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简单土坡稳定可靠度计算方法的研究 总被引:4,自引:2,他引:4
根据土条间的几何关系提出了土坡稳定分析的辐向条分法,并利用高斯积分法计算出安全系数和极限状态方程的系数,再用改进的JC法求出土坡最小安全系数和最小可靠度指标,辐向条分法是一种高效、准确的土坡稳定性计算方法。 相似文献
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土工织物加筋土坡稳定的塑性极限分析法 总被引:6,自引:3,他引:6
在塑性极限分析理论的基础上,本文给出了土工织物加筋土坡稳定数的上限解。与无筋土坡的已有解比较表明,该解是可靠的,从而为土工织物加筋土坡的稳定分析提供了一个有效的方法。此外,本文的计算结果表明,各种因素对土坡稳定性的影响程度随坡角的增大而减小。 相似文献
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加筋土稳定可靠度分析 总被引:2,自引:0,他引:2
将可靠度分析的JC法运用于加筋土坡稳定分析中,以瑞典法为计算模型,以土的抗剪强度指标C,ψ为基本随机变量,结合工程实例探讨了加筋土坡稳定可靠度分析中的若干规律性问题,得出了一些有益的结论。 相似文献
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煤矿区深部粘性土吸附结合水含量测定及其意义 总被引:6,自引:0,他引:6
通过测定两煤矿区深部粘性土代表土样的吸附结合水含量,结合文献(1)中测试结果,总结出由粘性土塑限(W),估算吸附结合水含量(Wg)的表达式,Wg=0.885W,用该式给出徐滩矿区深部粘性土吸附结合水含量大小,并从粘性土结合水含量方面,解释了徐滩地区采用冻结井时深部冻结管断裂的原因,讨论了深部土层失水后土体压缩变形的特点。 相似文献
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为研究坡顶加载条件下黏性土坡的承载特性和变形规律,进行了素土坡和土钉加固土坡的加载离心模型试验。测量了土坡的承载和变形过程。通过对比两种土坡的承载特性和变性规律,土钉的加固作用体现在:限制了土坡向坡面方向的位移,使土坡的承载能力得到了明显提高;在加固土坡内形成的土钉影响区域改善了加载底板边缘处的薄弱程度;增大了土坡中上部土体的竖向压缩变形,减小了剪切变形,增强了土坡的稳定性。土坡上部土钉的加固效果随着坡顶荷载的增大而越明显;土坡中下部土与土钉的相互作用越靠近坡面越强 相似文献
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降雨往往足引起热带和亚热带膨胀土、残积土边坡失稳的主要促发因素,考虑降雨影响的土坡稳定性预测预报是一个亟待解决的复杂的工程问题.简要介绍了一套能考虑气候影响的非饱和土边坡稳定性分析的极限平衡分析方法和一套可考虑土体非线性和几何非线性的边坡稳定分析及变形计算的有限元方法.提出了一个降雨条件下土质边坡稳定性预测预报模型,其具体思路是:首先用数值方法计算渗流场,然后利用非饱和土的强度理论推求出整个场的强度分布,再利用极限平衡分析方法或有限元方法进行边坡稳定性分析,寻求斜坡稳定安全因数与降雨特征参数(雨强,降雨持时等)相关关系,如此,即可依据气象预报进行土坡稳定性预报. 相似文献
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水位下降是导致滑坡的重要原因之一,而土钉是加固土坡的有效手段。进行离心模型试验,再现了水位下降时土钉加固土坡的变形和破坏过程,测量了土坡的位移变化。试验结果表明,水位下降条件下土钉加固土坡的破坏模式以绕钉破坏为主,滑裂面从坡顶逐渐向下发展至坡面;土钉加固土坡的破坏过程与变形局部化过程表现出显著的耦合变化;土钉加固机制主要表现为通过土钉与坡体的相互作用,减小土坡的变形和变形局部化程度,从而提高土坡的稳定性。增加土钉长度使得滑裂面向坡内部移动,显著减小土坡的变形及变形局部化程度,从而提高了土坡安全性。 相似文献
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目前对均质边坡稳定性受岩土体抗拉强度影响程度的看法不一,尤其是对不同坡度的边坡受抗拉强度的影响甚至有相反意见。基于有限差分程序FLAC3D提供的考虑张拉-剪切复合破坏的Mohr-Coulomb准则,采用强度折减法对多个典型均质边坡进行一系列数值计算,研究土体抗拉强度对不同坡度边坡稳定性的影响。结果表明:边坡越陡,土体抗拉强度对安全系数的影响越大;抗拉强度取值对直立边坡的稳定安全系数及变形破坏特征影响显著,对45°及以下边坡的影响相对较小。总体来说,对于坡角超过60°的陡坡,土体抗拉强度不同引起的边坡安全系数变化幅度可达10%以上,应在边坡稳定分析中特别注意,避免因土体抗拉强度取值过大或过小而导致计算结果偏于危险或过于保守。 相似文献
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System effects should be considered in the probabilistic analysis of a layered soil slope due to the potential existence of multiple failure modes. This paper presents a system reliability analysis approach for layered soil slopes based on multivariate adaptive regression splines (MARS) and Monte Carlo simulation (MCS). The proposed approach is achieved in a two-phase process. First, MARS is constructed based on a group of training samples that are generated by Latin hypercube sampling (LHS). MARS is validated by a specific number of testing samples which are randomly generated per the underlying distributions. Second, the established MARS is integrated with MCS to estimate the system failure probability of slopes. Two types of multi-layered soil slopes (cohesive slope and c–φ slope) are examined to assess the capability and validity of the proposed approach. Each type of slope includes two examples with different statistics and system failure probability levels. The proposed approach can provide an accurate estimation of the system failure probability of a soil slope. In addition, the proposed approach is more accurate than the quadratic response surface method (QRSM) and the second-order stochastic response surface method (SRSM) for slopes with highly nonlinear limit state functions (LSFs). The results show that the proposed MARS-based MCS is a favorable and useful tool for the system reliability analysis of soil slopes. 相似文献
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鄂西北山区降雨型边坡失稳模式和评价方法 总被引:2,自引:1,他引:1
2003年6月的一次连续降雨诱发了鄂西北山区郧漫公路沿线多处边坡失稳。根据边坡岩土体的组成和结构特征,总结出了5种典型的暴雨型边坡失稳模式:浅层堆积体滑移、含软弱面顺层滑移、切层边坡水压劈裂破坏、碎裂岩似弧形追踪破坏和块裂岩楔体滑移。根据边坡破坏特点和降雨作用形式提出了相应的评价方法,认为浅层堆积体在暴雨下含水量,即85%~100%液限含水量时易发生滑移,通过平面无限斜坡评价法计算边坡稳定性;含软弱面顺层边坡及块裂楔形体均为剪切滑移失稳,采用简化的刚体极限平衡法计算其稳定性;切层边坡中陡倾裂缝经历了卸荷张开-水压开裂-贯通破坏的过程,通过Ⅰ型裂缝扩展判据评价边坡稳定性;碎裂岩边坡发生类似弧形滑移的追踪破坏,采用连续介质圆弧法计算边坡稳定性。 相似文献
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祁连山大野口流域土壤水热空间变化特征研究 总被引:4,自引:2,他引:2
土壤水热对水源涵养功能的发挥影响较大,为了研究流域空间上的水源涵养功能变化规律,在祁连山大野口流域布设90个土壤水热监测探头,对已取得的100多万个数据采取相关分析、变异系数等方法,研究土壤水热空间的变化特征.结果表明:随海拔增大,土壤水分呈波动性增大趋势,增大率约为2.35%·(100m)-1,土壤温度呈波动性降低趋势,降低率约为0.74℃·(100m)-1.半阴坡土壤水分比半阳坡高1.2倍、比阳坡高1.7倍,半阳坡土壤水分比阳坡高1.4倍.半阴坡土壤温度比半阳坡低1.6倍、比阳坡低2.2倍,半阳坡土壤温度比阳坡低1.3倍.土壤水分与其深度呈二次函数的抛物线变化关系,土壤温度与其深度呈线性函数关系,深度每增加10 cm,其温度降低约0.536℃.亚高山灌丛林比乔木林土壤水分高1.5倍、比草地高1.7倍,乔林比草地土壤水分高1.2倍.亚高山灌丛林比乔木林土壤温度低1.6倍、比草地低2.3倍,乔木林土壤温度比草地低1.4倍.高海拔半阴坡灌丛林土壤温度变化最剧烈,低海拔阳坡草地土壤变化较小.研究成果可为探索流域水资源管理及利用提供科学依据和参考资料. 相似文献
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Lower bound dynamic shakedown theory is a limit state method. It is employed herein to investigate the safety, which is associated with permanent displacement, of slopes under repeated dynamic loads, mainly earthquakes. An efficient numerical method, previously applied to the static shakedown of pavements, is extended to the dynamic shakedown of slopes in this study. It is shown that dynamic shakedown, unlike other limit state methods, is able to consider the dynamic properties of both the load and subsoil. The effect of the soil strength parameters and dynamic features of the soil and loads are examined thoroughly and some illustrative examples are employed. The short-term and long-term behavior of slopes under seismic loads are studied as well, comparing results of the present study with the well-known displacement method of Newmark. 相似文献
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Evaluating relationships between soil chemical properties and vegetation cover at different slope aspects in a reclaimed dump 总被引:1,自引:0,他引:1
Xiaoyang Liu Yingui Cao Zhongke Bai Jinman Wang Wei Zhou 《Environmental Earth Sciences》2017,76(23):805
Conducting research about the relationships between soil chemical properties and vegetation coverage at different slope aspects is especially important in reconstructed ecosystems of vulnerable ecological regions. This study was conducted in the first reclaimed dump within the Pingshuo mining area of Shanxi Province, China, to analyze patterns of soil chemical properties (soil organic matter (SOM), soil total nitrogen (STN), soil available phosphorus (SAP) and soil available potassium (SAp) and vegetation coverage (NDVI) and their correlations at different slope aspects. In the reclaimed dump, 26 quadrats were established along four slope aspects (i.e., shady, semi-shady, sunny and semi-sunny slopes). There was no significant difference in SOM or STN among different slope aspects, while SAP differed between shady slopes compared to semi-shady, sunny and semi-sunny slopes; SAP differed significantly between semi-shady and semi-sunny slopes. The NDVI of semi-sunny slopes differed significantly from that of the other three aspects. There was variation in the relationships between NDVI and soil chemical properties, depending on the slope aspects. The logarithm of SOM and NDVI was related linearly on shady and semi-shady slopes, while NDVI was inversely related to the natural logarithm of the logarithm of SOM on sunny and semi-sunny slopes. STN and NDVI had a first-order function relationship on shady and semi-shady slopes, yet a quadratic function relationship on sunny and semi-sunny slopes. The relationships between SAP and NDVI were inverse on all types of slopes. On shady and semi-shady slopes, NDVI had a quadratic relationship with the logarithm of SAp, but it was well fitted by using a cubic function on sunny and semi-sunny slopes. The sensitivity coefficients of soil chemical properties and NDVI were different, and soil chemical properties changed differently depending on changes in NDVI at different slope aspects. 相似文献
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《Geomechanics and Geoengineering》2013,8(1):51-62
The fundamental principles of the strength reduction method (SRM) are incorporated into the rock failure process analysis (RFPA) code to produce an RFPA–SRM method for analysing the failure process and stability of rock and soil slopes. The RFPA–SRM method not only satisfies the global equilibrium, strain-consistent, and non-linear constitutive relationship of rock and soil materials but also takes into account the heterogeneous characteristics of materials on the micro- and macro-scales. When the proposed method is used for slope stability analysis, both the critical failure surface and the safety factor can be obtained directly without any assumptions regarding the shape and location of the failure surface. The numerical results agree well with those obtained using conventional limit equilibrium and other FEM strength reduction methods. The proposed technique is applied to a number of more complex cases, including slopes in mixed rock–soil formations, rock layer formations, and highly jointed rock masses. It is shown that the RFPA–SRM method can describe the mechanism of failure of slopes and has potential applications in a large range of geoengineering problems. 相似文献