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2005-06-02_REVISION - M1980193
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2005-06-02_REVISION - M1980193
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Entry Properties
Last modified
6/15/2021 2:43:12 PM
Creation date
11/22/2007 12:49:10 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1980193
IBM Index Class Name
Revision
Doc Date
6/2/2005
Doc Name
sokol pit
From
dmg
To
Rocky Mountain Materials
Type & Sequence
AM1
Media Type
D
Archive
No
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Site Type: Rangeland Sandy <br />MLRA: 69 -Upper Arkansas Valley Rolling Plains R069XY026CO <br />Representative Soil Features <br />The soils of this site are very deep but also include moderately deep and deep soils. Typically, they <br />are somewhat excessively drained to well drained and have moderately rapid, moderate or <br />moderately slow permeability. Typically, these sails formed in alluvium and eolian deposits derived <br />from mixed sources. They occur on plains, fans, and terraces. The available water capacity is <br />typically high for the deep and very deep soils and low to moderate for the moderately deep soils. <br />The soil surface layer ranges from 3 to 16 inches thick and is typically sandy loam or very fine sandy <br />loam. The subsoil is typically sandy clay loam, but includes sandy loam or clay loam. The pH ranges <br />from neutral to moderately alkaline in the surface and subsoil, and slightly alkaline to strongly alkaline <br />in the substratum. The soil moisture regime is typically ustic aridic, but ranges to aridic in the driest <br />areas of MLRA 69. The soil temperature regime is mesic. <br />The Historic Climax Plant Community (HCPC) should portray slight to no evidence of rills. Water flow <br />paths, if present, are broken, irregular in appearance or discontinuous with numerous debris dams or <br />vegetative barriers. Wind scoured areas and pedestaled plants may exist in areas but should be <br />minor. The soil surface is stable and intact. Sub-surface soil layers are non-restrictive to water <br />movement and root penetration. <br />Major soil series correlated to this ecological site include: <br />Ascalon, Ascalon dry, Bresser, Fort, Fort Collins, Nelson, Olney, Otero, Oterodry, Satanta, Stoneham, <br />Sundance, Truckton dry, Vona, and Vonid. <br />Soils that will be correlated to other MLRA's when outdated soil surveys are updated are: <br />Ascalon, Bresser, Fort Collins, Otero, and Vona. These soils have and aridic ustic moisture regime. <br />Other soil series that have been correlated to this site include: none <br />Parent Material Kind: eolian deposits and alluvium <br />Parent Material Origin: mixed sedimentary <br />Surface Texture: sandy loam, fine sandy Icam, loamy sand, loamy fine sand <br />Surface Texture Modifier: none, but includes gravelly <br />Subsurface Texture Group: sandy loam, fine sandy loam, sandy clay loam, clay loam <br />Surface Fragments < 3" (% Cover): 0 to 35 percent <br />Surface Fragments > 3" (%Cover): 0 to 15 percent <br />Subsurface Fragments < 3" (% Volume): 0 to 35 percent above 40 inches <br />Subsurface Fragments > 3" (% Volume): 0 to 35 percent above 40 inches <br />Rock fragments generally average less than 15 percent, but ranges to 35 percent below a depth of 20 <br />inches. <br />Minimum <br />Drainage Class: <br />Permeability Class: <br />Depth (inches): <br />Electrical Conductivity (mmhos/cm)*: <br />Sodium Absorption Ratio*: <br />Soil Reaction (1:1 Water)*: <br />Soil Reaction (0.1M CaCl2)*: <br />Available Water Capacity (inches)*: <br />Calcium Carbonate Equivalent (percent)*: <br />somewhat excessively <br />moderately rapid <br />20 <br />0 <br />0 <br />6.8 <br />6.4 <br />2.0 <br />0 <br />*These attributes represent 0-40 inches in depth or to the first restrictive layer. <br />Maximum <br />well <br />moderately slow <br />60 <br />3 <br />5 <br />8.4 <br />8.2 <br />7.0 <br />35 <br />Technical Guide USDA NRCS <br />Section IIE 3 Rev. 3/04 <br />
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