A Cambisol in the World Reference Base for Soil Resources (WRB) [1] is a soil in the beginning of soil formation. The horizon differentiation is weak. This is evident from weak, mostly brownish discolouration and/or structure formation in the soil profile .

Cambisol, one of the 30 soil groups in the classification system of the Food and Agriculture Organization (FAO). Cambisols are characterized by the absence of a layer of accumulated clay, humus, soluble salts, or iron and aluminum oxides. They differ from …

The ‘typical’ Cambisol profile has an ABC-horizon sequence with an ochric, mollic or umbric A-hori-zon over a cambic B-horizon that has normally a yellowish-brown colour but that may also be an in-tense red. Cambisols in poorly drained terrain positions may show ‘redoximorphic’ features. The soil texture is loamy to clayey.

初育土是指土壤发育程度微弱，土壤剖面层次分异不明显，母质特征显著，土壤保持相对的幼年阶段，并明显区别于地带性土壤的一些土壤类型。其剖面类型多为A—C或A—R型。初育土相当于美国分类中的新成土(entisols)，始成土(inceptisols)；相当于联合国分类的浅层土(eptosols)、粗骨土(regosols)、始成土 ...

A Cambisol is a soil type from the FAO soil classification, consisting of the words cambiare (“change” in Latin and Italian) and sol (you guessed it: “soil”). We love the soil type and its profile, but there are more relevant reasons why Cambisol was picked as the name of this environmental consultancy bureau.

The plant available water holding capacity of the Cambisol (S3) at Slavkov Forest CZO is 83 mm, more than twice that of the reference profile D4 at Damma Glacier. The profile with the greatest thickness and plant water holding capacity (126 mm) is profile K5—the manmade terrace at noncultivated condition.

Cambisols occur mainly in the temperate and boreal regions of the world, where the soil’s parent material is still young or where low temperatures slow down the processes of soil formation.

2016年1月1日 · 'Cambisols' published in 'Encyclopedia of Soil Science' Origin. Weathering by hydrolysis is the characteristic process though it is not advanced and consequently appreciable quantities of weatherable minerals (feldspars and ferromagnesians for example) persist in the soil.

Cambisol Définition Cambisols combine soils with at least an incipient subsurface soil formation. Transformation of parent material is evident from structure formation and mostly brownish discoloration, increasing clay percentage, and/or carbonate removal. Other soil classification systems refer to many Cambisols as Braunerden and Terrae ...

Reference soil China 34: Cambisol CN034 Cambisols occur mainly in the temperate and boreal regions of the world, where the soil’s parent material is still young or where low temperatures slow down the processes of soil formation.