Pedological Investigation of Soil Quality Indicators in Tapioca Growing Soils

Q3 Agricultural and Biological Sciences
V. Sabareeshwari, Jemila Chellappa, C. Krithika, K.V. Haina Johnson
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Abstract

Background: Manihot esculenta, the most important tropical root crop which supply dietary staple food for about 800 million populations worldwide. Twenty soil profiles that represent the soil Pedology and soil quality are similar in their concept in relation to soil formation. In this regards, soil quality can be considered as part of the science of pedology. Significant differences in yield of Tapioca (Manihot esculenta) with selected soil properties and subsequent interpretations as influenced by land use are explained. Methods: Soil samples were taken from designated pedogenic horizons for physico-chemical properties in the laboratory. Soil textural class, saturated hydraulic conductivity, Cation Exchange Capacity, Base Saturation Percentage, soil organic carbon, exchangeable cations, available N, P, K content and available micronutrients were analysed. The general fertility of the soils in the area is discussed highlighting their potentials and constraints. Result: A comprehensive analysis of soils in the study area showed that shallow soil depth of less than 47 cm and more clay of 44% with high bulk density of 1.4 gcc-1, low hydraulic conductivity of 0.12 cmhr-1, low base saturation percentage of 77%, more exchangeable sodium percentage of 7.96% with low available N, P and K of 110, 10.75 and 142.25 kg ha-1, respectively in low yielding soils are the major constraints in the tract might behind the yield differences in Cassava.
木薯种植土壤中土壤质量指标的土壤学调查
背景:Manihot esculenta 是最重要的热带根茎作物,为全球约 8 亿人口提供主食。代表土壤的 20 个土壤剖面 在与土壤形成有关的概念上,土壤学和土壤质量是相似的。因此,土壤质量可被视为土壤学的一部分。本文解释了木薯(Manihot esculenta)产量与选定土壤特性之间的显著差异,以及受土地利用影响的后续解释。方法:从指定的成土层中提取土壤样本,在实验室中进行物理化学性质检测。分析了土壤质地等级、饱和导水率、阳离子交换容量、碱饱和度、土壤有机碳、可交换阳离子、可利用的氮、磷、钾含量和可利用的微量营养元素。讨论了该地区土壤的总体肥力,强调了其潜力和制约因素。结果对研究地区土壤的综合分析表明,土壤深度小于 47 厘米,粘土含量多达 44%,容重高达 1.4 gcc-1,导水率低达 0.12 cmhr-1,碱饱和度低达 77%,可交换钠含量多达 7.96%,可利用氮、磷和钾含量低,分别为 110、10.75 和 142.25 kg ha-1,这些低产土壤是造成木薯产量差异的主要制约因素。
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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来源期刊
Indian Journal Of Agricultural Research
Indian Journal Of Agricultural Research Agricultural and Biological Sciences-Soil Science
CiteScore
1.00
自引率
0.00%
发文量
143
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