Official Series llescnpnon -1vuNrv genes
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<br />degrees F, and mean summer temperature is 59 to 79 degrees F. The mollic epipedon is 7 to 19 inches
<br />thick, depth to lime is 10 to 30 inches, and the solum is 16 to 46 inches thick. Organic carbon in the
<br />mollic epipedon ranges from .8 to 3 percent. The soil is typically 90 to 100 percent base-saturated. Rock
<br />fragments aze typically less than 5 percent and range from 0 to 15 percent. The soil temperature at depth
<br />of 20 inches is 41 degrees F or warmer for about 200 to 240 days. The soils are moist in some part of the
<br />.:.oisture control section for about 56 to 152 days while the soil temperature is 41 degees F or above.
<br />The A horizon has hue of SY to 7.SYR, value of 4 or 5, 2 or 3 moist, and chroma of t to 3. Usually it
<br />has granular or crumb structure but the structure is subangulaz blocky in some pedons. This horizon is
<br />soft or slightly hard. It is slightly acid to slightly alkaline.
<br />The Bt horizon has hue of SY to 7.SYR, value of 3 to 7, 2 to 6 moist, and chroma of 2 to 5. It is typically
<br />clay, silty clay loam or clay loam and has 35 to 50 percent clay, 15 to 45 percent silt, and 15 to 45
<br />percent sand with more than 15 percent, being fine sand or coarser. Some pedons have sandy clay loam
<br />textures in the lower parts of the azgillic layer, however, the weighted clay average is greater than 35
<br />percent in the control section, It is slightly acid to moderately alkaline. CEC of the Bt horizon ranges
<br />from 60 to 90 millequivalents per 100 grams of clay.
<br />The Bk or C horizon has hue of SY to 7.SYR, value of 5 to 7, 4 to 6 moist, and chroma of 2 to 4. They
<br />aze typically clay loam with more than 28 percent clay, however, where the C horizon has less than 28
<br />percent clay it contains more than 15 percent fine or coarser sand and has a texture of sandy clay loam,
<br />loam or sandy loam. These horizons are slightly alkaline to strongly alkaline and have 4 to 15 percent
<br />calcium carbonate equivalent.
<br />COMPETING SERIES: These are Ashfork, Bethune, Blackoioe, Boneek, Boquillas, Cha in, Collbran,
<br />Collide, Emigrant, Hueains, Kube, Laden, Loma, Nuncho, uerq Rednun, Richfield, Rvus, Savo,
<br />Showlow, Standlev, Thunderbird, Weld and Wormser series. Ashfork, Bethune, Chapin, Thunderbird
<br />and Wormser soils have lithic contact at depths of 20 to 40 inches. Blackpipe, Boquillas, Emigrant,
<br />Huggins, Leyden and Querc soils have paralithic contact at depths of 20 to 40 inches. Boneek, Kube,
<br />Richfield, Savo and Weld soils have less than 15 percent fine sand or coarser in the Bt horizon.
<br />Collbran, Collide, Loma and Rednun soils have hues redder than 7.SYR in the Bt. Ryus soils are
<br />calcareous throughout. Showlow soils have a calcic horizon. Standley soils have greater than 15 percent
<br />coarse fragments in the Bt horizon. The Nuncho soils have soil temperatures at 20 inches that are greater
<br />than 41 degrees F. for less than 200 days.
<br />GEOGRAPHIC SETTING: The Nunn soils are on terraces or alluvial fans, or in drainageways. Slope
<br />gradients range from 0 to 25 percent. The soils formed in mixed alluvium. At the type location the
<br />average annual precipitation is 13 inches, 9 inches of which falls during the months of April through
<br />September. Mean annual air temperature is 47 to 53 degrees F, and an average summer temperature is
<br />67 degrees F. The frost-free period is 120 to 210 days.
<br />GEOGRAPHICALLY ASSOCIATED SOII,S: These are the competing Weld soils and the Fort
<br />Collins, Platner and Satanta soils. Fort Collins and Satanta soils have less than 35 percent clay in the Bt
<br />horizon. Platner soils have an abrupt textural boundary between the A and B horizons.
<br />DRAINAGE AND PERMEABILTI'Y: Well drained; negligible to very high runoff depending on
<br />slope; moderately slow or slow permeability. Some small areas are seasonally wet due to seepage from
<br />imgation.
<br />USE AND VEGETATION: A large percentage of the Nunn soils aze now under irrigation where they
<br />http://ortho.ftw.nres.usda.gov/cgi-bin/osd/osdname.cgi?-P 4/29/2004
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