江西地区红壤性水稻土形成的特点
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THE PECULIARITY OF SOIL FORMATION OF THE PADDY SOILS DERIVED FROM RED EARTH IN KIANGSI, CHINA
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    摘要:

    红壤性水稻土是我国中亚热带地区的主要水稻土类型。根据江西省土壤普查的初步统计资料(1960),总面积约占全省水稻土的50%以上。红壤性水稻土基本性质的研究,已经累积了许多资料[1]。侯光炯和马溶之首先从形态发生的角度、研究了江西南昌地区某些红壤性水稻土的特性,以及形成过程中物质移动的淀积特征[2]

    Abstract:

    The paddy soils derived from red earth are one of the essential paddy soil types in the middle sub-tropical regions of china. From the preliminary study on soil forming process of these soils in Kiangsi province, it was found that they possess not only the characteristics common to the soil forming process of ordinary paddy soils, but also their own specific properties. First, in the condition of double rice cropping system, the accumulation of soil organic matter, both in quantity and quality, represents certain zonality. Second, under the effect of dressing organic fertilizers and liming, it results in rebasification of the soil, and forms a paddy soil having a higher percentage of base saturation. Third, the redox process and leach-illuviated process are stronger, causing the ferric and manganic oxides in soil profile to redistribute obviously. Nevertheless, the paddy soils derived from red earth have also inherited some properties from the soil materials to a certain extent. The silica-alumina ratio and clay mineral types are similar to red soils.

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曹升賡.江西地区红壤性水稻土形成的特点[J].土壤学报,1964,12(2):155-163. TSAO SUNG-KUNG. THE PECULIARITY OF SOIL FORMATION OF THE PADDY SOILS DERIVED FROM RED EARTH IN KIANGSI, CHINA[J]. Acta Pedologica Sinica,1964,12(2):155-163.

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  • 在线发布日期: 2013-02-25
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