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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 />

13.3.52 Landfill gas migration monitoring points were installed off-site to the north of the main landfill<br />

area. Monitoring records show the maximum concentration of methane recorded was 1.5%<br />

v/v. The maximum concentration of carbon dioxide was also 1.5%v/v.<br />

13.3.53 Leachate sampling is currently undertaken on a monthly basis at the landfill and the results are<br />

held by Clackmannanshire Council. It is of note that leachate is currently extracted from the<br />

site using a perimeter leachate extraction drain, installed in 1996. The leachate is collected in<br />

two holding chambers prior to being pumped to the sewage treatment works.<br />

Superficial Deposits<br />

13.3.54 According to the BGS digital data provided by emapsite, the south-eastern part of the site and<br />

access road are both underlain by reclaimed intertidal deposits (see Figure 13.3). The northwestern<br />

part of the site is underlain by raised tidal flat deposits of Flandrian Age.<br />

13.3.55 Previous site investigations state that the site is underlain by grey very fine sands, silts, organic<br />

silty clays and clayey silts, these are locally known as the Carse Clays. These range in<br />

thickness from 1m to 12m.<br />

13.3.56 Trial pits extended in the area of the wetlands adjacent to the landfill were also within the<br />

Carse Clays. This material was used to cap the landfill during the restoration in 2005.<br />

13.3.57 A thin layer of Sands and Gravels underlie the Carse Clays, generally less than 3m in<br />

thickness.<br />

13.3.58 The Sands and Gravels are underlain by a layer of Boulder Clay (glacial till). However, this<br />

was only noted at some locations on the site to the west of the site adjacent to the River Forth<br />

and to the north of the main landfill site.<br />

Solid Geology<br />

13.3.59 According to the BGS digital data provided by emapsite, the bedrock beneath the site consists<br />

of Lower Coal Measures. North-east/south-west trending faults are present at the northwestern<br />

part of the site. The bedrock geology is presented in Figure 13.4.<br />

13.3.60 However, the coal measures are expected to comprise a repetitive sequence of sandstones,<br />

siltstones, mudstones and coal seams. The Passage Group sandstones underlie the coal<br />

measures at depth.<br />

13.3.61 No bedrock has been encountered in the previous intrusive investigations at the site.<br />

BGS Data<br />

13.3.62 Two borehole logs from the site were obtained from the BGS. The boreholes are located<br />

adjacent to the track to the north of the landfill and on the edge of the site near to the mouth of<br />

the Black Devon River.<br />

November 2010 Chapter 13 Page 16<br />

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

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