Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Biophysical Characteristics of Medo Watershed, Central Rift Valley Area of Ethiopia

View through CrossRef
Abstract Characterizing the biophysical features at a watershed level have a significant input for further improvements to promote sustainable and productive livelihood through the integration of different watershed components in participatory approach. The objective of this study was to assess the current biophysical of characteristics of Medo watershed, West Arsi Zone of Oromia, Ethiopia. To do so relevant data and tools were used; ArcGIS, Microsoft Excel sheet and fundamental formulae were applied for the analysis are some. The results of the study indicated that the major land use types in the watershed are agricultural land covering 50%, vegetation (shrubs, forests and, plantations) covering 24% and settlement covering 16% out of the total land use. Slope gradient of Medo watershed ranges from zero to more than 20 and the slope gradient of 2–5 and 5–10 cover the greatest in area coverage representing 201 ha and 170 ha respectively. We can also observe that about 8% out of the total area is subjected to severe erosion. Sandy clay loam was the dominant soil textural classes in the surface soils and Phaeozems, Retisols and Andosols are the dominant soil types, which cover 57%, 36% and 7% of the sub-watershed area for lower, middle and upper slope positions, respectively. Mean annual rainfall of the area ranges from 960.09 mm at lower part of the watershed to the 1304.93 mm at upper part of the watershed. Accordingly, Medo sub-watershed is laid in majority of at sub humid agro ecological zone. An assessment of the trees within the landscape of watershed showed some remnant natural forests and a wide variety of shrubby vegetation is encountered at all landscapes. About 40 percent of the watershed, is under high to extremely severe soil loss values (> 45 ton per hectare per year). The baseline study also identified that that natural resources degradation such as land, and or/ soil fertility, reduction and recent changes in the areas’ weather condition in line of climate change prevailing in current years are few of the many factors that are contributing to the land and crop productivity reductions in the area. Therefore, prioritizing the identified problem and preparing intervention of different technologies and development plans by participating communities and different potential stakeholders to solve the problems by taking into consideration the existing opportunities of the watershed.
Title: Biophysical Characteristics of Medo Watershed, Central Rift Valley Area of Ethiopia
Description:
Abstract Characterizing the biophysical features at a watershed level have a significant input for further improvements to promote sustainable and productive livelihood through the integration of different watershed components in participatory approach.
The objective of this study was to assess the current biophysical of characteristics of Medo watershed, West Arsi Zone of Oromia, Ethiopia.
To do so relevant data and tools were used; ArcGIS, Microsoft Excel sheet and fundamental formulae were applied for the analysis are some.
The results of the study indicated that the major land use types in the watershed are agricultural land covering 50%, vegetation (shrubs, forests and, plantations) covering 24% and settlement covering 16% out of the total land use.
Slope gradient of Medo watershed ranges from zero to more than 20 and the slope gradient of 2–5 and 5–10 cover the greatest in area coverage representing 201 ha and 170 ha respectively.
We can also observe that about 8% out of the total area is subjected to severe erosion.
Sandy clay loam was the dominant soil textural classes in the surface soils and Phaeozems, Retisols and Andosols are the dominant soil types, which cover 57%, 36% and 7% of the sub-watershed area for lower, middle and upper slope positions, respectively.
Mean annual rainfall of the area ranges from 960.
09 mm at lower part of the watershed to the 1304.
93 mm at upper part of the watershed.
Accordingly, Medo sub-watershed is laid in majority of at sub humid agro ecological zone.
An assessment of the trees within the landscape of watershed showed some remnant natural forests and a wide variety of shrubby vegetation is encountered at all landscapes.
About 40 percent of the watershed, is under high to extremely severe soil loss values (> 45 ton per hectare per year).
The baseline study also identified that that natural resources degradation such as land, and or/ soil fertility, reduction and recent changes in the areas’ weather condition in line of climate change prevailing in current years are few of the many factors that are contributing to the land and crop productivity reductions in the area.
Therefore, prioritizing the identified problem and preparing intervention of different technologies and development plans by participating communities and different potential stakeholders to solve the problems by taking into consideration the existing opportunities of the watershed.

Related Results

Back‐arc rifting in the Izu‐Bonin Island Arc: Structural evolution of Hachijo and Aoga Shima Rifts
Back‐arc rifting in the Izu‐Bonin Island Arc: Structural evolution of Hachijo and Aoga Shima Rifts
Abstract Multi‐ and single‐channel seismic profiles are used to investigate the structural evolution of back‐arc rifting in the intra‐oceanic Izu‐Bonin Arc. Hachijo and Aoga ...
Velocity Modelling and Depth Conversion Uncertainty Mitigation in GS327 Oil Field, in Gulf of Suez Basin
Velocity Modelling and Depth Conversion Uncertainty Mitigation in GS327 Oil Field, in Gulf of Suez Basin
Abstract The Gulf of Suez rift initiated in the Late Oligocene, probably propagating northwards, and intersecting a major east-west structural boundary of Late Eocen...
Effects of Internal Audit Function on Financial Performance in Rift Valley Bottlers Limited Eldoret, Kenya
Effects of Internal Audit Function on Financial Performance in Rift Valley Bottlers Limited Eldoret, Kenya
The purpose of this study was to investigate effect of internal audit function on financial performance of Rift Valley Bottler’s Limited, Eldoret. The researcher seeks to answer th...
Magmatic centers and rift segmentation: insights from the Late Quaternary Menengai Caldera, Central Kenya Rift
Magmatic centers and rift segmentation: insights from the Late Quaternary Menengai Caldera, Central Kenya Rift
<p>In magmatically active continental rifts, crustal deformation is often accompanied by caldera volcanism along the rift axis. These caldera volcanoes help to charac...
Early onshore basaltic alteration and its natural hydrogen potential in the Asal–Ghoubbet rift, Republic of Djibouti.
Early onshore basaltic alteration and its natural hydrogen potential in the Asal–Ghoubbet rift, Republic of Djibouti.
The East African Rift (EAR) is a large opening system that allows the observation of all stages of rift evolution from continental opening in the south to oceanization in the north...
Groundwater Recharge Estimation in Upper Gelana Watershed, South-Western Main Ethiopian Rift Valley
Groundwater Recharge Estimation in Upper Gelana Watershed, South-Western Main Ethiopian Rift Valley
Estimating the spatial and temporal patterns of groundwater recharge through integrated water balance modeling plays an important role in sustainable groundwater resource managemen...
Discovery of Intracratonic Rift in the Upper Yangtze and Its Control Effect on the Formation of the Anyue Giant Gas Field
Discovery of Intracratonic Rift in the Upper Yangtze and Its Control Effect on the Formation of the Anyue Giant Gas Field
Abstract —According to drilling and seismic data, the Late Sinian–Early Cambrian intracratonic rift was found in the Deyang–Anyue area of the Upper Yangtze craton. T...

Back to Top