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1.
基于物理和常规变形特性分析,认为某水电站坝基碎屑岩力学特性异常复杂,故采用岩石三轴伺服仪开展了系列的蠕变力学特性试验研究。首先,探讨了轴向、侧向及体积蠕变特性和速率变化规律;其次,分析了蠕变对偏应力-应变特性影响并开展了破坏岩样微细观电镜扫描试验;最后,在采用等时曲线簇法确定长期强度的基础上,以实际延性扩容为依据,认为岩石侧向体积扩容速率大于轴向压缩速率的临界点为快速蠕变破坏的标志,提出确定长期强度的新方法。结果表明,碎屑岩表现出显著的蠕变特性,蠕变曲线主要分为初始衰减和稳态蠕变两阶段,且最后一级应力施加后呈现加速蠕变现象;应力增加导致蠕变变形加剧,最终破坏表现出轴向压缩变形过大、体积延性扩容明显、稳态蠕变速率较大等特点,且蠕变速率与应力符合指数函数关系。岩样长期强度与三向稳态蠕变速率交点和侧向体积扩容应力阀值基本一致,为常规强度的54%~80%。试验结果旨在为相关岩石工程长期稳定分析及蠕变模型构建提供可靠的依据。  相似文献   

2.
Roof falls in coal mines may occur within a few months to a few years after excavation. In this paper, we proposed the use of relaxation tests as a substitute for time-dependent tests. The relation between creep behavior and relaxation behavior was numerically investigated and demonstrates that the material assigned with creep model can show relaxation behavior. Then the relaxation model was developed by modifying the Burgers creep model. Numerical simulation of a relaxation test on a simulated rock model in 3DEC yielded results that were similar to theoretical prediction. A relaxation test was performed on two groups of specimens under varying load conditions. Results from the laboratory tests validated the approach of using relaxation test to determine time-dependent properties. Finally, time-dependent properties were investigated by performing relaxation tests at different stages of a complete stress–strain curve. The relaxation test during strain-softening was unsuccessful; however, the relaxation behavior at residual stage in post-failure region was more significant than that in pre-failure region and the sudden drop in stress indicated there was strength deterioration due to the accumulation of viscous strain.  相似文献   

3.
EPS颗粒轻质混合土的蠕变模型研究   总被引:1,自引:0,他引:1  
高洪梅  刘汉龙  刘金元  沈扬 《岩土力学》2010,31(Z2):198-205
EPS颗粒轻质混合土是一种新型轻质填土材料,相比EPS泡沫块体,具有更广泛的应用前景。EPS颗粒轻质混合土的基本物理及力学性质已得到了较多的研究,但其蠕变特性研究较少。通过不同围压下EPS颗粒轻质混合土的三轴不排水蠕变试验,采用三种常用的经验模型:Singh & Mitchell模型、Mesri模型和Findley模型对EPS颗粒轻质混合土的蠕变变形进行模拟,结果表明:Singh & Mithcell模型和Mesri模型能反映蠕变趋势,但是不能拟合应变初始快速上升段,用来描述EPS泡沫块体的Findley模型在应力水平较高时,拟合效果最好,某种程度上说,EPS颗粒轻质混合土的蠕变性与EPS泡沫块体相似。推导出了一种新的半经验半理论蠕变模型,用元件模型描述弹性变形部分,用经验模型描述塑性变形部分,拟合结果表明,不管应力水平的高低,新推蠕变模型都不仅能够很好地反映EPS颗粒轻质混合土的初始快速上升段变形,也能够比较准确地拟合长期变形,即蠕变性。  相似文献   

4.
Gupta  Neel  Mishra  Brijes 《Acta Geotechnica》2021,16(5):1575-1595

Time is one of the often-neglected factors in the assessment of the erratic failure of shale rock. Laboratory-creep experiments showed that constant stress induces time-dependent failure in brittle shale. However, the microscopic reason for time-dependent deformation in shale is still unknown. In the current study, triaxial creep and recovery experiments showed that the brittle shale specimens exhibit viscoelastic and viscoplastic creep deformation at constant stress state. In addition, the X-ray computed tomography scan of Marcellus shale showed that the shale specimens contained significant volume of preexisting microcracks. The statistical correlation among permanent strain during the triaxial experiment and stress-induced change in the three-dimensional geometry of microcracks showed that the microcracking is the microscopic reason for viscoplastic creep deformation in shale. In addition to the time and level of constant differential stress, factors such as orientation of bedding planes and specimen heterogeneity also influence the nature of creep deformation.

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5.
The evolution of rock failure with discontinuities due to shear creep   总被引:2,自引:1,他引:1  
A two-dimensional brittle creep model for rock provides insight into the initiation of shear fracture along weak discontinuities in rock. The model accounts for material heterogeneity and introduces the concept of a mesoscopic renormalization to capture the cooperative interaction between cracks in the transition from distributed to localized damage. A series of shear creep tests on rock with discontinuities were performed to simulate the initiation and propagation of crack along a pre-existing weakness under sustained shear stress and normal stress. The investigation showed that shear stress level and the normal stress level might have significant effect on the long-term behavior of rock with weak discontinuities. Moreover, a case study of rock slope instability was also investigated, where the numerically simulated instability failure of rock slope with discontinuities showed that both tensile and shear damage at the weakest elements are the trigger for the failure surface initiation in the rock slope. Once damage occurs, redistributed stress concentrations would then intensify fracture propagation and coalescence within these damage zones, leading to the progressive development of a failure surface. Moreover, failure surface extending is not only dominated by the properties and the position of discontinuities but also influenced remarkably by the complex interaction between existing discontinuities and fracture propagation. The results are of general interest because they can be applied to the investigation of time-dependent instability in rock masses, to the mitigation of associated rock hazards in rock engineering, and even to a better understanding of the physical phenomena governing the stability of rock slope.  相似文献   

6.
软硬相接岩层在长时间跨度内的蠕变变形可能极为不协调,这对开挖工程安全稳定造成严重威胁。对某水电站引水隧洞同一开挖断面内砂质泥岩和泥质砂岩两种软硬相差较大的岩石进行卸荷条件下的蠕变试验和数值模拟,结果表明:在卸围压条件下,试样侧向蠕变变形较轴向发展更为迅速,呈现出显著的侧向扩容;初始围压水平较高时,试样卸荷蠕变破坏的侧向扩容效应更加显著;泥质砂岩在稳态蠕变阶段变形速率比砂质泥岩更慢,蠕变破坏时的应变值均比砂质泥岩蠕变破坏时的应变值要小,征兆性更弱。基于Burgers模型,引入损伤变量,建立带损伤的蠕变本构模型,模型曲线较好地描述了岩石破坏偏应力水平之前的线性蠕变特征和破坏偏应力水平下的非线性加速蠕变特征;软硬相接岩层蠕变数值模拟表明,蠕变变形初期,软硬相接点变形差别幅度不大,随着时间增长,在交接面处发生层间错动,对围岩整体稳定十分不利,工程实践中应予以足够关注。  相似文献   

7.
杨超  黄达  蔡睿  黄润秋 《岩土力学》2018,39(1):53-62
高应力条件下较多岩体工程在开挖卸荷过程中表现出显著的时效变形特征。为研究裂隙岩体在卸荷状态下的蠕变特征,以锦屏I级水电站大理岩为原样制备模型试样,开展了恒轴压分级卸围压三轴卸荷蠕变试验。试验结果表明:试件在破坏时对应应力差最小的是倾角为30°裂隙试样,其次为倾角为60°裂隙试样,倾角为90°裂隙试样最大。从破坏形式来看,完整试件与倾角为90°裂隙试件均呈整体剪切破坏模式,倾角为30°和60°裂隙试件均从裂纹尖端扩展至破坏。变形特征方面,均可采用Burgers模型对各裂隙试样不含加速蠕变阶段的蠕变曲线进行拟合,试样在不同裂隙类型和应力水平下的变形特点则通过参数数值加以区分。该结论与Lemaitre应变等效原理和Sidoroff能量等价原理中有关损伤材料和无损材料间相关关系的基本观点一致。基于此,提出了裂隙岩体损伤蠕变模型,该模型建立了完整岩石与裂隙岩体间的相关关系,对裂隙岩体时效变形特征的进一步研究具有较好的参考价值。  相似文献   

8.
层状盐岩蠕变变形相互作用研究   总被引:2,自引:1,他引:1  
王安明  李小根  杨春和  黄志全 《岩土力学》2010,31(12):3964-3969
考虑泥岩夹层和盐岩的弹性性质和稳态蠕变性质,通过数值试验方法计算层状复合盐岩体在单轴和低围压三轴荷载作用下蠕变变形过程中力学相互作用和变形时效规律,分析泥岩夹层和盐岩层因蠕变率不匹配对层状盐岩蠕变的影响,初步讨论了层状复合岩体的复合材料研究方法。结果表明,层状盐岩中泥岩夹层与盐岩因弹性参数不匹配产生的初始应力集中在蠕变过程中发生松弛,因泥岩夹层与盐岩层蠕变率不匹配导致两者之间应力重分布,泥岩夹层对盐岩层的蠕变有明显抑制作用。这些分析体现了层状盐岩蠕变过程的非线性性质,为建立层状盐岩体合理本构模型奠定了基础。  相似文献   

9.
Zhang  Genbao  Chen  Changfu  Zornberg  Jorge G.  Morsy  Amr M.  Mao  Fengshan 《Acta Geotechnica》2020,15(8):2159-2177

This study aims at investigating the influence of moisture conditions on interface shear behavior of element-grouted anchor specimens embedded in clayey soils. The tests involved comparatively short embedment lengths and a device that was specially designed to facilitate moisture conditioning. Rapidly loaded pullout tests as well as pullout tests under sustained (creep) loading were conducted to characterize both the short-term and long-term ultimate shear strength of anchor–soil interfaces. Both values of the interface shear strength were found to decrease exponentially with increasing moisture content values, although their ratio was found to show a linearly decreasing trend with increasing moisture content. The interface shear creep response under pullout conditions was characterized by a rheological hybrid model that could be calibrated using experimental measurements obtained under increasing stress levels. The accuracy of the hybrid model was examined by evaluating the stress-dependent prediction model as well as its governing parameters. This investigation uncovers the coupled impact of soil moisture condition and external stress state on the time-dependent performance of grouted anchors embedded in clayey soils by correlating the interface shear strength with soil moisture content and associating the creep model with stress levels applied to the grout–soil interface.

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10.
考虑到天然岩石存在不同程度初始损伤以及蠕变过程中岩石受载后裂隙扩展而导致的新损伤,对具有初始损伤的岩石蠕变特性进行全面描述。根据不闭合结构面应力与法向变形之间的关系,提出裂隙岩石塑性变形体元件,描述岩石蠕变过程中的瞬时塑性变形。引入初始损伤影响因子,建立具有初始损伤的岩石损伤变量演化方程,构建模拟岩石加速蠕变的蠕变损伤体元件。将裂隙岩石塑性变形体和蠕变损伤体与描述瞬时弹性变形和黏弹性变形的广义开尔文模型进行串联组合,形成能够反映具有初始损伤的岩石瞬时弹-塑性变形、稳定蠕变和加速蠕变的蠕变全过程本构模型,提出了进行少量蠕变试验既能解析模型参数的方法,在不同应力水平下模型理论曲线与蠕变试验曲线吻合。  相似文献   

11.
Rock bolts are widely used for rock reinforcement in hard-rock mining and civil engineering since a long time. However the use of fully grouted rock bolts and cable bolts is limited in coal mines. In order to improve performance of the rock bolts as a supplementary roof support system for any type of roof condition in coal measured formations, it is necessary to have a good understanding of the behavior of the bolt–grout and grout–rock interactions as well as the mechanism of load transfer in rock bolts.As the performance of grouted bolts depends on bond strength, extensive laboratory pullout as well as pushout tests were conducted in the present investigations with the variations in the bolt diameters, length and cement–water mixing ratios of grout. The load–displacement curves were developed and were verified with the numerical results obtained from finite element analysis using ALGOR software.Numerical models were validated for pushout tests and a detailed analysis was carried out to know the displacement, stress, strain distribution along the bolt.  相似文献   

12.
温度周期作用下大理岩三轴蠕变试验与理论模型研究   总被引:2,自引:0,他引:2  
梁玉雷  冯夏庭  周辉  房敬年 《岩土力学》2010,31(10):3107-3112
为了解温度周期作用对大理岩蠕变力学特性的影响,采用温度-应力-渗流耦合的岩石力学三轴流变试验系统对大理岩进行了不同温度及温度周期变化下三轴压缩蠕变试验。基于试验结果,研究了大理岩试样在不同温度及温度周期变化下轴向应变随时间的变化规律,分析了不同温度及温度周期变化下蠕变的变形机制,掌握了温度对大理岩三轴蠕变影响的基本规律,并且建立了考虑温度及温度周期变化影响的改进的Burgers模型。理论值与试验结果非常接近,表明考虑温度及温度周期变化的改进Burgers模型适合描述大理岩的黏弹性蠕变特征。为长期暴露于外部环境下的岩质边坡的长期稳定性分析提供了重要的参考依据。  相似文献   

13.
A series of triaxial creep tests were conducted on warm frozen silts extracted from Qinghai–Tibet Plateau at temperature of ?1.5 °C under confining pressures of 0.5, 1.0, and 2.0 MPa, respectively. The applied test stress levels were 30, 50, 60, and 70% of triaxial shear strength, respectively. The test results indicate that the creep strain increases with the increase in applied stress level and there is a stress threshold, based on which the test results can be classified into two types of creep strain curves. The creep strain curve only includes primary and secondary creep stages when the stress level is less than the threshold value. When the stress level exceeds the threshold value, the creep strain velocity gradually increases and the specimen quickly fails in tertiary creep stage. Based on the creep test results, a fractional order rheological element model is established for warm frozen silt, which is also generalized from uniaxial stress state to the three-dimensional stress state. From the analysis on the features of the stress threshold, a creep strength criterion is also proposed simultaneously. Comparing the calculated results of the warm frozen silt with the tested ones, it is found that the predicted results of the proposed model are in good agreement with the test results. In the proposed fractional order model, the relationship between the damage factor and time is established to describe the damage degree of the specimen. Compared with the existing creep constitutive model of frozen soil, the proposed fractional order model has advantages of fewer model parameters, higher simulation precision and wider applicability in analyzing the mechanical properties of warm frozen silt.  相似文献   

14.
Effect of specimen shape on creep response of a frozen sand   总被引:1,自引:0,他引:1  
The stress—strain and strength behavior of frozen soils is most often studied in a conventional uniaxial or triaxial compression test. However, available experimental evidence shows that the results obtained in such a test may be considerably affected by the test conditions, i.e., by the specimen shape and the method of axial load transfer to the specimen ends, both of which affect the uniformity of stress and strain distribution in the sample. The methods proposed for solving the problem of load transfer to the specimen ends differ considerably for brittle and ductile materials, respectively. Since a frozen soil may behave either as a brittle or as a ductile material, depending on strain rate, temperature and confining pressure, it is considered that the load transfer method selected should correspond to the expected sample behavior. In this paper, the results of a series of compression and creep tests are presented, in which the effects of specimen shape and end conditions on the behavior of a frozen sand were systematically investigated and compared. a frozen sand were systematically investigated and compared.  相似文献   

15.
Creep tests on asphalt mixtures have been undertaken under four stress levels in the laboratory while the discrete element model (DEM) has been used to simulate the laboratory tests. A modified Burger’s model has been used to represent the time-dependent behaviour of an asphalt mixture by adding time-dependent moment and torsional resistance at contacts. Parameters were chosen to give the correct stress-strain response for constant strain rate tests in Cai et al. (2013). The stress-strain response for the laboratory creep tests and the simulations were recorded. The DEM results show reasonable agreement with the experiments. The creep simulation results proved to be dependent on both bond strength variability and positions of the particles. Bond breakage was recorded during the simulations and used to investigate the micro-mechanical deformation behaviour of the asphalt mixtures. An approach based on dimensional analysis is also presented in this paper to reduce the computational time during the creep simulation, and this analysis is also a new contribution.  相似文献   

16.
深部岩体工程处于高应力环境中,开挖破裂后的工程岩体在持续的高地应力作用下具有很强的时间效应,深入研究其峰后蠕变特性,具有重要的理论和实际应用价值。先采用RMT-150B型岩石力学试验系统对完整岩样进行单轴峰前屈服、峰后破裂卸载试验,制备出具有不同破裂损伤程度的峰前屈服、峰后破裂的损伤岩样;再采用RLW-2000型微机伺服岩石三轴流变仪对其进行单轴蠕变试验,研究其单轴蠕变力学特性。研究结果表明:损伤岩样波速与完整岩样相比,均出现了不同程度的降低;损伤岩样各级应力水平下,瞬时应变量均是随着应力水平的增加而逐步增加,且均符合线性函数关系;相同应力水平下,峰后破裂损伤岩样瞬时应变明显大于峰前屈服损伤岩样;各级应力水平下,总体上各蠕变量随着应力水平的增加而逐步提高,且均符合指数函数关系;相同应力水平下,峰后破裂损伤岩样蠕变量明显大于峰前屈服损伤岩样,且随着荷载水平的进一步提高,两者差异程度增加;损伤岩样各瞬时变形模量随着应力水平的增加均逐步提高,两者之间符合线性函数关系;各应力水平下对应的瞬时变形模量存在明显差异,岩样损伤程度越高,瞬时变形模量越低;各损伤岩样在各级应力水平下,改进的西原模型能够较好地模拟其单轴蠕变特征。  相似文献   

17.
Summary The results of creep tests on the Esterhazy-and the Patience-Lake-types of potash salt rocks from Saskatchewan, Canada are presented. The investigations involved over 6 years of time-dependent experiments in uniaxial compression using potash from the Rocanville and the Lanigan mines of the Potash Corporation of Saskatchewan. A creep test at a given load would last from 2 to 8 months, with most tests conducted over a 4-month period.Since the yield stress of both types of potash lies between 9 and 11 MPa, there is very little creep below 11 MPa. Between 11 and 13 MPa, creep strain production increases sharply through plastic deformation. Above about 13 MPa, however, plastic creep is dominated by brittle creep caused by microcracking. As a result, the lateral and volume creep strain curves may then display the transient and the steady-state, or all three stages of creep, while the axial strain, which is not affected by microcracking, usually attenuates for the whole duration.Two different interpretations of the results are offered. Identifying the last (the fourth) month of testing with the steady-state model, the stress dependence of the steady-state rate has been established for both rock types. A unimodal rate model for the axial strain and a bimodal model for the lateral strain are suggested. The alternate interpretation proceeds on the assumption that under 13 MPa, both the axial and the lateral strain can be modelled through the power function formulation of transient strain.  相似文献   

18.
针对锦屏二级水电站深埋长大隧洞围岩在开挖过程中呈现明显的流变劣化特征,基于分数阶微积分理论,用Abel黏壶替换西原模型中的牛顿黏壶,推导出基于分数阶导数的蠕变本构方程,同时考虑岩石在蠕变过程中,尤其是所受应力超过其长期强度时,蠕变参数是非定常的特征,把蠕变参数的非定常性引入本构方程中,建立了基于分数阶导数的非定常蠕变本构模型。结合锦屏二级水电站引水隧洞主要围岩之一的大理岩的室内剪切蠕变试验的结果,对模型中的参数进行反演,结果表明,基于分数阶导数的非定常蠕变本构模型能够在蠕变初期和拐点处与试验结果很好地吻合,并且可以克服西原模型不能反映蠕变第3阶段的不足。通过对模型中参数的敏感性进行分析,得出分数阶阶数、非定常参数对岩石蠕变的影响规律。研究结果表明,提出的基于分数阶导数的非定常蠕变模型能够很好地反映大理岩的蠕变全过程。  相似文献   

19.
The altered granite gneiss is a special rock with loosely-structured and well-developed pores and cavities. The microstructure and mineral composition of the rock were analysed by SEM-EDS and creep triaxial tests were carried out and the axial and lateral deformations over time were discussed. Both the axial and the lateral creep curves show the typical three distinct creep stages (decay creep, steady state creep, accelerated creep). At a low stress level, the axial creep strain is unnoticeable, and only when loaded at a high stress level will the creep strain increase at an increasing rate until the rock specimen fails. The lateral creep strain is smaller than the axial creep strain, but the creep rate (dε/dt) in the lateral direction is higher than that in the axial direction at all stress levels. The failure pattern, which is affected by many factors, shows a shear failure with rather broken and rough failure surfaces.  相似文献   

20.
The post-construction settlement of rockfill dams and high filled ground of airport, which is a phenomenon of much significance, is mainly caused by the time-dependent breakage of the rockfill material. In this paper, a random virtual crack DEM model is proposed for creep behavior of rockfill in PFC2D according to the theory of subcritical crack propagation induced by stress corrosion mechanisms. The bonded clusters are adopted to represent the rockfill particles so as to simulate their irregular shapes. Virtual cracks are set at the bonds of the clusters, and the length of the crack is considered as a random value, which leads the crushing strength of a single particle to follow the Weibull’s statistical model and the corresponding size rules. Oedometric creep tests for rockfill are simulated by using this proposed model. The results show that the model, validated preliminarily by some test data, can reflect qualitatively the creep mechanism as well as the size effects reasonably. Particles can develop various breakage patterns during creep, including global breakage, local breakage and even complex mixed breakage. The increase in stress levels and particle size will lead to an obvious growth of the creep strain and creep rate of the rockfill. The scale effects on the creep behavior of rockfill are analyzed through 35 specimens, and formulas including the effects of scales and stress levels are tentatively proposed.  相似文献   

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