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Birhanu E Akalu

Susceptibility of fine grained soils to swelling and shrinkage problems is crucial for safe design of infrastructure, construction and maintenance. However, quantification of soil response and measurement of their geotechnical properties... more
Susceptibility of fine grained soils to swelling and shrinkage problems is crucial for safe design of infrastructure, construction and maintenance. However, quantification of soil response and measurement of their geotechnical properties is time taking, expensive and involves destructive tests. Therefore, dependable forecasting models are necessary that calculate swell percentage from results of quick, inexpensive and non-destructive tests. In this paper, a three-layer feedforward neural network (ANN-TFN) was applied in order to envisage swell percentage of fine grained soils and the results were compared with that of multiple regression (MR). The parameters considered as input were activity, clay, liquid limit, plastic limit, plasticity index and fines while swell percentage was used as output. The best ANN-TFN model demonstrated root mean square errors (RMSE) of 1.529, sum of squares errors (SSE) of 369.3, and coefficient of correlation (R 2) of 0.80. MR model displayed 1.756 (RMSE), 487.2 (SSE), and 0.508 (R 2). The maximum R 2 values obtained by simple regression was 0.5. Overall, the established three-layer feedforward neural network models (ANN-TFN 1-6) showed significantly higher prediction performances than either multiple regression or simple regression models. Moreover, the use of Levenberg-Marquardt as training parameter and tan sigmoid as transfer function were noted to be more appropriate for good prediction performance in this problem. Hence, the result of the present study concludes that practice of the ANN-TFN model to determine swell percentage of fine grained soil is a promising approach for increasing the confidence of making accurate decisions during the soil engineering works.
Susceptibility of fine grained soils to swelling and shrinkage problems is crucial for safe design of infrastructure, construction and maintenance. However, quantification of soil response and measurement of their geotechnical properties... more
Susceptibility of fine grained soils to swelling and shrinkage problems is crucial for safe design of infrastructure, construction and maintenance. However, quantification of soil response and measurement of their geotechnical properties is time taking, expensive and involves destructive tests. Therefore, dependable forecasting models are necessary that calculate swell percentage from results of quick, inexpensive and non-destructive tests. In this paper, a three-layer feedforward neural network (ANN-TFN) was applied in order to envisage swell percentage of fine grained soils and the results were compared with that of multiple regression (MR). The parameters considered as input were activity, clay, liquid limit, plastic limit, plasticity index and fines while swell percentage was used as output. The best ANN-TFN model demonstrated root mean square errors (RMSE) of 1.529, sum of squares errors (SSE) of 369.3, and coefficient of correlation (R2) of 0.80. MR model displayed 1.756 (RMSE), 487.2 (SSE), and 0.508 (R2). The maximum R2 values obtained by simple regression was 0.5. Overall, the established three-layer feedforward neural network models (ANN-TFN 1-6) showed significantly higher prediction performances than either multiple regression or simple regression models. Moreover, the use of Levenberg–Marquardt as training parameter and tan sigmoid as transfer function were noted to be more appropriate for good prediction performance in this problem. Hence, the result of the present study concludes that practice of the ANN-TFN model to determine swell percentage of fine grained soil is a promising approach for increasing the confidence of making accurate decisions during the soil engineering works.
A Thesis Submitted to the School of Graduate Studies in Partial Fulfillment of the Requirement for the Degree of Master of Science in Engineering Geology
In the present study landslide hazard zonation (LHZ) was carried out in an area around Alemketema town, central Ethiopia, about 120 km north of Addis Ababa. For LHZ map preparation, GIS based expert evaluation technique was followed. The... more
In the present study landslide hazard zonation (LHZ) was carried out in an area around Alemketema town, central Ethiopia, about 120 km north of Addis Ababa. For LHZ map preparation, GIS based expert evaluation technique was followed. The parameters considered are; slope geometry, slope material, structural discontinuities, landuse and landcover, groundwater, seismicity, rainfall and manmade activities. For landslide hazard evaluation the study area was divided into 273 slope facets and thematic layers on slope facets and intrinsic parameters were prepared in GIS environment from secondary data, topographical map and satellite images. Later, primary data on various parameters was collected facet wise from the field and as per actual observations suitable modifications were made to the thematic maps. Further, geo-processing in GIS environment was done to know the type of parameter classes that fall within each slope facet. Based on the presence of various intrinsic and triggering parameters class within a slope facet, appropriate ratings were assigned to the parameters as per expert evaluation. Later, sum total of all ratings for various parameters form the basis to prepare the LHZ map in GIS. As per prepared LHZ map, 66.9% of the area falls into 'high hazard zone' and 33.1% falls into 'moderate hazard zone'. Validation of this LHZ map revealed that about 80% of past landslides fall within 'high hazard zone'. This reasonably confirms the rationality of adopted methodology, considered parameters and their evaluation in producing LHZ map.