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Characterization and classification of soils of Wolkite University research sites, Ethiopia

机译:埃塞俄比亚沃尔科特大学研究地点的土壤特征与分类

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The main purpose of this study was to characterize and classify soils of Wolkite University research sites, Gurage zone, Ethiopia. In each five research sites, Wabe (RS1), Geche (RS2), Yefereze (RS3), Kotergedra (RS4) and Keratemo (RS5), representative pedons were opened and described. Almost all the pedons were deep (150 cm) with argillic B horizons and had clay textural class. The pH of the surface soils ranged from strongly acidic (4.5) to moderately acidic (5.6). The soils had medium (2.60%) to high (3.84%) organic carbon content and very low (1.46 mg kg-1) to low (10.34 mg kg-1) available phosphorus. The status of cation exchange capacity (CEC) and base saturation were ranged from medium (23.15) to very high (66.32 cmolc kg-1) and low (33%) to high (99%), respectively. According to WRB classification, pedon RS1 was classified as Haplic Vertisols (Hypereutric) with USD equivalent of Typic Haplusterts. Pedons RS2 and RS3 were classified as Vertic Alisols (Hyperdysric), which is correlated with Ultisols (Typic Haplustults) in USDA classification. Pedon RS4 and RS5 classified as Vertic Luvisols (Hypereutric), which is correlated with Alfisols (Vertic Haplustalfs) in USDA classification. Generally, the soils of the research sites were acidic with low status of available phosphorus, which need amelioration of soil acidity and nutrient management.
机译:这项研究的主要目的是对埃塞俄比亚古拉格地区沃克特大学研究地点的土壤进行表征和分类。在Wabe(RS1),Geche(RS2),Yefereze(RS3),Kotergedra(RS4)和Keratemo(RS5)这五个研究地点中,都有代表性的脚踏板被打开并进行了描述。几乎所有的脚踏板都深(> 150 cm),带有泥质B级地平线,并且具有粘土质地等级。表层土壤的pH值范围从强酸性(4.5)到中酸性(5.6)。土壤中的有机碳含量为中(2.60%)至高(3.84%),有效磷非常低(1.46 mg kg-1)至低(10.34 mg kg-1)。阳离子交换容量(CEC)和碱饱和度的范围分别从中等(23.15)到极高(66.32 cmolc kg-1)和低(33%)到高(99%)。根据WRB的分类,pedon RS1被归类为Haplic Vertisols(Hypereutric),相当于美元的Typic Haplusterts。 RS2和RS3踏板被分类为垂直糊化剂(Hyperdysric),在USDA分类中,其与Ultisols(典型的Haplustults)相关。 Pedon RS4和RS5被分类为Vertic Luvisols(Hypereutric),在USDA分类中与Alfisols(Vertic Haplustalfs)相关。通常,研究地点的土壤呈酸性,有效磷含量较低,需要改善土壤的酸度和养分管理。

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