| 塔里木盆地潮湿冲积新成土形成特点 |
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| 引用本文： | 季方,樊自立,马英杰,李和平.塔里木盆地潮湿冲积新成土形成特点[J].干旱区研究,2000,17(1):1-4. |
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| 作者姓名： | 季方 樊自立 马英杰 李和平 |
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| 作者单位： | 中国科学院新疆生态与地理研究所,乌鲁木齐,830011 |
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| 基金项目： | 中国科学院资源与生态环境重大项目!(KZ951-B1- 2 13- 0 2 - 0 3)，国家重点基础研究发展规划项目!(G19990 4 350 3) |
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| 摘 要： | 干旱内陆地区的潮湿冲积新成土主要位于大河两岸的河滩地，它的地下水位高，土壤水分为潮湿状态。受到洪水的影响，虽然盐分已具有表聚，但缺乏盐结皮层。由于不断有新的泥沙沉积物加入，土壤无明显发育，而且其性状受土壤质量地影响。
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| 关 键 词： | 潮湿冲积新成土 形成特点 塔里木盆地 土壤分类 |
| 修稿时间： | 1999-08-26 |
Formation Characteristics of Aqu-Alluvic Entisols in Tarim Basin |
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| Ji Fang,Fan Zili,Ma Yingjie,Li Heping.Formation Characteristics of Aqu-Alluvic Entisols in Tarim Basin[J].Arid Zone Research,2000,17(1):1-4. |
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| Authors: | Ji Fang Fan Zili Ma Yingjie Li Heping |
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| Abstract: | Aqu-Alluvic Entisols was located in the flood land of river in arid inland area. The ground water table of the soil is high and soil moisture regime is aquic. Although salt had begun to accumulate in soil surface, there was no salic crust horizon in its surface. As new sediment was often inputted to soil surface, soil developing process was not obvious, its property is affected by soil texture to a great degree. |
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| Keywords: | Aqu-Alluvic Entisols formation characteristics Tarim Basin |
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