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PERMFILE102095
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PERMFILE102095
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Last modified
8/24/2016 9:56:07 PM
Creation date
11/24/2007 8:29:29 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981028
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
APPENDIX L SOILS & VEGETATION
Media Type
D
Archive
No
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9 <br />This, combined with the slightly higher silt and <br />clay content of the Osgood soils suggest that they <br />would be slightly more resistant to wind erosion, <br />have a slightly higher water holding capacity and <br />thus should provide a better medium for plant growth <br />and be more stable. An inch of water would pene- <br />trate about 18 inches into the sand surface soils <br />when initially dry (calculations made from soils <br />laboratory data, appendix B). This calculated depth <br />of water penetration is in agreement with a field <br />observation made on 24 October when it was found <br />that water had penetrated the sand to 28 inches <br />after 1.9 inches of precipitation on 21-23 October. <br />3. Plant available P levels are sufficient in the <br />surface horizons but decline rapidly with depth. <br />Alteration of the surface soil during the typical <br />redistribution process may result in mixing of <br />existing topsoil and subsoil materials and could <br />result in lower available P levels. Thus, compos- <br />ite surface soil samples should be obtained follow- <br />ing topsoil redistribution to determine the P status <br />of the soil at that time. <br />4. Organic matter levels are highest in the surface <br />~ layers and decrease rapidly with depth. <br />5. Available R levels appear to be adequate in all <br />horizons of all soils except for the C horizon of <br />one of the Valent soil profiles and the Cca horizon <br />of one of the Osgood soil samples. <br />6. Critical levels for zinc, iron, copper, and mangan- <br />ese relative to deficiencies of these elements on <br />native range are not well known. In general, the <br />available levels of these elements in the surface <br />soils are adequate for most agronomic crops, thus <br />it is assumed that they are adequate for most <br />species that would be grown in the area. Avail- <br />able iron is considered adequate throughout the <br />entire profile in all soils investigated. In <br />general, the same is true for copper and manganese. <br />Available zinc, on the other hand, is low except <br />for the surface layers. However, it must be <br />remembered that the low rating is based on the zinc <br />status for agronomic crops. Perhaps zinc should be <br />considered suspect but not limiting in all materials <br />with zinc levels below 0.5 ppm. <br /> <br />
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