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1.
利用数字式高速摄影与透射式动态焦散线光学技术相结合的方法,对含异型双夹杂三点弯曲梁在冲击载荷作用下的动态断裂力学行为进行了研究.实验研究结果表明:裂纹扩展过程中,裂纹扩展速度v经历了波动性增大再减小的过程;在裂纹扩展至夹杂中间区域过程中,圆形双夹杂对裂纹的阻裂作用最强,三角形双夹杂和正方形双夹杂的阻裂作用较弱;裂纹在距离夹杂较远处向夹杂扩展过程中,裂尖应力强度因子波动性增加;当裂尖靠近夹杂时,其裂尖应力强度因子达到最大值.当裂纹扩展超出夹杂所对应中间区域,裂尖应力强度因子出现波动性降低趋势.研究成果为含异型夹杂结构的强度评估及断裂分析提供实验依据及科学基础.  相似文献   

2.
混凝土结构是一种脆性材料,其抗压强度较高而抗拉强度很低,其破坏源于材料内部原有的微裂纹,通过微裂纹的产生、扩展、贯通,到宏观裂缝出现并扩展,最终导致混凝土破坏的过程。为了延长结构的使用寿命,设计不同的加固方案,采取补救措施。  相似文献   

3.
将动态焦散线方法与高速摄影技术相结合,研究了低速冲击载荷作用下3种异型夹杂(方形夹杂、圆形夹杂和三角形夹杂)与基体裂纹的相互作用.通过记录不同夹杂情况下裂纹尖端自起裂到贯穿的动态焦散斑图,分析了Ⅰ型裂纹的动态应力强度因子KdΙ和裂纹扩展速率v与时间的关系.实验结果表明:不同形状的夹杂会对裂纹尖端产生不同的阻裂效果,其中方形夹杂阻裂效果最明显;裂纹尖端焦散斑的畸变程度受到试件中夹杂形状的影响,圆形和方形夹杂对裂尖焦散斑畸变影响程度较大;三角形夹杂试件在裂纹扩展过程中裂尖动态应力强度因子值普遍高于圆形与方形夹杂试件,3组试件在断裂过程中裂尖由于受到反射波的扰动,其扩展速度、特征尺寸和动态应力强度因子值均呈现一定的波动性.研究结果为含异型夹杂构件的强度设计及抗冲击性能评估提供了依据.  相似文献   

4.
裂隙岩体爆破理论研究进展   总被引:1,自引:0,他引:1  
节理裂隙对岩体爆破效果有很大的影响.本文从裂隙岩体爆破、冲击荷载作用下岩石特性、岩体爆破数值模拟等方面论述、评价了岩体爆破理论的研究现状.在其基础上对节理岩体的质量综合评价、力学模型的研究、数值模拟的研究、理论与试验相结合等方面的发展趋势提出了几点看法.  相似文献   

5.
为了分析不同倾角结构面对裂隙岩体强度及变形性质的影响,本文通过数值模拟的方法,分析了0°、15°、30°、45°、60°、75°、90°7种典型倾角结构面岩体在三轴压缩条件下的应力应变响应,并从微观角度分析了结构面的变形性质.研究结果表明:在相同围压条件下,随着结构面倾角的增大,不同倾角结构面岩石试件抗压强度呈先减小后增大趋势;含有90°倾角结构面的岩石试件的抗压强度与含有0°倾角结构面岩石试件的相等;随着结构面倾角的增大,结构面上的剪应力的变化趋势是由中部向结构面倾向方向的两侧扩展,并且逐渐趋于集中.  相似文献   

6.
应用材料破坏分析软件MFPA2D(Material Failure Process Analysis),模拟了平面应力下双向应力比不断变化条件下脆性材料的不同破坏失稳过程,以玻璃为例,重点研究了玻璃在复杂应力状态下不同双向应力比对脆性材料裂纹扩展和断裂的影响.研究结果表明,裂纹失稳扩展时的应力强度因子值随着双向应力比的升高而升高.该结果证明双向应力确实对脆性材料的断裂韧性有影响.通过将理论分析得出的应变失效准则与数值模拟研究结果及试验结果的比较研究表明,应变失效准则作为脆性材料在双向应力下的断裂准则是可行的.  相似文献   

7.
节理化岩体强度与力学参数估计的地质强度指标GSI法   总被引:2,自引:0,他引:2  
确定大体积节理化岩体强度与力学参数是很困难的,这主要是由于节理化岩体试件尺寸太大及岩体所含节理裂隙所致.然而广义HOEK-BROWN准则的出现,为此提供了解决问题的新途径.本文提出了一种确定大体积节理化岩体强度与力学参数的简易经济的新方法——地质强度指标GSI法.  相似文献   

8.
目前,用强度折减法分析边坡失稳的判据分析都是从边坡破坏的机理出发。本文从边坡破坏机理和有限元自身特点两方面出发,借助ABAQUS有限元软件对两个经典边坡实例进行计算,分析了三种判据的差异性和统一性。最后得出在有限元分析边坡稳定中,塑性区贯通和特征部位的位移发生突变这两种判据具有统一性;有限元计算不收敛与以上两种判据具有差异性;塑性区贯通在边坡破坏机理和有限元计算中存在差异性。  相似文献   

9.
在RMT-B型岩石力学试验机上,对预置倾斜单裂纹的大理岩板试样进行单轴压缩试验,分析了预置裂纹在荷载作用下闭合面摩擦系数及裂纹倾角对裂纹扩展的影响。试验结果表明,当设定摩擦系数后,预置裂纹倾角大于45°时,同样应力水平下裂纹面上有效剪力Q明显趋大;在达到相同有效剪力水平下,预置裂纹倾角大于45°时,所需应力水平值变小,此时预置裂纹倾角为开始裂纹扩展的最不利方向。分析表明,大理岩板中最不利裂纹方位角介于45°~67.5°。该大理岩板材中预置裂纹倾角为60°时,更容易发生裂纹扩展。此外,大理岩板承受单轴压缩时,裂纹扩展与裂纹倾角方向还和裂纹面上摩擦系数相关。裂纹扩展由裂纹面上有效剪力引起,其断裂过程为I-II复合型。  相似文献   

10.
丹江口枢纽泄洪坝段下游基岩冲刷问题的研究   总被引:1,自引:0,他引:1  
总结了20年来丹江口枢纽泄洪坝段下游冲刷坑监测资料,表明岩石破碎断裂带控制最大冲坑部位与范围,裂隙密度、胶结强度、充填质、缓倾角裂隙决定最大冲刷深度。初步统计分析说明坚硬岩质河床冲刷坑的深度、形态、发展速度均受地质条件的制约。其中断层破碎带的性质及形状,节理裂隙充填胶结程度以及相互组合起决定性作用。  相似文献   

11.
Under tension and shear conditions related to unloading of rock mass, a jointed rock mass model of linear elastic fracture mechanics is established. According to the model, the equations of stresses, strains and displacements of the region influenced by the crack but relatively faraway the crack (the distance between the research point and the center of the crack is longer than the length of crack) are derived. They are important for evaluating the deformation of cracked rock. It is demonstrated by the comparison between computational results of these theoretical equations and the observed data from unloading test that they are applicable for actual engineering.  相似文献   

12.
To evaluate the columnar jointed basalts in the dam site of Baihetan hydropower station in southwest China, we developed a basic conceptual model of single jointed rock mass. Considering that the rock mass deformation consists of rock block deformation and joints deformation, the linear mechanical characteristics of the cell (including the elastic joints and the nonlinear mechanical behaviors of the cell) with a combined frictional-elastic interface were analyzed. We developed formulas to calculate the rock block deformation, which can be adapted for multiple jointed rock mass and columnar jointed basalts. The formulas are effective in calculating the equivalent modulus of multiple jointed rock mass, and precisely reveal the anisotropic properties of columnar jointed basalts. Furthermore, the in situ rigid bearing plate tests were analyzed and calculated, and the types of loading-unloading curves and the equivalent modulus along different directions of columnar jointed basalts were obtained. The analytical results are in close compliance with the test results.  相似文献   

13.
裂纹顶端的扩展准则   总被引:1,自引:0,他引:1  
在应用断裂力学和塑性力学对裂纹顶端的分析基础上,提出了裂纹顶端塑性区内方向应变能的概念,并建立了基于此概念上的裂纹扩展准则,引入裂纹顶端临界扩展本征区概念,消除了应变能积分中的奇异性。与其它裂纹扩展准则的比较结果表明:在此基础上建立的裂纹扩展准则是合理可行的。  相似文献   

14.
The mechanism and criterion of crack initiation and propagation of rocks were investigated by many researchers,And the creep behaviour of rocks was also theoretically and experimentally studied by some scientists and engineers.The characteristics of crack initation and propagation of rocks under creep condition.however,are very improtant for rock engineering and still not paid enough attention by researchers,In this paper,the criterion and mechanism of crack initiation and propagation under creep condition were investigated using specimens collected from sandstone rock formations outcropping in the Emei Mountain,the Sichuan Province of China.Cuboid specimens under three point bending were used in this investigation.All specimens were classified into four sorts and used for Mode-I fracutre of creep frcture tests.The experimental result shows that due to creep deformation.rock crack will inevitably initialt and propagate under a load of KI,which is less than fracture toughness KIC but not less than a constant(marked as KIC2),KIC2 indicates the ability of rock to resist crack initiation and propagation under creep conditions and is less than fracture tough ness KIC.defined as creep fracture toughness in this paper,KIC2 should be considered as an importnat parameter on design and computation of rock engineering.The microstructureal mechanism for crack initiation and propagation of rock materials under creep condition was introduced based on competitive model between softening effect and hardening effect,and the validity of test result was explained.The test result was also verified in rheological theory.When KI is more than KIC2 but less than KIC,rock crack will initiate and propagate after a time interval of sustained loading under creep condition.In order to find the relation between duration of sustained lading.which can lead to crack initiation and propagation,and the initial stress intensity factor KI,an unequal0interval time sequence forecasting and predicting model was introduced,and the relation was obtained for homogeneous and isotropic fine-grained red sandstone.Finally a modified fracture toughness formula was given,in which the influence of fracture process zone(FPZ) was fully considered.  相似文献   

15.
为了模拟井下压裂作用下胶凝酸和清洁酸作用时的碳酸盐岩破裂机制,了解两种酸液体系作用后的强度劣化效应,进行了拟三轴岩石力学试验以及3-D扫描。试验结果表明:与胶凝酸反应后,碳酸盐岩弹性模量、泊松比和抗压强度均呈降低趋势,其中泊松比降低幅度明显,酸蚀90 min时,降幅达到18.15%;与清洁酸反应后,碳酸盐岩弹性模量、抗压强度在酸蚀初始阶段小幅提高,当酸蚀时间达到90 min后,两者降幅分别为21.04%及23.55%,泊松比降幅为4.36%,岩石力学性质劣化效应明显,脆性指数升高12.09%;与胶凝酸反应90 min后,碳酸盐岩的脆性指数提高58.56%,破裂压力呈下降趋势;与清洁酸反应后,裂缝壁面粗糙程度明显降低,裂缝导流能力呈降低趋势。酸压后的力学性质劣化特征可为酸化压裂设计及参数优化提供基础数据。  相似文献   

16.
针对采用爆破施工时确定参数大多是靠工程经验,而没有进行机理分析问题;通过引入有效应力强度因子,从岩石断裂力学和爆生气准静态理论角度分析了岩石裂纹的启裂、止裂判据和扩展规律,为爆破参数的合理设计提供了理论依据。  相似文献   

17.
Probabilistic analysis of linear elastic cracked structures   总被引:1,自引:0,他引:1  
This paper presents a probabilistic methodology for linear fracture mechanics analysis of cracked structures. The main focus is on probabilistic aspect related to the nature of crack in material. The methodology involves finite element analysis; sta- tistical models for uncertainty in material properties, crack size, fracture toughness and loads; and standard reliability methods for evaluating probabilistic characteristics of linear elastic fracture parameter. The uncertainty in the crack size can have a significant effect on the probability of failure, particularly when the crack size has a large coefficient of variation. Numerical example is presented to show that probabilistic methodology based on Monte Carlo simulation provides accurate estimates of failure prob- ability for use in linear elastic fracture mechanics.  相似文献   

18.
对于岩体力学的学科属性问题,人们一直存在不同的认识。如何正确理解和认识岩体力学的学科属性,对于该学科的教学和研究都具有重要意义。岩体力学发展至今已经形成了多学科交叉的知识体系,如果仍将其看做是力学的一个分支已经不符合该学科的真正涵义。岩体力学研究必须以岩体的地质特征研究为基础,密切结合岩体工程实际,建立正确的力学分析模型。脱离岩体的地质体特征和岩体工程实际将会使岩体力学研究走入误区,并使其研究结果失去实际意义。因此应该将岩体力学看做是工程地质学、土木工程学和力学相互交融而形成的边缘学科,这样认识岩体力学的学科属性才能有利于该学科更好地应用于工程实践。  相似文献   

19.
根据岩石力学的基本原理开发了岩石与岩体力学参数估算的虚拟仿真实验软件,为学生提供虚拟仿真实验。学生通过该软件可进行岩石力学实验、岩石试件物理力学参数分析、岩体结构面识别、岩体力学参数分析的虚拟仿真实验,进而掌握岩石及岩体力学参数的估算方法。该虚拟仿真实验不仅是传统室内岩石力学实验的有益补充,也是对岩体力学参数测定试验的尝试性拓宽,有利于提高学生的学习效果。  相似文献   

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