Characterization and Classification of Soils of Askate Sub-watershed, Northeastern Ethiopia

Mulugeta Tufa, S. Ahmed, Kefyialew Tilahun, Mulugeta Fiseha, Tadla Guadie
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引用次数: 1

Abstract

Characterization and classification of soil is the main central information source for judicious soil management and enhance agricultural economy. Therefore, this study was conducted with the objective of characterization and classification of soil on Askate sub-watershed, northeastern Ethiopia. Four representative soil pedons were opened along topographic position and described on each identified genetic horizons basis on the field for their morphological characteristics following the soil field description guidelines. The morphological properties were examined in the field while physical and chemical properties were analyzed in laboratory. The results of the study were revealed variation in morphological, physical, and chemical properties of the soils. Soil textural classes were sandy loam to loam sandy. The bulk density ranged from 1.04 to 1.60 g cm-3. The soil reaction rated as slightly acidic to moderate acidic (5.4 to 6.7). The OM ranged from 0.41 to 3.23% while available P ranged from 0.72 to 9.36 mg kg-1 which was low to medium rate. The exchangeable bases ranged from low to medium rate in the study area. CEC was medium to high rate, which implies the medium nutrient reservoir of the soil. Finally, three soil types, Humic Cambisols, Haplic Luvisol, and Cambic Umbrisols were identified in the study area according to World Reference Base. Using the soils according to their potential and applications of integrated soil fertility managements are essential to keep the sustainability of soil fertility and nutrient availability.
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埃塞俄比亚东北部Askate流域土壤特征与分类
土壤特征与分类是土壤管理和农业经济发展的主要信息来源。因此,本研究以埃塞俄比亚东北部Askate子流域土壤特征和分类为目的。沿着地形位置打开4个具有代表性的土壤土墩,并根据土壤田描述指南,在每个确定的遗传层上对其形态特征进行描述。实地考察了其形态特性,实验室对其理化特性进行了分析。研究结果揭示了土壤的形态、物理和化学性质的变化。土壤质地分级为砂壤土~壤土砂质。堆积密度为1.04 ~ 1.60 g cm-3。土壤反应等级为微酸性至中酸性(5.4至6.7)。土壤有机质含量为0.41 ~ 3.23%,有效磷含量为0.72 ~ 9.36 mg kg-1,为中、低处理。研究区可交换碱基的比率从低到中不等。CEC为中高速率,说明土壤具有中等的养分储层。最后,根据世界参考数据库,在研究区鉴定出腐殖质cambisol、单质Luvisol和cambisol 3种土壤类型。根据土壤的潜力和土壤肥力综合管理的应用来利用土壤是保持土壤肥力和养分有效性的可持续性的必要条件。
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