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____________________________________________________________________________________________<br />

J-3999.7-FM Flood Risk Assessment & SUDS Design, Cave Farm, Nr Pitney, Somerset V2<br />

___________________________________________________________________________________________<br />

4.0 FLOODING MECHANISMS<br />

A number of possible flooding mechanisms have been considered <strong>at</strong> the site, and are<br />

discussed below.<br />

4.1 Groundw<strong>at</strong>er Flooding<br />

Investig<strong>at</strong>ion of ground w<strong>at</strong>er flooding has been undertaken within the South Somerset SFRA.<br />

Springs showing the emergence of ground w<strong>at</strong>er <strong>at</strong> the surface have been identified and are<br />

shown in Appendix D. Several springs are loc<strong>at</strong>ed north of the site near Bramwell, however,<br />

no springs are loc<strong>at</strong>ed within the region of the site. A large area to the north of the River<br />

Cary is low-lying (around 5m AOD) and requires significant land drainage in the form of<br />

rhynes, and ditches etc. The site is loc<strong>at</strong>ed between 35m AOD and 50m AOD, which suggests<br />

it should not suffer from similar ground w<strong>at</strong>er issues<br />

The SFRA does report on suspected ground w<strong>at</strong>er flooding events around Langport, however,<br />

this was recorded in 1954. Ground w<strong>at</strong>er as a source of flooding is particularly difficult to<br />

identify. Areas are typically assessed with respect to their geological properties and historic<br />

events , The SFRA continues with:<br />

“The available records appear to indic<strong>at</strong>e emerging groundw<strong>at</strong>er (i.e. in excess of the norm)<br />

in response to extreme rainfall. These appear to be localised and may in part rel<strong>at</strong>e to poor<br />

“land” drainage. None of the recorded occurrences appear to be widespread and do not<br />

therefore appear to be a reflection of regional rises in groundw<strong>at</strong>er level.”<br />

Given th<strong>at</strong> the <strong>development</strong> is non-residential, the site topography is high/steep rel<strong>at</strong>ive to the<br />

surrounding area, and, th<strong>at</strong> the <strong>solar</strong> panels are supported on frames which give limited<br />

resistance to the flow of w<strong>at</strong>er, ground w<strong>at</strong>er flooding will not be considered further within<br />

this report.<br />

4.2 Overland Sheet Flow<br />

The site is set in a rural environment with fields surrounding the entire site. Due to the sites<br />

elev<strong>at</strong>ion rel<strong>at</strong>ive to the surrounding topography, and the loc<strong>at</strong>ion of the nearby w<strong>at</strong>ercourses<br />

which can intercept overland flows, the risk of any significant overland flows being gener<strong>at</strong>ed<br />

th<strong>at</strong> can effect the site are considered to be small and will not be considered further within<br />

this report.<br />

Surface w<strong>at</strong>er runoff gener<strong>at</strong>ed by the <strong>development</strong> of the site is considered further in section<br />

6 of this report.<br />

4.3 Fluvial (River) Flooding<br />

The EA’s Indic<strong>at</strong>ive Flood Map illustr<strong>at</strong>es th<strong>at</strong> the entire site is loc<strong>at</strong>ed within Fluvial Flood<br />

Zone 1. This implies the site has gre<strong>at</strong>er than a 1 in 1000 year chance of being affected by<br />

fluvial flooding.<br />

As discussed in Section 3.0, the closest w<strong>at</strong>ercourse/drainage ditch to the site has a very<br />

small c<strong>at</strong>chment of less than 1km 2 and will therefore, have limited capacity to gener<strong>at</strong>e<br />

significant flows.<br />

As such the fluvial flooding will not be considered further within this report.<br />

P:\Job Files 3900-3999\J-3999-FM AEE Flood Risk Assessments\J-3999.7-FM Cave Farm\Report V2<br />

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