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首页> 外文期刊>Journal of Soil Science and Environmental Management >Assessment of selected soil physicochemical properties on different land-use systems and landscape positions at Hamesa watershed, Wolayita zone, Southern Ethiopia
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Assessment of selected soil physicochemical properties on different land-use systems and landscape positions at Hamesa watershed, Wolayita zone, Southern Ethiopia

机译:南埃塞俄比亚南部水田区不同土地利用系统与景观姿势的选定土壤理化性质评价

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The investigation was undertaken at Hamesa watershed of Wolayita Zone with the aim to assess the consequences of land-use systems and topography on the physical and chemical properties of selected soils. Surface soil samples taken at 0-15 and 15-30 cm depths from three land-use systems (enset, grassland and maize fields) were collected under three slope positions (upper, middle and lower). Both the clay and bulk density increased with depth, while total nitrogen (N), OC, available P and micro-nutrients (Fe, Zn, Mn, and Cu) decreased. On the landscape positions, increase in exchangeable Ca and K, pH, bulk density and available Mn down the slope was observed; whereas total N, OC, available P and available Fe showed decreasing trend down the slope. At 0-15 cm soil depth, grassland soils exhibited higher bulk density and lower porosity as a result of livestock movement which was compacted. Grasslands had higher OC and TN compared to the other two land-use systems, due to the accumulation of humus in the root system in the grassland. Application of household refuses and manure contribute to increasing available P, TN, Zn, Ca and K contents in enset farmland. On the contrary, maize land use had lower CEC, K, PBS, Mg, TN and OC, which might be due to crop removal, erosion phenomena, and excessive tillage activities. These results suggest that for sustainable crop production, proper management practices should be in place by considering different slope positions and land-use systems.
机译:该调查是在Wolayita地区的豪达流域进行,旨在评估土地利用系统的后果和地形对所选土壤的物理和化学性质。在三个坡度位置(上部,中下)收集从三个土地使用系统(钻孔,草地和玉米)收集的0-15和15-30cm深度的表面土壤样品。粘土和散装密度都随深度的增加而增加,而总氮气(N),OC,可用的P和微营养(Fe,Zn,Mn和Cu)降低。在景观位置,观察到斜坡的可交换CA和K,pH,批量密度和可用Mn;虽然总N,OC,可用的P和可用FE显示斜坡下降趋势。在0-15厘米的土壤深度下,由于牲畜运动,草地土壤呈现较高的堆积密度和较低的孔隙率,这是压实的。由于草原根系中的腐殖质积聚,草原与其他两种土地使用系统相比,草原与其他两种土地使用系统相比具有更高的OC和TN。家庭拒绝和粪肥的应用有助于在野营农田中增加可用的P,TN,Zn,Ca和K内容。相反,玉米土地使用具有较低的CEC,K,PBS,MG,TN和OC,这可能是由于作物去除,侵蚀现象和过度耕作活动。这些结果表明,对于可持续的作物生产,应通过考虑不同的坡度和土地使用系统来解决适当的管理实践。

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