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GSM's concern that Bench 1 material may not be a suitable substitute for Lift B material seems to be <br />primarily based on the EC and rock content of this material. Bench 1 material was sampled in TP06, <br />TP07 and TP08 in the Substitute Subsoil Redistribution Area at three different depths. The suitability <br />criteria for Bench 1 material is very similar to the Lift B material. According to Map 2.05.4 -6 Morgan <br />Property Topsoil Replacement Plan as of June 2010, Bench 1 material has been used as subsoil in Zone 1 <br />on the eastern portion of the property. TP06, TP07 and TP08 are located in Zone 1. Based on the data, <br />the Bench 1 material was within the threshold limits for all of the parameters. The EC threshold for <br />Bench 1 material in Zone 1 is 6mmho /cm, the EC found in these test pits were 4.4, 5.0 and 4.3 mmho /cm. <br />Rock fragments measured in the Bench 1 material was well below the threshold level for Lift B and <br />Bench 1 material. If the EC threshold was lowered to 4mmho /cm, similar to item #2 above, it is likely the <br />soils could be managed to account for the excess salt content of the soil. <br />4.) OSM's review has determined that the practice of significantly mixing C horizon material of <br />inadequately proven quality with prime B horizon soils for creating the B lift substrate for prime <br />farmland reclamation contravenes the requirements at 2.06.6(2)(d), 2.06(4)(c), 4.06.2(3), 4.25.3(2), <br />4.25.4(4). <br />Overall this issue is similar to item #1 above; it does not appear the stockpiles material was significantly <br />contaminated with C horizon material. Apossible exception to this is the elevated levels of Electrical <br />Conductivity (EC) within the stockpiles. The stockpile data would indicate the EC levels in the stockpiles <br />is higher on average than in the undisturbed area. The average EC found in the horizons of the <br />undisturbed areas (including lower B and Upper C horizons) in TPO1 -TP05 yielded EC values of 4.22, <br />1.92, 1.32, 2.36 and 4.16 mmho /cm for each of the test pits. Sample Pile's A, B, C, D, and E yielded an <br />average EC of 3.68, 3.71, 4.10, 4.21 and 3.46mmho /cm respectively. Based on the 1998 IRI soil survey <br />samples and the 2011 samples from the undisturbed area on the Morgan property, it does not appear EC <br />levels were as high as the level's found in the soil stockpiles even within the lower B and C horizons. <br />Given this, it is unlikely the C horizon significantly affected the EC of the lift B material. Based on the <br />analysis of Sample Pile B, this lift B material does meet the suitability criteria approved in the permit. <br />Given the parameters required for a soil to classify land as prime farmland as discussed above, depending <br />on the rooting zone of the plants to be established on the site and the depth of the lift B material to be <br />placed, it may be necessary to revise the threshold for Lift B material to 4mmho /cm. If the EC threshold <br />level was decreased to 4mmho /cm, only a portion of Lift B material would be outside of the acceptable <br />limit. The overall EC average for the lift B material was measured to be less 4mmhos /cm, but any excess <br />salts could be managed during reclamation and future farming practices. <br />The question becomes, what would cause the EC values to be different on average between the <br />undisturbed material and the stockpiled material? Electrical conductivity in soils is a function of <br />precipitation, evapotranspiration, irrigation techniques, irrigation water quality and the properties of the <br />soil material. The EC levels vary inconsistently throughout the soil profiles of the undisturbed land that <br />the elevated EC levels of the soil stockpiles cannot be tied conclusively to the mixing of C horizon <br />material with other horizons. Perhaps the function of stockpiling this material exposes the soil to an <br />increased amount of evaporation leaving an increased amount of minerals in the soil increasing the EC <br />level. Spraying water on the stockpiles with even low salinity could result in salt accumulation within <br />soil stockpiles according to research (Page 25, Guidelines for Mining in Arid Environments; Department <br />of Minerals and Energy; Western Australia, 1996). It is unclear what would cause the EC values to be <br />different on average between the undisturbed material and the stockpiled material. <br />5.) Instead of receiving the balance of the B horizon soils salvaged from Zone 4, which had been <br />previously identified as prime soils by the NRCS, as a substitute Zone 4 is to receive a mixed (50150) <br />layer of C and B horizon materials as the B lift for reclamation. As per OSM's review of the <br />permit, this substitution was approved by DRMS without demonstration that the substitute has <br />Page 7 of 10 <br />