Liya Weldegebriel

University of California, Berkeley

Subject Areas: Hydrology

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ABSTRACT:

Soil profile texture analysis was done using hydrometer and dry/wet sieve analyses on total of 27 soil samples from three hillslope transects, three hillslope position and three soil profile depths. Saturated hydraulic conductivity was measured in the field using Guelph Permeameter and soil water potential was measured using WP4C and HYPROP instruments in the lab from 9 soil samples from one hillslope transect. Details on all methods used for soil characterization and soil hydraulic properties as well as background information on Debre Mawi watershed from where the soil samples were taken can be found in https://doi.org/10.1016/j.jhydrol.2022.129031

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ABSTRACT:

Particle size analysis was performed using wet seive analysis on soil samples collected to represent dominant soil types in Lake Tana basin, Ethiopia. Guelph permeameter was used to determine undisturbed saturated hydraulic conductivity (Ksat) at each sample locations.

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ABSTRACT:

Particle size analysis was performed using wet seive analysis on soil samples collected to represent dominant soil types in Lake Tana basin, Ethiopia. Guelph permeameter was used to determine undisturbed saturated hydraulic conductivity (Ksat) at each sample locations.

Show More
Resource Resource

ABSTRACT:

Soil profile texture analysis was done using hydrometer and dry/wet sieve analyses on total of 27 soil samples from three hillslope transects, three hillslope position and three soil profile depths. Saturated hydraulic conductivity was measured in the field using Guelph Permeameter and soil water potential was measured using WP4C and HYPROP instruments in the lab from 9 soil samples from one hillslope transect. Details on all methods used for soil characterization and soil hydraulic properties as well as background information on Debre Mawi watershed from where the soil samples were taken can be found in https://doi.org/10.1016/j.jhydrol.2022.129031

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