Fentie Sabiela Fekad, Jembere Kehali, Fekadu Endalkachew, Wasie Dessale
Department of Natural Resources Management, University of Gondar, P.O. Box 196, Gondar, Ethiopia.
Department of Soil and Water Resources Management, Woldia University, P.O. Box 400, Woldia, Ethiopia.
ScientificWorldJournal. 2020 Sep 1;2020:1479460. doi: 10.1155/2020/1479460. eCollection 2020.
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.
长期以来,土地利用变化一直被视为导致土壤物理和化学退化的众多因素之一。本研究旨在评估埃塞俄比亚特吉巴拉流域30年(1989年至2019年)间土地利用和土地覆盖(LULC)变化及其对当前土壤物理和化学性质的累积影响。分别使用ERDAS IMAGINE 2014和ArcGIS 10.4软件进行图像分析和LULC分类。为了测定土壤性质,采用了四种土地利用类型(天然林、桉树种植园、耕地和放牧地)和两个土壤深度(0 - 20厘米和20 - 40厘米)。从每种土地利用类型和土壤深度采集了三份复合土壤样本。对于物理性质(质地和容重)以及化学土壤性质如电导率(EC)、有机质(OM)、总氮(TN)和有效磷(AP)的测定,采用了标准实验室程序。所有研究年份的图像分析结果表明,耕地面积增加是以森林和放牧地为代价的。作为主要影响因素,土地利用对粉粒含量、黏粒含量、有效磷和pH有显著影响,而土壤深度和土地利用的交互作用仅对总氮和有机质有显著影响。有效磷含量最高值(10.1毫克/千克)和最低值(4.9毫克/千克)分别出现在森林地和放牧地。土壤总氮含量在森林地最高(0.32%),在耕地最低(0.06%)。关于有机质含量,最高值(11.0%)和最低值(0.8%)分别出现在森林地和耕地上。总体而言,本研究表明土地利用变化减少了森林和放牧地的面积覆盖,并对土壤性质产生了负面影响。这意味着在没有适合该地区土壤肥力措施的情况下进行土地利用变化可能会加剧土地退化,从而降低研究区域土壤的生产力。