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Dynamics of soil fertility as influenced by different land use systems and soil depth in west Showa zone, Gindeberet district, Ethiopia

机译:埃塞俄比亚金德贝雷特区昭和西部地区不同土地利用方式和土壤深度对土壤肥力的影响

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Land use change from natural forest to cultivated land, grazing land and subsequent changes in soil physicochemical properties was widespread in Ethiopia. Thus, assessing land use-induced changes in soil properties are essential for addressing the issues of agro-ecosystem transformation and sustainable land productivity. The aim of the study was to determine selected soil physicochemical properties of forest land, cultivated land and grazing land and make investigation among the soil properties. Standard procedures were employed for the analyses of soil parameters. One way ANOVA was employed to compare the soil parameters at particular and overall soil depth. Textural class of all land use types was clay indicating similarity in parent materials distribution of bulk density in all soil depths of cultivated land were higher compared to both forest and grazing land. Soil moisture content was significantly increasing with increasing soil depths. The highest soil pH in all soil depth was observed under forest land compared to both grazing and cultivated land. The highest soil OM contents were observed in the surface soils (0-10 cm) of forest land while least Figures were from subsurface (10-20 cm) layers of the cultivated land. TN, CEC, exchangeable (Ca, Na and Mg) of the forest land soil were improved when compared with both cultivated and grazing land soil.
机译:在埃塞俄比亚,土地利用从天然林变为耕地,放牧地,其后土壤理化性质发生了广泛变化。因此,评估土地利用引起的土壤性质的变化对于解决农业生态系统转型和可持续土地生产力的问题至关重要。研究的目的是确定林地,耕地和牧场的土壤理化性质,并对土壤性质进行调查。采用标准程序分析土壤参数。一种方法是采用ANOVA比较特定深度和整体土壤深度的土壤参数。所有土地利用类型的质地类别均为黏土,表明在所有耕地土壤深度中,母体材料的堆积密度分布相似,高于森林和牧场。随着土壤深度的增加,土壤水分含量显着增加。与放牧和耕地相比,林地下所有土壤深度的土壤pH最高。在林地表层土壤(0-10厘米)中观察到最高的土壤有机质含量,而最少的数字来自耕地的表层(10-20厘米)。与耕地和草场土壤相比,林地土壤的TN,CEC,可交换性(钙,钠和镁)均得到改善。

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