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Titlebook: The Red Soils of China; Their Nature, Manage M. J. Wilson,Zhenli He,Xiaoe Yang Book 2004 Springer Science+Business Media New York 2004 Eros

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書目名稱The Red Soils of China
副標(biāo)題Their Nature, Manage
編輯M. J. Wilson,Zhenli He,Xiaoe Yang
視頻videohttp://file.papertrans.cn/919/918314/918314.mp4
圖書封面Titlebook: The Red Soils of China; Their Nature, Manage M. J. Wilson,Zhenli He,Xiaoe Yang Book 2004 Springer Science+Business Media New York 2004 Eros
描述The red soils of China are typical in their chemical, physical and mineralogical characteristics of red soils in other tropical and sub-tropical areas of the world, particularly in South America, Africa and south-east Asia. For the most part, these soils are highly weathered and inherently infertile. They are acidic, nutrient- deficient, poor in organic matter and have a low water-holding and supplying capacity. They cannot sustain arable cropping systems without the most careful management and are highly susceptible to soil erosion, particularly on sloping land. It is the purpose of this book to present recent research showing how the problems associated with using the red soils in China for sustainable agricultural production can be overcome, using a variety of traditional and novel approaches. In principle, these approaches should be useful in other tropical and sub-tropical countries faced with the problem of making the best use of their fragile red soil resources. The term "in principle" is used deliberately because, of course, the different red soil countries invariably operate within dissimilar socio-economic frameworks. At the present time, China may be considered to be in
出版日期Book 2004
關(guān)鍵詞Erosion; biomass; development; production; soil; soil quality; sustainability
版次1
doihttps://doi.org/10.1007/978-1-4020-2138-1
isbn_softcover978-90-481-6597-1
isbn_ebook978-1-4020-2138-1
copyrightSpringer Science+Business Media New York 2004
The information of publication is updating

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978-90-481-6597-1Springer Science+Business Media New York 2004
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ical areas of the world, particularly in South America, Africa and south-east Asia. For the most part, these soils are highly weathered and inherently infertile. They are acidic, nutrient- deficient, poor in organic matter and have a low water-holding and supplying capacity. They cannot sustain arab
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