Characterization and classification of soils under different land use systems in the upper Brahmaputra valley of Assam

Ravindra Kumar Rekwar
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Abstract

For characterization of soils, soils were collected from Jorhat and a Golaghat district during 2016-2017under different land uses systems i.e. bamboo, sugarcane, tea and rice. Results indicated that surface soils of different land use systems varied from greyish brown (10YR 5/2) to brownish yellow (10YR 6/8).The structure was found predominantly sub-angular blocky and loam to clay loam in texture. The soil soils of all horizons of bamboo, tea plantation and rice were extremely acidic (pH <4.5) except sugarcane horizons (strongly acidic pH 5.0-5.50).Soil cation exchange capacity(CEC) in bamboo, sugarcane, tea plantation and rice varied from 6.20 to 7.29 cmol (p+)/kg, 8.19 to 9.92 cmol (p+)/kg, 5.54 to 6.88 cmol (p+)/kg, and 6.99 to7.58 cmol (p+)/kg, respectively due to variation in clay content. Sugarcane and tea plantation soils showed clay alleviation with more than 1.2 times in sub-surface horizon over surface horizon with low base saturation <35%to place them in the Ultisol and classified as fine-loamy, mixed, hyperthermic family of Typic Hapludults.In bamboo plantation, the soil had cambic horizon with base saturation <35%and classified as coarse loamy, mixed, hyperthermic family of Typic Dystrudepts, whereas, in case of rice soil, the gleyed sub-surface horizon was observed with base saturation <35% and classified as loamy, mixed, hyperthermic, Typic Endoaquepts.The correlation coefficient (r) among physico-chemical of soil properties in profiles under different land use systems in upper Brahmaputra valley of Assam showed organic carbon was positively and significantly correlated with base saturation. The pH showed positive and significant correlation with CEC and clay content
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阿萨姆邦雅鲁藏布江上游河谷不同土地利用制度下土壤特征与分类
为了表征土壤,在2016-2017年期间从Jorhat和Golaghat地区收集了不同土地利用系统(竹子、甘蔗、茶叶和水稻)下的土壤。结果表明:不同土地利用系统的表层土壤呈现灰褐色(10年5/2)至棕黄色(10年6/8)的变化趋势;结构以亚角块状为主,质地为壤土-粘壤土。除甘蔗层呈强酸性pH 5.0 ~ 5.50外,竹林、茶园和水稻层土壤均呈极酸性(pH <4.5)。竹林、甘蔗园、茶园和水稻土壤阳离子交换容量(CEC)受粘土含量变化的影响,分别为6.20 ~ 7.29 cmol (p+)/kg、8.19 ~ 9.92 cmol (p+)/kg、5.54 ~ 6.88 cmol (p+)/kg和6.99 ~ 7.58 cmol (p+)/kg。甘蔗和茶园土壤在地下层比地表层减少1.2倍以上,基底饱和度低,<35%,属于Ultisol,属于细壤土、混合型、超温型单元型。竹林土壤为形成层,基质饱和度<35%,属于粗壤土、混合、超热的典型失稳类;水稻土壤为层状层,基质饱和度<35%,属于壤土、混合、超热、典型失稳类。阿萨姆邦雅鲁藏布江上游河谷不同土地利用方式剖面土壤理化性质的相关系数(r)表明,有机碳与碱基饱和度呈显著正相关。pH与CEC、粘土含量呈极显著正相关
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