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首页> 外文期刊>Annals of Agri Bio Research >Morpho-electrochemical characterisation and nature of soil acidity as influenced by topography and vegetation in some acid soils of Kamrup district, Assam.
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Morpho-electrochemical characterisation and nature of soil acidity as influenced by topography and vegetation in some acid soils of Kamrup district, Assam.

机译:地形和植被对阿萨姆邦坎普普地区某些酸性土壤的形态电化学特征和土壤酸度的影响。

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摘要

Some acid soils (Utisols and Alfisols) representing Kamrup district, Assam, India, were studied to characterize the nature of soil acidity, electro-chemical properties and their variations as influenced by topography (slope) and vegetation (forest).The positive difference between pH (H2O) and pH (KCl) reflected appreciable amount of reserve acidity in all the pedons. Organic carbon content varied from 3.0 to 13.1 g kg-1 of soil, wherein the highest being recorded under moderately thin forest vegetations with 3-5% slope. Cation exchange capacity (CEC) as determined by three different methods was compared; showing NH2OAc-CEC and effective-CEC (ECEC) as the best method in acid soils. Lime requirement was positively correlated with % Al saturation, exchangeable and extractable acidity (r=0.874, 0.962 and 0.788), respectively, the highest value (5.4 tonnes ha-1) being recorded in moderately sloped soft having lower soil pH. Exchange acidity varied from 1.00 to 4.00 cmol (p+) kg-1 and contributed 13.4to 30.1% of the extractable acidity. Extractable acidity ranging from 7.1-15.0 cmol (p+) kg-1 showed positive correlations with ECEC, % Al saturation and clay content (r=0.715, 0.678 and 0.558), respectively. Major portion of the total potential aciditywas pH dependant (69.9 to 86.5%) that varied from 6.1 to 11.25 cmol (p+) kg-1. Effect of topography and vegetation on exchange acidity was negligibleil.
机译:研究了代表印度阿萨姆邦坎鲁普区的一些酸性土壤(Utisols和Alfisols),以表征土壤酸度的性质,电化学性质及其受地形(坡度)和植被(森林)影响的变化。 pH(H2O)和pH(KCl)反映了所有花粉中明显的储备酸度。土壤有机碳含量从3.0到13.1 g kg-1不等,其中最高的记录是在坡度为3-5%的中等稀薄森林植被下。比较了通过三种不同方法确定的阳离子交换容量(CEC);表明NH2OAc-CEC和有效CEC(ECEC)是酸性土壤中的最佳方法。石灰需求分别与铝饱和度%,可交换和可萃取酸度(r = 0.874、0.962和0.788)呈正相关,最高值(5.4吨ha-1)记录在土壤pH较低的中度倾斜软土中。交换酸度为1.00至4.00 cmol(p +)kg-1,占可萃取酸度的13.4%至30.1%。可萃取酸度范围为7.1-15.0 cmol(p +)kg-1,与ECEC,%Al饱和度和粘土含量呈正相关(r = 0.715、0.678和0.558)。总潜在酸度的主要部分取决于pH(69.9至86.5%),范围为6.1至11.25 cmol(p +)kg-1。地形和植被对交换酸度的影响可忽略不计/无。

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