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SSS 3 ,3. 3.3 3.4,3.5,3.6. Applications on microfiche file with the EHD reveal that there 1) <br /> have been seven permits issued for repairs/replacements/additions to existing systems on Foppiano C3•Z 33) <br /> Lane. This can be considered a high number of permits. As referenced, the Morada area has <br /> always had a significantly high number of repair/replacement permits due to the clayey soil, and �33•�� <br /> may also be due to inadequate systems originally installed. <Ol79ti/ Z�tq <br /> The project site has relatively level terrain; consequently, there will be no need to incorporate <br /> design considerations for slopes within the disposal area. <br /> B. SOIL PHYSICAL CHARACTERISTICS AND ANALYTICAL TEST RESULTS <br /> The United States Department of Agriculture- Soil Conservation Service (USDA-SCS) indicates <br /> CI ti I the on-site soils to consist of Jacktone clay(#180). As noted from the perc test results,this clay <br /> I soil type possesses slow permeability. <br /> SSS§ 5.2. The surface and subsurface soil investigation and testing began on June 9, 2012 with <br /> the drilling of the test borings using a B-24 Mobile Drill Rig and solid stem auger. Soil samples <br /> for chemical analyses from the 42 inch depth representative of the future leachline trenches and the <br /> 24.75 ft depth representative of the future seepage pit were retrieved from the soil cuttings. <br /> NLS§ 1.1,1.2. As the noted on the A&L Laboratory Soil Analysis Reports, the chemical analyses <br /> of the two soil samples quantify several constituents that influence nitrate loading from this <br /> project. The important parameters for nitrate loading assessment are the organic matter,pH, cation <br /> exchange capacity(CEC), clay content, along with nitrate-nitrogen content of the soil. <br /> As noted, the organic matter in the surface soils is low and actually more than doubles at the 24 ft <br /> depth. A low surface soil organic matter may be attributable to the fact the property has not been <br /> farmed in many years. The deeper organic matter occurred millennia ago. Organic matter is <br /> / needed for denitrification and could be a reason for decreased nitrate concentrations in the <br /> groundwater in this area. <br /> The nitrate-nitrogen concentration is 8 ppm at 42", but almost doubles in concentration at the 24 ft <br /> depth to 15 ppm. This increase in nitrate-nitrogen concentration suggests mobility of nitrate, but <br /> �.� this concentration apparently could be significantly higher if not for the clay soils and organic <br /> matter. <br /> Because septic effluent is composed predominately of ammonium (NH4),the pH, along with the <br /> CEC, are significant influences on ammonium molecules. The pH of the soil is very slightly <br /> alkaline which may have little effect on ammonium formation and stability. The CEC measures <br /> the ability of the soil to theoretically trap and hold ammonium molecules. Cation Exchange <br /> J Capacities of the soil samples are high due to the high clay content. This means there is a large <br /> potential for the retention of ammonium molecules for microbial uptake, and denitrification <br /> potential. <br /> 3 <br />