Experiment on the strength characteristics and failure modes of granite with pre-existing cracks
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摘要: 為了探究單軸壓縮條件下裂隙巖石的強度特性、裂紋起裂規律及破壞模式, 采用水刀切割技術預制裂隙花崗巖試件, 利用GAW2000剛性試驗機對單裂隙花崗巖試樣進行單軸壓縮試驗.試驗結果表明: 與完整試樣相比, 裂隙巖石試樣單軸抗壓強度明顯降低, 降低幅度與預制裂隙和外荷載方向的夾角β密切相關, β=75°時, 強度最低, 降幅達到84.5%, 基于最大畸變能準則計算了裂隙花崗巖的峰值抗壓強度與裂隙傾角的關系, 試驗結果與數值解吻合; 裂隙的存在改變了巖石的破壞模式, 裂紋起裂角隨裂隙傾角的增加而單調增大, 巖石試樣的破壞模式由剪切破壞為主轉變為張拉破壞占主導.真實裂隙巖石試樣的力學性質及裂紋起裂特征更準確地揭示了單裂隙花崗巖的強度變化規律和破壞模式, 為巖土工程設計和巷道裂隙圍巖體的支護提供科學依據.Abstract: Rock masses are typically anisotropic discontinuous materials composed of joints, fractures, and interlayers. Many instability and failure cases in geotechnical engineering have been induced by the expansion and transfixion of cracks in the rock masses. The mechanical properties and fracture characteristics of joints usually determine the bearing capacities and fracture modes of rocks. As such, the investigation of the crack initiation and expansion law, strength, and deformation characteristics of fractured rock masses has great significance. In this study, the rock samples investigated were taken from deep zones in the Sanshandao gold mine, where the surrounding rock masses are fractured and the maintenance costs of deep tunnels are very high. To investigate the mechanical behaviors of fractured rock masses, uniaxial compression experiments were conducted on granite samples with pre-existing cracks. First, cracks were generated in cylindrical rock samples by a water-jet cutter. Then, the rock samples with cracks and intact samples were compressively tested using a rigid testing machine (GAW2000) to determine their strength characteristics, crack initiation rules, and failure modes. The experimental results show that the uniaxial compressive strength (UCS) values of granite samples with pre-existing cracks are lower than those of intact samples, and the extent of the UCS reduction is closely related to β, i.e., the angle between the pre-existing crack and the direction of the external load. When β is 75°, the UCS values of the samples are at their minimum, and the reduction rate reaches 84.5%. These experimental results are in good agreement with the numerical solution of the maximum distortion energy criterion. Pre-existing cracks change the failure modes of rocks. With an increase in the dip angle of a pre-existing crack, the crack initiation angle increases monotonically, and the failure mode of the rock sample changes from shear failure to tensile failure. The mechanical properties and crack initiation characteristics of real-fracture rock samples can more accurately reveal the strength characteristics and failure modes of fissured granite, and thereby provide a scientific basis for the support of fractured rock masses and geotechnical engineering design.
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表 1 試樣參數
Table 1. Sample parameters
試樣編號 直徑/mm 高/mm 密度/(g·cm-3) I-1 50.20 101.00 2.583 I-2 50.26 100.32 2.595 K-1 50.20 100.00 2.615 K-2 50.10 100.18 2.605 表 2 單軸壓縮下巖樣力學參數
Table 2. Mechanical parameters of rock specimens under uniaxial compression
試樣編號 單軸抗壓強度/MPa I-1 121.85 I-2 131.80 K-1 131.19 K-2 129.53 表 3 不同裂隙傾角的花崗巖試樣強度參數
Table 3. Strength parameters of granite specimens with pre-existing fissures at different angles
裂隙傾角/(°) 平均單軸抗壓強度/MPa 0 116.80 15 98.28 30 79.77 45 44.96 60 44.34 75 25.91 90 39.66 259luxu-164 -
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