江西红壤之气候问题
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Discussion on Laterization in Kiangsi
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    摘要:

    气候对于成土作用之影响至大且巨,故论者常以气候为成土作用之唯一动力,往往以某地之气候情形推断某地之土壤分布;亦复由土壤而推知其气候。此种立论乃系往日土壤学者日积月累之经验,其中尤以俄人之贡献最多。然按诸事实,则不尽然,盖成土作用之动力,不仅限于气候,同时某地之气候,亦并非一定不变老也;目前所见之土壤并非仅限于气候性土壤,而真正之气候性土壤亦非即为该区之区域性土壤也,二者时可合而为一,有时则大不相同,而决不能混作一谈也。

    Abstract:

    Laterite and lateritic soils are very universal in Kiangsi and occupy an immense area. According to the scheme of climatical soil classification, the whole province is considered as red earth region. In other words laterite and lateritic soil of Kiangsi, covering such a large area, were not only named as regional soils but climatical soils as well. And even some podologists considered that the laterization process in the southern part is comparatively more intensive than that in the north, for this is the micro-climatical variations within the province.

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朱显谟.江西红壤之气候问题[J].土壤学报,1948,0(1):51-56. Chu Shien-Mu. Discussion on Laterization in Kiangsi[J]. Acta Pedologica Sinica,1948,0(1):51-56.

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  • 在线发布日期: 2013-02-25
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