Drained shear strength parameters of saprock from a weathering profile over porphyritic biotite granite at Km 31 of the Kuala Lumpur - Karak Highway, Peninsular Malaysia

bgsm742022
Author : John Kuna Raj
Publication : Bulletin of the Geological Society of Malaysia
Page : 43 - 53
Volume Number : 74
Year : 2022
DOI : doi.org/10.7186/bgsm74202203

Bulletin of the Geological Society of Malaysia, Volume 74, November 2022, pp. 43 – 53

 

Drained shear strength parameters of saprock from a weathering profile over porphyritic biotite granite at Km 31 of the Kuala Lumpur – Karak Highway, Peninsular Malaysia

 

John Kuna Raj

No. 83, Jalan Burhanuddin Helmi 2, Taman Tun Dr. Ismail, 60000 Kuala Lumpur, Malaysia

Author email address: jkr.ttdi.tmc@gmail.com

 

Abstract: Three broad zones can be differentiated at the weathering profile; an upper, 9.4 m thick, pedological soil (zone I), an intermediate, 31.7 m thick, saprock (zone II) and the bottom bedrock (zone III). The saprock (zone II) comprises gravelly silty sands that distinctly preserve the minerals, textures and structures of the original bedrock and can be separated into sub-zones II A, II B, II C and II D based on differences in preservation of relict structures and content of litho-relicts (core-boulders). To characterize the drained strength of saprock, samples were collected from sub-zones II B, II C and II D, and their physical and soil index properties determined before consolidated, drained triaxial tests were carried out on remolded specimens. Three individual specimens from each sub-zone were consolidated for 24 hours and compressed at a rate of 0.152 mm/min under confining pressures of 138 kPa, 207 kPa and 276 kPa. The tests yielded effective cohesions (c’) of 30.6 kPa, 9.5 kPa, and 20.2 kPa, and friction angles of 33.2°, 31.4° and 34.4°, for the samples from sub-zones II B, II C and II D, respectively. Regression analyses show effective cohesions (c’) to increase with increasing moisture contents retained at 4.19 pF (1,500 kPa) suction; a feature indicating the influence of negative pore water pressures (matric suction). Regression analyses also show effective friction angles to increase with increasing sand, and sand and gravel, contents; a feature indicating increased inter-locking and resistance to displacement of coarse particles during shear. It is concluded that the saprock is characterized by an average effective cohesion of 14.5 kPa, and friction angle of 34.3°; these parameters influenced by the moisture content retained at 1,500 kPa suction, and the sand and gravel contents.

 

Keywords: Consolidated drained triaxial tests, saprock, gravelly silty sand, effective cohesion, effective friction angle

 

References

Bishop, A.W., & Henkel, D.J., 1957. The measurement of soil
properties in the Triaxial Test. Edward Arnold, London. 189 p.

Brand, E.W., 1982. Analysis and design in residual soils.
Proceedings Conference on Engineering & Construction in Tropical &
Residual Soils, ASCE, Honolulu, Hawaii, 89-129.

Dearman, W.R., 1974. Weathering classification in the
characterization of rock for engineering purposes in British practice. Bulletin
International Association of Engineering Geology, 9, 33-42.

Easton, Z.M., 2016. Soil and soil water relationships. College
Agriculture & Life Sciences, Virginia State University, Publication
BSC-194P (https://ext.vt.edu>agriculture>water). 9 p.

Faisal, H.A., Bujang B.K. Huat, & Low, T.H., 2005. Infiltration
characteristics of granitic residual soil of various weathered grades. American
Journal Environmental Sciences, 1, 64-68.

GSL (Geological Society of London), 1990. Tropical residual soils.
Geological Society Working Group Report, Quarterly Journal Engineering Geology,
23, 1-102.

Haile, N.S., Stauffer, P.H., Krishnan, D., Lim, T.P., & Ong,
G.B., 1977. Palaeozoic redbeds and radiolarian cherts: Reinterpretation of
their relationships in the Bentong and Raub areas, West Pahang, Peninsular
Malaysia. Bulletin of the Geological Society of Malaysia, 8, 45-60.

IAEG (International Association Engineering Geology), 1981. Rock and
soil description for engineering geological mapping. Bulletin International
Association of Engineering Geology, 24, 235-274.

Lambe, T.W., & Whitman, R.V., 1973. Soil mechanics. Wiley
Eastern Private Ltd., New Delhi. 553 p.

Leong, E.C., Rahardjo, H., & Fredlund, D.D., 2001. Application
of unsaturated soil mechanics in geotechnical engineering. Proceedings 8th East
Asian Pacific Conference on Structural Engineering & Construction,
Singapore, 5-7 Dec. 2001, 67 p.

Lumb, P., 1975. Slope failures in Hong Kong. Quarterly Journal
Engineering Geology, 8, 31-36.

Mohd Raihan, T., Md. Kamal Hossain, Zamri Chik, & Khairul Anuar
Mohd Nayan, 1998. Geotechnical behavior of a Malaysian residual granitic soil.
Pertanika Journal of Science & Technology, 7(2), 151-169.

Ng, T.F., 1992. Petrography, structure and geotechnical studies of
the Kuala Lumpur Granite, eastern part of Kuala Lumpur, Peninsular Malaysia.
M.Phil. Thesis, Institute for Advanced Studies, University of Malaya. 527 p.

Rahardjo, H., Leong, E.C., & Rezaur, R.B., 2003. Shear strength
characteristics of residual soils in Singapore. Keynote Lecture, Proceedings
International Conference on Problematic Soils, Nottingham, July 28-30, 2003,
United Kingdom. 12 p.

Rahardjo, H., Aung, K.K., Leong, E.C., & Rezaur, R.B., 2004.
Characteristics of residual soils in Singapore as formed by weathering.
Engineering Geology, 73, 157-169.

Raj, J.K., 1983. A study of residual soils and their cut slope
stability in selected areas of Peninsular Malaysia. Ph.D. Thesis, Faculty of
Science, University of Malaya. 462 p.

Raj, J.K., 1985. Characterization of the weathering profile
developed over a porphyritic biotite granite bedrock in Peninsular Malaysia.
Bulletin International Association of Engineering Geology, 32, 121-128.

Raj, J.K., 2009. Geomorphology. In: Hutchison, C.S., & D.N.K.
Tan (Eds.), Geology of Peninsular Malaysia, University of Malaya and Geological
Society of Malaysia, Kuala Lumpur, 5-29.

Raj, J.K., 2010. Soil moisture retention characteristics of earth
materials in the weathering profile over a porphyritic biotite granite.
American Journal of Geosciences, 1, 12-20.

Raj, J.K., 2021. Saturated hydraulic conductivity (Ks) of earth
materials in the weathering profile over a porphyritic biotite granite in
Malaysia. Bulletin of the Geological Society of Malaysia, 71, 1-8.

Rao, S.M., & Revanasiddappa, K., 2005. Role of micro-fabric in
matrix suction of residual soils. Engineering Geology, 80, 60-70.

Salih, A.G., 2012. Review on granitic residual soils: Geotechnical
properties. Electronic Journal Geotechnical Engineering, Bundle T, 17,
2645-2658.

Salih, A.G., & Kassim, K.A., 2012. Effective shear strength
parameters of remolded residual soil. Electronic Journal Geotechnical
Engineering, Bundle C, 17, 243-253.

Salih, A,G., & Ismael, A,M., 2019. Influence of clay contents on
drained shear strength parameters of residual soil for slope stability
evaluation. International Journal of Geotechnical Construction Materials &
Environment (GEOMATE), 17(59), 166-172.

Tan, Y.C., & Gue, S.S., 2001. The determination of shear
strength in residual soils for slope stability analysis. Proceedings Seminar
Cerun Kebangsaan 2001, Cameron Highlands, 14-15 May 2001, 1-18.

Thamer, A.M., Faisal Hj. Ali, S. Hashim, & Bujang B.K. Huat,
2006. Relationship between shear strength and soil water characteristic curve
of an unsaturated granitic residual soil. American Journal Environmental
Sciences, 2 (4), 142-145.

Thomas, M.F., 1974. Tropical geomorphology – A study of weathering
and landform development in warm climates. Macmillan Press Limited, London. 332
p.

Vanapalli, S.K., Fredlund, D.D., & Clifton, A.W., 1996. Model
for the prediction of shear strength with respect to soil suction. Canadian
Geotechnical Journal, 33(3), 379-392.

Vaughan, P.R., 1988. Characterizing the mechanical properties of in
situ residual soil. Keynote Paper, Proceedings Second International Conference
on Geomechanics in Tropical Soils, Singapore, 2, 469-487.

Wesley, L., 2009. Behaviour and geotechnical properties of residual
soils and allophone clays. Obras y Proyectos, 6, 5-10.

 

Manuscript received 21 December 2020

Received in revised form 26 June 2022

Accepted 5 July 2022

Available online 30 November 2022

 

0126-6187; 2637-109X / Published by the Geological Society of Malaysia.

 

© 2022 by the Author(s). This is an open access article distributed under the terms of the Creative Commons Attribution (CC-BY) License 4.0.

 

DOI: https://doi.org/10.7186/bgsm74202203

 

 


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