埃塞俄比亚东南部巴莱高原奥罗米亚 Dinsho 县 Danka 流域不同土地利用类型下的土壤肥力评估和地形图绘制

M. Eshetu, Lemma Wogi, Negash Demissie
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引用次数: 0

摘要

土壤肥力评估和绘图是埃塞俄比亚高地(如巴勒高地)起伏坡耕地提高肥料使用效率、决策者、规划者和土壤管理的基础。这项研究旨在评估和绘制埃塞俄比亚东南部巴莱高原 Dinsho 区 Danka 流域不同土地利用类型下地表序列的土壤肥力状况。在最初的实地勘察调查之后,研究人员从三种土地利用类型(天然林、放牧和耕地)的三个坡度位置,即下坡(0 - 10%)、中坡(10 - 15%)和上坡(15 - 30%),土壤深度为 0 - 20 厘米处,制备了 54 份复合土壤样本。最后,使用 ArcGIS 软件 10.5 中的 IDW 插值技术对实验室结果进行插值,绘制土壤肥力状况图,并使用 R 软件 4.1.1 版对平均值分离进行进一步分析。研究结果表明,该研究的土壤质地等级在上坡、中坡和下坡位置分别为壤土至粘壤土、粘壤土和粘土至粘壤土。研究结果显示,土壤 pH 值、有机质、全氮、可利用磷和 CEC 值的变化范围分别为 5.81 - 6.66%、2.07 - 6.25%、0.13 - 0.71%、2.83 - 17.56 克/千克和 14.04 - 38.80 毫摩尔(+)/千克。在本研究中,丹卡流域的大部分土壤肥力状况为:天然林 > 草地 > 耕地,下坡 > 中坡 > 上坡。总之,导致该地区土壤肥力状况下降的主要因素是单一作物种植、作物秸秆全部清除、水土流失、养分淋失和土壤管理不当。本次研究的结果为农民、规划者、决策者和其他农业相关利益方的工作提供了依据。在所有坡位的耕地上,最好采用生物物理土壤保持措施进行综合土壤肥力管理。此外,建议在丹卡流域的起伏田地开展基于坡位的作物响应肥料评级研究,以实现农业精准化,确保粮食安全。
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Soil Fertility Assessment and Mapping under Different Land Use Types along Toposequence at Danka Watershed in Dinsho Districts of Bale Highland Oromia, Southeastern Ethiopia
Soil fertility assessment and mapping bases, to increase fertilizer usage efficiency, decision-makers, planners, and soil management in undulating slopes farming of Ethiopian highlands like Bale Highland. The study aimed to assess and map soil fertility status along toposequence under different land use types at the Danka watershed of Dinsho District Bale Highland, Southeastern Ethiopia. Following the initial reconnaissance field survey, 54 composite soil samples were prepared from the three land use types (natural forest, grazing, and cultivated) at three slope positions lower (0 - 10%), middle (10 - 15%), and upper (15 - 30%) at a soil depth of 0 to 20 cm. Finally, the laboratory results were interpolated using the IDW interpolation technique in ArcGIS software 10.5 for the soil fertility status map and further analyzed using R software 4.1.1 Version for mean separation. The study findings indicate that the soil texture class of the study was loam to clay loam, clay loam, and clay to clay loam at the upper, middle, and lower slope positions, respectively. The finding revealed that the values varied from 5.81 – 6.66, 2.07 – 6.25%, 0.13 – 0.71%, 2.83 – 17.56 gm/kg, and 14.04 -38.80 cmol (+)/kg) for the soil pH, organic matter, total nitrogen, available phosphorus, and CEC, respectively. In this study, most of the soil fertility status of the Danka watershed was as follows: natural forest > grassland > cultivated land use types and lower slope > middle slope > upper slope positions. In conclusion, the main factors contributing to the area's declining soil fertility status were monocropping, total crop residue removal, soil erosion, nutrient leaching, and inadequate soil management. The results of the current study offer the basis for the work of farmers, planners, decision-makers, and other agriculture-related stakeholders. Integrated soil fertility management with biophysical soil conservation measures is advisable for cultivated land at all slope positions. Further, a study on slope position-based crop response fertilizer rating for agricultural precision and ensuring food security is recommended in undulating fields of the Danka watershed.
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