PERMFILE100364

• Permit No: M1985203
• IBM Index Class Name: Permit File
• Doc Date: 12/3/1985
• Doc Name: 110 Permit Application
• Section_Exhibit Name: Index
• Media Type: D
• Archive: No

64
SOIL SURVEY
TABLE 5. Estimated engineering
Depth to Classi cation Coarse
seasonal Depth fraction
Soil series and high from USDA texture greater
map symbols water surface than 3
table inches
Unified AASHTO
r.rr r~~e., rrrrem
Stroupe: StE________________ >6 0-0 Stony loam, very stony loam__._ SM, ML A-4 45-70
9-25 Stony clay, very stony clay, GC A-6, A-7, A-2 30-50
very stony clay loam.
25 Unweathered bedrock.
Table 5fountain: TM__._..._ >6 0-7 Loam, fine sandy loam, clay GL-hf L, CL, A-4 0
loam. SC-F M, SC
7-60 Loam, silt loam, silty clay loam_ CL-SS L, CL A-4 0
• Travessilla: ToD, TrG...._.. >6 0-14 Sandy loam, gravelly sandy Sbf, SC-SM A-? 0-'L5
Rock outcrop par[ of TrG loam.
is too variable to esti- 14 Unweathered bedrock.
mate.
Yalent: Va ... .............. >6 0-4 Fine sand, loamy sand_____-_.. SM, SC-SM A-^ 0
4-60 Fine sand, sand______________ SP-SM,SM A-2, A-3 0
Vumer: VmE _ _ _ _ _ _ _ _ _ _ _ _ _ > 6 0-12 Very stony loam, very stony GC A-6 30-60
Ruck outcrop part is too clay loam.
vuriable to estimate. 12 Unweathered bedrock.
Vona:
Vo ........................ 76 0-8 Sandy loam_____________.._ SM, SC-SM A-2, A-1 0
8-:10 Fine sandy loam, sandy loam___ SM, SC-SM A-2, A-3 0
30-60 Sandy loam, loamy fine sand.__- SM A-2 0
Vn, Vs2___________________ >6 0-8 Loamy fine sand, loamy sand-_. SM A-2 0
Fur Otero part of Vs2, 8-30 Fine sandy loam, sandy loam_ _ _ SM, SC-SM A-2, A-4 0
see Otero series. 30-60 Sandy loam, loamy fine sand_.. _ Sbl A-'3 0
Wetmore: WE______________ >6 0-1.3 Gravelly coarse sandy loam____. SC-SM, SC A-2 5-20
For Mortenson part, see 1'?-18 Gravelly coarse sandy loam, SC, GC A-'? 5-40
Mortenson series. sandy clay loam.
18 Unweathered bedrock.
Wiley: Wk_________________ >6 0-6 Silt loam, loam__________....__ CL-tit L, CL A-4, A-6 0
For Kim part, see Kim 6-15 Silty clay loam, silt loam..... _ _ CL A-6 0
series. 15-50 Silt loam, silty clay loam, loam_ CL-ML, CL A-4, A-6 0
50-60 Wen[hered shale and s;mds[one.
Wunnser: Wo_________ __ __ >6 0-4 Silt loom. _.._____ .._ AI L, CL A1L A-•1 0
4-33 Clay loam, clay, silty clay loam_ CL A-6, A-7 0
33 Unweathered bedrock.
Depth to bedrock is the distance from the surface
• of Che ,oil to the rock layer (ti y;. 7).
Depth to seasonal high water table is the distance
from the surface of the soil to the highs,[ level that
ground ++•ater reaches in the soil in most }ears.
Soil texture is described in table 5 in the standard
terms used by the Department of Agriculture. These
terms take into account the relative percentages of
sand, silt, and clay in soil material that is less than 2
millimeters in diameter. "Loam," for example, is soil
material that is 7 to 27 percent clay, 28 to 50 percent
silt, and less than 52 pet•cent sand. If the soil contains
gt•avel or other particles coarser than sand, an ap-
propriate modifier is added, for example, "gravelly
loamy sand." "Sand," "silt," "clay," and some of the
other terms used are defined in the Glossary of this
soil survey.
Permeability is that quality
tri lrunsniit water cir air. IL i>
of tho..e ;nil ch.u•~irtcristics
partii•ularly atru+~ture and te:
table 5 do not take into accoun
transient .oil features as plow
available water capacity is
hold water for use by most pl;
fined as the difference betvvee
in the soil at field capacity and
ing point of most crop plants.
Reaction is the degree of at
soil, expressed as a pH value. '
rued to describe soil t•eactiot
Glossary.
Salinity refers to the amour
soil. It is expressed as the elect
of a soil that enable; it
cstinutlcrl un the basis
observed in the field,
tore. The estimates in
lateral seepage or such
.ass and surface crusts.
the ability of soils to
nts. It is commonly de-
i the amount of water
the amount at the wilt-
dity or alkalinity of :i
he pH value and term.;
are explained in the:
of soluble salting in the
cal conductivity of thr