Effects of Physical Soil and Water Conservation Structures and Slope Gradients on Soil Physicochemical Properties in West Oromia, Ethiopia

2019 ◽  
Vol 15 (1) ◽  
pp. 1-7
Author(s):  
Muktar Mohammed ◽  
Gutema Takele ◽  
Kibebew Kibret
2020 ◽  
Author(s):  
Siraj Mammo ◽  
Adugna Tolesa ◽  
Eve Bohnett

Abstract BackgroundLand degradation in the form of soil erosion and fertility depletion is the major environmental problem in Ethiopia. However to curb this problem, Soil and Water conservation (SWC) measures are commonly practiced in many rural parts of Ethiopia. This study was conducted to assess the effects of SWC measures on selected soil quality indicators in Ejersa Lafo District. For this study two peasant associations (kebeles) were selected from the district based on the severity of soil erosion and information on SWC practices. A total of 12 composite soil samples from soil 0 to 20cm depth from two sub watersheds with SWC and without SWC practices at Jamjam laga batu and Koriso Odo guba from three landscape positions (upper slope, middle slope, and bottom) were collected. All the soil samples were analyzed following the standard and recommended procedures in Ambo University chemistry laboratory and subjected to ANOVA using the SPSS computer program. ResultMost of the selected soil physicochemical properties were affected by watershed management intervention. Comparing the two farmlands, the highest bulky density of 1.37gcm-3 was observed from unconserved farmland. The results of the study also showed higher values of Soil electrical conductivity (EC), Total nitrogen (TN), Cation exchange capacity (CEC), Soil Organic matter (SOM), Organic Carbon, Available Phosphorus (Av. P) and Available Potassium (Av. K) in conserved land and those all significantly varied between farm plots. On the other hand, Sandy, pH, SOM, TN, Av. P and Av. K values were significantly affected (p<0.05) by slope and all increased from upper (>30%), middle (15-30%) and lower (8-15%). ConclusionThe contribution of watershed management intervention to improve soil physicochemical properties is significant in the study area as it improved some of the selected soil physicochemical properties of soil. Furthermore, efforts are required to enhance community adoption towards soil and water conservation. Additionally, further research has to be carried out on socio-economic aspects and impacts of the intervention on crop productivity for better understanding of the sustainable use of the land and to make a comprehensive conclusion.


2021 ◽  
Vol 2021 ◽  
pp. 1-11
Author(s):  
Adugna Tolesa ◽  
Siraj Mammo ◽  
Eve Bohnett

Land degradation in the form of soil erosion and fertility depletion is the major environmental problem in Ethiopia. However, to curb this problem, soil and water conservation (SWC) structures are commonly practiced in many rural parts of Ethiopia. This study was conducted to assess the effects of SWC structures on selected soil physicochemical properties in Ejersa Lafo district. For this study, two kebeles (peasant associations) were selected purposively from the district based on the severity of soil erosion and information on SWC practices. The research design employed in this study was systematic, randomized, complete block design. A total of 12 composite soil samples were collected from the depth of 0 to 20 cm at two subwatersheds, namely, Jamjam laga batu and Koriso Odo guba with SWC and without SWC structures at three landscape positions. All the soil samples were analyzed following the standard and recommended procedures. The effect of independent variables (SWC practices and landscape positions) on the dependent variables (soil properties) was statistically tested using the SPSS computer program 21. In this study, most of the selected soil physicochemical properties were affected by watershed management intervention (SWC) structures. Soil moisture content (SMC), clay, pH, electrical conductivity (EC), total N (TN), available (AP), available K (AK), and organic carbon (OC) were higher in the subwatershed treated with SWC structures (conserved), whereas bulk density, silt, and sand were higher in the subwatershed without SWC structures (nonconserved). Most of the selected soil chemical properties were significantly varied ( p < 0.05 ) between conserved and nonconserved farm land except EC. All the selected soil physicochemical properties did not show any significant variation ( p < 0.05 ) at landscape positions except sandy soil. The physicochemical soil properties of selected parameters were in good conditions in the conserved areas with higher N and OM and lower BD, indicating fertility of the soil compared with the nonconserved land. The implementation of SWC structures improved some of the physicochemical properties of soil, such as SMC, clay particle, pH, EC, total N, AP, AK, and OC in the study area. Furthermore, efforts are required to enhance community adoption towards soil and water conservation. Additionally, further research has to be carried out on socioeconomic aspects and impacts of the intervention on crop productivity for better understanding of the sustainable use of the land.


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