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Characterization of problem soils in and around the south central Ethiopian Rift Valley

机译:埃塞俄比亚中部裂谷中南部及其周围问题土壤的特征

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Some soils in Ethiopia reduce plant productivity due to physical and/or chemical limitations. The morphological, physical and chemical properties of problem soils, including sodic, acidic, and saline soils, around southern Ethiopia were characterized and are described in this chapter. The intention is to characterize the soils and better understand the specific nature of the limitations. Sodic soils of Alage, acid soils of Hagereselam, and saline soils of Zeway areas were sampled to represent the problem soils. The soil properties determined included color, electrical conductivity (EC), structure, consistency, bulk density, texture, pH, organic carbon (OC), total nitrogen, available phosphorus (P) and K, exchangeable bases and available micro-nutrients. The soils had considerable heterogeneity in solum and regolith thickness, horizon depth, structural development in surface soils and subsurface horizons, pH, EC and available nutrients. The classification of these soils was made according to Soil Taxonomy and World Reference Base for Soil Resources systems. The sodic soils of Alage had high pH and sodium (Na) content, and low level of OC, available P, copper (Cu) and zinc (Zn). The epipedon was classified as an ochric and the profile also had variation in clay content down the profile to satisfy the requirements of having an argilic horizon and therefore these soils were classified as Typic Natragids. Soils of Hagereselam had very low available P. Available Cu and Zn contents were found to be at the marginal levels for production of most crops. The Hagereselam profile had an argilic horizon with umbric epipedon and was classified as Typic Paleustults. The saline soils in Zeway area had relatively high amounts of calcium and low OC. The profile was found to have ochric epipedon and these soils are classified as Typic Haplocambids. Application of fertilizer including P, Cu and Zn, and removal of sodium and salts from the soil profile may be means of improving the productivity of these soils. Application of organic amendments including manures and crop residues may also be beneficial in increasing the fertility as well as organic carbon content.
机译:由于物理和/或化学限制,埃塞俄比亚的某些土壤降低了植物的生产力。埃塞俄比亚南部周围的问题土壤,包括苏打,酸性和盐渍土壤的形态,物理和化学特性已得到表征,并在本章中进行了描述。目的是表征土壤并更好地了解限制的具体性质。采样了Alage的钠盐土壤,Hagereselam的酸性土壤和Zeway地区的盐渍土壤,以表示问题土壤。确定的土壤特性包括颜色,电导率(EC),结构,稠度,堆积密度,质地,pH,有机碳(OC),总氮,有效磷(P)和钾,可交换的碱和有效的微量营养素。土壤在贫民窟和re石厚度,层位深度,表层土壤和地下层位的结构发育,pH,EC和可利用的养分方面具有很大的异质性。根据土壤分类法和世界土壤资源系统参考库对这些土壤进行分类。 Alage的钠盐土壤具有较高的pH和钠(Na)含量,而OC含量较低,有效磷,铜(Cu)和锌(Zn)较低。附睾被分类为石,并且剖面也沿剖面向下具有粘土含量的变化,以满足具有防锈层的要求,因此这些土壤被分类为典型的Natagids。 Hagereselam土壤的有效磷非常低。发现大多数作物的有效铜和锌含量都处于边际水平。 Hagereselam剖面的地貌呈伞状,表层为伞状,被归类为“典型古埃及”。 Zeway地区的盐渍土中钙含量较高,OC较低。发现该剖面具有状表皮,这些土壤被分类为典型的Haplocambids。施用包括P,Cu和Zn的肥料以及从土壤剖面中去除钠和盐可能是提高这些土壤生产力的手段。施用有机改良剂(包括肥料和农作物残留物)也可能有益于增加肥力以及有机碳含量。

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