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Forthbank Wind Energy Development - Partnerships for Renewables

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<strong>Forthbank</strong> <strong>Wind</strong> <strong>Energy</strong> <strong>Development</strong><br />

13.3.72 A vertical section of <strong>Forthbank</strong> No.1 Mine shows the rockhead is detailed to be 19.2m bgl, with<br />

the Mosie Seam at 22.85m bgl, the Lower Five Foot at 32m bgl and the Alloa Splint at 41.14m<br />

bgl.<br />

13.3.73 Extensive mine workings are noted to the north of the Turbine 1 location and off-site to the<br />

east. From this plan, the workings appear to be in the Alloa Splint Coal and consist of room<br />

and pillar mining.<br />

Hydrogeology<br />

Groundwater Bodies<br />

13.3.74 A search of the SEPA RBMP GIS Database was undertaken to provide in<strong>for</strong>mation on the<br />

groundwater body in the region of the site. The database indicates that the site is underlain by<br />

the Alloa bedrock and localised sand and gravel aquifers groundwater body. The quality of the<br />

groundwater body has been classified by SEPA as ‘poor’ with a high degree of confidence and<br />

the quantity of the groundwater has been classified as ‘good’ with a high degree of confidence<br />

in 2008. Pressure types which exist on the groundwater body are noted as mining and<br />

quarrying of coal, which is classified as a diffuse pollution source.<br />

13.3.75 A search of the SEPA RBMP GIS database show that, like much of Scotland, the site is within<br />

a Drinking Water Protection Area. The site is not within a Nitrate Vulnerable Zone.<br />

Hydrogeological Classification<br />

13.3.76 According to the Hydrogeological Map of Scotland, the site is underlain by an aquifer of limited<br />

potential and without significant groundwater, referring to the superficial deposits. This is<br />

expected to be underlain by the Lower Coal Measures, which is expected to be a highly<br />

productive (but not extensive) aquifer. This aquifer is classified by SEPA as IFH, a highly<br />

productive aquifer with intergranular flow.<br />

Groundwater Vulnerability<br />

13.3.77 The BGS groundwater vulnerability map of Scotland indicates that the site is underlain by<br />

strata which is moderately permeable, i.e. fractured or potentially fractured rocks that do not<br />

have a high primary permeability. The aquifers at the site vary in classification from<br />

Vulnerability Class 1 (Only vulnerable to conservative pollutants in the long-term when<br />

continuously and widely discarded and leached) to Vulnerability Class 3 (Aquifers are classed<br />

as being vulnerable to some pollutants) in SEPA vulnerability classification scheme.<br />

Site Investigation Data<br />

13.3.78 From the intrusive investigations carried out, it was noted that Carse Clay had horizons of sand<br />

which are likely to have high permeabilities. Plastic silt (i.e. low permeability silt) was noted to<br />

be present at some locations.<br />

November 2010 Chapter 13 Page 18<br />

Copyright <strong>Partnerships</strong> <strong>for</strong> <strong>Renewables</strong> <strong>Development</strong> Co. Ltd 2010 ©

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