110 SUIT. SURVEY
<br /> measurements made in many soil borings and on other A typical pedon of Albinas loam is located 72 feet west
<br /> observations during the soil mapping. The kind of bedrock and 240 feet south of the northeast corner of section 28,
<br /> and its hardness as related to ease of excavation are also T.12N., R.51W.
<br /> shown. Rippable bedrock can be excavated with a single- Ap—O to 6 inches, grayish brown (iOYR 5/2) loam, very' dark grayish
<br /> tooth ripping attachment on a 200-horsepower tractor, but brown (IOYR 3/2) moist; weak fine granular structure, slightly
<br /> hard bedrock generally requires blasting. hard, friable; neutral (pH 7.0); abrupt smooth boundary. (4 to s
<br /> Potential frost action refers to the likelihood of damage inches thick)
<br /> to pavements and other structures by frost heaving and B1-6 to 12 inches; dark grayish brown (IOYR -1/2) loam, very dark
<br /> low soil strength after thawing. Frost action results from grayish brown(IOYR 3/2)moist; weak medium prismatic parting to
<br /> the movement of soil moisture into the freezing tempera- moderate subangular blocky structure, hard, friable; very thin
<br /> patchy- clay films on faces of peds; neutral (pH 7 2); clear smooth
<br /> ture zone in the soil, which causes ice lenses to form. Soil boundary (3 to 6 inches thick)
<br /> texture, temperature, moisture content, porosity, permea- B21t--12 to 1S inches, grayish brown (IOYR 5/2) light clay loam, very
<br /> bility, and content of organic matter are the most impor- dark grayish brown (IOYR 312) moist, moderate medium prismatic
<br /> tant soil properties that affect frost action. It is assumed parting to moderate subangular blocky structure, hard,friable; thin
<br /> that the soil Is not covered by insulating vegetation Or patchy clay films on faces of peels; neutral (pH 7.2); clear smooth
<br /> boundarv.(6 to 10 inches thick)
<br /> snow and is not artificially drained. Silty and clayey soils B22t--I8 to 29 inches; grayish brown (iOYR 5/2) light clay loam, very
<br /> that have a high water table in winter are most suscepti- dark grayish brown (IOYR 3/2) moist; moderate medium prismatic
<br /> ble to frost action. Well drained very gravelly or sandy parting to moderate medium subangular blocky structure; hard, fri-
<br /> soils are the least susceptible. able; thin patchy clay films on faces of peds; neutral(pH 7.2); clear
<br /> smooth boundary (S to 1.1 inches thick)
<br /> B3ca--29 to 32 inches,gray(IOYR 6/1)loam,dark grayish brown(IOYR
<br /> 4/2)moist;moderate medium prismatic parting to moderate medium
<br /> Classification of the Soils
<br /> subangular blocky structure; hard,friable, thin patchy clay films on
<br /> ped faces,calcareous; mildly alkaline(pH 7.8);clear smooth bounda-
<br /> In this section, the soil series recognized in the survey ry.(3 to 5 inches thick)
<br /> area are described, the current system of classifying soils Clca-32 to 43 inches; light gray (IOYR 7/2) loam, light brownish gray
<br /> is defined, and the soils in the area are classified accord- (IOYR 6/2) moist; massive; hard. very friable; calcareous with thin
<br /> ing to the current system. lime seams and streaks, moderately alkaline (pH 8.2); gradual
<br /> smooth boundary.(9 to 14 inches thick)
<br /> C2 -43 to 52 inches, light brownish gray GOYR 6/2) very fine sandy
<br /> Soil Series and Morphology loam, brown (10YR 5/3) moist, massive; slightly hard, very friable;
<br /> calcareous, mildly alkaline(pH 7.8); clear smooth boundary.(9 to 17
<br /> In this section, each soil series recognized in the survey inches thick)
<br /> area is described in detail. The descriptions are arranged I10-52 to 60 inches;yellowish brown(IOYR 5/4)gravelly coarse sand,
<br /> in alphabetic order by series name. brown QOYR 5/2) moist; single grained, loose, dry and moist; cal-
<br /> Characteristics of the soil and the material in which it careous;mildly alkaline(pH 7.6).
<br /> formed are discussed for each series. The soil is then Thickness of the mollic epipedon ranges from 20 to 40 inches. Depth
<br /> compared to similar soils and to nearby soils of other se- to horizons of calcium carbonate accumulations is 20 to 30 inches. Con-
<br /> ries. Then a pedon, a small three-dimensional area of soil trasting C horizons are common below depths of 40 inches.
<br /> The A horizon has color value of 4 or 5 dry, 2 or 3 moist and chroma
<br /> typical of the soil series in the survey area, is described. of 2 or 3. It is a loam or fine sandy loam.Texture of the B2t horizon is
<br /> The detailed descriptions of each soil horizon follow stan- loam,clay loam or sandy clay loam.Texture of the C horizon is a loam,
<br /> dards in the Soil Survey Manual (4). Unless otherwise silt loam or fine sandy loam.
<br /> noted, colors described are for moist soil.
<br /> Following the pedon description is the range of impor- Aida Series
<br /> tant characteristics of the soil series in this survey area. The Aida series consists of deep, somewhat poorly
<br /> Phases, or mapping units, of each soil series are described drained soils that formed in calcareous, stratified alluvium
<br /> in the section "Soil Maps for Detailed Planning." underlain by a mixture of sand and gravel. Aida soils are
<br /> on low terraces and bottomlands and have slopes of 0 to 1
<br /> Albinas Series percent. Average annual precipitation ranges from 13 to
<br /> The Albinas series consists of deep, well drained soils 19 inches and the mean annual temperature is about 49
<br /> that formed in calcareous alluvial materials. Albinas soils degrees F.
<br /> are on upland flood plains and alluvial fans and in Aida soils are similar to the Loveland soils. They are
<br /> drainageways and have slopes of 0 to 3 percent. Average near the Loveland, Hayford and Westplain soils. Loveland
<br /> annual precipitation ranges from 13 to 19 inches and soils have loam and light clay loam underlying layers.
<br /> mean annual temperature is about 48 degrees F. Hayford soils have heavy clay loam or clay 132t horizons.
<br /> Albinas soils are similar to the Satanta and Haxtun Westplain soils have sand and gravel at depths less than
<br /> soils. They are near the Satanta, Rago, Kuma, and Keith 20 inches.
<br /> soils. Satanta and Keith soils have dark colored surface A typical pedon of Alda loam is located 690 feet west
<br /> layers extending to less than 20 inches. Haxtun, Rago and and 500 feet north of the SE corner of section 33, TAON.,
<br /> Kuma soils have buried sola within 40 inches. R.50W.
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