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<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
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