贵州石漠化地区降雨条件下红粘土剪切强度特性随含水量变化关系探讨

西南喀斯特地区的石漠化已经严重影响了人民正常的生产生活。水土流失是石漠化过程中一个关键环节。喀斯特地区地表广泛覆盖的红粘土在降雨条件下随着含水量的增加和人工垦殖的影响,剪切强度会产生变化,更易发生水土流失。本文以贵州普定石漠化研究区（陈旗村）的红粘土为例,以原状土模拟未经扰动的土样,以重塑土来模拟经过开垦被扰动后的土样,设计了原状土和重塑土在不同含水量下的直剪试验,初步地研究了这一变化规律。结果表明:在含水量大于35%时,石漠化地区红粘土粘聚力和内摩擦角均随着含水量的增加显著降低;在同一含水量水平下,原状土的抗剪强度明显优于重塑土,且随着含水量的增加,重塑土的强度衰减较之原状土快许多,表明了经过人工垦殖后的红粘土在降雨条件下更易发生水土流失。       

不同加载状态下TA2钛合金绝热剪切破坏响应特性

一般认为绝热剪切现象在宏观上表现为材料动态本构失稳,即热软化大于应变硬化.本文采用帽型受迫剪切试样研究TA2钛合金的动态力学特性和本构失稳过程.首先对剪切区加载应力状态进行理论和数值分析,通过合理设计帽型试样,剪切区变形可近似按剪切状态处理;结合二维数字图像相关法(two-dimensional digital image correlation,DIC-2D)直接测试试样剪切区应变演化,给出帽型受迫剪切实验的等效应力-应变响应曲线.进一步,利用Hopkinson压杆对TA2钛合金开展动态压缩及帽型剪切对比试验研究,比较压缩、剪切试验得到的等效应力-应变曲线,采用"冻结"试样方法分析试样中绝热剪切局域化演化过程,探讨不同加载状态下TA2钛合金的绝热剪切破坏现象及其动态力学响应特性.实验结果表明,在塑性变形初始阶段,动态压缩及剪切加载下的等效应力-应变曲线符合较好,但随塑性损伤发展及绝热剪切带形成,两者出现分离,表明损伤及绝热剪切演化过程与应力状态相关.剪切试样实验得到的本构"软化"特性能够反映绝热剪切带起始、破坏演化过程的力学响应特性,而在动态压缩实验中,即使试样中已出现双锥形的绝热剪切带及局部裂纹分布,其表观等效应力-应变曲线并不出现软化特征,动态压缩实验无法得到关于绝热剪切起始、发展以及破坏的本构软化响应特性.     

三轴试验土样剪切破坏过程的判别

本文在土工三轴试验中应用土样全表面变形数字图像测量系统,通过跟踪包裹土样的橡皮膜表面的标记点,得到加载过程中其全表面的变形和应变分布。根据土样表面的应变分布和实测的应力应变关系曲线,可以得到每一时刻土样表面的应力分布。于是,土样表面剪切破坏开始出现的时刻和剪切破坏带贯穿的时刻可分别依据应变和应力判定。依据应变,将橡皮膜上各点的轴向应变的拐点最晚出现的时刻作为剪切带完全贯穿的时刻;依据应力,将全部点中某一个或几个点最早达到峰值应力的时刻作为剪切带开始出现的时刻;土样各点相继达到应力峰值的过程就是剪切破坏的过程。以剪切破坏的起始点和剪切带贯穿的点为分界,土样剪切破坏过程可以划分成三个阶段:破坏前阶段、破坏阶段和破坏后阶段,在不同阶段土样具有不同的变形特点和变形机理。     

卸荷条件下粉质粘土变形性状研究

通过室内应力控制的三轴试验研究卸荷条件下土体的应力-应变关系和孔隙水压力变化特征,得到变形模量的确定方法。研究表明:在初始偏压应力固结条件下,无论是轴向压力保持不变而侧向压力不断卸荷,还是轴向压力和侧向压力同时卸荷,其应力-应变关系均表现为较好的双曲线函数关系。而且,侧向固结压力愈大,强度值愈大。在卸荷过程中,随剪切应力的增大和剪切应变的发展,土样呈现剪胀趋势并在后期产生较大的负孔隙水压力。不排水条件下由于负孔隙水压力的存在,土样的表观强度略有增大。     

一个改进的混凝土非线性双剪切强度准则

通过对混凝土、岩石等材料强度理论的分析研究,基于普遍形式强度理论及双剪切强度理论,考虑混凝土在多轴荷载作用下材料强度性质在π平面和拉伸压缩子午线上不同的变化规律,将混凝土的强度准则定义为两个较大主剪切应力平方和的函数;并考虑其对应剪切应力作用面上的正应力和静水压力的影响,推导了一个考虑中间主应力效应和复杂极限面情况的非线性双剪切强度准则;通过实验数据获得了相关参数。结果表明该强度准则可以较好地描述混凝土材料的破坏特性。     

压缩-剪切复合应力下PMMA材料的静态力学特性研究

通过压缩具有一定倾斜角(0°,10°,15°,20°和25°)试件和双剪切模型试件,实现了单轴压缩、压缩-剪切复合应力以及纯剪切三种应力状态,得到PMMA(聚甲基丙烯酸甲酯)在相应应力状态下的应力-应变曲线,同时对不同应力状态下试件的破坏模式进行了分析。结果表明:在不同受力环境中材料的强度和破坏的机理不同;同单轴压缩状态下相比,材料在压缩-剪切复合应力状态下屈服极限、强度极限以及破坏应变均不同程度的增大,呈现明显的"剪切增强"现象。单轴压缩与压缩-剪切应力状态下试件的破坏模式均为在试件短对角面上出现明显的剪切屈服带,由应力分析得出试件剪应力在短对角面上达到最大,引起在此平面上分子链间滑动从而产生应变软化形成剪切屈服带;双剪切试件的破坏模式为与剪切面呈45°的斜面。     

切口类型变化对复合材料双切口层间剪切强度的影响规律研究

利用三维有限元模型和试验对复合材料双切口试件层间剪切强度进行了研究,通过改变双切口试件的切口类型(标准双切口、半V型切口和V型切口),对比分析切口类型变化对试件剪切面应力水平、破坏模式和剪切强度的影响,对侧面夹具为Hopkinson金属棒的半V型切口试件剪切面应力水平进行了分析。结果表明,三种切口类型的试验都不是单纯、均匀的剪切强度试验:标准双切口(DNS)试件剪切面剪应力分布不均匀,横向压应力较大,它仅能得到复合材料的表观层间剪切强度;半V型切口(0.5DVS)试件剪切面剪应力分布最不均匀,横向压应力较小,所得剪切强度偏小;V型切口(DVS)试件剪切面剪应力分布最均匀,但横向压应力较大。DNS试件和0.5DVS试件破坏模式为单纯剪切破坏,两者所测剪切强度离散性相对较小,而DVS试件破坏时初始失效点不在剪切面上,存在二次失效,所测剪切强度离散性较大。综上所述,DNS试件最适合静态层间剪切强度测试。与含Hopkinson金属棒的试件相比,改变切口类型的试件之所以不能改善剪切面的应力水平,是由输入输出区刚度偏小造成的。     

考虑温度效应的层状复合岩石力学损伤试验及模型研究

为研究层状复合岩石高温作用下的力学特性,对相似材料制备的层状复合岩石进行20℃（室温）,100℃,200℃和300℃热处理,并开展单轴压缩试验获取其物理力学参数。结果表明,随着温度升高,层状复合岩石质量变化率与体积膨胀率呈上升趋势,且在100℃时增幅明显。拟合各力学参数的经验公式发现,峰值强度及弹性模量趋于劣化并呈线性降低,峰值应变与温度成正相关。随着温度升高,层状复合岩石呈剪切–滑移型破坏,单一类岩石由剪切破坏向张拉–剪切破坏转化,破坏时微裂纹数量增多,在300℃时延性特征显著。引入考虑温度效应的岩石本构模型并拟合了不同温度下的应力应变曲线,该模型较好地表征了热处理后层状复合岩石的损伤演化规律及破坏特征,合理地揭示了层状复合岩石高温作用后的损伤机理。     

不同围压下C60混凝土三轴压缩过程能量分析

针对复杂应力状态下高强混凝土受压变形破坏过程中的能量演化机制问题,开展不同围压下C60高强混凝土试样三轴压缩试验,分析其在受力全过程中的变形与破坏特征。根据试验结果,探究了不同围压下高强混凝土三轴压缩过程能量演化机制。研究结果表明:围压越大,混凝土试样破坏时,其峰值应力与峰值应力对应的轴向应变越大,破坏形式由张拉破坏向剪切破坏过渡;峰值应力前,混凝土试样主要以弹性应变能储存为主,峰值应力对应的输入能密度和耗散能密度均随围压的增大而增大,且均与围压满足指数函数关系,其形状改变系数FX与轴向应力呈正比关系,体积改变系数FV与轴向应力呈反比关系;达到峰值应力时,体积改变系数FV小于形状改变系数FX;峰值应力后,主要以弹性应变能释放为主,并随着混凝土试样的破坏转化为各种形式的能量耗散。研究结果可为今后从能量角度研究高强混凝土本构关系提供有益参考。     

基于临界状态的砂土本构模型研究

砂土孔隙比及所受压力是其力学特性的重要影响因素. 本文基于砂土临界状态线特性分析,采用以e-(p/p_a)ξ平面内的线性关系描述其等向压缩线. 通过对比分析两种不同压缩线函数 与临界状态线函数之间的关系提出更适合描述砂土在等向压缩下的参考压缩线,并给出了基于参考压缩线的等向硬化规律. 建议了适用于 描述砂土剪切特性的屈服面函数,并给出利用等向压缩和等p路径确定屈服面形状参数μ的方法. 将不同应力比对应的压缩线作为砂土状态参量参考线,以获取潜在强度M_f与特征状态应力比M_c,进而描述砂土压缩与剪切特性;基于等向压缩与等p路径建立了当前应力比与状态参量参考线之间的相关关系,从而实现了砂土状 态参量参考线由参考压缩线向临界状态线平稳过渡. 建立的砂土本构模型共11个参数,均能够通过常规土工试验或经验获取. 基于模型预测与Toyoura砂的等向压缩、三轴不排水剪切试验及排水剪切试验的对比结果,本文建立的砂土本构模型很好地描述了Toyoura 砂在不同孔隙比和不同压力下的压缩与剪切特性.      

Experimental investigation on strength and failure behavior of pre-cracked marble under conventional triaxial compression

Fractures in natural rocks have an important effect on the strength and failure behavior of rock mass, which are often evaluated in rock engineering practice. The theoretical evaluation of mechanical behavior of fractured rock mass has no satisfactory answer due to the role of confining pressure and crack geometry. Therefore, in this paper, conventional triaxial compression experiments were carried out to study the strength and failure behavior of marble samples with two pre-existing closed cracks in non-overlapping geometry. Based on the experimental results of a number of triaxial compression tests, the effect of crack coalescence on the axial supporting capacity and deformation property were investigated with different confining pressures. The results show that intact samples and flawed samples (marble with pre-existing cracks) have different deformation properties after peak stress, which change from brittleness to plasticity and ductility with the increase of confining pressure. The peak strength and failure mode are found depending not only on the geometry of flaw, but also on the confining pressure. The strength of flawed samples shows distinct non-linear behavior, which is in a better agreement with non-linear Hoek–Brown criterion than linear Mohr–Coulomb criterion. For a kind of rock that has been evaluated as a Hoek–Brown material, a new evaluation criterion is put forward by adopting optimal approximation polynomial theory, which can be used to confirm more precisely the strength parameters (cohesion and internal friction angle) of flawed samples. For intact samples, the marble leads to typical shear failure mode with a single fracture surface under different confining pressures, while for flawed samples, under uniaxial compression and a lower confining pressure (σ₃ = 10 MPa), tests for coarse and medium marble (the coarse and medium refer to the grain size) exhibit three basic failure modes, i.e., tensile mode, shear mode, and mixed mode (tensile and shear). Shear mode is associated with lower strength behavior. However, under higher confining pressures (σ₃ = 30 MPa), for coarse marble, the axial supporting capacity is not related to the geometry of flaw. The friction among crystal grains determines the strength behavior of coarse marble. For medium marble, the failure mode and deformation behavior are dependent on the crack coalescence in the sample. The present research provides increased understanding of the fundamental nature of rock failure under conventional triaxial compression.     

Fractal model for virgin compression of pure clays

The well-known linear relation between the void ratio and the logarithm of pressure for the one-dimensional consolidation has widely incorporated into elastoplastic constitute equation of soils, however, it is not at all straight line for more compressible clays and has several physically unaccepted properties. The compression of clays is explained by fractal theory, and is seen as a balance between the vertical pressure and repulsive force between clay plates. The distance between clay plates depends on the structure formation of the clay flocculation and clay surface. The structure formation of the clay flocculation and clay surface can be modeled by fractal approach. A new formulation of one-dimensional virgin compression of pure clays, expressed by the linear function of ln ν–ln p or ln e–ln p, is proposed based on the fractal model for clay structure. The linear function of ln ν–ln p is suitable to express the virgin compression of the extremely high plasticity clays up to the high pressure of 5000 kPa. For low plasticity clays, the virgin compression satisfies with the linear relationship of ln e–ln p at the pressure higher than 100 kPa. These too are show to be in satisfactory agreement with experimental data. The gradient of the plots of ln ν–ln p and ln e–ln p is related to the fractal dimensions of clay structure, the fundamental material parameters for the first time.     

An anisotropic elastic–viscoplastic model for soft clays

Experimental evidences have shown deficiencies of the existing overstress and creep models for viscous behaviour of natural soft clay. The purpose of this paper is to develop a modelling method for viscous behaviour of soft clays without these deficiencies. A new anisotropic elastic–viscoplastic model is extended from overstress theory of Perzyna. A scaling function based on the experimental results of constant strain-rate oedometer tests is adopted, which allows viscoplastic strain-rate occurring whether the stress state is inside or outside of the yielding surface. The inherent and induced anisotropy is modelled using the formulations of yield surface with kinematic hardening and rotation (S-CLAY1). The parameter determination is straightforward and no additional experimental test is needed, compared to the Modified Cam Clay model. Parameters determined from two types of tests (i.e., the constant strain-rate oedometer test and the 24 h standard oedometer test) are examined. Experimental verifications are carried out using the constant strain-rate and creep tests on St. Herblain clay. All comparisons between predicted and measured results demonstrate that the proposed model can successfully reproduce the anisotropic and viscous behaviours of natural soft clays under different loading conditions.     

饱和超固结黏性土的三剪弹塑性本构模型研究

针对饱和超固结黏性土现有下加载面修正剑桥模型中破坏应力比为定值、土体黏聚力为零,以及不能准确反映不同应力状态下土的强度差异这些问题,基于三剪统一强度准则以及应力坐标平移法得到了扩展破坏应力比,其特点是能更好地反映应力状态变化以及土体黏聚力的影响。在此基础上提出了饱和超固结黏性土的三剪弹塑性本构模型,该模型的特点是能描述土体受力时的中间主应力效应,应力区间效应和拉压差影响,同时也能更好地考虑土体黏聚力的影响。基于该模型对ABAQUS软件进行了二次开发,并利用其模拟了饱和超固结黏性土在排水和不排水条件下的真三轴和常规三轴压缩试验特性。对常规三轴压缩条件下土体力学特性作了模拟和试验结果对比。结果表明所提模型能很好地反映不同超固结比下土体的变形、剪胀、孔隙水压力变化特性。     

动力排水固结模型试验装置的研制

为了实现大尺度室内模拟动力排水固结法来加固吹填粘性土,本文特设计了室内试验装置。该装置由模型槽、动力装置、夯锤以及监测和数据采集系统等4部分组成,其主要特点有：(1)可同时实现半模和全模试验,可模拟单点夯和全夯,弥补了目前只有半模或1/4模和单点夯等小尺度模型试验的缺陷;(2)可实现实时观察立面裂隙、特征点的变化,对孔压、位移、动应力等进行实时监测和采集;(3)可实现自动起吊和自动脱锤,可以很好地模拟现场施工工况;(4)可实现以下加固工况的模拟实验：不同的夯击参数、不同的加固土层厚度、不同的排水方式等,从而达到不同加固方案的对比,优化加固方案;(5)拆装方便,还可用于模拟边坡、路基、挡墙、滑坡等,适用性较广。目前利用该模型装置已进行了两组不同排水系统的模型夯击试验,试验设备运行良好,可满足试验要求。     

泥质岩膨胀势判断及其破坏机理分析

应用曲永新提出的"不规则岩块干燥饱和吸水率判别法"和成岩胶结系数指标法,对山西某一煤矿巷道中泥质岩的膨胀性进行综合判定,其属于非膨胀性泥质岩。并对巷道中岩样的矿物组成成分进行分析,岩石中石英和铁矿的含量较多,且分布极不均匀,所含粘土矿物主要为高岭石。最后,从岩石的矿物组成、结构构造、节理面及微节理面的特征以及岩石在受压力时裂隙的扩张情况等角度,综合分析得出泥质岩以脆性破坏为主。     

An analysis of the shear failure of rigid-linear hardening beams under impulsive loading

A theoretical rigid-plastic analysis for the dynamic shear failure of beams under impulsive loading is presented when using a travelling plastic shear hinge model which takes into account material strain hardening. The maximum dynamic shear strain and shear strain-rate can be predicted in addition to the permanent transverse deflections and other parameters. The conditions for the three modes of shear failure, i.e., excess deflection failure, excess shear strain failure and adiabatic shear failure are analyzed. The special case of an infinitesimally small plastic zone is discussed and compared with Nonaka's solution for a rigid, perfectly plastic material. The results can also be generalized to examine the dynamic response of fibre-reinforced beams.     

龙游石窟岩面水岩作用研究

在龙游石窟砂岩胶结物的粘土矿物类型及特性研究的基础上,对窟内的积水、洞室顶部的裂隙渗水、地表水及衢江水等水样进行化学分析,结果表明石窟砂岩的矿物组成及构造, 决定了洞室渗水的水质,是造成水质不同的主要原因。对石窟洞室砂岩试样分别浸沉在上述水及蒸馏水中,并定期对浸沉水样进行化学分析,研究了石窟砂岩与水的相互作用机理,结果表明：由大气降水入渗而形成的渗透水对石窟的影响主要是渗透过程中发生的水化、溶脱、氧化等反应,从而导致洞室砂岩的矿物组成及构造产生变化,同时也直接影响了渗透水的水质。因此,粘土矿物与水之间有着相互制约,相互影响的作用,但是岩石中所含粘土矿物特性是使砂岩发生风化的主要原因。     

岩体结构面蠕变损伤机理研究

通过对伯格斯模型和西原模型的分析比较,选取西原模型研究岩体结构面的蠕变损伤特性。在τ0<τs情况下,由西原模型推出剪切模量的表达式,以剪切模量为变量定义损伤变量,得到结构面的损伤变量表达式。并以泥岩剪切试验为例,计算了相同正压力作用下的结构面剪切模量和损伤量。结果表明：当τ0<τs时,剪切模量、损伤量均随时间趋于稳定,且结构面蠕变的前两个阶段损伤量较小,而当τ0≥τs时,一段时间后,其损伤量开始突变;剪应力越大,其初始剪切模量越大,随时间降低越快,达到稳定蠕变阶段时降低量也相应越大;剪应力越大,结构面损伤量随时间增长越快,在达到稳定蠕变阶段时,损伤量也越大。