鄂西山地的酸性棕壤和灰棕壤形成条件及理化性质
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FORMATION CONDITIONS AND PHYSICO-CHEMICAL PROPERTIES OF ACID BROWN SOILS AND GREY BROWN SOILS IN THE MOUNTAINOUS AREAS OF WEST HUBEI
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    摘要:

    根据鄂西山地的自然成土条件,分析了酸性棕壤、灰棕壤诊断层和诊断特性,主要理化性质和粘土矿物组成,结果表明:酸性棕壤和灰棕壤同属于亚热带中山上部或亚高山中上部冷湿条件下形成的森林土壤.其理化性质与我国北方同类土壤又有较大差别.酸性棕壤分布在中山上部,居暗黄棕壤之上,分布高度为鄂西南高于鄂西北,是亮针叶阔叶落叶林带的森林土壤;灰棕壤分布在神农架亚高山上部,海拔2500m以上,植被为暗针叶林带,其土壤形成的环境比酸性棕壤更为冷湿.

    Abstract:

    The profile morphology,main physico-chemical properties and clay mineral composition of acid brown soil,grey brown soil are disscussed according to the natural conditions of the mountain soil formation in the west Hubei.The results show that both of the acid brown soil and grey brown soil belong to the forest soils formed in the middle and upper parts of subalpine and medium mountain areas in the subtropic climatic zone under cold and humid conditions.But their physico-chemical properties differed obviously with the same soil types in the northern China.The acid brown soils are distributed in the middle and upper parts of the medium altitude mountains,with an altitude higher than the dark yellow-brown soils,being the forest soils with the vegetations of bright conifer and broadleaf deciuous scrubs.Their distribution altitude is higher in the southwest Hubei than in the Northwest Hubei.Grey brown soil is the forest soil formed under colder and more humid conditions than the acid brown soil and located at a higher altitute than the acid brown soil about 2500m above the sea level in Shen nongjia region,and its vegetations are dark conifer forests.

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阳海清.鄂西山地的酸性棕壤和灰棕壤形成条件及理化性质[J].土壤学报,1996,33(2):166-174. DOI:10.11766/trxb199407090207 Yang Haiqing. FORMATION CONDITIONS AND PHYSICO-CHEMICAL PROPERTIES OF ACID BROWN SOILS AND GREY BROWN SOILS IN THE MOUNTAINOUS AREAS OF WEST HUBEI[J]. Acta Pedologica Sinica,1996,33(2):166-174.

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  • 收稿日期:1994-07-09
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  • 在线发布日期: 2013-02-25
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