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Titlebook: Microfloral and faunal interactions in natural and agro-ecosystems; Myron J. Mitchell,James P. Nakas Book 1986 Martinus Nijhoff/Dr W. Junk

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書(shū)目名稱(chēng)Microfloral and faunal interactions in natural and agro-ecosystems
編輯Myron J. Mitchell,James P. Nakas
視頻videohttp://file.papertrans.cn/634/633250/633250.mp4
叢書(shū)名稱(chēng)Developments in Biogeochemistry
圖書(shū)封面Titlebook: Microfloral and faunal interactions in natural and agro-ecosystems;  Myron J. Mitchell,James P. Nakas Book 1986 Martinus Nijhoff/Dr W. Junk
描述MYRON J. MITCHELL* The biota of soils constitute an integral part of both natural and agronomic ecosystems. The soil microflora and fauna in conjunction with the belowground portion of the Metaphyta or higher plants constitute the living milieu, components of which are in intimate association with each other as well as the abiotic constituents of the soil. Since these associations or interactions are important in regulat- ing both the flux and availability of energy and nutrients, the central theme of the present book focuses on these interactions. The effects of microfloral and faunal inter- actions with regard to overall ecosystem dynamics and specific critical processes will be examined. HISTORICAL ASPECTS The coverage of this volume is an extension of a vast body of literature which dates back to the 18th century. A brief compendium of major books and reviews published from 1960 to 1983 is given chronologically in Tables 1 and 2, respectively. Russell (1961) has reviewed work in the 1800‘s during which some of the basic tenets on the relationships between plant nutrition and soil properties became estab- lished. In this period agricultural science was founded and the study of s
出版日期Book 1986
關(guān)鍵詞Assimilat; Flora; cyclin; ecosystems; microorganism; nitrogen; residue; residues; soil
版次1
doihttps://doi.org/10.1007/978-94-009-5173-0
isbn_softcover978-94-010-8789-6
isbn_ebook978-94-009-5173-0
copyrightMartinus Nijhoff/Dr W. Junk Publishers, Dordrecht 1986
The information of publication is updating

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Book 1986on with the belowground portion of the Metaphyta or higher plants constitute the living milieu, components of which are in intimate association with each other as well as the abiotic constituents of the soil. Since these associations or interactions are important in regulat- ing both the flux and av
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Biodegradation of Organic Residues in Soil,s and its macromolecular components by extracellular enzymes as a prelude to assimilation and mineralization of soluble low molecular weight products; and (2) the formation and fate of polyaromatic substances and polysaccharides (.... humus) arising during microbial metabolism.
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The Role of Microflora in Terrestrial Sulfur Cycling,y to the combustion of fossil fuels and the smelting of ores) provide a substantial contribution of S to the atmosphere and thus to aquatic and terrestrial ecosystems. Kellogg.. (1972) concluded that by A.D. 2000, the anthropogenic input of S to the atmosphere will exceed natural inputs in the Northern Hemisphere.
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Myron J. Mitchell a technique that can be viewed as a type of inverse operation to tailoring. Here the start is P which is gradually enlarged as much as possible, by inserting new surface along slits. In a sense, repeated verte978-3-031-47513-9978-3-031-47511-5
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O. W. Heal,J. Dighton a technique that can be viewed as a type of inverse operation to tailoring. Here the start is P which is gradually enlarged as much as possible, by inserting new surface along slits. In a sense, repeated verte978-3-031-47513-9978-3-031-47511-5
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