关于在slon洼地石膏上形成的石灰土

Soil Forming Factors and Processes from the Temperate Zone Pub Date : 2012-03-08 DOI:10.15551/FPPZT.V4I1.319

M. Parichi, A. Stănilă, V. Duca, N. Rizea

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引用次数: 0

摘要

到目前为止，在我国还没有完全隔离使用锌石膏的地区。在大多数情况下，这些类型的土壤与其他土壤一起出现。在德拉吉纳河谷的上盆地发现了双形成纪的双形成纪，它们位于山岗形态接触上，受Pintenul de homor(古近系构造)的限制。这些土壤可以在地图上表示出来。在很大的地区，在不同的斜坡条件下只出现形成层的斑纹。这些土壤的分析数据表明，粘土含量高(52- 56%)，中性反应阳离子交换容量中大型(34-49 me/100 g土壤)，腐殖质含量中大型。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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ABOUT RENDZINA SOILS WHICH IS FORMED ON GYPSUM FROM SLON DEPRESSION

By now, in our country wasn ׳ t separated areas with exclusit rendzine gypsom. In most cases, these types of soils apear in association with other soils. We found rendzina and cambic rendzina in upper basin of Drajna valley witch, is locate on mountain-hill morphological contact and limited from cast by Pintenul de Homorâciu (Paleogen structure). These soils are possibly, to represent on maps. On large areas appear only cambic rendzina in various conditions of slopes. Analytic data about these soil indicate a large content of cley (52-56 per cent), neutral reaction middle-large cation exchange capacity (34-49 me/100 g soil) and middle-large humus content.

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Soil Forming Factors and Processes from the Temperate Zone

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