首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 167 毫秒
1.
为了阐明地震滑坡的运动特性并对其进行致灾距的预测,基于遥感影像解译和野外调查数据,借助经验公式法,分析了汶川地震滑坡水平最大运移距离L与前后缘高差H之间的相关性,给出了经验公式;探讨了不同滑坡之间滑程的差异与异常。结果表明:若已知H,可用L=aH+b或L=aHb对总位移进行预测初探;将视摩擦系数H/L=0.45作为汶川地震高速远程型滑坡的上限较合适;滑坡体积、源区破裂面积与L呈正相关,与H/L呈负相关;地震滑坡易发生在山脊线平行于断裂带、垂直于地震波传播方向的山体两侧;崩塌型滑坡易发前后缘高差范围在10~100m之间,大型高速远程型滑坡易发前后缘高差大于200m;滑坡源区易发坡度分布在25°51°之间,滑床坡降变化范围为0~58°,高速远程型滑坡的滑床坡降主要在8°20°之间;分析认为滑程差异和异常是距离效应、能量传递与岩体挡板效应、滚动润滑与气垫效应、体积与破裂面积效应、地质因子、地形因子、颗粒级配与颗粒流效应等因素综合作用的结果,考虑上述因素有益于滑坡-碎屑流致灾距的预测分析。   相似文献   

2.
本文对浙、赣、闽地区的陆上火山碎屑流沉积物,从实测地质剖面、粒度分析、原生构造以及岩石组合与火山机构的关系等方面进行了研究。发现该地区陆上火山碎屑流沉积剖面的特征比R.S.J.Sparks等人提出的“标准熔结凝灰岩单元流层”模式更为完整和典型。对比该区典型地质剖面之后,本文提出了陆上火山碎屑岩相的分析,初试确立陆上火山碎屑流形成机制与相鉴别标志的联系,建立了陆上火山碎屑岩各种类型的相模式。  相似文献   

3.
全周边注浆法处治碎屑流技术在雁门关隧道中的应用   总被引:1,自引:0,他引:1  
阐述了山西大运高速公路北段新广武—原平间‘雁门关隧道’(我国已建成高速公路中最长的公路隧道)的地质地形特点,由于隧道段为构造隆起上升区,属剥蚀、侵蚀中山区,在隧道ZK110+883—ZK110+918洞段施工中,发生了大规模的碎屑流。采用"全周边注浆法"对碎屑流进行了全方位的处治。详细描述了该方法封堵碎屑流具体的步骤,为高速公路长隧道碎屑流病害处治提供了宝贵经验。对同类工程建设施工起到借鉴和指导作用。  相似文献   

4.
通过整理分析大量的崩塌滑坡位移-时间曲线发现,孕育期地表位移时序曲线典型类型主要有稳定型、渐进型和突发型3类,其中稳定型分为蠕滑稳定型和波动稳定型2亚类,渐进型分为三阶段渐进型、振荡渐进型和多台阶渐进型3亚类;孕育期地下位移时序曲线典型类型主要有单滑裂面型和多滑裂面型2类,并发现滑带处位移时序曲线与地表的具有相似的演化规律;从孕育、成灾到形成崩滑堆积体的全过程位移时序曲线典型类型只有生长型一类。基于崩塌滑坡滑裂面上锁固段数量、位置和强度,结合变形状态空间区划效应及外界因素对锁固段的加卸载特征,对孕育期地表典型位移时序曲线形成机制进行了探讨。   相似文献   

5.
通过岩心描述以及粒度、薄片资料的综合分析,结合区域古地貌特征、地震相研究成果,详细论述了琼东南盆地陵水凹陷北部梅山组砂质碎屑流砂岩沉积构造特征及识别标志,并在此基础上建立了研究区砂质碎屑流沉积模式。研究区梅山组砂质碎屑流砂岩主要为厚层块状构造粉砂岩-极细砂岩以及具有丰富同生变形构造的粉砂质泥岩、泥岩与粉砂岩互层2种岩性组合,成因为陆架坡折之上的三角洲前缘、前三角洲沉积物发生整体性"冻结"滑动、滑塌再沉积所形成,其平面分布主要受陆架坡折所控制,大致呈平行于陆架坡折带分布的舌形形态。结合区域油气成藏要素研究认为研究区砂质碎屑流砂岩可通过沟源断层沟通深部烃源岩,形成下生上储型岩性油气藏,为琼东南盆地大中型油气藏勘探突破的重点领域。   相似文献   

6.
莺歌海盆地东方气田莺二段发育浅海砂质碎屑流,对其沉积特征与模式的研究具有重要意义。从岩心精细描述入手,结合测井曲线特征、地震剖面、地球化学实验,综合国内外重力流研究进展,确定了研究区浅海砂质碎屑流的岩心、测井、地震相特征,并通过分析研究区沉积背景,进一步探讨了东方气田莺二段ⅡL、ⅢU气组浅海砂质碎屑流的沉积模式。研究结果表明:该区砂质碎屑流的岩心相为富漂浮泥岩碎屑的块状砂岩、"泥包砾"等典型砂质碎屑流特征;测井相上表现为齿化现象十分严重的逆粒序漏斗型及无粒序钟型-漏斗型复合型特征;地震相上表现为中振幅平行席状反射和低频平行-亚平行空白反射特征;剖面上呈席状和平缓透镜状展布。研究厘定了研究区砂质碎屑流为西侧三角洲前缘由于风暴作用引起沉积物滑塌再搬运和北侧红河洪水重力流共同作用形成的浅海砂质碎屑流沉积模式。   相似文献   

7.
砂土三轴剪切过程中细观孔隙结构演化与其宏观力学性质之间存在着紧密联系。基于南京大学自主研发的微型三轴仪,对南京粉砂试样进行了三轴剪切试验,利用显微CT扫描,获得了加载过程中试样的三维孔隙结构演化特征。结果表明:试样表现出应变软化-硬化型的应力-应变关系曲线;端部摩擦阻碍试样体积膨胀,发生鼓形区状破坏;试样整体体孔隙率从初始的46.3%减小到40.9%,后增大到43.0%附近,且试样破坏区孔隙率显著增大;统计区状破坏区表征单元体孔隙参数,发现破坏前孔隙被压密消失,孔隙数量减少32.4%,平均孔隙半径减小48.8%,导致孔隙半径分布趋于集中,破坏后破坏区域内出现大量大半径的孔隙;颗粒间错动导致颗粒棱角破碎,使孔隙形状趋于规则。  相似文献   

8.
四川石棉熊家沟曾于2013年7月4日爆发泥石流,该次泥石流物源类型多样、形成机理复杂,并发生堵塞主河的次生灾害链,具有代表性。通过研究,本次泥石流是在强降雨条件下,以中上游沟道松散物为启动点、沿程下切拉槽、崩滑不断参与运动的一场由自然因素形成的地质灾害。泥石流形成因素分为强降雨、沟道物源启动、崩滑规模扩大3个方面。参与熊家沟泥石流启动汇集的物质来源为沟道物源和崩滑物源,其中,沟道物源量占总量的81.55%。物源补给以沟道松散物为主,崩滑直接提供物源量小分散。经过“7·04”灾害后,流域沟道淤积抬升,形成新的沟道松散物,为下次泥石流埋下了隐患。熊家沟泥石流的成灾模式类型多样,表现为淤积抬高、撞击冲毁、堵塞主河、淹没上游。通过堵河经验公式判别,“7·04”熊家沟泥石流的形成特征极易发生堵河,当地政府与防灾减灾部门应有的放矢做好地质灾害防治工作。   相似文献   

9.
滑坡稳定性评价是滑坡防治中关键问题之一, 滑坡失稳破坏判据研究可为滑坡稳定性评价提供支持。为了提高滑坡稳定性评价的精度, 以滑坡深部位移监测数据为基础的滑坡失稳破坏判据不失为一种有效方法。基于滑坡深部位移监测数据, 引入滑带完整性指标, 推导得到了滑带完整性指标与滑坡抗剪强度参数之间呈正比例关系; 运用滑坡稳定性计算方法和三峡库区堆积层滑坡简化模型, 获得了滑带完整性指标与滑坡的稳定性系数之间呈正比例关系。建立了考虑滑带完整性指标的三峡库区堆积层滑坡失稳破坏判据, 即: 当滑坡滑带土完整性指标大于滑坡滑带土完整性指标的临界值时, 滑坡处于稳定状态; 当滑坡滑带土完整性指标小于滑坡滑带土完整性指标的临界值时, 滑坡发生失稳破坏。以三峡库区典型堆积层滑坡——五尺坝滑坡为例, 通过实例分析发现该判据具备可靠性, 对堆积层滑坡适用性好。研究成果表明, 滑带完整性指标失稳破坏判据可以用于评价滑坡的稳定状态, 为滑坡失稳破坏判据研究提供了一种新思路。   相似文献   

10.
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   

11.
岩性识别作为人工智能和大数据在地质工程细分领域的实践应用方向, 可以为相关人员野外地质工作提供有效助力。为了更好地促进岩性识别在专业领域的应用, 通过对巢湖北部山区的岩石图像采集、数据预处理、迁移学习、网络搭建、网络训练及模型测试等步骤, 实现了基于岩石图像的大数据深度学习识别; 并在归纳总结前人工作的基础上, 提出了多尺度岩性识别方法。根据岩石细观图像建立多尺度模型并赋予一定权重, 与岩石识别模型共同识别得到综合结果, 对岩石岩性整体识别的同时兼顾局部纹理、粒径等细观信息。研究结果表明, 本模型对岩石识别的适用性强, 多尺度方法对于提高识别结果的正确率具有一定的帮助, 模型的测试正确率达到95%以上, 能很好地识别岩石岩性。   相似文献   

12.
Analyzing large prehistoric rock avalanches provides significant data for evaluating the disaster posed by these relatively infrequent but destructive geological events. This paper attempts to study the characteristics and dynamics of the Ganqiuchi granitic rock avalanche, in the middle of the northern margin of Qinling Mountains, 30 km to the south of Xi’an, Shaanxi Province, China. In plane view, this rock avalanche is characterized by source area, accumulation area and dammed lake area. Based on previous studies, historical records and regional geological data, the major trigger of the Ganqiuchi rock avalanche is considered to be a strong paleo-earthquake with tremendous energy. The in situ deposit block size distributions of the intact rock mass and the debris deposits are presented and analyzed by using a simple model for estimating the number of fragmentation cycles that the blocks underwent. The results show that the primary controlling factor of the fragmentation process is the pre-existing fractures, and there is a relationship between the potential energy and the fragmentation energy: the latter is approximately 20% of the former. Based on the dynamic discrete element technique, the study proposes a four-stage model for the dynamic course of the Ganqiuchi rock avalanche:(1) failing;(2) highspeed sliding;(3) collision with obstacles;(4) decelerated sliding, which has implication for hazard assessment of the potential rock avalanches in China and other countries with similar geological setting.  相似文献   

13.
《山地科学学报》2020,17(7):1581-1595
The great diversity and complexity of geological hazards in terms of flowing materials, environment, triggering mechanisms and physical processes during the flow bring great difficulties to the numerical parameter selection for the discrete element method. In order to identity the significance of individual parameters on the landslides dynamic process and provide valuable contribution to the runout analysis of similar landslide, the dynamic process and associated microscopic mechanism of the Turnoff Creek rock avalanche in Canada are simulated. The present numerical results are compared with the field survey data and the results of depth-integrated continuum method. The final deposit range matches well with the field survey data. It is illustrated that the discrete element method is robust and feasible to capture the dynamic characteristics of large rock avalanche over a complex terrain. Besides, a new method to assess the landslide hazard level based on the discrete element method is proposed. According to the parameter sensitivity analysis, it is demonstrated that the basal friction coefficient and bond strength are essential to the final deposit while rolling coefficient and restitution coefficient have little effects on it.  相似文献   

14.
The effect of blasting vibration waves on surrounding rock and supporting structures is an important field in underground engineering. In this paper, the separation variable method is used to solve the displacement potential function for the propagation of the blasting vibration waves. In the axis coordinate system, the particle motion and stress change with axial distance, radial distance and time is obtained in surrounding rock. The peak particle velocity law in surrounding rock under different blast loads and surrounding rock parameters is discussed. In addition, the particle vibration characteristics in the surrounding rock are studied using numerical simulations method. The results shows that the peak particle velocity in surrounding rock appears negative exponent attenuation with the increase of axial distance, but it appears positive and negative fluctuations in radial direction. This phenomenon is a new discovery and it has been rarely investigated before. Moreover, the peak particle velocity attenuates more quickly and intensely in the near blasting field, which means that the supporting structure in a shorter distance away from the heading face is vulnerable to the impact of blasting vibration. The attenuation of blasting vibration velocity is closely related to charge length, blasting load amplitude, attenuation index and rock elastic modulus. The numerical simulation accomplishes the same results and then demonstrates the validity of theoretical results.  相似文献   

15.
Mountain hazards with large masses of rock blocks in motion – such as rock falls, avalanches and landslides – threaten human lives and structures. Dynamic fragmentation is a common phenomenon during the movement process of rock blocks in rock avalanche, due to the high velocity and impacts against obstructions. In view of the energy consumption theory for brittle rock fragmentation proposed by Bond, which relates energy to size reduction, a theoretical model is proposed to estimate the average fragment size for a moving rock block when it impacts against an obstruction. Then, different forms of motion are studied, with various drop heights and slope angles for the moving rock block. The calculated results reveal that the average fragment size decreases as the drop height increases, whether for free-fall or for a sliding or rolling rock block, and the decline in size is rapid for low heights and slow for increasing heights in the corresponding curves. Moreover, the average fragment size also decreases as the slope angle increases for a slidingrock block. In addition, a rolling rock block has a higher degree of fragmentation than a sliding rock block, even for the same slope angle and block volume. Finally, to compare with others' results, the approximate number of fragments is estimated for each calculated example, and the results show that the proposed model is applicable to a relatively isotropic moving rock block.  相似文献   

16.
Clogging effect, as a new concept in geological engineering, is a phenomenon of permeability decreasing under seeping in reservoir dam foundation of the alluvial and diluvial deposits with deep and thick layer, coarse particle and high permeability in mountains-gully rivers of Tibetan Plateau. A clogging infiltration instrument has been designed successfully and a series of simulation tests have been done. Based on large amounts of data, it is confirmed that the existence of the clogging effect and the law of infiltration clogging is found out. Three indexes are proposed such as "optimal size of particle", "optimal size range of particle" and "characteristic pore", which are closely related with effect of infiltration clogging. The concept and results can offer a new idea to solve problems on anti-seepage of dam foundation in mountains-gully rivers environment and to study artificial clogging, meanwhile supplement of the concept of seepage deformation.  相似文献   

17.
目前,偏振遥感已被用于气溶胶卫星和地基遥感中,其仅对小粒子敏感。本研究以2007-2008年间的POLDER(Polarization and Directionality of the Earth’s Reflectances)和AERONET(Aerosol Robotic Network)合肥站的气溶胶数据为研究对象,探讨了偏振遥感对气溶胶粒子尺度的敏感性。利用AERONET合肥站的尺度分布数据和折射指数数据,计算了不同尺度范围内气溶胶粒子的光学厚度,并与对应的POLDER反演结果作拟合,通过寻找最佳拟合对应的尺度范围确定偏振遥感敏感的粒子尺度。结果表明,偏振遥感并非对所有尺度的小模式气溶胶粒子都敏感,在865 nm波段,其敏感的气溶胶粒子上限半径约为0.3 μm左右。这一结果对指导气溶胶偏振遥感,以及理解和应用偏振遥感气溶胶产品等具有重要意义。  相似文献   

18.
A pair of flumes with variable inclinations were employed to investigate the entrainment mechanics and dynamical evolution of a debris avalanche/flow. A fixed quantity of solid and water mixture was released from a constant elevation and accelerated along a higher chute to impact substrate materials with different water contents and particle size distributions in the lower chute. Two high-speed cameras, pore and earth pressure detecting devices, were placed in the substrate materials where severe scouring occurs in order to collect multiple measurements of dynamical and mechanical parameters. The entrainment dynamics were verified by geometrical analysis and quasi-static simulation. The results show that wet and fine materials that are placed in the lower chute with steeper slopes are easily entrained during debris flow initiation, the pattern of which can be described by Coulomb friction and the Mohr-Coulomb law. Elaborate measurements of dynamical parameters enable the results of an elementary computational framework to predict the time-dependent scouring depth ht, which provides insight into rapidly determining debris flow propagation. Finally, the post-entrainment dynamics were studied. The results indicate that the propagation and the amplification of debris flows along erodible beds are dominated by the velocity and the solid volume fraction of the mixed substrate, and the coarse particle group of the substrate is a key feature affected by momentum changes.  相似文献   

19.
The right-bank slope of the Dagangshan hydropower station located in Southwest China is a highly unloaded rock slope. Moreover, large-scale natural faults were detected in the slope body; some excavation-induced unloading fractures were discovered at elevations between 1075m and 1146m. Because of poor tectonic stability, the excavation work was suspended in September 2009, and six largescale anti-shear galleries were employed to replace the weak zone in the slope body to reinforce the rightbank slope. In this study, based on microseismicmonitoring technology and a numerical-simulation method, the stabilities of the slope with and without the reinforcement are analysed. An in-situ microseismic-monitoring system is used to obtain quantitative information about the damage location, extent, energy, and magnitude of the rocks. Thus, any potential sliding block in the right-bank slope can be identified. By incorporating the numerical results along with the microseismic-monitoring data, the stress concentration is found to largely occur around the anti-shear galleries, and the seismic deformation near the anti-shear galleries is apparent, particularly at elevations of 1210, 1180, 1150, and 1120m. To understand the interaction mechanism between the anti-shear gallery and the surrounding rock, a 2D simulation of the potential damage process occurring in an anti-shear gallery is performed. The numerical simulation helps in obtaining additional information about the stress distribution and failure-induced stress re-distribution in the vicinity of the anti-shear galleries that cannot be directly observed in the field. Finally, the potential sliding surface of the right-bank slope is numerically obtained, which generally agrees with the spatial distribution of the in-situ monitored microseismic events. The safety factor of the slope reinforced with the anti-shear gallery increases by approximately 36.2%. Both the numerical results and microseismic data show that the anti-shear galleries have a good reinforcement effect.  相似文献   

20.
西南矿区山体崩塌成因机制分析及防治对策   总被引:1,自引:0,他引:1  
西南地区的矿区具有相似的地理、地质环境,通过四川芙蓉煤矿白岩崩塌的典型实例,对西南矿区山体崩塌的成灾环境进行调查研究,揭示了西南矿区山体崩塌的成因机制,并简要提出了对该煤矿开发与综合治理建议,指出了加强防治工作的紧迫性,强调开展系统工程防灾的重要性,并为该煤矿解决正常采掘接替及工作面的布置问题作出了科学的指导.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号