Abstract
Rock mass classification systems are used to categorize and estimate the role of the most significant parameters influencing rock mass behavior to represent an equivalent continuum. Generally, in these methods, the impact of the related parameters is considered uniform in all directions. Hence, these systems describe the rock mass as an isotropic medium. In some cases, in particular, for layered strata and systematically fractured rocks, the assumption of isotropic behavior may not provide realistic results. Hence, in this paper, to characterize the rock mass anisotropy, a directional rock mass rating (DRMR) has been proposed based on the well-known rock mass rating (RMR). So, DRMR provides a three-dimensional rock mass rating, quantitatively. By means of statistical distribution of DRMR, a classification for the degree of anisotropy of rock mass has been proposed. Furthermore, a criterion to identify the prominent rock mass, isotropic/transversely isotropic/anisotropic situation, is presented. Then the stereonet has been used to demonstrate an all-round graphical representation of DRMR. This with DRMR provides an illustrative insight into the actual rock mass condition and can assist to select the appropriate method for further analysis. Also, the method can be used as a basis to develop practical solutions for many rock engineering issues, such as characterizing the mechanical parameters of rock mass as an anisotropic equivalent continuum, selective directional rock mass improvement, and proper selection of rock tunnel and rock cavern alignments. Finally, the results of some practical applications of the method, based on field data, are presented.
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Abbreviations
- A:
-
Constant (Donath, 1961 equation)
- AI :
-
Anisotropy index based on DRMR
- AI m :
-
Anisotropy index of average DRMR
- B:
-
Constant (Tziallas et al. 2013 equation)
- CR k :
-
Condition Rating of kth discontinuity
- CR k i :
-
Condition Rating of kth discontinuity along i-direction
- D:
-
Constant (Donath, 1961 equation)
- Dip :
-
Dip angle of discontinuity set
- Dip ip :
-
Dip angle of isotropic plane of intact rock
- DipDir :
-
Dip direction of discontinuity set
- DipDir ip :
-
Dip direction of isotropic plane of intact rock
- DR1:
-
Directional Rating of uniaxial compressive strength
- DR2:
-
Directional Rating of fracture frequency
- DR3:
-
Directional Rating of discontinuities conditions
- DR4:
-
Directional Rating of groundwater conditions
- DRMR:
-
Directional Rock Mass Rating
- DRMR ave :
-
Average value of DRMR
- DRMR max :
-
Maximum value of DRMR
- DRMR min :
-
Minimum value of DRMR
- GSI:
-
Geological Strength Index
- P wl :
-
Percentage of soft layers thickness in heterogeneous rock strata
- R c :
-
Anisotropy index of intact rock
- R cm :
-
Anisotropy index of rock mass
- RMR:
-
Rock Mass Rating
- RQD:
-
Rock Quality Designation
- RQD i :
-
Rock Quality Designation along i-direction
- \( {\overline{S}}_i \) :
-
Average spacing of discontinuities along i-direction
- UCS i :
-
UCS of anisotropic intact rock along i-direction
- X, Y, Z :
-
Global Cartesian axes
- a :
-
Constant (Hoek-Brown failure criterion)
- c i :
-
Cohesion of intact rock
- c j :
-
Cohesion of discontinuities
- i :
-
Arbitrary direction to calculate DRMR
- k :
-
Discontinuity number (k = 1 to n)
- n :
-
Number of discontinuity sets
- s :
-
Constant (Hoek-Brown failure criterion)
- \( {\overline{s}}^k \) :
-
Average spacing of kth discontinuity set
- u ip :
-
Unit normal vector of isotropic plane of intact rock
- \( {u}_X^{ip} \), \( {u}_Y^{ip} \), \( {u}_Z^{ip} \) :
-
Components of uip in global Cartesian coordinates
- u k :
-
Unit normal vector of kth discontinuity
- \( {u}_X^k \), \( {u}_Y^k \), \( {u}_Z^k \) :
-
Components of uk in global Cartesian coordinates
- v :
-
Unit vector of arbitrary direction i
- v X ,, v Y, v Z :
-
Components of v in global Cartesian coordinates
- v x , v y , v z :
-
Components of v in local Cartesian coordinates
- x, y, z :
-
Local Cartesian axes
- β :
-
Angle between loading direction and isotropic plane/discontinuity
- β m :
-
Angle β at which the UCS of anisotropic rock is minimum
- \( {\theta}_i^k \) :
-
Angle between normal vector of kth discontinuity and i-direction
- \( {\theta}_i^{IP} \) :
-
Angle between normal vector of isotropic plane and i-direction
- λ i :
-
Cumulative linear frequency of discontinuities along i-direction
- λk :
-
linear frequency of kth discontinuity set
- \( {\lambda}_i^k \) :
-
Linear frequency of kthdiscontinuity set along i-direction
- ρ :
-
Trend of arbitrary direction
- ρ d :
-
Trend of pole of discontinuity
- ρ ip :
-
Trend of pole of isotropic plane of intact rock
- σ 1f :
-
Major principal stress at failure
- σ 3 :
-
Confining minor principal stress
- σ ci :
-
Uniaxial compressive strength of intact rock
- \( {\sigma}_{ci}^{max} \) :
-
Maximum uniaxial compressive strength of intact rock
- \( {\sigma}_{ci}^{min} \) :
-
Minimum uniaxial compressive strength of intact rock
- σ cm :
-
Equivalent uniaxial compressive strength of jointed rock mass
- \( {\sigma}_{cm}^{max} \) :
-
Maximum uniaxial compressive strength of rock mass
- \( {\sigma}_{cm}^{min} \) :
-
Minimum uniaxial compressive strength of rock mass
- \( {\sigma}_{ci}^h \) :
-
Equivalent strength of intact rock in heterogeneous medium
- \( {\sigma}_{ci}^S \) :
-
Uniaxial compressive strength of stronger rock layers in heterogeneous medium
- σ cβ :
-
UCS of anisotropic rock at orientation angle β
- φ i :
-
Internal friction angle of intact rock
- φ j :
-
Internal friction angle of discontinuities
- ψ :
-
Plunge of arbitrary direction
- ψ d :
-
Plunge of the pole of discontinuity
- ψ ip :
-
Plunge of pole of isotropic plane of intact rock
- ω :
-
Rotation angle of the local coordinates
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Maazallahi, V., Majdi, A. Directional rock mass rating (DRMR) for anisotropic rock mass characterization. Bull Eng Geol Environ 80, 4471–4499 (2021). https://doi.org/10.1007/s10064-021-02143-3
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DOI: https://doi.org/10.1007/s10064-021-02143-3