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Role of Clay in Recovery of Organic Matter in Arable Black Soils of India: An Inverse Pyramid Relation

机译:粘土在印度可耕黑土中有机质恢复中的作用:反金字塔关系

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摘要

We studied the logic of blanket recommendation of Walkley Black Recovery Factor (WBRF) with a set of-1000 shrink-swell soil samples with varying clay content, representing two important food growing zones namely the Indo-Gangetic Plains and the Black Soil Region (BSR). Since clay and organic matter form strong clay complexes, we investigated how quantity of clay can influence recovery of organic matter from soils analyzed following standard procedure. Increase in clay content, soil depth and aridity (low rainfall) have similar effect in increasing WBRF due to decreased organic matter recovery. While the relation is a straightforward in low clay soils, the study showed that recovery of organic matter remains unaffected for BSR soil clays > 60% warranting a new initiative for an inter facial research to link pedology and edaphology.
机译:我们研究了Walkley黑色恢复因子(WBRF)一揽子推荐的逻辑,该一组包含1000个具有不同粘土含量的收缩膨胀土壤样品,代表了两个重要的食物生长区,即印度恒河平原和黑色土壤区域(BSR) )。由于粘土和有机物形成了坚固的粘土配合物,因此我们按照标准程序研究了粘土的量如何影响土壤中有机物的回收。由于有机质回收率降低,粘土含量,土壤深度和干旱(低降雨)的增加对WBRF的增加具有相似的作用。尽管在低粘土土壤中这种关系是直接的,但研究表明,对于> 60%的BSR土壤粘土,有机物的回收仍然不受影响,因此有必要开展一项新的计划,以开展将岩石学和水文学联系起来的界面研究。

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