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1.
Shan  Yibo  Chen  Shengshui  Zhong  Qiming  Mei  Shengyao  Yang  Meng 《Landslides》2022,19(6):1491-1518

The existing empirical models do not consider the influence of material composition of landslide deposits on the peak breach flow due to the uncertainty in the material composition and the randomness of its distribution. In this study, based on the statistical analyses and case comparison, the factors influencing the peak breach flow were comprehensively investigated. The highlight is the material composition-based classification of landslide deposits of 86 landslide cases with detailed grain-size distribution information. In order to consider the geometric morphology of landslide dams and the potential energy of dammed lakes, as well as the material composition of landslide deposits in an empirical model, a multiple regression method was applied on a database, which comprises of 44 documented landslide dam breach cases. A new empirical model for predicting the peak breach flow of landslide dams was developed. Furthermore, for the same 44 documented landslide dam failures, the predicted peak breach flow obtained by using the existing empirical models for embankment and landslide dams and that obtained by using the newly developed model were compared. The comparison of the root mean square error (Erms) and the multiple coefficient of determination (R2) for each empirical model verifies the accuracy and rationality of the new empirical model. Furthermore, for fair validation, several landslide dam breach cases that occurred in recent years in China and have reliable measured data were also used in another comparison. The results show that the new empirical model can reasonably predict the peak breach flow, and exhibits the best performance among all the existing empirical models for embankment and landslide dam breaching.

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2.
A strong earthquake of magnitude 8 in Richter scale, occurred in Sichuan Province, China on 12 May 2008, triggered about 257 landslide dams. The erodibility of fresh landslide deposits plays an important role in evaluating the initiation and development of breaching of such landslide dams. In this research, field jet index tests were conducted shortly after the earthquake at 27 locations on the Hongshihe landslide dam and the Libaisi landslide dam. The purpose of these tests was to investigate the erodibility of freshly deposited landslide soils. The landslide deposits are broadly graded. The bulk density increases and the coefficient of erodibility decreases with the depth of deposition. The erodibility of the fresh landslide deposits falls into a moderately resistant category and the fresh deposits are much more erodible than the native geomaterials before the earthquake. The main factors that control soil erodibility are found to be grain-size distribution, void ratio, fines content, and plasticity index. Particularly, the coefficient of erodibility decreases exponentially with the degree of compaction. Two empirical equations are developed for estimating the coefficient of erodibility and critical erosive shear stress of the freshly deposited landslide soils based on their basic soil properties.  相似文献   

3.
天然土石坝稳定性初步研究   总被引:13,自引:0,他引:13  
滑坡堵塞江河形成的天然土石坝是自然作用的产物,不同于人工土石坝,天然土石坝形成后有些存在几十年,几百年,有些形成后不久就溃决,这与坝体本身的性质和河水入流量有关,依据野外实测资料,证了土石坝的稳定性的主要是同土石坝的物质组成,几何形状和堰塞湖入流量等因素决定的,这一研究为天然土石坝的稳定性预测奠定了基础。  相似文献   

4.
Predictive displacement-based methods provide a useful index of the seismic performance of earth dams and embankments and can be used in preliminary assessments of these structures. In practice, simplified Newmark-type sliding block methods are commonly used for this purpose. Using a database of 122 previously published case histories of permanent deformations of earth dams and embankments, the performance of six simplified sliding block models was examined. The results show that all six simplified methods underpredict seismic displacement for many of the embankment and earth dam cases that were examined, sometimes by a significant amount. An empirical correlation was developed by performing linear multiple regression analysis utilizing multiple slope and ground motion input parameters. This approach is believed to more properly reflect strong ground motion characteristics than the use of a single ground motion parameter such as the peak ground acceleration, the approach that has been previously employed in other correlations of this type. After exploring numerous functional forms, the final resulting seismic displacement correlation that was proposed was determined to be a function of the critical acceleration, the critical acceleration ratio, the slope height, the peak ground acceleration, the peak ground velocity, the spectral acceleration, and the predominant period of earthquake shaking. The proposed empirical equation yields better correlation with the case history database than does other existing empirical correlations or simplified sliding block models.  相似文献   

5.
堰塞坝溃坝模型实验研究综述   总被引:1,自引:0,他引:1  
堰塞坝是天然形成的坝体,结构比较松散、稳定性差、渗透作用强,发生溃决危险性大、概率高、突发性强,而且破坏可能性高及产生的洪水威胁人们的生命和财产安全,因此需要系统、全面的研究。作者从单坝溃坝、级联溃坝及堰塞坝处置的溃坝试验进行详细的回顾,总结及分析了国内外学者在堰塞坝溃坝模型实验取得的成果及局限性,进一步分析了单坝溃决的颗粒级配、密实度、含水率、沟床坡度等因素,最后讨论了溃坝因素与溃决模式、溃决特征、溃决流量、溃口演化的关系。基于模型实验相似理论及模型比尺、实验测试手段、堰塞坝处置三个方面,提出了今后的研究重点。  相似文献   

6.
堰塞坝是由于崩塌、滑坡、泥石流等形成的天然坝体,不同于人工土石坝,堰塞坝坝体结构松散,颗粒级配不均匀,在较高水头作用下坝体可能发生渗透破坏而导致溃坝,严重威胁下游人民群众的生命及财产安全。由于堰塞坝存在较大粒径颗粒,常规的渗透试验装置难以满足要求,本文研制了直径为60cm的大直径渗透试验仪,进行了不同堰塞坝级配材料的渗透破坏试验,并探讨了堰塞坝体材料渗透特性的主要影响因素。研究发现:(1)堰塞坝材料的渗透破坏形式取决于材料级配,粗颗粒含量较多时为管涌破坏,细颗粒含量较多或粒径缺失时为流土破坏;(2)堰塞坝渗透系数随干密度的增大而减小,主要取决于细料填充粗料孔隙的程度,单独使用不均匀系数或曲率系数不适用于评价渗透系数的变化;(3)基于试验数据提出了用于堰塞坝渗流破坏形式的判别公式,并推导出堰塞坝管涌破坏的临界水力坡降计算公式。  相似文献   

7.
红石河堰塞湖漫顶溃坝风险评估   总被引:6,自引:1,他引:5  
四川省青川县红石河堰塞湖是2008年5月12日汶川大地震形成的34座大型堰塞湖之一,是由东河口滑坡堵塞红石河形成的。该堰塞体高度约50 m、宽度约250 m、顺河向长度约500 m、形成的最大库容约400万m3。本文作者对红石河堰塞体做了较详尽的现场试验,包括土的冲蚀试验、土的基本物性试验等。基于现场试验数据,对土的冲蚀性和漫顶溃坝风险做了详细的分析。结果显示,从土的抗冲蚀性角度考虑,只要有水溢出就会有土体被冲蚀,这说明红石河堰塞体的漫顶溃决可能性较高。本文还提出经验公式来预测红石河堰塞体漫顶的溃决时间,大约为4.5d,如果考虑到大石块对抗冲蚀稳定性的有利影响,这一数值会增大。此外,还研究了溃决深度随时间的变化规律。  相似文献   

8.
Global warming in high mountain areas has led to visible environmental changes as glacial retreat, formation and evolution of moraine dammed lakes, slope instability, and major mass movements. Landslide dams and moraine dams are rather common in the Cordillera Blanca Mountains Range, Peru, and have caused large damages and fatalities over time. The environmental changes are influencing the rivers’ and dams’ equilibrium, and the potential induced consequences, like catastrophic debris flows or outburst floods resulting from dam failures, can be major hazards in the region. The studies of past landslide dam cases are essential in forecasting induced risks, and specific works on this topic were not developed in the study region. Reflecting this research gap, a database of 51 cases and an evolution study of landslide dams in the Cordillera Blanca Mountains is presented. The main morphometric parameters and information of the landslide, the dam body, the valley, and the lake, if any, have been determined through direct and indirect survey techniques. Low variability in some of the main morphometric parameter distributions (valley width and landslide volume) has been shown, most likely due to an environmental control connected to the regional tectonic and glacial history. In order to analyze present and future landslide dam evolution, a morphological analysis was carried out using two recently developed geomorphological indexes employed on the Italian territory. The results of the Cordillera Blanca analysis have been compared with a large Italian landslide dam inventory, highlighting as much the differences as the similarities between the two datasets. The long-term geomorphological evolution changes are evaluated. Many of the stable dams are in disequilibrium with their surrounding environment and their classification result is of “uncertain determination.”  相似文献   

9.
This paper deals with prediction of collapse settlements due to saturation of rockfill, mainly in embankment dams. After some brief considerations about the physical basis and the practical importance of the phenomenon, a research program on this subject developed in LNEC is presented. Using non linear elastic models (and adequate loading and unloading-reloading criteria) whose parameters are quantified by laboratory tests and data from a field test, it is concluded that is possible and reliable to predict collapse settlements due to saturation of rockfill embankments. As a result of a parametric study the relative importance of the different parameters in the model is analyzed.  相似文献   

10.
A practical methodology has been developed for predicting flows generated by dam failures or malfunctions in a complex or a series of dams. A twofold approach is followed. First, the waves induced in the downstream reservoirs are computed, as well as hydrodynamic impacts induced on downstream dams and dikes are estimated. Second, the flood wave propagation and the inundation process are simulated in the downstream valley, accounting for possible dam collapse or breaching in cascade. Two complementary flow models are combined: a two-dimensional fully dynamic model and a simplified lumped model. At each stage, the methodology provides guidelines to select the most appropriate model for efficiently computing the induced flows. Both models handle parametric modeling of gradual dam breaching. The procedure also incorporates prediction of breach formation time and final width, as well as sensitivity analysis to compensate for the high uncertainties remaining in the estimation of breach parameters. The applicability of the modeling procedure is demonstrated for a case study involving a 70-m high-gravity concrete dam located upstream of four other dams.  相似文献   

11.
近年来,频发的地质构造活动和极端气候灾害诱发了大量堰塞坝,严重威胁上下游群众的生命财产安全。开挖泄流槽是最常用降低堰塞坝溃决风险的措施,由于时间非常急迫、交通极度瘫痪,其开挖量非常有限,因此如何利用有限的开挖量将溃坝风险降低至最小是亟待解决的问题。本文基于水土耦合冲刷机理,提出了考虑不同泄流槽方案的堰塞坝溃决机理分析方法,并应用于唐家山堰塞坝。该方法根据水力学参数和坝体抗冲刷性参数动态计算瞬时坝体冲刷率,进而分析泄流槽对溃决全过程的影响,从而自动获取最优的泄流槽设计方案。将此方法应用于唐家山堰塞坝案例发现:唐家山堰塞坝泄流槽最优设计时溃坝洪峰流量为1700m3·s-1,小于实际峰值流量6500m3·s-1,主要是因为增大泄流槽的纵坡率,显著增强溃坝前的冲刷并形成双洪峰,从而有效降低了溃决峰值流量。由于复合槽相对较小的水力半径限制了溃坝前的冲刷,使得临溃时水位较高,因此溃坝峰值流量比单槽大,溃坝风险降低效果不如单槽。  相似文献   

12.
Risk assessment development considering the failure of landslide dams often requires the estimation of peak outflow through the breach. The empirical equations based on data from case studies tend to be the first direct approach. This paper conducted an uncertainty analysis when these empirical relations were utilized to predict the peak outflow of a breached landslide dam. The results suggest that the relations derived from manmade dams or embankments typically overestimate the peak outflow about 1/5 to 3/4 of an order of magnitude; and the relations derived from the database of landslide dams have much smaller mean prediction errors and also exhibit broad uncertainty bands. Application of the uncertainly analysis was illustrated by the Tangjiashan landslide dammed lake, formed during 2008 Wenchuan earthquake. In addition, the predicted results from Eq. 1 deduced herein were considered to be the reliable estimate of peak outflow through the breach of landslide dam.  相似文献   

13.
In recent years, many high rockfill dams have been constructed in China for the purpose of hydropower generation. One of the critical aspects of rockfill dam design is the analysis of slope stability. Triaxial compression tests show that the failure envelopes of rockfills are curved and that nonlinear shear strength criteria yield better predictions of the shear strengths of rockfills than the Mohr–Coulomb criterion. Because the determination of shear strength parameters involves uncertainties, a reliability-based methodology was developed for use in evaluating the failure probability of rockfill dam slopes by integrating Bishop’s simplified method, Duncan’s nonlinear strength criterion and the first-order second-moment reliability method presented in this paper. A computer program, SCU-SLIDE, was developed and its outputs validated by comparison with Monte Carlo simulation results. The approach developed was used to study the stability of the Shuang Jiang Kou rockfill embankment dam, which when completed will be the tallest dam in the world. The results of the stability analysis are discussed and conclusions are presented in this paper.  相似文献   

14.
针对缺乏地形条件和工程处置措施对堰塞坝溃决过程影响研究的现状,采用4种河床坡度(0°、1°、2°、3°)和3种泄流槽横断面型式(三角形、梯形、复合型),开展了堰塞坝溃决的模型试验。通过分析堰塞坝的溃决流量、溃决历时、溃口发展和坝体纵截面演变过程,研究了不同河床坡度和泄流槽横断面对堰塞坝溃决过程的影响规律。试验结果表明:(1)堰塞坝溃决过程可分为3个阶段。阶段Ⅰ:溃口形成阶段,溃决流量较小;阶段Ⅱ:溃口发展阶段,水流下蚀及侧蚀强烈,溃决流量到达峰值;阶段Ⅲ:衰减-平衡阶段,粗化层形成,溃口停止发展。(2)河床坡度增加意味着下游坝坡、坝顶及泄流槽的坡度增加,导致水流侵蚀能力增强,溃口下切迅猛,因此在0°~3°范围内河床坡度越大,峰值流量越大,峰现时间越早,溃决流量过程曲线越趋于“高瘦型”,且残留坝高越小。(3)泄流槽横断面型式不同导致其槽深、槽宽和侧坡坡度不同,进而影响溃口发展和溃决流量。三角形槽的水土作用面积小,溃口下切及展宽速率最高,峰值流量最大,峰现时间最早;梯形槽的槽底高程最高,水土作用面积最大,溃口下切速率最低,峰现时间最晚;而复合槽介于前两者之间。试验成果将为堰塞坝应急抢险和工...  相似文献   

15.
High core rockfill dams exhibit complex deformation mechanisms because of complicated geological conditions, many material partitions and severe weather conditions. When realistic parameters cannot be obtained through laboratory tests or engineering analogies because of effects of size or time, back analysis is necessary to predict deformation characteristics. This paper proposes a method of deformation back analysis based on the response surface method and genetic optimization theory. The parameters of the creep and Duncan–Chang models for the Pubugou gravelly soil core rockfill dam are sequentially calculated. Back analysis performed using this method efficiently yields more precise results than those obtained from laboratory-determined parameters.  相似文献   

16.
土体抗剪强度指标的概率分布类型研究   总被引:25,自引:5,他引:20  
土的抗剪强度指标概率分布的类型,影响着风险评价和可靠度分析的结果。通过收集整理的多个水利工程中丰富的长序列的抗剪强度试验资料,在此基础上利用K-S法对土体抗剪强度指标的概率分布类型进行了统计分析,发现一般情况下抗剪强度指标均可以接受正态分布和对数正态分布,而选择对数正态分布能够避免出现物理量为负的现象,在许多情况下这样处理更为合理、简便。  相似文献   

17.
改进的遗传算法在堆石体参数反演中的应用   总被引:1,自引:0,他引:1  
张社荣  何辉 《岩土力学》2005,26(2):182-186
在研究堆石坝问题中,堆石体参数的合理估计非常重要,根据工程实测值反演堆石体参数不失为一种有效估计参数的新思路。在传统遗传算法操作过程中,引入模拟退火的Metropolis接受准则,并结合系统识别的基本原理改进了遗传算法。将改进的新算法应用于堆石坝主要堆石料的参数反演,结果显示其误差很小、收敛速度快、精度高的优越性,克服了传统的梯度优化方法和单纯形法所具有的搜索速度随反演参数增多呈级数减慢、容易陷入局部极值点和误差传递导致不收敛等缺点,值得在本领域参数优化中推广。  相似文献   

18.
基于搜集的国内多座土石坝堆石料的动力试验成果,研究了堆石料的振动残余变形特性。在整理试验数据过程中,尝试对沈珠江模型进行改进,改进模型充分考虑固结比对堆石料振动残余变形特性的影响,并能更好地拟合试验数据。通过对理想面板堆石坝进行地震动残余变形计算,对比分析了与沈珠江模型、孔宪京改进模型以及凌华改进模型的异同,阐述了本次改进模型的合理性。此外,在统计大量试验数据的基础上,给出了 - 与 - 关系曲线的平均线及上、下包络线,采用该统计曲线对理想面板堆石坝进行了地震残余变形敏感性分析。计算结果表明:参数c4、c5对坝体残余变形影响较大,参数c1、c2影响程度较小;选取均值曲线参数可应用于缺乏动力试验的中小型土石坝抗震设计。  相似文献   

19.
An Ms 6.5 earthquake shocked the Ludian County, Yunnan Province, China, on 3 August 2014 and triggered the Hongshiyan landslide dam. The dam, with a height of 83 m and a lake capacity of 260?×?106 m3, threatened more than 10,000 people. A unique feature of this landslide dam was that it formed between a man-made dam and a hydropower plant. An existing drainage tunnel connecting the lake and the hydropower plant became a natural drainage conduit for the landslide dam, which played an important role in the mitigation of the landslide dam risks. This paper reports a quantitative risk assessment for the Hongshiyan landslide dam considering both engineering and non-engineering risk mitigation measures. The risk assessment is divided into three stages according to the implementation of two engineering measures: construction of a diversion channel and excavation of a branch drainage tunnel. The dam breaching hydrographs, flood zones, population at risk, and likely fatalities in each of the three stages are analysed. The optimum evacuation strategy in each stage is also studied based on the principle of minimum total consequence. It is found that the diversion channel decreases the dam breaching peak discharge and the associated risks significantly. The branch drainage tunnel prevent the landslide dam from overtopping failure in non-flooded period; however, the landslide dam may fail by overtopping in a future flood if the inflow rate is larger than the outflow rate through the drainage tunnels, resulting in serious losses of lives and properties. The dam breaching risks in all the three stages could be largely reduced by the optimal evacuation decision, which shows that timely evacuation is vital to save life and properties. The study provides a scientific basis for decision making in landslide dam risk management.  相似文献   

20.
Shortly before midnight on Wednesday, July 27, 2011, the landslide dam forming a lake on the Matthieu River, Dominica, West Indies rapidly breached. The complete draining of the lake caused major flooding along the lower Layou River Valley. No fatalities or injuries resulted despite significant property and infrastructure damage. Government estimates place the cost for immediate cleanup and long-term repairs between ECD$9 million and ECD$18 million. The lake created by the landslide dam was unusual for having persisted nearly 14 ?years. Formation of the Matthieu landslide dam was associated with formation and breaching of two smaller landslide dams on the Layou River in 1997. Available evidence is consistent with breaching due to landsliding on the face of the landslide dam. Landslides removed sufficient material to permit the lake to flow over the dam and erode the dam to about the level of the pre-existing channel of the Matthieu River.  相似文献   

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