NOT PROTECTIVELY MARKED SUB-APPENDIX A2: SOIL ANALYTICAL SUITES

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SUB-APPENDIX A2: SOIL ANALYTICAL SUITES

A2.1.1 There will be three soil analytical suites summarised in Table 3 in the text. Details of the analyses to be carried out in each suite and the methodologies to be used are provided here. a) Soil Analytical Suite 1: Characterisation of in situ Soil Conditions Ahead of Site Preparation Works A2.1.2 Soil determinations to be carried out before the start of ground preparation works, to provide a robust baseline of in situ soil conditions against which to compare restoration soil conditions at each AD site, are as follows: soil texture % sand, silt and clay (using methodology in BSI, 1990a). (Ref. 1) as well as a crude determination of % w/w organic matter content. soil ph (methodology in MAFF, 1968) (Ref. 2). total P, K and Mg (using the methodology in MAFF, 1968) (Ref. 2). soil bulk density both topsoil and subsoil measured using both hand-held cone penetrometer and via sampled soil cores, subsequently analysed in the laboratory. The method to be used will be that described in BSI (1990a) (Ref 1). soil moisture content at plastic limits determined using the methodology described in BSI (1990a) (Ref. 1). percentage stoniness by volume. The method to be used will be that described in BSI (1990a) (Ref. 1); and aggregate stability testing. The method to be used will be that described in Black et al. (1965) (Ref. 3). A2.1.3 The determination of soil texture will use the methodology described in BSI (1990a) BS 1377-2 Methods of test for soils for civil engineering purposes. Classification Tests (Ref. 12). b) Soil Analytical Suite 2 Soil testing of soils in stockpiles ahead of restoration activities A2.1.4 A2.1.5 The following suite of in situ and laboratory analyses will be carried out on soils sampled from stockpiles immediately before, but not more than four weeks ahead of, restoration activities. In situ determinations: compaction/density, using a hand-held penetrometer (to determine whether in-situ treatment is required (such as ripping or harrowing) to alleviate soil compaction; soil moisture content (%) to determine whether in-situ treatment is required to assist soil drying; soil structure using simple hand excavation technique and wet sieving. Type and strength of peds will be recorded; and odour (qualitative) indication of anaerobism to determine if in situ treatment is required to assist aeration during restoration.

A2.1.6 Laboratory analyses: ph (determined in both distilled water and CaCl 2 ); organic Matter content (%) determined using both LOI and Walkley Black (some soils are derived from limestone and LOI is inaccurate in such soils); conductivity; total P, K and Mg (for all soils to be reinstated/restored for agricultural purposes). This will permit calculation of fertility indices to allow calculation of required fertilizer application rates for proposed cropping end uses; aggregate stability (wet sieving method); and assessment of topsoil stoniness (%) to ensure that contamination with stony phase has not occurred A2.1.7 Soils stockpiled appropriately for restoration purposes are considered, as a result of the pre-development Site Investigation results, to be uncontaminated and hence no further contaminant analyses will be carried out at the site restoration phase. c) Soil Analytical Suite 3 in situ soil in restoration compartments after works are completed A2.1.8 The analyses to be carried out in all reinstated or restored areas of land will be those described as follows; ph (determined in both distilled water and CaCl2); organic Matter content (%) determined using both LOI and Walkley Black (some soils are derived from limestone and LOI is inaccurate in such soils); conductivity; total P, K and Mg (for all soils to be reinstated/restored for agricultural purposes). This will permit calculation of fertility indices to allow calculation of required fertilizer application rates for proposed cropping end uses; 2M KCl-extractable inorganic N (NH4-N and NO3-N). These will give an indication of plant (crop)-available inorganic N; aggregate stability (wet sieving method); in situ bulk density (by taking 5cm diameter x 10cm cylindrical auger cores in the field at 10cm intervals horizontally down each excavated soil profile through the stockpile); and assessment of topsoil stoniness (%) to ensure that contamination with stony phase has not occurred.

References 1 British Standards Institute (BSI) (1990a) BS 1377-2 Methods of Test for Soils for Civil Engineering Purposes. Classification Tests. 2 MAFF (1968) The Analysis of Agricultural Materials by Hislop J and Cooke IJ. Booklet RB427. 3 Black, C.A. (Ed) et al. (1965) Methods of Soil Analysis. Part 1: Physical and Mineralogical Properties. No 9 in the series Agronomy, pp 511-519. America Society of Agronomy Inc., Madison, Wisconsin, USA.