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  • 1
    Publication Date: 2014-11-26
    Description: Catchment management is favoured by the Water Framework Directive as a solution to the problem of rising nitrate levels in groundwater. The directive requires that member countries achieve a good, or improving, status in all water bodies by 2015. Currently, Cambridge Water relies on treatment or blending to reduce end-of-pipe nitrate concentrations to below the drinking water standard. The effectiveness of catchment management measures at 21 boreholes in Cambridgeshire was assessed with a combination of models, representing groundwater and soil zone processes. These sources are in predominantly arable catchments; they abstract from the Chalk aquifer, which is covered by Glacial Till in the south and east. Only seven sources showed a response to the catchment management scenarios within 40 years when compared with the current practice scenario. However, nitrate concentrations were not reduced at any sources by 2015 with the simulated catchment management measures. The seven sources that are most responsive to changes in land use or land management are those already affected by high nitrate levels. Catchment management may need to be used in conjunction with treatment and/or blending in the short to medium term so that Cambridge Water can continue to provide compliant drinking water to customers.
    Print ISSN: 1470-9236
    Topics: Geosciences
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  • 2
    Publication Date: 2018
    Description: 〈span〉〈div〉Abstract〈/div〉The study presents data from a geochemical till survey conducted in the Oppdal/Berkåk area of Central Norway. Using a 1 × 2.5 km grid, 877 samples were taken to cover a 2000-km〈sup〉2〈/sup〉 survey area (one site per 2.2 km〈sup〉2〈/sup〉). The samples were air dried, sieved to 〈2 mm and analysed for 51 elements following an aqua regia extraction. A number of geochemical anomalies, related to lithology, a prominent fault zone, mineralization or environmental processes, are delineated for a large number of elements. Four main anomalies are outlined. A large, elongated (40 km long) multi-element anomaly is associated with normal faults and adjacent rhyolitic-andesitic rocks occurring in the area. Elements associated with gold (As, Sb) form an anomaly on the central high-altitude area just to the east of the fault related anomaly. Two further areas that display high concentrations for many elements are located around Orkelsjøen and Soknedal. Climatic/topographic conditions have a strong influence on the Hg and Se distribution. Several areas that display geochemical anomalies, where more detailed studies could be conducted were also identified.〈strong〉Supplementary material:〈/strong〉 Geochemical maps for all elements, boxplots showing till samples grouped in tectonic units, and boxplots showing till samples grouped by main lithologies are available at 〈a href="https://doi.org/10.6084/m9.figshare.c.4038950"〉https://doi.org/10.6084/m9.figshare.c.4038950〈/a〉〈/span〉
    Print ISSN: 1467-7873
    Electronic ISSN: 1467-7873
    Topics: Chemistry and Pharmacology , Geosciences
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