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《岩土力学》2015,(11):3128-3134
基于三剪统一强度准则和非饱和土双应力状态变量抗剪强度,考虑中间主应力效应、材料拉压不等特性和强度准则差异的影响,建立了非饱和土抗剪强度三剪统一解,并在此基础上推导了非饱和土条形地基太沙基极限承载力的计算公式。通过可行性分析及算例论证,验证了所推公式的正确性,探讨了中间主应力效应、强度准则、基质吸力、有效内摩擦角和有效黏聚力等参数对非饱和土条形地基极限承载力的影响规律。研究结果表明:中间主应力效应和强度准则对非饱和土条形地基太沙基极限承载力具有显著影响,中间主应力效应越显著,极限承载力越高,说明考虑中间主应力效应可以更加充分发挥材料的强度潜能,也说明强度准则差异对地基极限承载力的预测具有重要作用。基质吸力对非饱和土条形地基太沙基极限承载力具有双重影响:在低基质吸力范围内,极限承载力随基质吸力的增大线性提高;当基质吸力增大到进气值时,极限承载力达到峰值;在高基质吸力范围内,极限承载力随基质吸力的增大逐渐降低,最终趋于稳定。非饱和土条形地基太沙基极限承载力随有效内摩擦角和有效黏聚力的增大显著提高。非饱和土太沙基极限承载力三剪统一解包含了多种屈服准则下地基承载力的计算公式,具有较广泛的适用性,可为实际工程应用提供参考。 相似文献
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用Hoek-Brown强度准则确定岩石地基极限承载力 总被引：6，自引：0，他引：6
岩石地基承载力,是地基稳定性分析中的强度问题,不仅控制建筑物的安全,而且客观上影响了工程的经济合理性,因此,精确确定岩基承载力至关重要。介绍基于Ｈｏｅｋ－Ｂｒｏｗｎ强度准则计算完整岩体,节理岩体,破碎岩体,软弱岩体,软弱岩体岩基承载力的极限平衡解法,以及参数ｍ,ｓ的确定方法。 相似文献
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《地质灾害与环境保护》1999,4(12):andt1
岩石地基承载力,是地基稳定性分析中的强度问题,不仅控制建筑物的安全,而且客观上影响工程的经济合理性,因此,精确确定岩基承载力至关重要。介绍基于Hoek－Brown强度准则计算完整岩体、节理岩体、破碎岩体、软弱岩体岩基承载力的极限平衡解法,以及参数m,s的确定方法。最后,以工程实例证明此方法的正确性和实用性。 相似文献
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深埋圆形隧道弹塑性位移统一解及其比较分析 总被引：1，自引：0，他引：1
基于统一强度理论和非关联线性流动法则,考虑塑性区的真实弹性应变,推导了深埋圆形隧道弹塑性位移统一解。位移统一解合理地考虑了中间主应力效应和围岩剪胀特性的影响,具有广泛的理论意义。经与文献简化位移解析解比较分析知,围岩塑性区的弹性应变对隧道位移影响显著,简化解析解所得结果偏小,简化解析解和文中统一解之间的差异与中间主应力效应和围岩剪胀特性密切相关;考虑中间主应力的影响,能更加充分发挥围岩的强度潜能;隧道支护设计应考虑围岩剪胀特性的重要影响 相似文献
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统一强度理论在地基承载力确定中的应用研究 总被引：3，自引：0，他引：3
基于统一强度理论,考虑中间主应力对地基承载力的影响,给出了静止侧压力系数 条件下的地基临塑与临界荷载公式。结合实例,对基于统一强度理论和Mohr-Coulomb准则的地基承载力计算结果进行了对比分析。新的理论公式更为确切地反映了地基承载力的实质,有利于地基土体强度的充分发挥。基于河北境内177组不同土质地基的土性指标及载荷试验资料的统计分析,对中间主应力系数b的取值进行了深入细致的探讨,研究表明,对于粉土及黏性土地基,b的取值范围在0～0.5之间变化,理论计算所得地基承载力特征值与载荷试验实测值间的相对误差一般不超过5% 相似文献
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基于塑性极限理论的上限分析法,借鉴已有数值分析和室内模型试验所揭示的带帽刚性桩破坏模式,构建了其运动许可速度场,并引入统一强度理论,根据能量平衡原理,推导了能考虑中主应力影响的带帽刚性桩极限承载力上限计算公式。同时通过参数分析,得到了带帽刚性桩极限承载力随桩帽尺寸、土的黏聚力和内摩擦角的变化规律。研究发现：考虑中主应力影响的带帽刚性桩的上限解较不考虑时有较大的提高,对于带帽刚性桩承载力计算时,实际统一强度理论中反映中主应力影响的参数取0.1～0.2附近较为合理。带帽刚性桩承载力随着桩帽尺寸的增大而增大,且桩帽直径与桩径之比 时,承载力增大趋势较为明显;承载力随着土体黏聚力和内摩擦角的增大而增大。通过与已有理论方法和试验结果对比分析发现,本文提出的方法不仅在理论上更严密,而且可得到更符合实际的计算结果。 相似文献
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基于连续介质理论中岩体的剪胀角与围压和塑性剪切应变密切相关,隧洞周边岩体的应力状态因开挖卸荷而发生应力重分布,迫使其围压由原地应力逐渐衰减,塑性剪切应变不断增加,引起剪胀效应呈非线性变化。首先,基于统一强度理论和非关联流动法则,将潜在塑性区围岩按等围压释放划分为若干同心圆,提出了考虑中间主应力和非线性剪胀性的有限差分法,计算应变软化围岩的力学问题,并以实例验证其正确性。其次,通过参数分析,研究塑性区内岩体的剪胀角受中间主应力、临界软化系数和支护力的影响规律。研究结果表明,中间主应力主要影响剪胀角的峰值,随着中间主应力效应增加,剪胀峰值增加;临界软化系数主要影响剪胀角的变化率,随着临界软化系数的增加,剪胀角变化缓慢;中间主应力和临界软化系数共同影响塑性区剪胀角的变化;随着支护力的增加,洞壁处的剪胀角增加;双剪强度理论计算的位移值较小,应谨慎采用,同时采用Mohr-Coulomb强度准则时可以适当考虑围岩的承载潜力。 相似文献
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In this paper, the strength envelope of rock masses is considered to follow a non-linear unified strength criterion that considers the effect of the intermediate principal stress. A unified slip line method for resolving the differential equation system that governs the stress field is established to research the ultimate bearing capacity, which can be adapted for a wide variety of rock masses. Through this new theory, a suitable characteristic method for rock masses of interest can be obtained, and the relationships between different types of characteristic methods are revealed. The characteristic methods are based on different strength criteria, such as the Hoek–Brown criterion, modified Hoek–Brown criterion, or non-linear twin-shear strength criterion; each of these criteria is a special case of the proposed theory. Moreover, a series of new characteristic methods can be easily derived from it. In terms of the proposed theory, the ultimate bearing capacity with the Hoek–Brown criterion forms the lower bound; the ultimate bearing capacity with a non-linear twin-shear strength criterion forms the upper bound; and a series of the ultimate bearing capacities ranging between these two bounds may be derived from a non-linear unified strength criterion. A comparison is made between existing numerical analyses and non-linear finite element analysis solutions with the Drucker–Prager strength criterion. It is shown that the present results are in good agreement with existing numerical analyses and non-linear finite element analysis solutions with the Drucker–Prager strength criterion. 相似文献
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In this paper, an anisotropic strength criterion is established for jointed rock masses. An orientation distribution function (ODF) of joint connectivity, is introduced to characterize the anisotropic strength of jointed rock masses related to directional distributed joint sets. Coulomb failure condition is formulated for each plane of jointed rock masses by joint connectivity, where the friction coefficient and cohesion of the jointed rock mass are related to those of the intact rock and joint and become orientation dependent. When approximating joint connectivity by its second‐order fabric tensor, an anisotropic strength criterion is derived through an approximate analytical solution to the critical plane problem. To demonstrate the effects of joint distribution on the anisotropic strength of jointed rock masses, the failure envelopes are worked out for different relative orientations of material anisotropy and principal stress axes. The anisotropic strength criterion is also applied to wellbore stability analyses. It is shown that a borehole drilled in the direction of the maximum principal in situ stress is not always the safest due to the anisotropic strength of the jointed rock mass. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
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L. Zhang 《Rock Mechanics and Rock Engineering》2008,41(6):893-915
Summary Although the Hoek–Brown strength criterion has been widely used in rock mechanics and rock engineering, it does not take account
of the influence of the intermediate principal stress. Much evidence, however, has been accumulating to indicate that the
intermediate principal stress does influence the rock strength in many instances. Therefore, researchers have developed three-dimensional
(3D) versions of the Hoek–Brown strength criterion. In this paper, three existing 3D versions of the Hoek–Brown strength criterion
are reviewed and evaluated. The evaluation shows that all of the three 3D versions of the Hoek–Brown strength criterion have
limitations. To address the limitations, a generalized 3D Hoek–Brown criterion is proposed by modifying the generalized Hoek–Brown
strength criterion. The proposed 3D criterion not only inherits the advantages of the Hoek–Brown strength criterion but can
take account of the influence of the intermediate principal stress. At a 2D stress state (triaxial or biaxial), the proposed
3D criterion will simply reduce to the form of the generalized Hoek–Brown strength criterion. To validate the proposed 3D
strength criterion, polyaxial or true triaxial compression test data of intact rocks and jointed rock masses has been collected
from the published literature. Predictions of the proposed generalized 3D Hoek–Brown strength criterion are in good agreement
with the test data for a range of different rock types. The difference of the proposed generalized 3D Hoek–Brown strength
criterion from and its advantages over the existing 3D versions of the Hoek–Brown strength criterion are also discussed. It
should be noted that the proposed 3D criterion is empirical in nature because it is an extension of the 2D Hoek–Brown strength
criterion, which is empirical. Because of the non-convexity of the yield surface for a biaxial stress state, the proposed
3D criterion may have problems with some stress paths.
Correspondence: L. Zhang, Department of Civil Engineering and Engineering Mechanics, The University of Arizona, Tucson, Arizona
85721, USA 相似文献
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白鹤滩柱状节理岩体真三轴模型试验研究 总被引：3，自引：1，他引：2
在柱状节理玄武岩工程地质调查、现场精细结构描述等工作基础上,开展了柱状节理玄武岩体的脆性材料模型真三轴物理模拟试验。研究了复合柱状岩体在不同卸荷-加载应力途径下的破裂、破坏机制及不同方向三轴主应力作用下的应力-应变关系及其强度特性;开展的8种不同应力比和6种不同受力方向下各向异性试验结果表明,柱状节理玄武岩体强度、变形特征受三向不等围压和柱状节理特性影响明显,强度变形的各向异性特征显著。试验结果表明,应力比 对试样的强度、变形和破坏模式具有控制作用,随着应力比的变化,试样的极限强度呈现分段特性;较小应力比下试样的变形和破坏模式受应力比和原生节理的共同影响;较大的应力比对试样的变形和破坏模式的影响比原生节理的影响显著;随着应力比的增大,中主应力由约束侧向变形变为主动加载,这一作用的变化影响了极限荷载和破坏模式。 相似文献
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为考虑中间主应力对岩石极限破坏强度作用,在广义Hoek-Brown强度准则幂率项中添加定量表征中间主应力项,构建新的三维Hoek-Brown强度准则。该准则在主应力空间是通过3个角点外接Hoek-Brown准则包络面的曲六面体,在 空间包络线是幂律型曲线。通过与Hoek-Brown准则、Drucker-Prager准则和Mogi准则分别对4组真三轴压缩强度试验数据的拟合对比分析,探讨其反映中间主应力效应的适用性。结果表明,修正的Hoek-Brown强度准则拟合试验数据效果总体最好,Mogi准则次之,Hoek-Brown准则和Drucker-Prager准则较差。从而修正的Hoek-Brown强度准则最适用于粗面岩、大理岩和花岗岩等硬脆性岩石的真三轴强度预测及中间主应力影响规律描述。 相似文献