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About Characterization of Aquifer System of Different Geological Formations is Based On
This research was conducted in Nekemte area which is bounded in 36o 30’ to 36o 40’ longitude and 9o 05’ to 9o 10’ latitude of western Ethiopia, for quantifying of the aquifer properties depending on the pumping test data as there is limited information on groundwater distribution. The study area was comprises different units like clay sediments, weathered and fractured basalt, and other quaternary sediments; and geological structures causes for different landforms and for primary and secondary permeability and porosity which are plays great role on the aquifer properties. For the achievement of the objectives the data of water bearing horizon, location depth of aquifer, analyze the draw down, discharge rate and pumping duration data, and characterize according to the given data were collected from geological field activities to fulfill the gaps in hydro geological field observation data recording and borehole depth to groundwater, and well completion reports. The discussed result indicates the type of aquifer is confined aquifer with confining layer clay from the top and weathered basalt from below and the pumping test data with maximum and minimum transmissivity of T=9.8*10-4m2/s and T=3.43*10- 4m2/s, respectively, and average transmissivity of T=6.6*10-4m2/s was indicates the heterogeneity of the aquifer materials. From this the transmissivity and hydraulic conductivity vary laterally with in formations, and the property of aquifer it can be inferred that the specific capacity of aquifer is high, but its transmissivity is negligible since porosity is less interconnected.
Detailed Information
| Author: | ['international journal of modern chemistry and applied science'] |
|---|---|
| Publication Year: | 2017 |
| Pages: | 13 |
| Language: | English |
| Format: | |
| Price: | FREE |
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