Distribution of forms of potassium in soils of Central and eastern Vidarbha region of Maharashtra.

S. Babar, P. Rathod, V. Salvi, V. Badole
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引用次数: 1

Abstract

Soil samples from fourteen profiles from five districts of Central and Western Vidarbha region of Maharashtra were studied for the distribution of different forms of potassium and for their relationship with some soil properties. The soils of Wardha, Nagpur, Chandrapur and Bhandara districts were slightly calcarious neutral to alkaline in reaction and the soils of Gondia district was non-calcarious and sightly acidic in reaction. The Central Vidarbha soils were clay in texture having high in organic carbon content. Whereas the soils of Eastern Vidarbha were clay loam, sandy clay loam and low in organic carbon content. No definite trend was observed in the forms of potassium except exchangeable and available K, they were decreased with increase in depth. The available K and exchangeable K increased with the increase in organic carbon (r = 0.4680**, r = 0.4526**). The availability of exchangeable K increased with increase in clay content (r = 0.2888**). The non-exchangeable K was also increased with clay content (r = 0.7141**) and EC (r = 0.6444**) in Eastern Vidarbha region. The availability of total K and lattice K increased with increase in organic carbon (r = 0.4303**, r = 0.4785*) and clay content (r= 0.5189*, r = 0.4631*) in Eastern Vidarbha region of Maharashtra.
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马哈拉施特拉邦中部和东部维达尔巴地区土壤中钾形态的分布。
本文研究了马哈拉施特拉邦中部和西部维达尔巴省5个区的14个剖面土壤样品中不同形态钾的分布及其与土壤性质的关系。瓦尔达、那格浦尔、钱德拉普尔和班达拉地区的土壤为轻度钙化、中性至碱性反应,冈迪亚地区的土壤为非钙化、轻度酸性反应。维达尔巴中部土壤为粘土质,有机碳含量高。而东维达巴土壤为粘壤土、砂质粘壤土,有机碳含量较低。除交换态钾和有效态钾外,钾的形态没有明显的变化趋势,均随深度的增加而降低。有效钾和交换钾随有机碳的增加而增加(r = 0.4680**, r = 0.4526**)。交换态钾的有效性随粘土含量的增加而增加(r = 0.2888**)。在维达尔巴东部地区,非交换性钾也随着粘土含量(r = 0.7141**)和EC (r = 0.6444**)的增加而增加。在马哈拉施特拉邦东部Vidarbha地区,总钾和晶格钾的有效性随着有机碳(r= 0.4303**, r= 0.4785*)和粘土含量(r= 0.5189*, r= 0.4631*)的增加而增加。
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