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抗滑桩内力计算“K”法的改进与应用 总被引：4，自引：0，他引：4
对传统的抗滑桩内力计算“K”法作了一些改进,如建立了滑动面上下统一的坐标系,将桩视为一个整体进行考虑,通过合理的假定,保证了桩身在滑动面处内力和位移的连续性,同时,采用名的MATLAB数学软件设计了“K”法的计算程序,适用于滑坡推力和桩前滑体抗力分布的各种形式以及抗滑桩为刚性桩和弹性桩的情况,实例计算结果表明,较之传统的查表法,该方法有效地提高了抗滑桩内力和位移计算速度和精度,同时可得到理想的可视化计算结果,有助于抗滑桩结构的优化设计。 相似文献
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分布荷载推力桩计算的p-y曲线法研究 总被引：2，自引：2，他引：0
为提高现有水平梯形分布荷载推力桩设计计算水平,提出了地基系数按非线性土抗力.水平位移(p-y)曲线抗力模式表达的水平梯形分布荷载推力桩位移和内力计算的有限差分数值分析方法,并详细推导了桩身位移的差分格式.基于这些公式,编制了全桩位移、内力及侧土抗力的计算和图形处理程序,可适用于滑坡抗滑桩和深基坑悬臂支护桩的设计计算.结合新型桩型现浇混凝土薄壁管桩(PCC桩)作为滑坡抗滑桩进行对比分析,算例表明:该方法方便可靠.当有限差分段划分得足够小时,可使数值解接近于真实解. 相似文献
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文章研究了深路堑高边坡中采用的多排预应力锚索抗滑桩内力计算方法。基于普通抗滑桩内力计算的地基系数法原理,考虑桩身和多排锚索位移的变形协调,提出了其内力计算的有限差分解法。与传统方法相比,该法通过编程计算,可很容易获得锚索拉力、全桩内力和位移值及其分布规律。工程实例计算结果与现场测试结果的对比分析表明,本文提出的方法可行,其计算结果较好反映了锚索桩的实际受力状态和变化规律。 相似文献
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地基系数法是弹性抗滑桩内力计算的常用方法,基于地基系数“m-k”法的基本原理,将抗滑桩作为整体进行内力分析,提出了弹性抗滑桩全桩内力计算的反力荷载法,详细推导了有关计算公式;运用Matlab语言编写了全桩内力计算和图形处理程序,可对全桩进行整体分析,不需要像传统方法那样以滑动面为界将抗滑桩分成受荷段和锚固段分别计算其内力;与有限差分法相比,无需利用滑动面处的连续性条件进行迭代计算;计算实例表明,其方法与传统方法计算结果能很好吻合,图形处理结果有利于抗滑桩结构设计,且程序运行时间短,可提高抗滑桩内力分析效率。 相似文献
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《岩土力学》2017,(12)
为了改进现有锚索抗滑桩计算中存在的不足,将传递矩阵算法应用于锚索抗滑桩结构内力计算。推导了适合抗滑桩计算的场矩阵和点矩阵,能够完成普通抗滑桩、桩顶作用集中荷载以及桩身有多个受力分段的抗滑桩内力计算,再结合具体的不同点矩阵形式,可以完成预应力锚索抗滑桩内力计算。根据预应力锚索抗滑桩的工作原理,给出了不同受力阶段的传递矩阵计算式。最后,通过具体的计算实例对预应力锚索抗滑桩不同受力阶段的内力和位移进行了计算分析,结果表明,在锚索预应力作用下,受荷段出现较大的剪力和弯矩,位移较小;进入变形协调阶段后,滑面处和锚固段的剪力明显增加,锚固段出现较大弯矩,桩顶出现向前的位移。 相似文献
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从岩土体性质、地下水、时间效应、深度、桩截面尺寸及桩周地基土的变形量方面,讨论了影响地基系数的几个因素,给出了线弹性地基反力法计算弹性桩内力的通解,比较了几种线弹性地基反力法的分布形式、适用条件及其不足之处.以三峡库区万州区二层岩滑坡为例,对于3种不同地质环境中的抗滑桩分别采用K法、C法、M法计算抗滑桩的内力,结果表明:M法计算得到的抗滑桩承受的弯矩、剪力最大,桩水平位移最大,对桩周岩土体的应力最小;K法计算得到的弯矩、剪力最小,桩水平位移最小,对桩周岩土体的应力最大.根据万州区滑坡抗滑桩嵌岩段岩土体的质量等级,认为万州区抗滑桩设计采用M法较适宜,这对万州区今后滑坡治理设计具有重要的指导作用. 相似文献
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门架式双排抗滑桩的弹塑性模型与计算分析 总被引：3，自引：0，他引：3
门架式双排抗滑桩的计算模型大部分将桩排间岩土体视为弹性材料,而岩土体为弹塑性材料,使得抗滑桩内力、位移计算结果与实际情况相差较大。假设桩排间岩土体为弹塑性材料,提出一种弹塑性计算模型,该模型将桩排间岩土体看作线弹性单元和塑性单元的组合,根据结构力学知识、土的本构关系和数值分析方法建立一种计算前后排抗滑桩内力的计算方法。首先,由已知的桩顶位移,并结合结构力学位移法求出桩间土总应力。根据Lade-Duncan模型导出这两个单元的基本参数,然后,结合数值分析方法计算出抗滑桩的内力,最后,结合工程实例,运用ANSYS有限元软件进行计算分析,得出门架式双排抗滑桩的内力图。对比监测数据和弹性模型计算结果表明,弹塑性模型的计算结果比弹性模型更加接近监测值。 相似文献
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抗滑桩变形过程中产生的竖向摩阻力可以形成反力矩,有助于抵抗滑坡推力,现对竖向摩阻力对抗滑桩嵌固段内力及变形的影响进行研究。在弹性地基系数法K法和小变形假设的基础上,假定竖向摩阻力与桩岩相对位移成正比,建立考虑竖向摩阻力的抗滑桩受力模型及其挠曲变形微分方程,并推导其求解过程。通过马家沟Ⅰ号滑坡抗滑桩实例计算,分析了竖向摩阻力对抗滑桩内力及变形计算的影响。竖向摩阻力形成的反力矩能减小抗滑桩的变形及内力,对抗滑桩剪力的影响最大,水平位移次之,对弯矩影响最小。考虑竖向摩阻力的抗滑桩计算模型能改善目前抗滑桩设计中剪力计算过大的问题,使抗滑桩设计更为合理。 相似文献
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弧形间隔排桩-桩顶拱梁空间抗滑结构理论研究 总被引：1，自引：0，他引：1
为充分利用地形、地质结构和混凝土的材料特性,优化直线排桩的不利受力状态和提高其整体稳定性,提出了弧形间隔排桩-桩顶拱梁新型空间抗滑结构,即根据滑坡地形及地质条件弧形布设抗滑桩,桩顶设置连系梁,连系梁两端设置抗力桩,形成空间结构以抵抗滑坡推力。以抗滑桩与连系梁之间的作用力为冗力,分别建立了连系梁和抗滑桩的计算模型,并对连系梁的内力和抗滑桩的位移进行了理论分析,根据连系梁与抗滑桩连接处的位移协调条件,建立了力法典型方程求解冗力。最终得出了连系梁的弯矩、剪力和轴力以及抗滑桩的位移、内力理论计算公式。通过算例分析并与悬臂桩及直线排桩-桩顶连系梁抗滑结构比较,结果表明：空间抗滑结构中弧形连系梁的内力分布更加合理,弧形连系梁对抗滑桩的位移约束效果明显。 相似文献
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西南地区岩溶水源地类型及开发技术条件 总被引：8，自引：7，他引：1
明确了岩溶水源地的定义,并提出了新的岩溶水源地分类方案。首先按岩溶含水层的埋藏分布、岩溶水出露状态,将岩溶水源地划分为天然出露的岩溶水源地及隐伏的岩溶水源地两大类。然后再根据岩溶水源地的岩溶含水介质特征（导水和赋水空间形态、结构及水动力特征）进一步将天然出露的岩溶水源地划分为暗河、泉、表层泉三个亚类,将隐伏的岩溶水源地划分为饱水带富水块段、表层带富水块段两个亚类。并研究评价了各个类型的岩溶水富集规律、动态特征、岩溶水资源、开发技术条件。 相似文献
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We studied the particle growth in a protoplanetary disk in a high-ionization environment and found that icy planet formation is inactive for a disk with an ionization rate 100 times higher than that of the present Solar System. In particular, in the case of M 10~(-7.4)M_☉yr~(-1), only rocky planet formation occurs. In such a case, all the solid materials in the disk drift inward, eventually reach the inner MRI front,and accumulate there. They form a dense, thin sub-disk of solid particles, which undergoes gravitational instability to form rocky planetesimals. The planetesimals rapidly grow into a planet through pebble accretion. Consequently, rocky planets tend to be much larger than planets formed through other regimes(tandem planet formation regime and dispersed planet formation regime), in which icy planet formation actively takes place. These rocky planets may evolve into hot Jupiters if they grow fast enough to the critical core mass of the runaway gas accretion before the dispersal of the disk gas, or they may evolve into super-Earths if the gas dispersed sufficiently early. 相似文献
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Frédéric Béjina Misha Bystricky Nicolas Tercé Matthew L. Whitaker Haiyan Chen 《Comptes Rendus Geoscience》2019,351(2-3):86-94
In situ X-ray diffraction was used to measure the isothermal bulk modulus at room conditions (KT0) of synthetic olivines with different iron contents. The chemical formulae of the olivine samples were with x = 0.45; 0.64; 0.82; 1, with 1% standard deviation (referenced as Fa45, Fa64, Fa82 and Fa100, respectively). All experiments were performed in the multi-anvil apparatus installed at NSLS beamline X17B2, to pressures up to about 7 GPa. Unit-cell volumes under hydrostatic conditions and differential stresses present in the samples were calculated using the method developed by Singh et al. (1998), and pressures measured using NaCl as a standard were then corrected for these stresses. Using a second-order Birch–Murnaghan equation of state, we obtained the isothermal bulk modulus of each composition: GPa, GPa, GPa and GPa. These values combined with data available in the literature show that the KT0 of Fe-rich olivines increases very slowly with the Fe content, but possibly not in a simple linear trend. 相似文献
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Ritsuo Morishita 《Mathematical Geology》1998,30(4):409-434
The concept of an ideal rock texture, in which crystals are distributed randomly in space, is proposed for use in general analysis of rock textures. The spatial correlation function for the ideal rock texture was examined and the function, a specific kind of spatial correlation function, is related to crystal size distribution and to some extent to crystal boundaries. The function is unity at distance zero, and monotonically decreases with increasing distance for the ideal texture. This behavior of the function is observed for any size distribution. In an ideal texture, the function is directly related to crystal size distribution and crystal shape. It is important in stereology because the crystal size distribution in three dimensions may be deduced from analyzing a function that is obtained from analyzing two-dimensional section images. Crystal shape is also related to the function. If crystals are concave in shape, or have inclusions of other phases, the function may show a hump or plateau when plotted against distance. However, the crystal shape effect cannot produce values smaller than zero. If values become negative, the texture is no longer considered ideal. The ideal textures for two model size distributions—step and delta functions—are considered. The rate of decrease of values is more strongly dependent on size distribution than on system dimension. 相似文献
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Jean-Jacques Macaire Christian Di-Giovanni Florent Hinschberger 《Comptes Rendus Geoscience》2005,337(8):735-744
Accumulation of organic matter in fens of fluvial valleys is often related to a low terrigenous matter delivery and to palaeoenvironmental conditions inducing low mechanical erosion. These assumptions come from the interpretation of contents in organic (MO) and mineral (MM) matters in sediments, expressed in percents, and then exactly anticorrelated. Calculation of mass accumulation rates of MO and MM , expressed in g?m?2?yr?1, shows that and generally are not anticorrelated and that high values of and could appear simultaneously. That expression of MO and MM accumulation makes it possible to precise the climatic and human impact on sedimentation. To cite this article: J.-J. Macaire et al., C. R. Geoscience 337 (2005). 相似文献
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