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                   Fig. 7.5 Specific groundwater nitrate
                   vulnerability map for England and Wales.
                   The vulnerability classes are derived from
                   a GIS overlay operation of: (i) simulated
                   mean nitrate concentrations in land
                   drainage assuming a uniform nitrogen
                                 −1
                   loading of 100 kg N ha ; (ii) soil types; (iii)
                   presence or absence of low permeability
                   superficial deposits; and (iv) aquifer types.
                   Regions of high groundwater vulnerability
                   to nitrate pollution (classes 1–4) are in
                   areas of major aquifers (compare with
                   Fig. 2.27). After Lake et al. (2003).



                   is that they provide a regional picture that is  7.3.2 Source protection zones
                   insufficiently detailed to demonstrate the actual
                   threat to the groundwater resource at a local scale.  In the definition of groundwater source protection
                   The true vulnerability can only be established with  zones, the proximity of a hazardous activity to a point
                   confidence through supporting, site-specific field  of groundwater abstraction (including springs, wells
                   investigations. Even so, groundwater vulnerability  and boreholes) is one of the most important factors in
                   maps are instrumental in conveying groundwater  assessing the pollution threat to an existing ground-
                   pollution potential to planners and can help achieve  water source. In principle, the entire recharge area
                   water quality objectives by influencing land-use   in the vicinity of a groundwater source should be
                   management.                                 protected, but this is unrealistic on socioeconomic
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