| 岷江上游半干旱河谷土壤成土特征研究：以大沟流域为例 |
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| 引用本文： | 陈学华.岷江上游半干旱河谷土壤成土特征研究：以大沟流域为例[J].资源开发与市场,1996,12(2):75-78. |
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| 作者姓名： | 陈学华 |
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| 作者单位： | 中国科学院成都山地研究所土壤室 |
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| 摘 要： | 岷江上游半干旱河谷位于新构造运动活动带，其土壤形成和发育过程有着鲜明的区域特征。本文结合该区域的自然地理特点，综合分析各成土因素和土壤性状，对该区域土壤的成土特征进行了深入的分析和研究。
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| 关 键 词： | 大沟流域 成土因素 成土特征 |
Research on Soil-Forming Feature Semi-Arid Basin at the Upper Section of Minjiang |
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| Chen Xuehua.Research on Soil-Forming Feature Semi-Arid Basin at the Upper Section of Minjiang[J].Resource Development & Market,1996,12(2):75-78. |
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| Authors: | Chen Xuehua |
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| Abstract: | The semi-arid basin at the upper section of Minjiang is located in the active area of New Structure Move. Its soil-forming has obvious regional specific property. After analyzing the natural characteristic, soilforming factor and soil feature,this paper deeply studied the soil-forming features in this area. |
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| Keywords: | Dagou basin soil-forming factor soil forming feature |
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