陕北地区黄绵土分类的研究
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DISCUSSION OF CLASSIFICATION OF YELLOW CULTIVATED LOESSIAL SOILS IN SHAANXI
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    摘要:

    黄绵土是在黄土母质上形成的幼年土壤,没有明显的发育层次,不具有地带性土壤剖面特征,土壤性状与母质类似,剖面层次由Ap—C层或A—C层组成。根据土壤诊断层和诊断剖面特性划分为原始黄绵土和淡黄绵土两个亚类。以作物生长季节(4—9月)土壤水热状况划分温灌黄绵土、温潮黄绵土、温润黄绵土、温干黄绵土、凉润黄绵土、凉干黄绵土等土属。以表层土壤质地和有机质含量的等级差异和组合划分出28个土种。黄绵土的分布,在延安以南海拔低于1200米以下的地区,阴、阳坡土壤均属温潮黄绵土,再向北,阴坡为温润黄绵土,阳坡为温干黄绵土。海拔高度在1400米以上阴阳坡两边的土壤属凉干黄绵土,阴凉沟底地土壤属凉润黄绵土。河川地土壤通常为温灌黄绵土。

    Abstract:

    Yellow loessial soils are infant soils developed on lossial material,without distinct development of genetic horizons and aonal characteristics of profile.The soils are similar to their parent material.The profile pattern is mainly composed of horizons of Ap-C or A-C.Based the diegnostic horizon and profile,the soils are divided into two subgroups,i.e.primary yellow cultivated loessial soils and Lightly yellow cultivated lossial soil.Based on the hydrothermal regimes of the soil in crop growing season (April to Sept.),the soils are subdivided into such soil families as warm-moist,warm-irrigated,warm-wet,warm-dry,cool-moist yellow cultivated lossial soils etc.Based on the texture and O.M.content,the soils are further subdivided into 28 soil species.The soil are mainly distributed in northern Shaanxi with an altitude of lower then 1200 m.

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黄自立.陕北地区黄绵土分类的研究[J].土壤学报,1987,24(3):266-271. Huang Zili. DISCUSSION OF CLASSIFICATION OF YELLOW CULTIVATED LOESSIAL SOILS IN SHAANXI[J]. Acta Pedologica Sinica,1987,24(3):266-271.

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  • 在线发布日期: 2013-02-25
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