新疆阿勒泰山区土壤形成特征及其垂直分布
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新疆维吾尔自治区重点实验室绿洲生态实验室开放课题资助


Soil of formation characteristics and soil vertical distribution in Altay mountains area, Xinjiang
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    摘要:

    新疆阿勒泰山区土壤形成特征有有机物质积累特征、粘化特征、钙积特征、盐积特征和相应的化学组成及粘土矿物特征。ba值0.99~2.41,粘粒Sa 3.53~4.84,Saf 2.63~3.57,土壤淋溶风化程度不高,R2O3在山地棕色针叶林土、山地灰色森林土中略有移动,粘土矿物以蒙脱石、伊利石为主。本区山体高大,土壤垂直分布完整,东西差距显著,具有温带荒漠草原土壤垂直分布的典型特征,在干旱中温带的山地土壤中有代表性。

    Abstract:

    The soil has organic matter accumulative characteristics, clayification characteristics, calcic characteristics, salic char- acterisfics, and their chemical component and clay mineral characteristics in the area. The ba value is 0.99 - 2.41, clay Sa is 3.53 - 4.84, Saf is 2.63 - 3.57. Tne soil leach and weathering is not so high. Tne R2O3 has httle move in the frost brown forest soil and grey forest soil. Tne clay mineral chiefly includes montmorillonite, illite. Tne mountains are huge in the area, and the vertical distribution is complete. Tnere are remarkable differences from the east to west. Tne soil has typical characteristics of vertical distribution of the temperate zone desert steppe soil, it is a representative in desert middle temperate zone mountains soil.

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徐华君,韩宝平.新疆阿勒泰山区土壤形成特征及其垂直分布[J].中国土壤与肥料,2008,(1):12-17.

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  • 收稿日期:2006-10-25
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