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F. Geology & Hydrology ( PDF | 31.0 MB ) - RWE.com

F. Geology & Hydrology ( PDF | 31.0 MB ) - RWE.com

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soil association, including the <strong>com</strong>prising soil series characteristics. The full<br />

NSRI Site Soil Report can be viewed in Annex D3 of the ES.<br />

Table 3.1 Soil Association Characteristics<br />

Hafren Brickfield 1 Wilcocks 2<br />

Description Loamy permeable upland<br />

soils over rock, with a<br />

wet peaty surface horizon<br />

and bleached subsurface<br />

horizon, often with thin<br />

ironpan. May include<br />

some peat on higher<br />

ground. Rock and scree<br />

locally.<br />

Comprising<br />

Soil Series<br />

Soil parent<br />

material<br />

Hafren (45%) – loamy<br />

material of lithoskeletal<br />

mudstone and sandstone<br />

or slate.<br />

Hiraethog (20%) – loamy<br />

material over lithoskeletal<br />

mudstone and sandstone<br />

or slate.<br />

Wilcocks (10%) – loamy<br />

drift with siliceous<br />

stones.<br />

Other (25%) – other<br />

minor soils.<br />

Palaeozoic slaty<br />

mudstone and siltstone.<br />

Source: National Soil Resources Institute (2009)<br />

Slowly permeable<br />

seasonally waterlogged<br />

fine loamy and fine silty<br />

soils, some with wet<br />

peaty surface horizons.<br />

Brickfield (30%) –<br />

medium loamy drift with<br />

siliceous stones.<br />

Wilcocks (25%) – loamy<br />

drift with siliceous<br />

stones.<br />

Greyland (10%) –<br />

medium loamy over<br />

clayey drift with siliceous<br />

stones.<br />

Cegin (10%) – medium<br />

silty drift with siliceous<br />

stones.<br />

Other (20%) – other<br />

minor soils.<br />

Drift from Palaeozoic<br />

slaty mudstone and<br />

siltstone.<br />

Slowly permeable,<br />

seasonally waterlogged<br />

loamy upland soils with a<br />

peaty surface horizon.<br />

Some very acid peat soils.<br />

Wilcocks (50%) – loamy<br />

drift with siliceous<br />

stones.<br />

Crowdy (15%) – humified<br />

peat, up to 1m in<br />

thickness.<br />

Winter Hill (15%) –<br />

mixed eriophorum and<br />

sphagnum peat, up to<br />

1.2m in thickness.<br />

Hafren (10%) - loamy<br />

material of lithoskeletal<br />

mudstone and sandstone<br />

or slate.<br />

Other (10%) – other<br />

minor soils.<br />

Drift from Palaeozoic<br />

sandstone, mudstone and<br />

shale.<br />

Figures 3.1 to 3.3 below show the profiles of the <strong>com</strong>ponent soil series for each<br />

of the above soil associations. Figures 3.1 and 3.2 show that the soil series<br />

<strong>com</strong>prising the Hafren and Brickfield 1 soil associations are characterised by<br />

shallow (10cm to 20cm) surface peaty horizons, beneath which are layers of<br />

clay or sandy silt loam. Figure 3.3 shows that two of the Wilcocks 2<br />

<strong>com</strong>prising soil series (Wilcocks and Hafren) are also characterised by shallow<br />

(10cm to 20cm) surface peaty horizons, again with clay loam or sandy clay<br />

loam horizons beneath. The Crowdy and Winter Hill horizons, however, are<br />

characterised by deep peat horizons, 100cm to 120cm thick. The Crowdy soil<br />

series <strong>com</strong>prises dark brown or black stoneless, humified peat with a massive<br />

structure. The Winter Hill soil series <strong>com</strong>prises dark reddish brown or dark<br />

reddish grey semi-fibrous, Eriophorum-Sphagnum peat, with a moderate to<br />

weak coarse platy structure in the top 70cm and a massive structure in the<br />

ENVIRONMENTAL RESOURCES MANAGEMENT <strong>RWE</strong> NPOWER RENEWABLES LTD<br />

7

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