Numerical analysis of dislocations of the face slabs of the Zipingpu Concrete Faced Rockfill Dam during the Wenchuan earthquake

The Zipingpu Concrete Faced Rockfill Dam （CFRD） was obviously damaged during the Wenchuan earthquake in 2008. A wide range of dislocations occurred along the horizontal construction joints at EL. 845m, between the face slabs constructed in the second and third stages. The maximum displacement of the dislocations reached 17cm. In this study, the slab dislocations were investigated using finite element （FE） analysis. The method based on strain potential was applied to compute the permanent deformation of the Zipingpu Dam during the Wenchuan earthquake. The calculated magnitude of the slab dislocation showed good agreements with the field measurements. The dislocation mechanism was discussed. The results show that the dislocation of the concrete slab is a subsequent damage after the permanent deformation of the rockfill materials. The effects of the shear strength and the direction of the construction joints, the reservoir water level and the seismic waves were studied. The shear strength and the direction of the construction joints, reservoir water level and have a significant effect on the dislocation displacement. The dislocation can be effectively reduced by measures such as changing the direction of the construction joints or improving the shear strength at the horizontal joints.

Analysis on residual strain of Zipingpu Concrete Faced Rockfill Dam after Wenchuan earthquake

The Zipingpu Concrete Faced Rockfill Dam （CFRD） was subjected to significant local damage in the ＂5.12＂ Wenchuan earthquake. It is the first rockfill dam of more than one hundred meters high to encounter a strong earthquake anywhere in the world. Based on the finite element smoothing method, the residual strains at a typical cross-section and a downstream slope of the dam were obtained by processing the dam monitored displacement data. The position of and reason for the dam settlement and deformation ofrockfill dilatancy in the earthquake were analyzed according to the section residual strain. The results show that the maximum settlement ratio on the dam body approximately occurs at 2/3 of the dam height; dilatancy occurs from the dam crest to 25-30 m in the upstream and downstream slope; the immediate cause of the face slabs horizontal construction joint dislocation is excessive residual shear strain. Meanwhile, the position of and reason for the dam fissure in the earthquake were analyzed according to the dam slope residual strain.

紫坪铺水库现状水沙情势变化与减淤措施研究

水库泥沙淤积是造成有效库容减少、运行成本增加以及水库寿命缩短的重要影响因素,科学判别水库的淤积形势以及开展合理的排沙措施是解决水库淤积的有效途径。紫坪铺水库自汶川地震后,入库沙量呈增加趋势,对水库的安全运行及下游用水安全产生了极大威胁。研究表明:汶川地震前,岷江上游径流量呈减小趋势,地震后有少许恢复,但仍处于偏枯状态;地震后入库沙量明显增加,截至2020年,水库淤积总量为1.952亿m^(3),占总库容的17.55%,泥沙总体淤积在库区中部,坝前淤积相对较少;为应对水库淤积问题,提出减少水库淤积的措施、异重流排沙、人工清淤以及工程措施与非工程措施结合的“上库调沙,下库调水”的综合减淤方式,以期为紫坪铺水库健康长效运行提供决策建议。

Research on Seismicity and Source Parameters of Small Earthquakes in the Zipingpu Reservoir before the Wenchuan M_S 8. 0 Earthquake

Based on the digital seismic waveform data observed from regional and reservoir seismic networks,the seismicity and source parameters in the Zipingpu reservoir area from January 1,2000 to May 11,2008 before the Wenchuan MS8.0 earthquake are studied. The analysis shows a continuous activity of small earthquakes before the Wenchuan MS8. 0 earthquake. The level of seismic activity was from ML2.0 to ML3.0 in recent years. The impoundment of Zipingpu reservoir started in September 2005 and the obvious increment of seismic activities occurred in February 2008,but according to the analysis of the longer time series,the frequency and intensity of seismic activities do not exceed its range,which means it is still a fluctuation of regional seismic activities or tectonic activity. At the same time,we also studied the spatio-temporal distribution and the change of apparent stress difference in the source region before the great earthquake,and the results show that the apparent stress values of small earthquakes are generally higher than fitted values of apparent stress in the reservoir area in the nearly three months before the Wenchuan MS8.0 earthquake. It can be seen from the spatial distribution of apparent stress difference,that the epicenter of the earthquake is located at a low stress distribution area,and the relatively high apparent stress difference is at the east of the epicenter. Apparent stress increment occurred in local areas.

The Focal Mechanism and Characteristic of Stress Field in the Zipingpu Area before the M_S8.0 Wenchuan Earthquake

Based on seismic wave records of the Chengdu digital seismic network and Zipingpu reservoir digital seismic network from August 16,2004 to May 12,2008 when the Wenchuan MS8.0 earthquake occurred,the parameters of focal mechanisms of 486 earthquakes with magnitude larger than M1.6 in the Zipingpu reservoir area were calculated using amplitude ratio method,meanwhile the temporal-spatial variation characteristics of mechanisms and stress field were analyzed based on these parameters.Results show a low ratio of thrust earthquakes and an increased number of strike-slip earthquakes in the reservoir water area in the period from 2006 to 2008.While in the areas far from the reservoir waterfront,the thrust earthquakes took up a high proportion and the strike-slip ones did not increase.The direction of mean principal compressive stress field was deflected and disturbed differently in each area before the Wenchuan MS8.0 earthquake.

Distribution Characteristics of the Seismicity of Zipingpu Reservoir Region after the Wenchuan Earthquake

815 earthquakes recorded by 12 seismic stations of the Zipingpu reservoir seismic network in 2009 were relocated using the double difference algorithm to analyze the seismic activity of the Zipingpu reservoir.Relocation results show that the earthquakes are concentrated relatively in three zones.The distribution characteristics of focal depth are obviously different among different concentration zones.This means earthquakes in different concentration zones may have different causes.Compared to relocation of earthquakes taking place before the Wenchuan earthquake done by other researchers,the seismic concentration zones in the reservoir area shifted obviously after the Wenchuan earthquake.These variations are related to local stress adjustment in the reservoir area and may also be related to the diffusion depth and range of increased pore pressure caused by rock failure in the course of Wenchuan earthquake.

Using Ambient Noise to Study the Seismic Velocity Changes Caused by the Rise and Fall of the Water Level in the Zipingpu Reservoir Region

We study the feature of media changes beneath the Zipingpu reservoir and discuss the process of permeation with the water level rise and fall of the reservoir from January 2005 to January 2008 from ambient noise cross correlation by using continuous seismic data recorded by the stations of Zipingpu seismic network and YZP station. A moving-window cross-spectrum technique has been used to calculate the relative seismic velocity changes between station pairs. Results revealed an obvious relationship between relative seismic velocity, and the water level changes with a time delay that may be caused by permeation during three main impoundments and two large scale disemboguements. Impoundment generates a fast and large impact on the superficial layer, and the changes of seismic velocity is the result of increased pressure and permeation during the impoundment. At the first impoundment, the main effect factor is pressure. During the next two process of impoundment, permeation becomes the main effect factor, affecting the fault at a depth of about 8kin.

考虑异重流的紫坪铺水库一维水沙数值模拟研究

水库异重流是河道挟沙水流潜入水库清水之下形成的一种特殊水沙运动现象,对水库减淤排沙具有重要意义。针对紫坪铺水库近年来沙量剧增、水库淤积严重的问题,耦合水动力学泥沙基本方程与异重流运动方程,构建了紫坪铺水库一维水沙数学模型并对水库水沙运动过程进行模拟研究。研究结果表明,模型可以对进出库流量、出库含沙量、深泓线以及库区淤积分布进行模拟,且具有较好的精度。该模型可为紫坪铺水库未来不同水沙情景模拟以及预测提供理论依据,为西南地区多沙水库水沙运动过程研究以及排沙调度提供技术支撑。

水库面对可能最大洪水时的应急调度优化研究

近年来极端气候事件呈现多发强发态势,由此引发的可能最大洪水等极端水文事件对水库安全产生了严重的威胁,而水库常规防洪调度规程在面对其威胁时存在失效隐患,因此对水库常规调度规程进行优化,形成针对极端情况的应急调度显得尤为重要。针对此问题,以位于岷江上游的不完全年调节水库紫坪铺水库为研究对象,基于HECRAS建立了库区河段的一维水动力模型,以确保水库安全的同时最大限度减轻洪水对下游的影响为目标,遵循“以空间换时间”的调度思路,采用“提前预泄结合加大泄量”的优化原则,开展了水库在面对可能最大洪水时调度方式及调度时机的寻优研究。研究发现,在面对总入库流量为水库防洪库容8倍的可能最大洪水时,通过调整水库泄洪方式的组合模式,结合对调度起止时间的科学寻优,实现了水库防洪库容随洪水历程的合理动态分配,为水库完成泄洪任务赢得了更多时间。优化后的应急调度方式有效规避了常规调度失效的隐患,度汛期间坝前水位峰值相较于原调度方式降低了18.4 m,确保库区水位始终处于安全范围;库区水面线变化控制在14.7 m以内,相较原调度降低了55.6%,库区整体水位变化更加稳定;并且优化方案下削峰率达74%,最大程度减轻了下游所受洪涝灾害的威胁。在此基础上,通过进一步对水库防洪潜力的定义分析,揭示了两种调度方式下水库度汛效果存在明显差异的原因,为水库面对极端洪水开展应急调度提供了新思路和新参考。

利用抽水蓄能实现紫坪铺水库反调节的思考

建设紫坪铺反调节工程是保护都江古堰运行安全和永续利用的必要措施,但原规划的杨柳湖反调节工程已经不能实施,另辟蹊径寻求紫坪铺水电运行的调节方式值得研究。笔者提出在紫坪铺水库库区内修建抽水蓄能电站以解决紫坪铺水库对都江堰供水的反调节问题,即由库内抽蓄电站承担电网调峰,改变紫坪铺水库直接参与调峰的现状,从而实现库水均匀下泄,满足都江堰水利工程引水的平稳与安全。

紫坪铺水库及邻区的微震检测与定位

首先对四川省地震局提供的1017次地震进行重定位,并将重定位后的578次高信噪比地震作为模板,利用基于图像处理器加速的匹配定位技术(GPU-M&L)对紫坪铺水库地震台网7个台站2005—2008年记录的连续波形数据进行扫描;然后利用基于深度学习算法的去噪技术(DeepDenoiser)设计出的卷积神经网络模型来进一步验证这些新检测到的地震事件;最后利用双差定位法对检测到的地震事件进行精定位。最终识别到的地震事件多达1万6836个,约为四川省地震局目录事件的13倍,地震目录的完备震级由M_(L)1.4降为M_(L)−0.1。定位结果显示,研究区的地震事件呈北东向线性分布,优势震源深度指示区域地壳内的滑脱层位置,结合b值和震源深度分析结果推测,研究区蓄水后的地震主要是构造应力积累导致的天然地震活动,并伴随水库触发地震混杂发生。

紫坪铺水利枢纽引水发电洞进水口边坡锚索预应力损失分析

四川岷江紫坪铺水利枢纽工程引水发电洞进水口边坡布置了大量预应力锚索进行加固,并安装了13台锚索测力计进行监测。本文在对锚索测力计监测资料整理分析的基础上,重点分析了锚索预应力随时间变化的关系、预应力损失情况及预应力损失的原因,对锚索预应力损失的控制有重要的借鉴意义。

利用三维孔隙弹性模型探讨紫坪铺水库对汶川地震的影响

本文基于三维孔隙弹性理论,建立了紫坪铺水库及周边地区的有限元模型.根据紫坪铺水库开始蓄水到汶川地震发震时刻的水位变化情况,计算了整个区域的孔隙压力和库仑应力.详细讨论了断层及周围地层的弹性模量和扩散系数对计算结果的影响.计算结果表明:从弹性角度看,断层的弹性模量对汶川地震震源处的库仑应力影响很小;震源处的库仑应力随着断层和周围地层的扩散系数增大而增大.当给定弹性模量和扩散系数代表性值的时候,计算结果表明在汶川地震发震时刻,震源处的库仑应力变化量为+1kPa左右,这表明紫坪铺水库使得汶川地震发震断层更加危险.是否这个量级的库仑应力就能够触发汶川地震还需要进一步探讨.通过分析库区周边小震的分布,发现小震分布区域均是库仑应力增加的地区,因此紫坪铺水库周边的小震应该与紫坪铺水库蓄水有直接关系.

紫坪铺水库库区地震精定位研究及分析

利用双差定位法,对紫坪铺水库台网8个地震台站记录到的2004年8月16日至2008年5月10日的1569个小震进行重新定位。结果显示,重新定位后的小震主要集中分布在龙门山推覆构造带的中央北川—映秀断裂、前山灌县-江油断裂和后山汶川—茂汶断裂上,其中大部分地震位于北川—映秀断裂并收敛于紫坪铺水库的两端,走向NE向;震源深度集中在5～15km范围内,平均深度为7.8 km,15～30 km也有少量地震发生。水库区域小震活动频度与水库水位存在一定的相关性。精定位后,到时残差的均方根平均值为0.048 s,震源位置的估算误差在水平方向上平均为0.63 km,在垂直方向上平均为0.51 km。文中还讨论了紫坪铺水库区震源分布和地质构造的关系。

紫坪铺水库区域地壳Q_s成像及其与渗透关系研究

利用衰减结构层析成像方法尝试对紫坪铺水库区域地壳Qs进行成像,获得该区浅层地壳静态及蓄水前、后的Qs变化特征,结合实验研究成果、岩体岩性、断裂构造、水文地质条件探讨库水的渗透作用及其对地壳介质的影响,对研究区内地震活动类型及发震成因的介质物性变化进行了讨论.研究结果表明:紫坪铺水库区域地壳Qs横向不均匀变化显著,库区周边近似存在低Qs值环形区域,主要包括水库东北、东南、西南、西北及库区中段五个区域.其中,水库东北、库区中段、西南低Qs区域与库水渗透关系密切,初步认为库水可能沿着通济场断裂中段和两端的岩石破碎带及节理、裂隙发育地区向地下渗透,使岩石孔隙中充满流体,内摩擦增大,地震波大大衰减,从而导致Qs值大幅下降.同时,在西南区诱发了水库小震群,在东北区和东南区诱发了部分水库小震群.另外,紫坪铺水库区域东北、东南、西南三个小震群基本位于高Qs值(低衰减)和低Qs值(高衰减)过渡区域,可能由于低Qs区地震波衰减大,不易积累能量,而高、低Qs值的过渡区域,介质介于"软"、"硬"之间,有可能积累应变能,孕育地震.当高、低Qs过渡区域岩石裂纹饱含水或部分含水后,水对裂纹边界起潮湿和润滑作用,降低了发震断层的抗剪强度,使滑动容易产生,从而诱发地震.

紫坪铺水库区小地震震源机制研究

用紫坪铺水库专用台网的地震记录测定紫坪铺水库区262次小震震源机制参数,结果表明:节面I的优势方向与断裂走向展布一致性很好;库区地震断层有逆断层、正断层、左旋和右旋走滑断层,走滑断层占45%;库区断层66%陡峻,35%几近直立;受水库蓄水的影响,2006年7月1日后以走滑断层活动方式明显增多,水库地震群时段走滑断层活动方式表现突出。

导流洞堵头常规设计方法的修正

常规的水工导流洞堵头设计中一般都忽略堵头变形产生的摩擦阻力,使得堵头长度过分偏于保守。根据堵头的工作机理,首次推导了堵头的变形压力,以及由此增加的阻滑力的表达式,并结合紫坪铺工程实例,分析了该因素对堵头整体稳定性的影响。计算结果表明,堵头的变形压力可以有效地提高堵头的抗滑稳定安全系数和减少堵头的设计长度,从而缩短工期,节约投资,具有良好的工程应用价值。

探讨紫坪铺水库在汶川地震发生中的作用

汶川MS8.0级地震位于紫坪铺水库库尾附近。2002年紫坪铺水库开始截流,2005年10月正式开始蓄水后,库区先后发生不少小震群。2006—2008年迅速增多的水磨震群与主震相距不足5km。因此,紫坪铺水库蓄水在汶川地震发生中的作用成为一个被广泛关注的热点问题,从断层的库仑应力变化出发有过很多讨论。文中以汶川MS8.0级地震前的紫坪铺水库地震台网数据为基础,通过分析龙门山断裂带以及库区小震的时空演化,研究水库附近流体压力扩散过程,得到以下认识:(1)紫坪铺水库所在区域存在一系列北东向展布的断裂,水库位于碳酸盐岩地层上,存在渗漏的地质背景。伴随水位波动升高,回水逐渐向西南淹没,地震分布范围也逐渐由大坝向南西扩展,二者关系密切。根据地震随时间的分布,分析了水压力的扩散过程,拟合得到水压力的宏观扩散系数为0.7m2/s。该扩散系数较好地勾画了紫坪铺水库蓄水和地震活动过程。扩散过程既与河流纵断面形态关系密切,也与地下流体孔隙压力扩散、水位变化有关。(2)紫坪铺水库蓄水前龙门山断裂带汶川段已处于高应力状态,库区正好位于汶川段西南区的闭锁部位。蓄水后龙门山断裂带有过三次地震增强和地震活动范围沿断裂扩展的过程,均发生在水位升高后。已有实验结果表明,在亚失稳应力状态下断层在失稳前的活动存在协同化过程。其作用是降低断层上弱部位的强度和扩大弱部位的总长度以提高断层协同化程度,从而增加断层强部位的应力。研究认为,3次高水位后地震活动的增强正反映了在强区域构造应力背景下库水渗透到部分闭锁断层段并使之弱化引起的连锁反应。汶川地震发生在高区域应力和水体的共同作用下,多次高水位起了弱化断层闭锁段的作用,使断层上协同化程度达到临界水平,在强部位的应力作用下造成了较长断层段的快速失稳错动。此项研究为进一步分析紫坪铺水库蓄水在汶川地震发生中的作用提供了新的事实和论据。

紫坪铺水库与汶川地震关系的讨论

利用紫坪铺水库专用地震台站和加密地震台站资料,使用双差法完成了震前930次地震、汶川8级主震和5789次余震的重新定位,探讨了紫坪铺水库与汶川地震之间的关系,获得了有利于证明它们之间密切关联的事实:1)紫坪铺水库2005年蓄水之后出现了水磨、深溪沟和都江堰震群,地震应变能释放增加了200%,与库水位变化密切相关,在汶川地震前呈现出加速释放的现象;2)野外调查表明存在1条贯穿紫坪铺水库库区、走向NE的同震地表破裂带,与中滩铺断层位置一致;3)余震分布以中滩铺断层为界,西北上盘多,东南下盘少;4)利用P波初始到时重新确定出的汶川主震发震时刻为27分59.5秒,初始破裂深度在6～9km左右,直接位于水磨震群之下;5)汶川主震与发生在2008年4月5日水磨震群中的1次小震的各个台站到时差相同。

汶川8.0级地震前紫坪铺水库小震活动及震源参数研究

利用区域和水库地震台网记录的数字地震波资料,研究了汶川8.0级地震前的2000年1月1日-2008年5月11日紫坪铺水库区的地震活动及震源参数。结果表明：汶川8.0级地震前该区域小震活动持续,地震活动水平为ML2-3,自2005年9月紫坪铺水库蓄水以来,特别是2008年2月地震活动明显增加,但从长期的序列来看,地震活动频次和强度仍在区域地震活动的正常起伏范围。汶川8.0级地震发生前近3个月内,中小地震的视应力差值Δσapp普遍大于0,计算得到的视应力总大于其拟合值。汶川8.0级地震震中位于低应力区,而相对较高的视应力差值分布在震中以东地区,局部出现视应力增加的现象。