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<br />fi4 <br />- <br />SOIL SURVEY <br />TABLE 5. Estimated engineering <br /> <br /> <br />Soil aeries and Depth to <br />seasons] <br />high <br />Depth <br />from <br /> <br />USDA texture Classification Coarse <br />fraction <br />greater <br />map eymbob water surface than 3 <br /> table inches <br /> Unified AASHTO <br /> Fw lnda P~m.t <br />Stroupe: StE________________ >6 0-9 Stony loam, very stony loam____ SM, ML A~ 45-70 <br /> 9-25 Stony clay, very stony clay, GC A-6, A-7, A-2 30-50 <br /> very stony clay loam. <br /> 25 Unweathered bedrock. <br />Table Mountain: TM________ >6 0-7 Loam,fineaandyloam,clay CL-ML,CL, A-4 0 <br /> loam. SC-SM, SC <br /> 7~0 Loam, silt loam, silty clay loam_ CL-ML, CL A~ 0 <br />Tnaveadlla: ToO,TrG_______ >6 0-14 Sandylogm,gravel~yeandy SM,SC~M A-2 0-25 <br />Rock outcrop part o[ TrG loam. <br />is too variable to eati- 16 Unweathered bedrock. <br />mate. <br />Valenta Va_________________ >6 0-4 Fine sand, loamy eand_________ SM, SC-SM A-2 0 <br /> d-60 Fine sand, eand_______________ SP-SM,SM A-2,A~ 0 <br />Vamer: VmE_______________ >6 0-12 Veryetonylaam,verystony GC A-6 30-60 <br />Rock outcrop part is too clay loam. <br />variable to estimate. 12 Unweathered bedrock. <br />Vona: <br />Vo________________________ >6 0-8 Sandy loam___________________ SM, SC-SM A-2, A~ 0 <br /> 8-90 Fine Bandy loam, sandy loam_ _ _ SM, SC-SM A-2, A-4 0 <br /> 30-60 Sandy loam, loamy fine eand____ SM A-2 0 <br />Vn Va2___________________ >6 0-8 Loamy fine sand, loamy eand___ SM A-2 0 <br />k`'or Otero part of Vat, 8-30 Fine sandy loam, Bandy loam___ SM, SC-SM A-2, A~1 0 <br />see Otero series. 30-60 Sandy loam, loamy fine eand____ SM A-2 0 <br />Wetmore: WE______________ >6 0-12 Gravelly coarse sandyloam_____ SC-SM,SC A-2 5-20 <br />For Mortensen part, see 12-18 Gravelly coarse sandy loam, SC, GC A-2 5~0 <br />Mortensen aeries aandy clay loam <br /> 18 Unweathered bedrock. <br />Wiley: Wk_________________ >6 0-6 <br />6 Silt loam, loam________________ <br />l <br />l <br />Sil <br />il <br />l CL-ML,CL <br />'CL A~,A-6 <br />A <br />6 0 <br />0 <br />For Kim part, see Kim fr1 ty c <br />ay <br />oam, s <br />t <br />oam_______ - <br />aeries. 15-50 Silt loam, silty clay loam, loam__ CL-ML, CL A-4, A-6 0 <br /> 60-60 Weathered shale and sandstone. <br />Wormser: Wo_______________ >6 0~ Silt loam_____________________ ML, CL-ML A-4 0 <br /> 4-33 Clay loam, clay, silty clay loam_ CL A-6, A-7 0 <br /> 93 Unweathered bedrock. <br />Depth to bedrock is the distance from the surface <br />of the soil to the rock layer (fig. ?). <br />Depth to seasonal high water table is the distance <br />from the surface of the soil to the highest level that <br />ground water reaches in the soil in most years. <br />Soil texture is described in table 6 in the standard <br />terms used by the Department of Agriculture. These <br />terms take into account the relative percentages of <br />sand, silt, and clay in soil material that is less than 2 <br />millimeters in diameter. "Loam," for example, is soil <br />material that is 7 to 27 percent clay, 28 to 60 percent <br />silt, and less than 62 percent sand. If the soil contains <br />gravel or other particles coal•ser than sand, an ap- <br />propriate modifier is added, far example, "gravelly <br />loamy sand." "Sand," "silt," "clay," and some of the <br />other terms used are defined in the Glossary of this <br />soil survey. <br />Permeability is that quality of a soil that enables it <br />to transmit water or air. It is estimated on the basis <br />of those soil characteristics observed in the field, <br />particularly structure and texture. The estimates in <br />table 5 do not take into account lateral seepage or such <br />transient soil features as plowpans and surface crusts. <br />Available water capacity is the ability of soils to <br />hold water for use by most plants. It is commonly de- <br />fined as the difference between the amount of water <br />in the soil at field capacity and the amount at the wilt- <br />ing point of most crop plants. <br />Reaction is the degree of acidity or alkalinity of a <br />soil, expressed as a pH value. The pH value and terms <br />used to describe soil reaction are explained in the <br />Glossary. <br />Salinity refers to the amount of soluble salts in the <br />soil. It is expressed as the electrical conductivity of the <br />