February 2016
  • 年:2016
  • 卷:75
  • 期:3
  • 全文大小:4,151 KB
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  • 作者单位:Manuela Lasagna (1)
    Domenico Antonio De Luca (1)
    Elisa Franchino (1)

    1. Earth Science Department, Turin University, Via Valperga Caluso 35, 10125, Turin, Italy
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:None Assigned
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1866-6299
文摘
This study aims to investigate the physical and chemical effects of interactions between groundwater and surface water (GW–SW)—particularly in streams—on nitrate contamination. The effects of GW–SW interactions are briefly reviewed, with a particular emphasis on processes and environments that influence increases or decreases in nitrate concentration. Then, this paper analyses nitrate concentrations in groundwater and surface water in the western Po plain (Northwestern Italy); this analysis includes the nitrate concentration profiles across the shallow aquifer and intersecting the main streams on the plain. The investigation highlights how the concentration trends are similar, even when nitrate levels in rivers and groundwater are not comparable. The maximum nitrate concentrations in the surface water were generally measured in areas with high-nitrate levels in groundwater. An analysis of the nitrate concentration profiles highlighted the mutual influences of GW–SW. The most important streams on the plain (the Po River and Stura di Demonte River), both of them gaining streams, seem to reduce the nitrate concentrations of groundwater at a study scale. The proposed conceptual model indicates how the near-stream environment (the riparian zone, wetlands, hyporheic zone and shallow organic-rich soils in the near-stream environment) and the groundwater flow systems in shallow and deep aquifers, from the recharge zone to the streams, could dramatically affect the nitrate concentrations.

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