Sains Malaysiana 41(3)(2012): 293–297

 

Korelasi Pekali Kekasaran Kekar dengan Sudut Geseran Puncak Satah Ketakselanjaran Batuan Syis, Semenanjung Malaysia

(Correlation of Joint Roughness Coefficient with Peak Friction Angles of Discontinuity Planes  of Schists, Peninsular Malaysia)

 

 

A. Ghani Rafek & M. Hariri Ariffin

Program Geologi, Pusat Pengajian Sains Sekitaran dan Sumber Alam

Fakulti Sains dan Teknologi, Universiti Kebangsaan Malaysia

43600 Bangi, Selangor D.E. Malaysia

 

T.L. Goh*

Geoscience Department, Subsurface Division, Petronas Research Sdn. Bhd.,

Lot 3288 & 3289, Off Jalan Ayer Itam, Kawasan Institusi Bangi, 43000 Kajang

Selangor D.E. Malaysia

 

Diserahkan: 26 April 2011 / Diterima: 19 Ogos 2011

 

 

ABSTRAK

 

Kekasaran permukaan amat mempengaruh tingkah-laku ricihan dan nilai sudut geseran puncak sesuatu satah ketakselanjaran. Oleh yang demikian, kekasaran permukaan merupakan faktor yang penting yang perlu dinilai dalam menentukan kestabilan struktur pengorekan dalam jasad batuan. Beberapa kaedah boleh digunakan untuk menentukan kekasaran permukaan ketakselanjaran. Kertas ini memperkenalkan satu pendekatan yang mudah dalam bentuk dua rumus polinominal yang boleh digunakan untuk mengkorelasi sudut geseran puncak ketakselanjaran (φp) batuan syis segar dan terluluhawa sedikit dengan pekali kekasaran kekar, PKK. Rumus polinominal ini ialah φp= -0.022PKK2 + 3.21PKK + 28.1 untuk ketakselanjaran segar dan φp= -0.025PKK2 + 3.24PKK + 26.6 untuk ketakselanjaran terluluhawa sedikit. Kedua-dua rumus ini memperlihatkan nilai pekali penentuan, R2 = 0.98. Hasil kajian ini menawarkan satu kaedah alternatif penganggaran φp satah ketakselanjaran daripada nilai PKK yang diukur pada permukaan ketakselanjaran di lapangan.

 

Kata kunci: Pekali kekasaran kekar; sudut geseran puncak; syis; ujian kemiringan

 

 

ABSTRACT

 

Shear behavior and value of peak friction angle of a discontinuity plane is strongly controlled by its surface roughness. As such, surface roughness is an important factor to be evaluated in determining the stability of structures excavated in rock body. Several approaches can be adopted for the determination of surface roughness of discontinuities. This paper presents a simple approach, in the form of two polynominal equations to correlate the peak friction angle (φp) with the Joint Roughness Coefficient (JRC) for discontinuity plane in fresh and slightly weathered schists. The polynomial equations are φp= -0.022JRC2 + 3.21JRC + 28.1 for fresh discontinuities and φp= -0.025JRC2 + 3.24JRC + 26.6 for slightly weathered discontinuity. Both equations exhibited coefficient of determination R2= 0.98. These results offer an alternative method to estimate φp of discontinuity planes by measuring the JRC values of the discontinuity planes in the field.

 

Keywords: Joint roughness coefficient; peak friction angle; schists; tilt test

 

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*Pengarang untuk surat-menyurat; email: gdsbgoh@gmail. com

 

 

 

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