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RANGE IN CHARACTERISTICS: (from the mineral soil surface) <br />Soil moisture: dry throughout the moisture control section for 60 to 150 days in most years and are dry <br />throughout the entire soil for periods of 10 to 30 days each year during the period soil temperature at 20 <br />inches is above 41 degrees F. Ustic moisture regime. <br />Mean annual soil temperature ranges from 40 degrees to 46 degrees F. <br />Mean summer soil temperature ranges from 48 degrees F. to 58 degrees F. with an O horizon. <br />Thickness of the solum: 18 to 40 inches. <br />Depth to lithic contact: 20 to 40 inches. <br />Weak skeletons occur on surfaces of peds in parts of the Bt horizon in some pedons. <br />Content of organic carbon in the A horizon: 1 to 3 percent and decreases uniformly with depth. <br />Base saturation: 60 to 100 percent . <br />Coarse fragment content: 0 to 35 percent, mainly angular granite pebbles and cobbles. <br />The sand fraction contains lazge amounts of medium and coazse angular granite sand. <br />Packing patterns of sand grains within the matrix tend to be cubical with a significant proportion of flat <br />bearing surfaces between sand grains. <br />Horizons of low organic matter content have a greater than normal differential inconsistence between <br />moist and dry conditions and the soils are said to be "hard setting" when dry. <br />The E horizon: <br />Hue: 2.5Y through 7.SYR <br />Value: 6 or 7 dry, 4 through 6 moist, <br />Chroma: 2 through 4 <br />Reaction: slightly acid to slightly alkaline <br />This horizon is usually platy but is granular or subangular blocky in some pedons. <br />It is soft to slightly hard. <br />The Bt horizon: <br />Hue: 2.SY through 7.SYR <br />Value: 5 or 6 dry, 4 or 5 moist <br />Chroma: 2 through 6 <br />Texture:, sandy clay loam <br />Clay content: 18 to 35 percent <br />Silt content: 5 to 30 percent <br />Sand content: 45 to 70 percent with more than 35 percent fine sand or coazser and with a relatively high <br />percentage of medium and coarse angular granitic sand. <br />When air dry, this horizon is extremely hard and semi-cemented. <br />It has driented clay films in some portions. <br />Reaction: slightly acid to slightly alkaline. <br />Some pedons have sandy clay loam C horizons below depths of 19 inches. <br />COMPETING SERIES: These are the Alderon (WY), Baverton (WY), Belltower (MT), Elbeth (CO), <br />Elbuck (NM), Elmark (MT), Hauean (MT), Hovt (MT), Jemco (CO), Kunz (UT), Losindios (IVM), <br />Lump~u~h (MT), Northrim (CO), PlPlome (CO), Rule (CO), Shoemaker (NM), Sweetweed (MT), and <br />Tunitcha (NM) series. <br />Alderon, Belltower, Elmark, and Rule soils: 20 to 40 inches to paralithic contact. <br />Bayerton soils: have secondary carbonates at depths of 15 to 36 inches <br />Elbeth, Elbuck, Haugan, Hoyt, Kunz, Losindios, Northrim, Plome, Sweetweed and Tunitcha, soils: lack <br />a lithic contact at depths of less than 40 inches. <br />Jemco soils: are dry in Mav and June. <br />Lumpgulch soils: lack B/E horizons. <br />http://ortho.ftw.nres.usda.gov/osd/daUA/ALLENS_PARK.html 09/10/2003 <br />