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                                                          Groundwater pollution remediation and protection  265







































                   Fig. 7.9 Schematic illustration of source protection zones showing the relationship between Zones I, II and III and the groundwater
                   source in four idealized hydrogeological situations representing: (a) a low effective porosity limestone aquifer; (b) a high effective
                   porosity sandstone aquifer; (c) a confined aquifer; (d) a spring. In reality, the size, shape and relationship of the zones will vary significantly
                   depending on the soil, geology, amount of recharge and volume of water abstracted. See text for an explanation of the definitions of Zones
                   I, II and III. After Environment Agency (1998).



                     Zone I, or the inner source protection zone, is  groundwater storage aquifers, such as sandstones,
                   located immediately adjacent to the groundwater  it is necessary, in order to provide adequate attenu-
                   source, and is designed to protect against the impacts  ation, to define further the outer protection zone to be
                   of human activity which might have an immediate  the larger of either the 400-day travel time area or the
                   effect upon the source. The area is defined by a 50-day  recharge catchment area calculated using 25% of the
                   travel time from any point below the water table   long-term abstraction rate for the source.
                   to the source and as a minimum 50-metre radius   Zone III, or the source catchment, is the remaining
                   from the source. This rule of thumb is used in other  catchment area of a groundwater source, and is
                   countries and is based on the presumed time taken  defined as the area needed to support an abstraction
                   for biological contaminants to decay in groundwater.  from long-term annual groundwater recharge. For
                   The land immediately adjacent to the source and   wells and boreholes, the source catchment area is
                   controlled by the operator of the source is included  defined by the authorized abstraction rate while,
                   within this zone.                           for springs, it is defined by the best known value of
                     Zone II, or the outer protection zone, is the area  average annual total discharge. In practice, the size
                   around the source defined by a 400-day travel time,  of Zone III will vary from tens to a few thousands
                   and is based on the requirement to provide delay and  of hectares depending on the volume of groundwater
                   attenuation of slowly degrading pollutants. In high  abstraction and the amount of recharge. In areas
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