岷江上游干旱河谷海拔梯度上的土壤发生特征
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国家重点基础研究发展计划课题(2006CB701401)和“十五”国家科技攻关课题(2004BA810B05)资助


Pedogenetic property variation with elevation in dry valley of the upper Minjiang River
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    摘要:

    了解岷江上游干旱河谷的土壤发生特征对区域植被恢复有着指导意义,为此选择不同海拔梯度上7个典型土壤剖面进行土壤发生特性分析。结果表明,受区域成土环境影响,土壤化学风化和成土作用弱;土壤质地较粗,土壤机械组成以粉砂为主,黏化作用不强。土壤全Fe含量和Fe游离度一般<50 g/kg和<30%;交换性盐基组成在土壤剖面中无明显分异。随海拔升高,土壤黏粉比、全Fe含量、Fe游离度增加。土壤表土有机碳同位素δ13C值随海拔升高偏负,反映区域植被类型由低海拔半干旱气候条件下的C4型灌丛植被向高海拔凉润气候条件下C3型针阔叶林自然过渡。基于干旱河谷地区土壤特征,其植被恢复应以提高土壤质量为基础,并应遵循海拔梯度上自然植被分布特征进行植被恢复和生态重建。

    Abstract:

    Understanding the pedogenetic properties in dry valley of the upper Minjiang River plays a key role in regional vegetation restoration. Seven typical soil profiles at different altitudes were selected to analyze for the soil-forming characters and genetic properties. The results showed that local environmental conditions contributed to weak soil weathering and pedogenesis. The soil texture in the studied area was coarse and dominated firstly by silt fraction and secondly by clay fraction. The pedogenesis and secondary argillification was weak. Fet content and Fed/Fet ratio were less than 50 g/kg and 30%, respectively. The vertical differentiation of composition of exchangeable cations was not obvious in all the soil profiles. The clay/silt ratio, Fet content and Fed/Fet ratio all increased with the elevation. Moreover, δ13Cvalues of soil organic matter decreased with the elevation increasing. Improving the quality of soil and products is very significant for regional vegetation restoration. Meanwhile, local vegetation restoration and ecological environment construction should be based on the characteristics of natural vegetation distribution with elevation.

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柏 松,黄成敏,唐 亚.岷江上游干旱河谷海拔梯度上的土壤发生特征[J].土壤,2008,40(6):980-985. BAI Song, HUANG Cheng-min, TANG Ya. Pedogenetic property variation with elevation in dry valley of the upper Minjiang River[J]. Soils,2008,40(6):980-985

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