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1.
The authors analyzed the engineering geological characteristics of the slope of the study area (K75+840-K76+340). Two typical cross-sections have been chosen to analyze the failure modes after the excavation of the highway. Different types of the failure modes have been calculated and analyzed. The results show that some dealing methods have been advised to ensure the stability of the slopes.  相似文献   

2.
针对泰山第四纪冰川有无的争议,在泰山南坡采集沉积物样品进行分析研究。孢粉分析结果显示优势植物种群为"松属+中华卷柏+蒿属+藜科",指示的沉积环境为湿冷环境。扫描电镜观察石英颗粒表面,显示出边缘棱角清晰、具贝壳状断口和解理片的冰川环境特征。通过热释光测试得样品年龄为(30.54±2.59)kaB.P.,相当于末次冰期主冰期中的Paudorf-Stillfried间冰阶。根据泰山现代气候环境推演泰山古气候温度和降水量,得出泰山地区在末次冰期时具备了形成冰川的基本气候条件。鉴于Paudorf-Stillfried间冰阶持续的时间较短,因此初步推断该沉积物指示的古气候环境为冰缘环境。  相似文献   

3.
模拟堆载作用的黄土边坡土体变形机理试验   总被引:3,自引:0,他引:3  
通过固结不排水剪试验,研究了堆载作用下不同深度、含水量和围压的原状黄土的变形和破坏特征,并从黄土的微观结构角度分析了产生这一现象的原因,结合黄土边坡特殊的工程地质条件,分析了堆载作用下黄土边坡土体的变形破坏过程。试验结果表明,不同深度、含水量和围压的原状黄土的应力应变曲线和抗剪强度具有不同的特征;特殊的工程地质条件,使黄土坡体的某些部位形成了堆载作用下不利于黄土材料强度保持的含水量和围压的组合,导致了这些部位黄土的变形破坏,进而诱发坡体的变形破坏。  相似文献   

4.
通过实地踏勘并辅以钻探等技术手段,对枞阳县高峰村同咀崩塌的边坡地形地貌、地层岩性、地质构造、水文地质条件、工程地质条件以及人类工程活动等条件进行调查,并在进行变形位移监测的基础上,对研究区崩塌灾害的发育特征、影响因素以及形成机制进行了分析,并采用极限平衡法对崩塌灾害的稳定性进行了评价。研究结果表明:2处崩塌灾害规模等级均属小型,破坏方式均为滑移式;影响因素主要包括人工切坡,钾长花岗岩强烈风化,构造裂隙、风化裂隙和卸荷裂隙发育和强降雨等; 2处崩塌在天然工况下处于基本稳定状态,在暴雨工况下处于欠稳定状态,需采取相关治理措施。依据分析评价结果对崩塌灾害治理提出了防治方案建议。  相似文献   

5.
基于可靠度理论建立顺层岩质边坡稳定的可靠性分析方法,获得顺层岩质边坡可靠指标和失稳概率的计算表达式。以某高切坡为例分析其稳定状态和失稳概率,并据此探讨不同粘聚力、内摩擦角、炸药量和爆心距条件下边坡失稳概率的变化规律。计算结果表明,粘聚力对边坡的失稳概率影响较大;随着内摩擦角的增加,边坡失稳概率近乎线性减小;当单孔药量从10 kg增大到160 kg后,失稳概率增幅97.10%;当爆心距小于20 m时,边坡的失稳概率减小的速度很快,而爆心距超过20 m后边坡失稳概率减小的幅度较小。考虑爆破振动的时效性,爆破荷载使边坡失稳概率增大49.61%,单次爆破振动的影响时间约6 s。  相似文献   

6.
该文说明“修正曲线方程”与“曲线方程”的差异及其建立的过程。曲线方程实质上是采用直线方程表达的两相关函数的关系式。但是,按直线方程发展趋势推测的范围较小,误差较大。而修正曲线方程是在曲线方程的基础上探索出的一种新的计算方法。它将曲线方程y=a+bx中的参数(a、b)由常数值导成随x变化的不定值(a_i、b_i)。因此,修正曲线方程则是拟合曲线自然发展的一种方程式。函数的变化规律基本上是沿曲线变化的。它推测的较远,结果误差较小,可广泛应用于水文地质、工程地质等不同学科的领域中。  相似文献   

7.
The E24 profile slope analyzed belongs to a series of excavated slopes of the Haizhou Opencast Coal Mine. It seems to be divided into Downslope Part and Upslope Part. Its profile comprises two noticeable coal seams, called the 8# and 9# weak layers, considered as the potential failure surfaces. In consideration of the actual configuration as in the perspective of any modification, assessing the stability of this slope with various profile forms under given conditions, and assessing the risk of instability and quantifying the influence of earthworks or other modifications to the stability of this slope, have constituted the primordial objectives carried out. From assumed potential failure surfaces, any specific profiles and specified slip surfaces are defined. A factor of safety (FoS) is computed for each specified slip surface; the smallest FoS found corresponds to the least favorable slip surface. The safety factor values obtained are compared to the suggested safety factor. Limit equilibrium methods of vertical slices implemented in Slope/W, computer program for slope stability analyses, have been adopted to perform the E24 slope stability analysis. The safety factor values computed with 9# weak layer are lower than for 8#; the factors of safety obtained with Sarma's method are the smallest; more, without groundwater (long term) overall values are greater than those determined under groundwater condition (short term). The lowest safety factor value is found for a profile depending on an adopted earthwork sequence. The E24 profile slope stability analysis shows the instability risk for the deepest weak layer, and also shows the short and long term stability of this slope for the envisaged earth movements. However it demonstrates the existence of instability risk for any earthwork firstly affecting the downslope part.  相似文献   

8.
The E24 profile slope analyzed belongs to a series of excavated slopes of the Haizhou Opencast Coal Mine. It seems to be divided into Downslope Part and Upslope Part. Its profile comprises two noticeable coal seams, called the 8# and 9# weak layers, considered as the potential failure surfaces. In consideration of the actual configuration as in the perspective of any modification, assessing the stability of this slope with various profile forms under given conditions, and assessing the risk of instability and quantifying the influence of earthworks or other modifications to the stability of this slope, have constituted the primordial objectives carried out. From assumed potential failure surfaces, any specific profiles and specified slip surfaces are defined. A factor of safety (FoS) is computed for each specified slip surface; the smallest FoS found corresponds to the least favorable slip surface. The safety factor values obtained are compared to the suggested safety factor. Limit equilibrium methods of vertical slices implemented in Slope/W, computer program for slope stability analyses, have been adopted to perform the E24 slope stability analysis. The safety factor values computed with 9# weak layer are lower than for 8#; the factors of safety obtained with Sarma's method are the smallest; more, without groundwater (long term) overall values are greater than those determined under groundwater condition (short term). The lowest safety factor value is found for a profile depending on an adopted earthwork sequence. The E24 profile slope stability analysis shows the instability risk for the deepest weak layer, and also shows the short and long term stability of this slope for the envisaged earth movements. However it demonstrates the existence of instability risk for any earthwork firstly affecting the downslope part.  相似文献   

9.
Stability is always the most important problem after high slope was excavated. The study analyzed the stress and strain inside the slope by Finite Element Method (FEM) and carried through stress distribution and failure zone, then analyzed the stability of the slope using three different methods and came to the conclusion that it is in unstable condition, so the designed retaining wall was put forward which makes the slope stable.  相似文献   

10.
Stability is always the most important problem after high slope was excavated. The study analyzed the stress and strain inside the slope by Finite Element Method (FEM) and carried through stress distribution and failure zone, then analyzed the stability of the slope using three different methods and came to the conclusion that it is in unstable condition, so the designed retaining wall was put forward which makes the slope stable.  相似文献   

11.
本文在分析横山山体地质条件及因地下采空而诱发出的山体变形破坏特征的基础上,对采空区地表山体的变形破坏进行了工程地质力学模拟研究。结果表明,横山山体之下3号煤层的采动坍陷是引起山体变形破坏的直接原因;毗邻山体的电厂区地表隆起变形破坏,是因采空区上覆岩层在坍陷时所产生的向电厂方向的蠕动,致使厂区地基土遭受挤压和变形的结果;随着3号煤层采动的结束及其上覆岩层坍陷过程的完成,电厂区将会恢复到稳定状态。 通过分析,山体岩层倾角增大时有无地下采空影响的山体变形破坏的不同特征,得出了同时具有地表侵蚀临空面和地下采空临空面的山体与仅有地表侵蚀临空面之斜玻的山体变形破坏是不同的。从不同模型材料所得实验结果的一致性,验证了此模拟实验在理论上和实际中都有很好的相似性。  相似文献   

12.
The stability of slopes is always of great concern in the field of rock engineering. The geometry and orientation of pre-existing discontinuities show a larger impact on the behavior of slopes that is often used to describe the measurement of the steepness, incline, gradient, or grade of a straight line. One of the structurally controlled modes of failure in jointed rock slopes is plane failure. There are numerous analytical methods for the rock slope stability including limit equilibrium, stress analysis and stereographic methods. The limiting equilibrium methods for slopes under various conditions against plane failure have been previously proposed by several investigators. However, these methods do not involve water pressure on sliding surfaces assessments due to water velocity and have not yet been validated by case study results. This paper has tried to explore the effects of forces due to water pressure on discontinuity surfaces in plane failure through applying the improved equations. It has studied the effect of water flow velocity on sliding surfaces in safety factor, as well. New equations for considering water velocity (fluid dynamics) are presented. To check the validity of the suggested equations, safety factor for a case study has been determined. Results show that velocity of water flow had significant effect on the amount of safety factor. Also, the suggested equations have higher validity rate compared to the current equations.  相似文献   

13.
丹崖山边坡稳定性是关系古文物蓬莱阁安全的关键问题。丹崖山边坡高差大、断层裂隙发育、岩体卸荷深度大,地质条件十分复杂,边坡在施工期和运行期的稳定性问题特别突出。该文介绍了丹崖山岩体加固后的监测布置,并对岩体表面变形趋势、空间分布形态、加固后变形趋势进行分析,通过对多点位移计、锚杆测力计、锚索测力计、表面裂缝计及地表变形等监测结果进行综合分析,得到边坡岩体的变形规律。  相似文献   

14.
受地形条件限制,我国西南山区大量房屋修建在滑坡上,存在安全隐患。探明滑坡对其上房屋的作用机理,科学指导滑坡上房屋设计和防护,对保障居民生命财产安全、促进人地和谐发展具有重要意义。基础是滑坡对其上房屋作用的直接对象,因此,以砌体结构房屋基础为研究对象,采用室内物理实验和数值模拟相结合的方法,对比分析试验与模拟中基础的变形特征,验证数值模型边界设置的可靠性,开展房屋基础在滑坡不同作用模式下变形破坏特征的研究。结果表明:建筑物基础在滑坡缓慢变形作用下的破坏模式可归纳为3种:张拉、剪切和挤压模式;房屋裂缝发育的位置与滑坡地表裂缝位置关系密切,随着滑坡主滑方向与房屋基础夹角的增大,房屋基础破坏越严重。因此,在房屋的选址和设计时,应优先利用滑坡挤压区或减小房屋长边中轴线与滑坡主滑方向的夹角。   相似文献   

15.
该文对传统护坡和生态护坡进行了比较分析,并以重庆市江津区大肚子河整治工程为实例,说明2种护坡组合应用可以扬长避短,为今后水利工程建设提供了较好的参考。  相似文献   

16.
随着工业化、城市化不断加快,临沂市人地关系矛盾不断加剧,可供开发利用的土地资源日益紧缺。基于临沂市低丘缓坡地资源禀赋特点,深刻剖析当前低丘缓坡综合开发利用的制约因素及原因,依此提出有关对策和建议。  相似文献   

17.
本文通过研究山东省废弃露天矿山现状,分析存在的矿山地质环境问题。在总结以往废弃露天矿山生态修复情况的基础上,以“双碳”战略目标为引领,对废弃露天矿山生态修复所涉及的对象、技术、修复方向等进行了系统的研究,总结了生态复绿、农业用地、科普教育基地、旅游业用地、建设用地5种废弃露天矿山生态修复模式。以山东省废弃露天矿山生态修复经验为例,说明5种矿山生态修复模式在历史遗留废弃露天矿山生态修复工作中的实践应用。  相似文献   

18.
露天矿山对区域土地与环境产生了复杂多样的负面影响,已成为生态系统修复等方面研究解决的焦点问题。本文分析、诊断、识别了废弃露天矿山修复目标、存在问题及特征,归纳总结了常用的治理模式;厘清了废弃露天矿山治理思路与方法,创新构建了更具针对性、实用性的技术体系;针对废弃露天矿山典型现状,归纳总结出研究区几种典型修复方法。旨在为泰安市山水林田湖草生态修复区废弃露天矿山生态修复治理提供技术参考,同时,对我国类似矿山开采区的恢复治理工作也具有一定的借鉴意义。  相似文献   

19.
本文以黄河上游某拟建水电站坝址场地为例,论证了圈闭地形内斜坡破坏的多期性和规律性问题。在充分的野外调查和室内研究资料的基础上,将区内的斜坡破坏分为两期,即第一期为已经失稳的老滑坡群;第二期为发育在第一期滑坡群圈闭状破裂壁之后的正处于蠕动和破坏阶段的变形坡体,进而将第一期的滑坡分为两个强度次序。同时,还揭示了圈闭地形内斜坡破坏的规律性,即随着期和序次的增高,斜坡破坏面积增大,滑坡个数增多,规模减小,强度降低,滑距变短,滑体破碎程度变弱。最后指出,上述多期性和规律性应具有普遍性意义。  相似文献   

20.
建立科学有效的规划层级传导机制是保障国土空间生态修复规划治理效力的重要前提。随着我国国土空间规划体系建立与完善,作为其重要专项规划的国土空间生态修复规划,需要明确各层级规划的定位、内容以及传导路径。本文基于国土空间生态修复规划编制实践,探讨了规划层级传导的基础与策略,提出了“4+4”规划层级传导框架,明确了规划层级传导要素及其传导方式,从政策和技术层面提出了规划层级传导的运行机制,以期为国土空间生态修复规划编制和分级管理提供参考。  相似文献   

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