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2002-07-08_GENERAL DOCUMENTS - M2002004 (3)
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2002-07-08_GENERAL DOCUMENTS - M2002004 (3)
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8/24/2016 2:18:41 PM
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DRMS Permit Index
Permit No
M2002004
IBM Index Class Name
GENERAL DOCUMENTS
Doc Date
7/8/2002
Doc Name
ATTACHMENT, PART 2
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HABITAT MGMT
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DRMS
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SMITH, REDENTE, and HOOPER <br />tal inoculation of revegetation <br />:a fungi has enhanced seedling <br />of revegetation species. Thus, <br />repetitive ability and productiv- <br />'cation of vesicular - arbuscular <br />is not been demonstrated even <br />ttion methods are in progress. <br />'loping commercial application <br />mphasize methods of maintain - <br />Drage periods or using direct re- <br />matter level in the plant growth <br />baseline conditions under a to- <br />sed in the post- mining reclama- <br />recommendation is important. <br />surrounding undisturbed areas <br />he rate at which C is lost from <br />:r content increases. Likewise, <br />,curbed soils may indicate long- <br />1 abundant supply for reclama- <br />horizon(s) having a greater per - <br />should be stockpiled separately <br />:t topsoil criteria. During over - <br />tion, the first -lift topsoil should <br />in the minesoil profile. <br />ion is the proposed post- mining <br />be about 75 percent of unculti- <br />vated baseline conditions under <br />le, if the pre- mining land use is <br />d use is cultivated cropland, op- <br />rf baseline values. <br />an estimate of what these rule - <br />ty vary with location. Through - <br />:r content ranges from 0.5 to 12 <br />.s of the West, levels are usually <br />nt of the Southwest virgin soil <br />t, whereas organic matter levels <br />2.5 to 6 percent. Mountainous <br />organic matter levels of 2 to 12 <br />- get levels for organic matter in <br />ve site and soil quality. Organic <br />niting criterion of soil material <br />SOIL ORGANIC MATTER <br />being evaluated for use as topsoil. The following organic matter application <br />and management recommendations can mitigate adverse conditions that <br />may exist in nontopsoiled plant growth media: <br />► If the major limitation of the plant growth media is a clay, loamy sand <br />or sand texture, or a loamy or sandy skeletal particle size class, at least 2.2 <br />t /ha of organic matter should be incorporated into the upper 8 cm of soil. <br />► If the major limitation of the plant growth medium is its sodic condi- <br />tion, up to 4.2 t /ha of organic matter could be incorporated into the upper <br />20 cm of soil to increase infiltration and permeability. This condition will <br />create an environment where, under irrigation or in higher rainfall areas, <br />application of Na replacement amendments, such as CaSO3, will optimize <br />Na cation displacement. <br />► If the slope of the reclaimed land exceeds 25 percent and annual pre- <br />cipitation exceeds 30 cm, or the area receives intense thunderstorms, 2.2 t /ha <br />or more of organic matter (straw mulch) should be applied, all other soil <br />conditions not limiting, to increase infiltration and minimize water erosion. <br />► Any area receiving applied organic matter with a C/N ratio exceeding <br />20:1 may need N fertilization. <br />► Soil areas to be stripped and then have the topsoil replaced directly <br />should be given consideration for rotoclearing prior to stripping. <br />► With the possible exception of the northern Great Plains, cropland <br />use of mined land is discouraged for several years after mining because of <br />the organic matter loss and, hence, accelerated erosion that may occur <br />under this form of management. <br />► Excessive applications (? 200 t /ha) of manure or sewage sludge <br />should be avoided in any type of plant growth media. <br />P. Applications of organic matter will raise the cation exchange capacity <br />of the soil. <br />► Application of organic matter to nontopsoiled or spoil plant growth <br />medium via the use of a leguminous covercrop should appreciably increase <br />the dynamic fraction and possibly accelerate processes of soil organic <br />formation when moisture is adequate. <br />REFERENCES <br />209 <br />1. Agricultural Research Service, U.S. Department of Agriculture. 1965. Predicting <br />rainfall- erosion losses from cropland east of the Rocky Mountains. Agricultural <br />Handbook 282. Washington, D.C. <br />2. Alexander, M. 1977. Introduction to soil microbiology. John Wiley and Sons, <br />Inc., New York, New York. 467 pp. <br />3. Allen, E. B., and M. F. Allen. 1980. Natural reestablishment of vesicular-arbus- <br />cular mycorrhizae following strip -mine reclamation in Wyoming. Journal of Ap- <br />plied Ecology 17: 139 -147. <br />4. Allison, F. E. 1973. Soil organic matter and its role in crop production. <br />Developments in soil science, 3. Elsevier Scientific Publishing Company, <br />Amsterdam, The Netherlands. 637 pp. <br />
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