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Land Use and Land Cover Dynamics and Properties of Soils under Different Land Uses in the Tejibara Watershed, Ethiopia

机译:埃塞俄比亚泰吉比亚水域不同土地利用土地利用和土地利用土壤

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Land use changes have long been considered among many factors responsible for physical and chemical soil degradation. This study was conducted to evaluate land use and land cover (LULC) changes and their cumulative effects over 30 years (from 1989 to 2019) on the current physical and chemical properties of soils in the Tejibara watershed, Ethiopia. Image analysis and LULC classifications were performed using ERDAS IMAGINE 2014 and ArcGIS 10.4 software, respectively. For the determination of soil properties, four land use types (natural forest, eucalyptus plantation, cultivated, and grazing lands) and two soil depths (0–20 and 20–40?cm) were used. Triplicate composite soil samples were collected from each land use type and soil depths. For the determination of physical (texture and bulk density) and chemical soil properties such as electrical conductivity (EC), organic matter (OM), total nitrogen (TN), and available phosphorus (AP), standard laboratory procedures were employed. The image analysis results for all of the years studied show that cultivated lands have increased in area at the expense of forest and grazing lands. Silt content, clay content, AP, and pH were significantly affected by land use as the main effect while the interaction effects of soil depth and land use were significant for total N and OM only. The highest (10.1?mg/kg) and the lowest (4.9?mg/kg) AP contents were observed in the forest and the grazing lands, respectively. Soil total N content was highest in the forest lands (0.32%) and lowest in cultivated lands (0.06%). Concerning OM content, the highest (11.0%) and the lowest (0.8%) values were recorded in the forest and cultivated lands, respectively. Generally, this study showed that land use changes have reduced the areal coverage by forest and grazing lands and have negatively affected the soil properties. This implies that land use change without soil fertility measures that are appropriate to the area could cause enhanced land degradation and thereby reduce the productivity of the study area soils.
机译:陆地利用变化已经考虑了负责物理和化学土壤退化的许多因素之间。本研究进行了评估土地利用和陆地覆盖(LULC)变化及其累积效应超过30年(从1989年至2019年)关于Tejibara流域的当前物理和化学性质,埃塞俄比亚。使用Erdas Imagine 2014和ArcGIS 10.4软件进行图像分析和LULC分类。用于测定土壤性质,使用四种土地使用类型(天然森林,桉树种植园,栽培和放牧地)和两种土壤深度(0-20和20-40厘米)。从每个土地使用类型和土壤深度收集三份复合土壤样品。为了确定物理(纹理和堆积密度)和化学土壤性质,例如导电性(EC),有机物(OM),总氮(TN)和可用磷(AP),标准实验室程序。研究结果的图像分析结果显示,耕地在森林和放牧地区的面积上增加了耕地。淤泥含量,粘土含量,AP和pH值受到土地利用作为主要效果的显着影响,而土壤深度和土地使用的相互作用效应仅为总N和OM。在森林和放牧地区分别观察到最高(10.1μmg/ kg)和最低(4.9×mg / kg)AP内容物。土壤总量N含量在林地(0.32%)和耕地中最低(0.06%)。关于OM含量,分别在森林和耕地中记录了最高(11.0%)和最低(0.8%)值。一般来说,这项研究表明,土地利用变化减少了森林和放牧土地的面积覆盖,并对土壤性质产生负面影响。这意味着土地利用改变没有适合该地区的土壤肥力措施可能导致降低土地退化,从而降低了研究区土壤的生产率。

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