Effects of Slope Position on Soil Physicochemical Properties of Cultivated Land Use Type in Danka Watershed of Dinsho District, Bale Highland, Oromia, Southeast Ethiopia

M. Eshetu, Lemma Wogi
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Abstract

Quantify and understand soil nutrient loss under different undulating topography farming bases for site-specific management and targeted fertilizer application rates. The study aimed to assess the effect of slope positions on soil physicochemical properties at the Danka watershed of Dinsho District Bale Highland, Southeastern Ethiopia. Consequent to the reconnaissance survey, soil samples were taken from the cultivated land use type in three replications at three different soil depths (0-0, 20-40, and 40-60 cm) and three slope positions (upper, middle, and lower), analyzed follow standard laboratory procedure and further analyzed using R software 4.1.1 version. The results showed soil physicochemical properties were significantly (P ≤ 0.05) influenced by the interaction between slope positions and soil depth. The results of soil physical properties varied from 1.29 -1.73 g cm-3, 2.47 – 2.74 g cm-3, 47.80 - 36.75%, 10.78 – 15.11%, 12.76 – 18.16%, and 4.06 – 8.16% bulk density, particle density, total porosity, FC, PWP, and AWHC, respectively. Selected soil chemical properties varied from 5.91 - 6.45, 0.64 - 3.20%, 0.04 - 0.25%, 1.14 - 5.60 gm/kg, and 10.24 - 37.24 cmol (+)/kg) soil pH, organic matter, total nitrogen, available phosphorus, and CEC, respectively. The values of exchangeable bases were concentration increased from the upper slope position toward the lower slope position and with increased soil depth. Soil micronutrients were increased with increased slope and decreased with increased soil depth. The lowest slope position had relatively better soil nutrient contents than other slope positions. It is advised that integrated soil fertility management, biophysical soil and water conservation, and slope-based, site-specific fertilizer rating for advance agricultural precision and ensure food security.
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斜坡位置对埃塞俄比亚东南部奥罗米亚州巴莱高原丁绍区丹卡流域耕地类型土壤理化性质的影响
量化和了解不同起伏地形下的土壤养分流失情况,为因地制宜的管理和有针对性的施肥量提供依据。本研究旨在评估埃塞俄比亚东南部 Dinsho 区 Bale 高地 Danka 流域坡度对土壤理化性质的影响。在勘察调查后,研究人员在三个不同的土壤深度(0-0 厘米、20-40 厘米和 40-60 厘米)和三个坡度位置(上坡、中坡和下坡),分三次重复从耕地类型中采集了土壤样本,按照标准实验室程序进行分析,并使用 R 软件 4.1.1 版本进行进一步分析。结果表明,土壤理化性质受坡度和土壤深度的交互作用影响显著(P ≤ 0.05)。土壤理化性质的结果分别为:容重 1.29 -1.73 g cm-3、2.47 - 2.74 g cm-3、47.80 - 36.75%、10.78 - 15.11%、12.76 - 18.16%、4.06 - 8.16%;颗粒密度、总孔隙度、FC、PWP 和 AWHC 的结果分别为:1.29 - 1.73 g cm-3、2.47 - 2.74 g cm-3、47.80 - 36.75%、10.78 - 15.11%、12.76 - 18.16%、4.06 - 8.16%。土壤 pH 值、有机质、全氮、可利用磷和 CEC 的变化范围分别为 5.91 - 6.45、0.64 - 3.20%、0.04 - 0.25%、1.14 - 5.60 gm/kg 和 10.24 - 37.24 cmol (+)/kg。土壤微量营养元素随坡度增加而增加,随土壤深度增加而减少。与其他坡位相比,最低坡位的土壤养分含量相对较高。建议通过土壤肥力综合管理、生物物理水土保持以及基于坡度、因地制宜的肥料等级评定来提高农业精准度,确保粮食安全。
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