| 论白浆土的形成和分类问题 |
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| 引用本文： | 曾昭顺,庄季屏,李美平.论白浆土的形成和分类问题[J].土壤学报,1963,11(2):111-129. |
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| 作者姓名： | 曾昭顺 庄季屏 李美平 |
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| 作者单位： | 中国科学院林业土壤研究所;中国科学院林业土壤研究所;中国科学院林业土壤研究所 |
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| 摘 要： | 我国黑龙江和吉林两省东部及其毗邻的苏联远东如伯力、沿海边区和阿穆尔州等地广泛分布着一种具有白色亚表层的土壤,我国当地农民称之为白浆土.关于这种土壤的形成过程问题,从К.Д.Глинка(1910)和В.А.Балъц、Б.Б.Полынов(1930)开始研究苏联远东和我国东北地区的土壤以来,中苏两国大多数土壤学家一直认为是灰化过程,称之为灰化土或生草灰化土.
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ON THE GENESIS AND CLASSIFICATION OF PAICHIANG SOILS |
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| C. S. TSENG,C. P. CHUANG and M. P. LI.ON THE GENESIS AND CLASSIFICATION OF PAICHIANG SOILS[J].Acta Pedologica Sinica,1963,11(2):111-129. |
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| Authors: | C S TSENG C P CHUANG and M P LI |
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| Institution: | Institute of Forest and Pedology, Academia Sinica;Institute of Forest and Pedology, Academia Sinica;Institute of Forest and Pedology, Academia Sinica |
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| Abstract: | A special soil group,characterized by a white subsurface and a chayly subsoil,is widely distributed in the east part of the Heilungkiang and Chilin provinces of Northeast China.This soil group has been described previously by some authors as podzolic and soddy-podzolic soils or solodi.A more systematic investigation of the soils by the present authors,both in field and laboratory,comes to the conclusions that the genesis of this soil group is of a hydromorphous bleached process developed periodically under the influence of temporary stagnation of soil water at the surface horizon.The Paichiang soils,according to the denomination of natives,should be regarded as a special group of hydromorphic soils and are tentatively subdevided into three subgroups-the Paichiang soil,the meadow-Paichiane soil and the glei-Paichiang soil. |
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