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Titlebook: Advances in Soil Science; Volume 9 B. A. Stewart Book 1989 Springer-Verlag New York Inc. 1989 Deforestation.environment.erosion.forest.soil

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期刊全称Advances in Soil Science
期刊简称Volume 9
影响因子2023B. A. Stewart
视频video
学科分类Advances in Soil Science
图书封面Titlebook: Advances in Soil Science; Volume 9 B. A. Stewart Book 1989 Springer-Verlag New York Inc. 1989 Deforestation.environment.erosion.forest.soil
影响因子Soil is formed from the physical and chemical weathering of rocks-processes described historically because they involve eons of time-by glaciation, and by wind and water transport of soil materials, later deposited in deltas and loessial planes. Soil undergoes further transformations over time and provides a habitat for biological life and a base for the development of civilizations. Soil is dynamic - always changing as a result of the forces of nature and particularly by the influences of man. Soils have been studied as long as history has been documented. W. H. Gardner told of writings on clay tablets, dating about 1700 Be, in his review, "Early Soil Physics into the Mid-20th Century;‘ published in Volume 4 of this series. Those writings gave specific instructions on cultivating the soil and seeding crops. Numerous references to soil are found in historical writings, such as Aristotle (384-322 Be), Theophrastus (372-286 Be), Cato the Elder (234-149 Be), and Varro (116-27 Be). Some of the earliest historical refer­ ences to soil 3000 or more years ago have to do with erosional forces of wind and water. The study of soils today has taken on increased importance because a rapidly ex
Pindex Book 1989
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0176-9340 soil 3000 or more years ago have to do with erosional forces of wind and water. The study of soils today has taken on increased importance because a rapidly ex978-1-4612-8144-3978-1-4612-3532-3Series ISSN 0176-9340
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Heavy Metals in Soils and Their Environmental Significance, society because of the range of metal products used. All-time usage of Cd, Cu, Pb, Ni, and Zn has been estimated to have been 0.5, 307, 241, 17, and 250 × 10. kg, respectively (Nriagu, 1979). The estimated total (all-time) and annual amounts of these metals dispersed through the atmosphere are pres
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Advances in Soil Science978-1-4612-3532-3Series ISSN 0176-9340
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C. A. Rains,J. R. Ray,P. VashishtaCa source on legumes and as a soil conditioner on sodic soils. Recent research has suggest that the utility of gypsum may extend to a greater range of soils and crops than previously acknowledged. The purpose of this review is to document both current practices and potential new uses of gypsum in ag
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Conference proceedings 19931st editionlable” to an extractant, usually acetic acid, ethylene diamine tetracetic acid (EDTA), diethylene triamine pentacetic acid (DTPA), etc. (e.g., Lindsay and Norvell, 1969; Viets and Lindsay, 1973; Ministry of Agriculture, Fisheries and Food, 1981). This is fortunate because the soil chemistry of trace
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https://doi.org/10.1007/978-3-642-60597-0ithin the near future. This development implies that more attention can be paid to soil survey interpretations and applications. The opportunity to emphasize use of soil survey data is particularly timely because of a change in the type of questions being asked by users of soil survey data and becau
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