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~~ ~ ~ <br />1$ I SOIL SURVEY <br />ately alkaline, and the underlying material is strongly <br />alkaline. The boot zone extends to a depth of more than <br />60 inches. Tliese soils are used for grazing. <br />Representative profile of Keyner• loamy sand, ill an <br />area of Arvada-Keyner association, in native grass, 500 <br />feet west alld 500 feet North of the southeast col•ller of <br />sec. 26, T. 19~ S., R. 62 W. <br />A2-0 to 5 inches, light brownish-gray (lOYR 6/2) loamy <br />fine sand, dark grayish brown (lOYR 4/2) when moist; <br />single grained; loose; nonsticky and nonplastic; moder- <br />ately alkaline; abrupt, smooth boundary. <br />B21t-5 to 9 inches, pale-brown (SOYR 6/3) sandy clay <br />loam, dark brown (lOYR 4/3) when moist; moderate, <br />medium, columnar structure; very hard, friable; slightly <br />sticky end plastic; thin, nearly continuous, clay films on <br />peds; calcareous; moderately alkaline; clear, smooth <br />boundary. <br />B22t-9 to 15 inches, pale-brown (lOYR 6/3) sandy clay <br />loam, brown (lOYR 5/3) when moist; moderate, medi- <br />um, prismatic structure; very hard, friable; slightly <br />sticky 'and plastic; thin, patchy, clay films on peds; <br />calcareous; strongly alkaline; clear, smooth boundary. <br />Clca-15 to 19 inches, very pale brown (IOYR 7/3) sandy <br />clay loam, brown (lOYR 5/3) when rtioist; moderate, <br />medium, prismatic structure; very hard, friable; slightly <br />sticky i and plastic; calcareous; common, large, soft <br />masses of bme; strongly alkaline; gradual, wavy <br />boundary. <br />C2ca-19 to 24 inches, light brownish-gray (2.SY 6/2) heavy <br />clay loam, dark grayish brown (2.5Y 4/2) and has <br />common, medium, strong-brown (7.5YR 5/6) mottles <br />when moist; weak, medium, subangular blocky struc- <br />ture; fiery hard, firm; sticky and very plastic; common, <br />large, soft masses of lime; strongly alkaline; gradual, <br />wavy boundary. <br />C3-24 to A4 inches, light-gra}• (2.5Y 7/2) sandy loam, <br />grayish brown (2.5Y 5/2) and has common, ~ small, <br />strong-brown (7.SY 5/6) mottles when moist; weak, <br />mediu`n, subangular blocky structure; slightly hard, <br />very friable; nonsticky and slightly plastic; calcareous; <br />strongly alkaline; gradual, wavy boundary. <br />C4-44 to 60 inches, very pale brown (lOYR 7/3) sandy <br />loam, brown (lOYR 5/3) and has a few, small, strong- <br />brown '(7.5Y 5/6) mottles when moist; single grained; <br />slightly hard, very friable; nonsticky and slightly plas- <br />tic; calcareous; strongly alkaline. <br />The A horizon is sandy loam to loamy sand as much as <br />9 inches thick. The B2t horizon is sandy clay loam to clay <br />loam 7 to 15 inches thick. The B21t horizon ranges from <br />moderately alkaline to strongly alkaline. The C horizon is <br />stratified and in places has layers of sand. In places there <br />is a Cg horizon between depths of 30 and 40 inches. <br />Ke-Keynes loamy sand, wet. This soil is mostly on <br />the flood plains of Chico Creek in the northeastern part <br />of Pueblo County. Tfle at•eas are rectangulal• in shape <br />and covel• as much as 1,000 acres. This soil has a profile <br />similar to the one described as representative of the <br />series, but the subsoil is thicker and the substratum is <br />stratified sandy loam and gl•avelly sand. Also, erosion <br />has removed the surface layer on about 5 percent of the <br />acreage, leaving barren slickspots. <br />Included ~a~ith this soil in mapping are areas of a <br />pom•ly drained clayey soil in narrow, winding swales <br />whel•e the µ~atel• table is at a depth of 18 inches. Also <br />included are areas of Glenberg and Havel•son soils near <br />drainageways and areas of Limon soils on ]ow benches. <br />These included soils make up about 25 percent of the <br />acreage. <br />Runoff is slow, and the hazard of erosion is moder- <br />ate. The soil is subject to occasional, brief flooding. <br />The water table is at a depth of 2 to 4 feet. There is a <br />moderate to ]iigh concentration of salts in the soil. <br />This soil has potential for waterfowl use if the habi- <br />tat can be improved. The native vegetation is mainly <br />alkali sacaton,inland saltgrass, greasewood, fourwing <br />saltbush, and cactus. Capability unit. VIw-1; Salt <br />Meadow range site.. <br />Kim Series <br />The Kim sel•ies consists of deep, well-dlailled soils. <br />These soils formed on alluvial fans in loamy alluvium. <br />The slope is 0 to 5 percent, and elevation is 4,600 to <br />5,000 feet. The average annual precipitation is 12 <br />inches. The average annual temperature is 53° F, and <br />the frost-free season is 145 to 175 days. The native <br />vegetation is mainly plains grasses. <br />In a representative profile the surface layer is light <br />bl•ownish-gray loam about 5 inches thick. The upper <br />part of the underlying material is pale brown loam <br />about 10 inches thick, the next part is vel•y pale blown <br />silt loam 20 inches thick, and the lower part is very <br />pale brown loam that extends to a depth of 60 inches <br />or more. <br />Pel•meability is moderate, and the available water <br />capacity is high. These soils are moderately alkaline. <br />Their 1•oot zone extends to a depth of 40 to 60 inches <br />or more. They are used fol• gl•azillg. <br />Representative profile of Kim loam, ill an al•ea of <br />Wiley-Kim looms, in grass, 0.35 mile not•th and 0.35 <br />mile east of the southwest corner of sec. 21, T. 26 S., <br />R. 60 W. <br />Al-0 to 5 inches, light brownish-gray (lOYR 6/2) loam, <br />dark grayish brown (lOYR 4/2) when moist; week, <br />medium, platy structure parting to moderate, fine <br />granular; slightly hard, very friable; nonsticky and <br />slightly plastic; calcareous; moderately alkaline; abrupt, <br />smooth boundary. <br />AC-5 to 15 inches, pale-brown (lOYR 6/3) loam, brown <br />(lOYR 5/3) when moist; weak, medium, prismatic struc- <br />ture parting to moderate, fine, subangular blocky; <br />slightly hard, very friable; nonsticky and slightly plas- <br />tic; calcareous; moderately alkaline; clear, wavy bound- <br />ary. <br />Clca-15 to 35 inches, very pale brown (lOYR 7/3) silt <br />loam, brown (lOYR 5/3) when moist; weak, medium, <br />prismatic structure parting to moderate, fine, angular <br />blocky; hard, very friable; nonsticky and slightly plas- <br />tic; calcareous; fine, generally rounded, soft masses of <br />lime; moderately alkaline; gradual, smooth boundary. <br />C2-35 to 52 inches, very pale brown (lOYR 8/4) loam, <br />yellowish brown (lOYR 6/4) when moist; weak, fine, <br />subangular blocky structure; slightly hard, very friable; <br />nonsticky and slightly plastic; calcareous; moderately <br />alkaline; clear, wavy boundary. <br />C3cs-52 to 60 inches, very pale brown (lOYR 8/4) loam, <br />light yellowish brown (lOYR 6/4) when moist; massive; <br />slightly hard, very friable; nonsticky and slightly plas- <br />tic; calcareous; scattered, fine crystalline gypsum; mod- <br />erately alkaline. <br />The A horizon is loam to sandy loam 3 to 6 inches thick. <br />Coarse fragments make up as much as 15 percent of the <br />soil, and they are commonly small sandstone fragments. The <br />AC horizon is loam to sandy loam 6 to 10 inches thick. The <br />C horizon ranges from loam to silt loam but is generally <br />loam. Depth to sandstone ranges from 40 inches to several <br />feet. In places calcareous cobbly gravel is below a depth <br />of 40 inches. <br />Kim soils in the Pueblo Area are mapped mostly with <br />Wile}- soils. <br />Km-Kim fine sandy loam. This nearly level soil is <br />on terraces along the south side of the Arkansas River. <br />B-4 <br />