Assessment Slope Stability Based on Deformation of Rock Joints and Soil with Simulation Method

HTML  XML Download Download as PDF (Size: 2428KB)  PP. 983-995  
DOI: 10.4236/ojg.2016.69074    2,519 Downloads   5,073 Views  Citations

ABSTRACT

The first area is rock instability in conglomerates walls, and the second area is soil instability in a slope composed of sand gravel and shale in the south of the study area. In the first area, rock slopes were studied by fractures condition, slope morphology, measured engineering features of rocks, and then interpreted by Dips software to define the fracture types for analysis of block toppling. The rock slope of the area was modeled by Rock plan by adding water penetration and earthquake. The results showed that in dry condition these slopes were stable, but by penetrating water and saturation of the open spaces of the fractures, the block toppling will occur. Also, seismic activities in the area caused the instability of the slopes, and landslide will happen. In the second area, landslides were spoon-shaped type. To investigate the soil slope stability, the condition of slope was modeled by using soil engineering properties and measuring the morphological condition of the slope such as slope dip, layers thickness, layers dip and slope elevation. It was shown instability of the soil slopes. To stabilize the sliding areas, the dip changing method and formation of stepped-style slope were done. However, the new condition changed the formation of sliding areas in the upper most part of the stairs. The retaining walls formed from the local materials were applied to the slope to provide the desire stability.

Share and Cite:

Gol, M. , Keykha, H. and Rahnama-Rad, J. (2016) Assessment Slope Stability Based on Deformation of Rock Joints and Soil with Simulation Method. Open Journal of Geology, 6, 983-995. doi: 10.4236/ojg.2016.69074.

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.