Effects of land uses and slope gradients on soil physicochemical properties in Woynwha watershed, Northwest Ethiopia

IF 1.3 Q3 AGRONOMY
Workineh Ejigu Mesfin, Degitu Wassie, Temesgen Gashaw Tarkegn, Yihenew G. Selassie, Eyayu Molla
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Abstract

Soil quality degradation has become a major problem that results in low agricultural productivity and increasing food insecurity in sub-Saharan Africa. Improving our understanding of how different land uses and slope positions affect soil properties is critical for developing best land management practices. The objective of this study was to examine effects of land uses and slope gradients on physicochemical properties of the soil in the Woynwha watershed, Northwest Ethiopia. Composite soil samples were collected from 0- to 20-cm depth in three major land uses (natural forest, cultivated, and grazing lands) and three slope positions (upper, middle, and lower) with three replications using an auger. In addition, undisturbed soil samples were collected using a core sampler for bulk density analysis. The collected soil samples were analyzed following standard procedures. The variation in soil properties among land uses and slope positions on soil properties was determined using analysis of variance. Means comparison was performed using the least significant difference test at a 5% significance level. The results revealed that land use types and slope gradients showed statistically significant (p < 0.01) differences in sand, silt, clay, bulk density, pH, available phosphorus (Av P), total nitrogen (TN), organic carbon (OC), cation exchange capacity (CEC), and exchangeable bases of the studied soil. The highest mean values of bulk density (1.64 g cm−3) and lowest total porosity (37.67%) were measured under grazing lands at steeper slopes. On the other hand, the highest total porosity (64.30%), clay (59.33%), silt (21.33%), soil pH (6.62), OC (3.58%), TN (0.32%), CEC (51.20 cmolc kg−1), Ca2+ (11.27), Mg2+ (2.50), K+ (1.63), and Na+ (0.43 cmolc kg−1) were observed in the lower slopes of natural forest. The highest (6.0 mg kg−1) and lowest (2.33 mg kg−1) contents of Av P were recorded in croplands of lower slopes and grazing lands of upper slopes, respectively. Hence, we conclude that integrated nutrient management and sound land use planning should be implemented for improving soil fertility and crop productivity in the study area and others having similar environment. However, soil properties variability under different depths and agroecologies needs to be examined through further research.

埃塞俄比亚西北部wynwha流域土地利用和坡度对土壤理化性质的影响
土壤质量退化已成为导致撒哈拉以南非洲农业生产力低下和粮食不安全加剧的一个主要问题。提高我们对不同土地用途和斜坡位置如何影响土壤性质的理解,对于制定最佳土地管理实践至关重要。本研究的目的是研究土地利用和坡度对埃塞俄比亚西北部温华流域土壤理化性质的影响。在3个主要土地利用(天然林、耕地和放牧地)和3个斜坡位置(上、中、下),从0 ~ 20 cm深度采集复合土壤样本,使用螺旋钻进行3次重复。此外,未受干扰的土壤样品收集使用芯取样器进行容重分析。采集的土壤样品按照标准程序进行分析。利用方差分析确定了不同土地利用方式和坡位对土壤性质的影响。采用5%显著性水平下的最不显著差异检验进行均值比较。结果表明,土地利用类型和坡度具有显著的统计学意义(p <;0.01)所研究土壤的砂、粉、粘土、容重、pH、有效磷(Av P)、全氮(TN)、有机碳(OC)、阳离子交换容量(CEC)和交换碱的差异。在坡度较陡的放牧区,容重均值最高(1.64 g cm−3),总孔隙度均值最低(37.67%)。土壤总孔隙度(64.30%)、粘土(59.33%)、粉砂(21.33%)、pH(6.62)、OC(3.58%)、TN(0.32%)、CEC (51.20 cmolc kg - 1)、Ca2+(11.27)、Mg2+(2.50)、K+(1.63)和Na+ (0.43 cmolc kg - 1)均在天然林下坡区最高。土壤中有机磷含量最高的是下坡农田(6.0 mg kg - 1),最低的是上坡放牧地(2.33 mg kg - 1)。因此,研究区和其他环境相似的地区应实施综合养分管理和合理的土地利用规划,以提高土壤肥力和作物生产力。然而,不同深度和不同农业生态条件下的土壤性质变异性需要进一步研究。
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来源期刊
Agrosystems, Geosciences & Environment
Agrosystems, Geosciences & Environment Agricultural and Biological Sciences-Agricultural and Biological Sciences (miscellaneous)
CiteScore
2.60
自引率
0.00%
发文量
80
审稿时长
24 weeks
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