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- haplic luvisols 弱发育淋溶土
- Then the Baijiang soil can he classified into alfisol class, cold alfisol subclass and albic cold luvisols class. 据此将白浆土划归淋溶土纲，冷性淋溶亚纲，漂白冷性淋溶土土类。
- Compared with it, the Hap-Udic Luvisols generated in the lower zone has less organic matter, but the structure of the organic matter is more complex. 与之相比，低海拔地区发育的简育湿润淋溶土有机质含量下降，但结构复杂，土壤具有粘化层。
- 5.Then the Baijiang soil can he classified into alfisol class, cold alfisol subclass and albic cold luvisols class. 据此将白浆土划归淋溶土纲，冷性淋溶亚纲，漂白冷性淋溶土土类。
- Solomon D.Lehmann J.Zech W Land use effects on soil organic matter properties of chronic luvisols in semi-arid northern Tanzania:carbon,nitrogen,ligning and carbohydrates 2000(78 杨景成.;韩兴国
- haplic acrisols 典型强淋溶土
- haplic andosol 薄层暗色土
- haplic andosols 弱发育暗色土
- ferric luvisols 铁质淋溶土
- haplic cambisols 普通始成土
- haplic castanozem 薄层栗钙土
- haplic chernozem 薄层黑钙土
- chromic luvisols 深色淋溶土
- luvisols 淋溶土
- haplic cherozems 普通黑钙土
- haplic ferralsols 普通黄红色铁铝土
- vertic luvisols 变性淋溶土
- calcic luvisols 石灰性淋溶土
- haplic gleysols 普通潜育土
- haplic kastanozems 普通栗钙土
