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Flood Risk Assessment Tesco Supermarket, Swaffham<br />

2.5 Hydrogeology<br />

The Environment Agency onl<strong>in</strong>e <strong>in</strong>dicative aquifer mapp<strong>in</strong>g and the<br />

Landmark Aquifer Designation Mapp<strong>in</strong>g identifies that the solid geology<br />

beneath the site is identified as a Pr<strong>in</strong>cipal Aquifer <strong>with</strong> the superficial<br />

deposits classified as Unproductive Strata.<br />

Pr<strong>in</strong>cipal Aquifers are classified as layers of rock or drift deposits that<br />

have high <strong>in</strong>tergranular and/or fracture permeability - mean<strong>in</strong>g they<br />

usually provide a high level of water storage. They may support water<br />

supply and/or river base flow on a strategic scale. In most cases,<br />

pr<strong>in</strong>cipal aquifers are aquifers previously designated as major aquifer.<br />

Unproductive Strata is classified as rock layers or drift deposits <strong>with</strong> low<br />

permeability that has negligible significance for water supply or river<br />

base flow.<br />

The subject site is located <strong>with</strong><strong>in</strong> an Environment Agency Source<br />

Protection Zone 3 (SPZ3) „Source Catchment Protection Zone‟.<br />

A Source Catchment Protection Zone is def<strong>in</strong>ed as the area around a<br />

source <strong>with</strong><strong>in</strong> which all groundwater recharge is presumed to be<br />

discharged at the source. In conf<strong>in</strong>ed aquifers, the source catchment<br />

may be displaced some distance from the source. For heavily exploited<br />

aquifers, the f<strong>in</strong>al Source Catchment Protection Zone can be def<strong>in</strong>ed<br />

as the whole aquifer recharge area where the ratio of groundwater<br />

abstraction to aquifer recharge (average recharge multiplied by outcrop<br />

area) is >0.75.<br />

The Landmark Aquifer Designation Mapp<strong>in</strong>g is reproduced for<br />

reference <strong>in</strong> Appendix D.<br />

2.6 Hydrology<br />

There are no watercourses <strong>with</strong><strong>in</strong> 1km of the site, although there are a<br />

number of small surface water ponds, the closest be<strong>in</strong>g a natural pond<br />

and several man made balanc<strong>in</strong>g/dra<strong>in</strong>age ponds situated some 100m<br />

to the north of the site. There are further natural surface water ponds to<br />

the east of the site (<strong>in</strong>clud<strong>in</strong>g Northwell Pond approximately 250m to<br />

the east).<br />

The follow<strong>in</strong>g hydrological catchment characteristics have been<br />

obta<strong>in</strong>ed from Flood Estimation Handbook (FEH) CD –<br />

Page 3<br />

Jubb Consult<strong>in</strong>g Eng<strong>in</strong>eers Limited February 2012<br />

P9632-G300C-Rep-120209-MH

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