SciELO - Scientific Electronic Library Online

 
vol.20 issue2Compaction and Collapse Characteristics of Dune Sand Stabilized with Lime-Silica Fume Mix author indexsubject indexarticles search
Home Pagealphabetic serial listing  

Services on Demand

Journal

Article

Indicators

Related links

  • On index processCited by Google
  • Have no similar articlesSimilars in SciELO
  • On index processSimilars in Google

Share


Earth Sciences Research Journal

Print version ISSN 1794-6190

Abstract

IKENNA NKPADOBI, Johnbosco; KUNA RAJ, John  and  FATT NG, Tham. Classification of cut slopes in weathered meta-sedimentary bedrocks. Earth Sci. Res. J. [online]. 2016, vol.20, n.2, pp.1-9. ISSN 1794-6190.  https://doi.org/10.15446/esrj.v20n2.52781.

In order of abundance, the meta-sedimentary rocks along Pos Selim Highway in Perak state Malaysia comprise quartz mica schist, graphitic schist and quartzite layers. Field investigations revealed that these meta-sedimentary rocks have gradational weathering profile based on differences particularly in textures, hardness, lateral changes in colour, and consistency of material extension. The results from uniaxial compressive strength tests confirmed field observations whereby failure occurred mostly on outcrops having joints almost perpendicular to foliation. From the kinematic analyses, the investigated cut slopes are unstable with possibilities of wedge and planar failures. Application of rock mass classification schemes including Rock Quality Designation (RQD) and Rock Mass Rating (RMR) yielded almost similar poor to good quality ranges for each investigated rock mass. While Slope Mass Rating (SMR) classified the cut slopes from stable to unstable slopes, this study categorized them into one actively unstable, four marginally stable and five stable slopes.

Keywords : Weathering; Uniaxial Compressive Strength; Slope stability; Rock Quality Designation; Rock Mass Rating; Slope Mass Rating.

        · abstract in Spanish     · text in English     · English ( pdf )

 

Creative Commons License All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License