共查询到19条相似文献，搜索用时 328 毫秒
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超高韧性水泥基复合材料是一种新型建筑材料。为分析超高韧性水泥基复合材料构件的力学性能,制作了超高韧性水泥基复合材料简支梁,并对集中荷载作用下的超高韧性水泥基复合材料梁的受剪性能进行了试验研究,分析了梁在荷载作用下的受力及变形特点。试验共包括9根超高韧性水泥基复合材料梁和1根混凝土对比梁,试验的主要参数为配筋率、配箍率及剪跨比。对试件规格、加载方式、加载制度及量测设备等方面进行了介绍,并对试验结果进行了分析。从试验破坏现象来看,表明梁具有较好的延性破坏特征;从荷载位移曲线、抗剪强度及箍筋应变结果来看,表明梁具有较好的韧性;超高韧性水泥基复合材料梁试件具有较好的抗剪性能。 相似文献
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进行了9个超高韧性水泥基复合材料(UHTCC)新型框架节点的抗震试验。研究了轴压比和核心区箍筋间距对新型节点承载能力、滞回特性和耗能能力的影响。结果表明,UHTCC节点出现了大量裂缝间距仅为1mm左右的微细斜向裂缝,节点的开裂荷载和抗剪承载力都有明显的提高。UHTCC材料可降低甚至消除节点核芯区箍筋的用量。在试验基础上,对UHTCC新型框架节点的开裂荷载和极限承载力进行了理论计算,计算值和试验结果总体吻合较好。 相似文献
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为了全面研究工程水泥基复合材料（ECC）加固桥墩的抗震性能，对采用聚乙烯醇纤维增强水泥基复合材料（PVA-ECC）加固的桥墩进行了拟静力试验。并基于有限元分析软件OpenSees建立了数值模型，通过对比数值模拟结果与试验结果，验证有限元分析的有效性，在此基础上对PVA-ECC加固桥墩进行数值参数分析，探讨轴压比、新旧材料厚径比及体积配箍率变化对桥墩抗震性能的影响规律。结果表明:数值模拟的滞回曲线与骨架曲线和试验基本吻合；与普通混凝土桥墩相比，新旧材料厚径比为0.10时，即可获得优异的延性性能，ECC加固的桥墩变形性能显著提升，极限位移提高，滞回曲线更加饱满，抗震性能更加优异。对于高轴压比情况，为了确保ECC加固桥墩的延性性能，应根据实际情况增加新旧材料厚径比；ECC材料可部分替代箍筋作用，适用于箍筋配置不足的桥墩加固，PVA-ECC具有较好的工程抗震加固的作用。 相似文献
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纤维增强材料对于改善水泥基材料的韧性和抗冲击性、大幅度提高混凝土的断裂能、防止混凝土发生脆性破坏具有重要意义;而"绿色"纤维在提高混凝土结构安全性的同时,具有环保、节能、利废、可降解再生等特性。本文介绍了"绿色"纤维的分类,分析了"绿色"纤维增强水泥基材料的特点,总结了"绿色"纤维在水泥基材料中应用、研究的进展。指出:"绿色"纤维与水泥基材料复合,适应循环经济和建材行业可持续发展的要求,是未来纤维增强水泥基复合材料发展的主要方向。 相似文献
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运水泥制品及构件是典型的脆性材料,抗裂性能差,容易产生大量的裂缝,降低了建筑物的使用功能、抗渗性和耐久性。为了解决上述问题,建议在水泥基材料中掺入纤维以增强水泥基材料的抗裂性能,提高建筑物的工程质量。从纤维砂浆的抗裂性能方面介绍了国内外的研究进展,从工作性能方面分析了纤维砂浆存在的问题,提出了相应的解决方法,为纤维砂浆这种新型水泥基材料的科研与工程应用提供了参考意见。 相似文献
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为研究聚乙烯醇纤维—水泥基复合材料(PVA-ECC)墩柱的抗震性能，以有限元分析软件ABAQUS为主要研究手段，结合已有的2个试件的实测数据，并以箍筋间距、箍筋直径、纵筋直径为变化参数进行了13个试件的拓展分析，探讨了各影响参数对PVA-ECC墩柱柱抗震性能的影响。研究结果表明：所建立的ABAQUS有限元模型在破坏形态和滞回曲线曲线上具有较高吻合度；箍筋直径和间距对抗剪承载力的影响在5%以内，增大纵筋直径能有效提高试件的抗震性能。 相似文献
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实际地震作用是多维的、随机的，框架节点在2个方向同时受力，其抗震能力相比于单向地震作用会降低。目前，对节点核心区在2个方向同时受力时抗剪承载力的研究尚未完善。在双向受力下，节点核心区2个方向传来的剪力形成合剪力作用面，在节点核心区内部形成不同于单向受力下的斜向斜压杆。本文基于软化拉-压杆模型，针对水平双向受力相同的空间边节点，在合剪力作用面内建立抗剪承载力计算模型，确定空间边节点核心区斜压杆以及钢筋拉杆的计算方法。利用有限元软件建立不同参数空间边节点模型，并收集部分空间节点试验数据，将剪力计算值与模拟值或试验值进行对比。结果表明，基于软化拉-压杆模型建立的双向受力下钢筋混凝土框架，其边节点抗剪承载力计算值与模拟值或试验值吻合良好。 相似文献
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This paper discusses the applicability of the tension-softening model in the determination of the fracture toughness of rocks,
where the fracture toughness evaluated based on the tension-softening model is compared with the crack growth resistance deduced
from laboratory-scale hydraulic fracturing tests. It is generally accepted that the fracture process is dominated by the growth
of a fracture process zone for most types of rocks. In this study, the J-integral based technique is employed to determine the fracture toughness of Iidate granite on the basis of the tension-softening
model, where compact tension specimens of different dimensions were tested in order to examine the specimen size effect on
the measured fracture toughness. It was shown that the tension-softening relation deduced from the J-integral based technique allowed us to determine the specimen size independent fracture toughness Kc of Iidate granite. Laboratory-scale hydraulic fracturing tests were performed on cubic specimens (up to a 10 m sized specimen),
where cyclic pressurization was conducted using a rubber-made straddle packer to observe the extent of the hydraulically induced
crack. The experimental results of pressure and crack length were then used to construct the crack growth resistance curve
based on the stress intensity factor K. The crack growth resistance obtained from the hydraulic fracturing tests was observed to initially increase and then level
off, giving a constant K value for a long crack extension stage. The plateau K value in the crack growth resistance curve was found to be in reasonable agreement with the fracture toughness Kc deduced from the tension-softening relation. It was demonstrated that the tension-softening model provides a useful tool
to determine the appropriate fracture toughness of rocks, which may be applicable for the analysis of the process of large-scale
crack extension in rock masses. 相似文献
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Apparent fracture toughness in Mode I of microcracking materials such as rocks under confining pressure is analyzed based
on a cohesive crack model. In rocks, the apparent fracture toughness for crack propagation varies with the confining pressure.
This study provides analytical solutions for the apparent fracture toughness using a cohesive crack model, which is a model
for the fracture process zone. The problem analyzed in this study is a fluid-driven fracture of a two-dimensional crack with
a cohesive zone under confining pressure. The size of the cohesive zone is assumed to be negligibly small in comparison to
the crack length. The analyses are performed for two types of cohesive stress distribution, namely the constant cohesive stress
(Dugdale model) and the linearly decreasing cohesive stress. Furthermore, the problem for a more general cohesive stress distribution
is analyzed based on the fracture energy concept. The analytical solutions are confirmed by comparing them with the results
of numerical computations performed using the body force method. The analytical solution suggests a substantial increase in
the apparent fracture toughness due to increased confining pressures, even if the size of the fracture process zone is small. 相似文献
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带构造柱和圈梁的约束砌体结构在四川灾区乡镇房屋重建中被广泛采用,其抗震性能是人们所关心的.基于绵竹市土门镇当地重建房屋常用建筑材料的实验数据以及通用有限元软件ANSYS中Solid 65单元的性质和特点,用有限元模型模拟了粘土砖砌体在不同压应力状态(σ-/fm)下沿通缝截面抗剪强度试验,给出了相关单元在模拟砖砌体开裂中闭合及开口剪力传递系数的建议值;利用这些结果,分别建立了带约束(构造柱、圈梁等)和不带约束砌体墙的有限元模型,进而分析了他们在单调荷载以及低周往复荷载作用下的抗震性能.结果表明,与不带约束的墙体相比,带约束墙体在单调水平荷载作用下的初裂性能、极值荷载和延性都有很大的提高,在低周往复荷载作用下其耗能能力得到了改善.所得结果可供相应结构抗震设计的参考. 相似文献
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W. Müller 《Pure and Applied Geophysics》1986,124(4-5):693-709
Fracture phenomena in rocks are associated with mainly mode I crack growth, sometimes superposed by shear or torsion. The present paper contributes to a fracture mechanics analysis of mode I and mixed mode crack propagation, by presenting reliable fracture toughness data for some rocks which include the effect of induced crack propagation rate, and the influence of effective pressure, and by numerical calculations on fracture propagation in layered rock formations. Empirical relations between fracture toughness,K
Ic' and induced crack opening displacement rate, as well as effective pressure, are given. The observedK
Ic pressure relation supports a theoretical model which takes into account the existence of microcracks in the crack tip region. Finite element calculations of fracture propagation in layered rock formations demonstrate the important effect of mixed mode crack growth. The numerical approach is particularly applied to single crack growth in hydraulic fracturing and in three point bending tests on layered single edge crack specimens. 相似文献
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FRP抗震加固混凝土梁柱节点的受剪承载力分析 总被引：2，自引：1，他引：2
通过采用SGFRP、HFRP加固的四个混凝土梁柱节点在低周反复荷载作用下的抗震性能对比试验研究,提出了FRP加固节点受剪承载力的计算公式,并基于分析给出了相关计算参数的工程设计建议取值,并对加固方式、纤维品种、纤维粘贴角度等主要因素对节点抗剪承载能力的影响机理进行了分析,结果表明:在节点核心区和梁柱端头粘贴纤维可以有效的提高节点的受剪承载能力;加固方式直接影响节点受剪承载能力的大小。 相似文献
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按照压剪应力场中袭纹具有的特点,简化成三种力学模型——狭长缺口、顺序闭合裂纹及初始闭合裂纹。利用文中建议的局部分析法,对其端部应力场做的一般分析,导出了他们的普遍表达式。用光弹性实验及有限元计算对所得结果做的分析表明,它们是成立的。这些结果有助于了解构造地震震源的破裂机制及其应力场分布的某些特点。 相似文献
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The superimposed basin must have undergone the changes of regional stress field. Study on the nature and switch of regional stress field of superimposed basin is very useful to understanding its stress state and tectonic events during its formation and evolution. As sensitive markers of small stress changes, joint and shear fracture, characterized by consistency of orientation over wide area, can be used to reconstruct paleostress state and its evolution. Detailed observations and analysis on the orientations, geometrical patterns, sequences of joints and shear fractures and their chronological relation to faults and folds show that, the NEE-SWW systematic joints and NNW-SSE systematic joints developed in the Mesozoic and Cenozoic strata are much more prominent than NW-SE systematic joints and shear fractures with different orientations. And the NWW-SEE and NW-SE systematic joints formed later than NEE-SWW systematic joints but earlier than shear fractures with different orientations. According to the relationships between joint and shear fractures and stress, the NEE-SWW systematic joints are inferred to result from lateral weak extension caused by the late Cretaceous regional uplift, while the NNW-SSE and NW-SE systematic joints are interpreted as syn-tectonic deformation relating to strong N-S compression in the Neogene. But some conjugate shear fractures occur probably due to sinistral strike-slip faulting in the Kuqa depression. At the beginning of the Neogene, the stress field changed and the maximal principal stress σ1 switched from vertical to horizontal. 相似文献