Anisotropy of the strength and deformation behaviors of fractured rock masses is a crucial issue for
design and stability assessments of rock engineering structures, due mainly to the non-uniform and nonregular
geometries of the fracture systems. However, no adequate efforts have been made to study this
issue due to the current practical impossibility of laboratory tests with samples of large volumes containing
many fractures, and the difficulty for controlling reliable initial and boundary conditions for
large-scale in situ tests. Therefore, a reliable numerical predicting approach for evaluating anisotropy of
fractured rock masses is needed. The objective of this study is to systematically investigate anisotropy of
strength and deformability of fractured rocks, which has not been conducted in the past, using a numerical
modeling method. A series of realistic two-dimensional (2D) discrete fracture network (DFN)
models were established based on site investigation data, which were then loaded in different directions,
using the code UDEC of discrete element method (DEM), with changing confining pressures. Numerical
results show that strength envelopes and elastic deformability parameters of tested numerical models
are significantly anisotropic, and vary with changing axial loading and confining pressures. The results
indicate that for design and safety assessments of rock engineering projects, the directional variations of
strength and deformability of the fractured rock mass concerned must be treated properly with respect
to the directions of in situ stresses. Traditional practice for simply positioning axial orientation of tunnels
in association with principal stress directions only may not be adequate for safety requirements.
Outstanding issues of the present study and suggestions for future study are also presented.
Anisotropy of the strength and deformation behaviors of fractured rock masses is a crucial issue fordesign and stability assessments of rock engineering structures, due mainly to the non-uniform and nonregulargeometries of the fracture systems. However, no adequate efforts have been made to study thisissue due to the current practical impossibility of laboratory tests with samples of large volumes containingmany fractures, and the difficulty for controlling reliable initial and boundary conditions forlarge-scale in situ tests. Therefore, a reliable numerical predicting approach for evaluating anisotropy offractured rock masses is needed. The objective of this study is to systematically investigate anisotropy ofstrength and deformability of fractured rocks, which has not been conducted in the past, using a numericalmodeling method. A series of realistic two-dimensional (2D) discrete fracture network (DFN)models were established based on site investigation data, which were then loaded in different directions,using the code UDEC of discrete element method (DEM), with changing confining pressures. Numericalresults show that strength envelopes and elastic deformability parameters of tested numerical modelsare significantly anisotropic, and vary with changing axial loading and confining pressures. The resultsindicate that for design and safety assessments of rock engineering projects, the directional variations ofความแข็งแรงและ deformability ของมวลหิน fractured กังวลต้องถือว่าถูกต้อง ด้วยความเคารพให้คำแนะนำของความเครียดใน situ ปฏิบัติแบบดั้งเดิมสำหรับเพียงตำแหน่งแนวแกนของอุโมงค์ในความสัมพันธ์กับความเครียดหลัก ทิศทางเท่านั้นไม่ได้เพียงพอสำหรับความต้องการความปลอดภัยนอกจากนี้ยังมีแสดงโดดเด่นประเด็นของการศึกษาปัจจุบันและข้อเสนอแนะสำหรับการศึกษาในอนาคต
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