栗钙土(chestnut soil)是温带半干旱大陆气候和干草原植被下经历腐殖质积累过程和钙积过程所形成的具有明显栗色腐殖质层和碳酸钙淀积层的钙积土壤。
... chestnut brown soil 栗钙土型棕钙土 chestnut coloured soil 栗钙土 chevron fold 尖顶褶皱 ...
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土壤理化性质土壤类型属于暗栗钙土。
Soil characteristics The soil belongs to dark chestnut soil.
栗钙土是内蒙古自治区最重要的一种土壤类型。
Chestnut soil is one of the main types of soil in Inner Mongolia.
结果表明，我国栗钙土与其它国家的软土系同一时期的产物，它们形成于大约6000年以前。
Results of radiocarbon dating showed that the chestnut soils of China and the mollisols in other countries of the world were the product of the same period, formed about 6000 years apo.
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