• <tr id="yyy80"></tr>
  • <sup id="yyy80"></sup>
  • <tfoot id="yyy80"><noscript id="yyy80"></noscript></tfoot>
  • 99热精品在线国产_美女午夜性视频免费_国产精品国产高清国产av_av欧美777_自拍偷自拍亚洲精品老妇_亚洲熟女精品中文字幕_www日本黄色视频网_国产精品野战在线观看 ?

    Monitoring result analyses of high slope of f ve-step ship lock in the Three Gorges Project

    2015-02-08 09:02:58QixiangFanHongbingZhuJunGeng

    Qixiang Fan,Hongbing Zhu,Jun Geng

    China Three Gorges Corporation,Beijing,100038,China

    Monitoring result analyses of high slope of f ve-step ship lock in the Three Gorges Project

    Qixiang Fan,Hongbing Zhu*,Jun Geng

    China Three Gorges Corporation,Beijing,100038,China

    A R T I C L E I N F O

    Article history:

    Received 19 January 2015

    Received in revised form

    2 February 2015

    Accepted 3 February 2015

    Available online 16 March 2015

    Three Gorges Project(TGP)

    Five-step ship lock

    Slope

    Monitoring analysis

    The construction of the double-lane f ve-step ship lock of the Three Gorges Project(TGP)was commenced in 1994,the excavation of the ship lock was completed by the end of 1999,and the ship lock was put in operation in June 2003.The side slopes of the ship lock are characterized by great height (170 m),steepness(70 m in height of upright slope),and great length(over 7000 m in total length).In association with the ship lock,the surrounding rocks in slope have a high potential to deform,with which the magnitude of deformation is restricted.Monitoring results show that the deformation of the f ve-step ship lock high slopes of the TGP primarily occurred in excavation period,and deformation tended to be stable and convergent during operation period,suggesting the allowable ranges of deformation.At present,the slopes and lock chambers are stable,and the ship lock works well under normal operation condition,enabling the social and economic bene f ts of the TGP.

    ?2015 Institute of Rock and Soil Mechanics,Chinese Academy of Sciences.Production and hosting by Elsevier B.V.All rights reserved.

    1.Introduction

    As one of the three most important structures of the Three Gorges Project(TGP),the ship lock is constructed by deep cutting and excavation in granite at the north of Tanziling on the left bank. The ship lock of the TGP consists of upstream and downstream approach channels,main lock chamber section,water conveyance system,and mountain drainage system.The total length of the ship lock is 6442 m,and the main section of the ship lock(chamber section)is 1621 m long.The high slopes are critical issues concerning the safe operation of the TGP.The maximum height of these slopes is 170 m,and the slopes higher than 120 m account for 460 m in length.Central rock piers with width of 54-57 m are placed in the double-lane lock chambers.Therefore,a bilateral doublegrooved slope is formed in the section of the main structure (Zhang,2001).The high slopes of the permanent ship lock are formed by deep cutting in the mountain side characterized by great height,complex topography,wide-spread range,complete stress relief,exhibiting marked unloading and heterogeneity characteristics.Thus the deformation and slope stability issues raise concerns for these slopes.As for the slopes of the permanent ship lock, the global and local stability problems of these slopes must be well addressed and the slopes deformation of these should be strictly controlled in order to satisfy normal operation of the miter gate of the ship lock(Fan,2004;Fan et al.,2011).The typical section and photo of the lock chamber of the double-lane f ve-step ship lock is shown in Figs.1 and 2,respectively.

    The f ve-step ship lock high slope ofthe TGP is a challenging issue not only in engineering geological investigation,mechanical properties and stability analysis of rock mass,and safety monitoring,but also in theories and methods for design of high slope,as well as construction safety.For such a large-scale project,no knowledge or practicalexperience is available.To solve the key issues encountered during construction,the following measures are taken:

    (1)Reasonable construction procedures are proposed to harmonize the relations between surface deformation and underground engineering in association with deep excavation and anchoring support.

    (2)The one-step complete excavation method of upright slope meets the technical requirements of the excavation.

    (3)Using the integrated control blasting technology,the impact of groove excavation blasting is kept in the allowable range of design,satisfying the requirements of engineering rock quality and construction progress.

    (4)The fore shaft support technology is utilized to control the deformation and collapse of rocks at the top of upright slopes for the purpose of slope stability and construction safety during construction period(and excavation period).

    (5)The major indexes for estimating the stability of side wall rocks are determined to deal with the relation between the curing time of concrete lining and controlled blasting.

    Fig.1.Typical pro f le of the high slope of the double-lane f ve-step ship lock of the TGP.

    These procedures are carefully proposed based on long-term scienti f c research.During design and construction stages of the TGP,the construction procedures and methods were adjusted and optimized continuously by f eld experimental investigation,accumulated experience during construction practices,and the integrated application of multi-discipline methods including engineering geological survey,rock mechanics test,numerical simulation,controlled blasting of engineering excavation,anchoring, and back analysis of the monitoring data.The design and construction techniques are considered to be ground-breaking in termsof large slope excavation gradient,novel geological survey method and technology,evaluation theory and method for rock mechanics property and seepage characteristics.The safety monitoring and feedback method,in terms of the dynamic design concept and method of super-high slope associated with other methods,is applicable to deep excavation of high rock slope.By the end of 1999, a high and steep slope with complex structure was completed after excavation,and the rock stability of the high slope was effectively controlled after anchoring measures used,indicating that the ship lock excavation of the TGP was successful.

    Fig.2.Photo of the high slope of the double-lane f ve-step ship lock of the TGP.

    In this paper,the deformations of the high slope of the TGP ship lock recorded during construction and operation periods were analyzed.It is shown that the deformation of the slope occurred mainly in construction period,and was kept stable in operation period.The deformations of side wall and the stresses of highstrength rock bolts are well controlled.

    2.Analysis of monitored deformation of high slope of the TGP ship lock

    Construction of the TGP ship lock began in April 1994.The excavation of lock chamber was basically completed in April 1999. By the end of December 2014,the slope of the ship lock remained stable for more than 14 years.In order to evaluate the high slope stability and the operation safety of the ship lock,nearly 1000 monitoring devices were laid out in various locations of the slope. To date,90%of the monitoring devices work well.

    2.1.Monitoring results of the TGP ship lock slope

    Since the completion of ship lock excavation in April 1999,the boundary conditions that in f uence the slope deformation magnitude have been basically identi f ed.Based on the measured results, the displacement after April 1999 kept nearly constant,with minor f uctuations.The variations of these measured values are mainly triggered by errors recorded in data observation,showing no obvious relations with temperature.

    2.1.1.Top of central piers

    The deformation of the central piers of the ship lock consists of the rebound deformation due to unloading during stress relief and the deformation induced by deadweight during the construction of the upright slopes.During excavation,stress relief happened in three directions of the central piers,namely,left and right sides, and the top.While at the lock head,stresses are released not only in the three directions but also in the free face downstream.Meanwhile,the geological condition and initial in-situ stress state vary at different parts of central piers.All of these factors contribute to the complicated deforming behaviors of the central piers.Typical deformation curves of central piers are shown in Fig.3.

    It can be seen form Fig.3 that there are signi f cant differences in magnitude and direction of displacement along the direction of lock chamber at different parts of the central piers.Most of the monitoring points at the south of the central piers deform towards south and the ones at the north towards north.Between the second and third lock heads,the direction of displacement at some parts of the central piers is the same.In December 2014,the measured displacements of the central piers towards the lock chamber were-19.49 to 33.59 mm and-5.89 to 23.76 mm at the north and south,respectively.

    In December 2014,the displacements of the central pier top measured downstream were-1.87 to 26.57 mm and-4.98 to 22.67 mm at the north and south,respectively.The measuring point TP119GP01,situated on the 160 m platform at the horizontal slope top of the third lock head,showed a maximum downstream displacement,which was primarily induced by unloading of the upright slope.

    The vertical displacement on the top of the central pier was mainly presented in form of settlement recorded in December 2014,with the measured values of-5.80 mm(rebound)to 15.27 mm(settlement).

    In order to analyze the convergence of surface deformation on the top of the central pier and to reduce the impact of observation errors,average annual values of the displacement towards the lock chamber were selected for comparison purpose(see Table 1).It can be observed from Table 1 that the annual average and the longterm average annual displacements(from 2000 to 2014)of the central pier top towards the lock chamber varied between ±1.5 mm,indicating that the central pier stays stable and the deformation of the central pier quickly converges after excavation.

    2.1.2.South and north high slopes

    The south and north slopes mainly deform towards the chamber (the direction of free face),with the horizontal displacement towards the lock chamber much greater than the horizontal and vertical displacements along the direction of water f ow.The typical deformation curves of the south slope are shown in Fig.4.

    The horizontal displacements of the north and south slopes towards the lock chamber slightly decrease with reduced elevation. By April 1999 when excavation was completed,the displacements of the north and south slopes towards the lock chamber were 9-39 mm and 4-53 mm,respectively;and the displacements of the slopes top towards the lock chamber were 11-27 mm and 4-35 mm,respectively.After that the displacements of the slopes increased slightly.By December 2014,the maximum displacements of the south and north slopes towards the lock chamber were74.27 mm and 58.82 mm,respectively.For the south slope,the maximum displacement was recorded at the measuring point TP41GP02 at elevation 185 m of the stake 15+930.The maximum displacements of north and south upright slopes top were 35.09 mm and 47.22 mm,respectively.

    Fig.3.Displacement of the measuring point TPBM68GP01 at elevation 160 m at the north of central pier top.

    The downstream displacements of the north and south slopes were small.The measured displacements in December 2014 were-2.53 to 33.96 mm,with the maximum value observed at the measuring point TP42GP02 at elevation 200 m bench on the south slope.This measuring point was situated at the corner of the broadened section of the vertical shaft,and its displacement was mainly triggered by unloaded downstream free face.

    The vertical displacement of north and south slopes was mainly in the form of settlement that was within 17 mm.The settlement roughly occurred during excavation.After completion of excavation,the displacement varied within a slight magnitude,and its increment was reduced with elapsed time and f nally tended to converge.

    The trend of displacement measured at each measuring point was different due to the differences in completion sequence of slopes,rock geological conditions and excavation state,as well as the effect of anchoring methods.By the end of December 2014,the displacement values of north and south slopes ranged between 0.57 mm and-20.86 mm,averaging 9.65 mm.The displacement increment in December of each year(from 1999 to 2014)decreased year after year,indicating that the deformation was convergent,as shown in Figs.5 and 6.Regression analysis was conducted for the displacement and the f tting curves can be expressed as follows:

    Table 1Annual average values of the horizontal displacement at the central pier top towards the lock chamber.

    wheretis the time(from April 1999);a,b,Kandmare the f tting parameters.For each measuring point,these four f tting parameters are different.

    According to the monitoring results,the deformation of slope was mainly induced by excavation.Most of the deformation was observed during excavation,and increased with increasing excavation depth.The deformation rate measured after excavation decreased.At present,the deformation of slopes has converted to a stable value,and the slopes are stable in a global sense.It is indicated that reservoir impoundment and navigation through the ship lock have no obvious effect on the deformation of north and south high slopes.

    The measured surface deformation was primarily in the direction towards the lock chamber.The convergence of the surface deformation rates of the north and south upright slopes were the fastest.Most of measuring points on the north and south slopes exhibited a fast convergence velocity of deformation,except for a few measuring points on the top.In view of rock lithology,the deformation rate of the measuring points in fresh and weakly weathered rocks converged faster,except for several measuring points characterized with a slow convergence velocity in the strongly weathered rocks on the top of north and south slopes.The relative deformations of the blocks measured in unloading zones of the upright slope have remained constant since completion of slope excavation and supporting in 1999,which indicates that the upright slope is stable.

    2.2.Deformations of lock head and side wall

    Normal and inverted plumb lines were deployed at each lock head to monitor the horizontal displacement of the lock head;and tension wire alignment was laid out in the pipeline gallery on the top of lift walls on the north and south slopes of all lock chambers to monitor the horizontal displacement of lift walls.Speci f cally,the vertical lines of the 1st and 5th lock heads were set in the 3rd block of the lock heads;and the vertical lines of the 2nd,3rd,4th,and 6th lock heads were set in the 2nd block of these lock heads.Theanchorage point of foundation plumb line holes of each lock head is roughly 42-63 m below the f oor elevation of the foundation gallery.

    Fig.4.Displacement of the measuring point TPBM94GP02 at elevation 168 m bench of the south slope.

    2.2.1.Lock head and gate pier

    The normal and inverted plumb lines at each lock head subsequently began to work between September 2001 and August 2002. By the end of December 2014,the measured deformation at lock heads is shown in Table 2,and the typical curves are shown in Fig.7.

    Table 2 and Fig.7 show that the displacement at the bottom of the lock head is smaller,with the value of-1.5 to 1.5 mm.The displacement at lock head top is-0.83 to 7.27 mm towards the lock chamber,and-3.93 to 7.71 mm towards the downstream direction. The deformation of the lock head does not affect the opening of the miter gate of the ship lock.In contrast,the measured deformations of the 5th and 6th lock heads are slightly greater and change periodically with temperature.This is mainly associated with the characteristic of mixed structure of abutment piers.The annual variation of displacement towards the lock chamber,induced by change of temperature,is approximately within 2 mm.Reservoir impoundment and lock f lling and discharge have a slight effect on the displacement of lock head top.

    Fig.5.Trend value of displacement at elevation 139 m on the top of north upright slope at the stake 15+787.

    Fig.6.Trend value of displacement at elevation 155 m on the top of south upright slope at the stake 15+770.

    2.2.2.Lock chamber side wall

    Table 3 shows the measured horizontal displacement,towards the lock chamber,of pipeline gallery in the south and north slopes by December 2014.It is shown that the values of the horizontal displacement change between-1.46 mm and 7.45 mm.The displacements of the 4th and 5th lock chambers are relatively large due to the gravity structure of the upper chambers.The displacement does not increase with elapsed time.

    General speaking,the changes in the horizontal displacement of foundation at the lock head,and the displacement of lock head top towards the lock chamber,upstream and downstream are minor. The vertical displacement of foundation of the north and south lines varies within±1 mm before and after impoundment each year.It is shown that a minor effect of impoundment on foundation deformation is observed.

    3.Monitoring of anchorage force of the TGP ship lock slope

    In order to enhance the stability of high slopes of the TGP ship lock,improve the stress state of slope rock,and prevent unloading excavation and development of cracks,a total of 230 sets of 1000-kN end anchor cables,666 of 3000-kN end anchor cables,and 1271of 3000-kN two-ended anchor cables were utilized to reinforce the slopes.In addition,a great number of blocks that have the potential of instability were encountered during excavation of the stage II at the upright slope of the ship lock.To enhance the stability of these blocks,1309 sets of 3000-kN end anchor cables and 528 of 3000-kN two-ended anchor cables were arranged(Fig.8).

    Table 2Range of measured displacement values on the top of each lock head(unit:mm).

    Fig.7.Correlation curves of horizontal displacement on the top of lock head I.

    Table 3Measured horizontal displacement of pipeline gallery on north and south slopes (towards the lock chamber).

    3.1.Prestress of anchor cables

    One hundred and f fteen anchor cable dynamometers were deployed to observe the long-term prestress state of anchor cables,of which two are bonded anchor cables,and others are unbonded cables.The statistics of prestress loss ratio after anchor cable lock-in is shown in Table 4,and typical process curves are shown in Fig.9.

    As can be seen from Table 4 and Fig.9,the measured prestress loss after anchor cable lock-in is-0.6%to 6.4%,averaging 2.8%.It was roughly 12.61%in average in December 2014.The change in anchor cable prestress loss is in agreement with the general rules of stress loss obtained in other cases.After one year of installation of the anchor cables,the average prestress loss after cable lock-in was 8%, most of the anchor cables being within 5%.Two years later,the prestress change was slight and almost kept constant,and an annual change of prestress due to the minor effect of temperature can be observed.

    Fig.8.Photo of anchor cables laid out at the high slope of double-lane f ve-step ship lock.

    There was a slight difference between the magnitude of prestress loss of the anchor cable on the blocks and non-block parts,and the prestress loss matched with its change rule.Takingthe block f1239 for example,its average prestress loss rate was about 7.2%after lock-in for one year,while the average prestress loss rate measured by other dynamometers at the south slope was around 7.6%one year after lock-in.Reservoir impoundment and ship lock navigation have no obvious impact on the anchorage force of the anchor cables,and no dramatic change has been observed in anchor cable prestress.This confrms that all slopes are stable.

    Table 4Measured prestress loss ratio of anchor cable by dynamometers.

    Fig.9.Process curves of prestress loss after lock-in of 3000-kN anchor cable at the south slope.

    3.2.Stress of high-strength anchor bolt

    The main part of the TGP ship lock is located within the deeply cut rock tank at the left side of Tanziling.The walls of the ship lock are of thin reinforced concrete lining structure combined with mixed(gravity+lining)structures.The lining structure bears loads associated with bed rocks behind the walls so as to meet the requirements of structural stability in terms of strength.At the same time,string stress gages were amounted on the free segment of the anchor bolt at interface of lining and bed rock to observe the stress of high-strength anchor bolt.

    The measured stresses of high-strength anchor bolt at the lock head I are shown in Table 5,and time-history curves of anchor bolt stressareshowninFig.10.AscanbeseenfromTable5andFig.10,the stress measured by 48 stress gages was within 315 MPa in December 2014.The maximum tensile stress recorded by the stress gages was within150MPa,except threestressgages,i.e.R4CZ21(EL.165.8mon the north slope of the 2nd lock chamber),R8CZ31(EL.152.03 m on thenorth slopeof the3rdlockchamber),andR1CZS53(EL.56.5mon the south slope of the 5th lock chamber),which had a maximum tensile stress of more than 200 MPa.In presence of the navigation of the ship lock in 2003,flling and discharge of lock chamber had a slight impact on variation of anchor bolt stress.On the whole,the measured stresses of anchorboltare generallysmalland farlessthan the design values of anchor bolts,which indicates that the lining structure of the ship lock is stable.

    Table 5Stress of high-strength anchor bolt on 15+060 section of lock head I.

    Fig.10.Stress of high-strength anchor bolt on the north slope of lock head I(R2-4CZ11).

    4.Conclusions

    Up to December 2014,the TGP ship lock had beenputin operation for over 10 years and experienced a 5-year reservoir impoundment testing.The monitoring results show that the slopes of the ship lock are stable,and the deformation of lock head and lift wall and the stress of high-strength anchor bolts are all within the allowable range.Reservoir impoundment has no signi f cant effect on the deformation of the ship lock,and the variations in deformation and stress at various key positions after monitoring are normal.The high slopes and ship lock are basically in a stable state and the upstream and downstream channels and linkage sections enjoy good shipping capability,suggesting the ef f cient operation of the TGP ship lock.

    Con f ict of interest

    The authors wish to con f rm that there are no known con f icts of interest associated with this publication and there has been no signi f cant f nancial support for this work that could have in f uenced its outcome.

    Dai Huichao.Research on rock mechanics problems of division pier of the Three Gorges permanent shiplock.Chinese Journal of Rock Mechanics and Engineering 2001;20(5):680-4(in Chinese).

    Fan Qixiang.Key technical issues of TGP permanent shiplock.Engineering Science 2004;6(1):48-52(in Chinese).

    Fan Qixiang,Zhu Hongbing,Chen Xuchun.Key rock mechanics issues related to the Three Gorges Project in China.Journal of Rock Mechanics and Geotechnical Engineering 2011;3(4):329-42.

    Zhang Chaoran.Practice and experimental veri f cation of TGP’s permanent shiplock slope.Engineering Science 2001;3(5):22-7(in Chinese).

    Dr.Qixiang Fangraduated from Gezhouba Institute of Hydro Electric Engineering with a B.S.in 1984,and obtained M.S.and Ph.D.from Tsinghua University in 1999 and 2010,respectively.He held several positions in the China Three Gorges(CTG)Project Preparatory Of f ce, including associate engineer in the Division of Technology in the Department of Construction Technology,project supervising engineer and leader of the supervision team of the Liyuan Project and later the Deputy Director of the Construction Division of the Liyuan Company.He served in CTG’s Construction Department as Deputy Director of the Division of General Management and later as the Director of the department,Director of the Division of Temporary Ship Lock Project and later the Director of the Division of Temporary Ship Lock and Ship Lift under the Left Bank Construction Department of the Three Gorges Project,the Deputy Director and later the Director of the Navigation Construction Department and Deputy Director of Management Department of Beijing National Aquatics Center(known as the Water Cube).He now is Executive Vice President of the CTG and is in charge of the construction of CTG’s Jinsha River hydropower projects.Dr.Fan is well experienced in management of large-scale complex hydropower projects,design,installation and testing of complex centralized control system,stability of high slopes,construction and installation of large-scale metal structures and structural concrete,etc.He has published over 80 papers.He has participated in the construction of several large-scale hydropower projects successively and made outstanding contribution to the construction and management of the TGP.

    *Corresponding author.Tel.:+86 10 57081690.

    E-mail address:zhu_hongbing@ctgpc.com.cn(H.Zhu).

    Peer review under responsibility of Institute of Rock and Soil Mechanics, Chinese Academy of Sciences.

    1674-7755?2015 Institute of Rock and Soil Mechanics,Chinese Academy of Sciences.Production and hosting by Elsevier B.V.All rights reserved.

    http://dx.doi.org/10.1016/j.jrmge.2015.02.007

    欧美激情在线99| 免费在线观看成人毛片| 两个人的视频大全免费| 精品人妻1区二区| 91久久精品电影网| 免费高清视频大片| 色播亚洲综合网| 18禁黄网站禁片午夜丰满| 尤物成人国产欧美一区二区三区| 国产精品国产高清国产av| 国产高清不卡午夜福利| 免费电影在线观看免费观看| 少妇裸体淫交视频免费看高清| 国产麻豆成人av免费视频| 精品人妻一区二区三区麻豆 | 国产精品一区二区三区四区免费观看 | 亚洲专区国产一区二区| 他把我摸到了高潮在线观看| 色精品久久人妻99蜜桃| 国产综合懂色| 日韩,欧美,国产一区二区三区 | 人妻久久中文字幕网| 波多野结衣巨乳人妻| 网址你懂的国产日韩在线| ponron亚洲| 国产国拍精品亚洲av在线观看| 18禁裸乳无遮挡免费网站照片| 国产视频内射| 免费在线观看日本一区| 欧美+亚洲+日韩+国产| 九色成人免费人妻av| 天天躁日日操中文字幕| 亚洲天堂国产精品一区在线| 国产精品1区2区在线观看.| 国产男靠女视频免费网站| 床上黄色一级片| 性色avwww在线观看| 高清在线国产一区| 动漫黄色视频在线观看| 精品久久久久久久久av| 精品无人区乱码1区二区| 真人做人爱边吃奶动态| 婷婷精品国产亚洲av在线| 亚洲18禁久久av| 69av精品久久久久久| 国产视频内射| 免费在线观看日本一区| 成人毛片a级毛片在线播放| 天堂动漫精品| 亚洲人与动物交配视频| 99久久成人亚洲精品观看| 99久久九九国产精品国产免费| 美女大奶头视频| 国产一区二区在线av高清观看| 毛片女人毛片| 国内精品久久久久精免费| 亚洲av二区三区四区| 少妇丰满av| 亚洲黑人精品在线| 男女那种视频在线观看| 成人高潮视频无遮挡免费网站| 婷婷精品国产亚洲av在线| 琪琪午夜伦伦电影理论片6080| 最后的刺客免费高清国语| 精品人妻一区二区三区麻豆 | 国产女主播在线喷水免费视频网站 | 色综合站精品国产| 国产成人影院久久av| 最近最新中文字幕大全电影3| 免费无遮挡裸体视频| 成人三级黄色视频| 精品免费久久久久久久清纯| 欧美成人免费av一区二区三区| 搡老熟女国产l中国老女人| 亚洲真实伦在线观看| 五月玫瑰六月丁香| 久久久色成人| 欧美极品一区二区三区四区| 91在线观看av| 国产女主播在线喷水免费视频网站 | 日韩中文字幕欧美一区二区| 欧美精品国产亚洲| 麻豆国产av国片精品| 99热精品在线国产| 日韩欧美国产一区二区入口| 91在线精品国自产拍蜜月| 中文字幕免费在线视频6| 欧美不卡视频在线免费观看| 精品人妻视频免费看| 天美传媒精品一区二区| 亚洲av电影不卡..在线观看| 日韩精品中文字幕看吧| 91麻豆精品激情在线观看国产| 嫩草影院新地址| 成熟少妇高潮喷水视频| 国产精品日韩av在线免费观看| 亚洲精品影视一区二区三区av| 午夜福利成人在线免费观看| 亚洲欧美日韩东京热| 久久国产乱子免费精品| 久久久久九九精品影院| 国产欧美日韩精品一区二区| 精品久久久久久,| 日日干狠狠操夜夜爽| 如何舔出高潮| 不卡一级毛片| 在线观看美女被高潮喷水网站| 国产精品久久久久久久久免| 在线天堂最新版资源| 亚州av有码| 午夜爱爱视频在线播放| 搞女人的毛片| 成人三级黄色视频| 日韩高清综合在线| 国产av麻豆久久久久久久| 国产爱豆传媒在线观看| 嫩草影院精品99| aaaaa片日本免费| 熟妇人妻久久中文字幕3abv| 男女下面进入的视频免费午夜| 亚洲aⅴ乱码一区二区在线播放| 日本三级黄在线观看| 成人国产综合亚洲| 亚州av有码| 亚洲人与动物交配视频| 国产精品乱码一区二三区的特点| 久久婷婷人人爽人人干人人爱| 一边摸一边抽搐一进一小说| 99热精品在线国产| 国产不卡一卡二| 日韩欧美精品免费久久| 看片在线看免费视频| av天堂在线播放| а√天堂www在线а√下载| 国产69精品久久久久777片| 黄色配什么色好看| 天堂√8在线中文| 国内精品久久久久久久电影| 亚洲av五月六月丁香网| 久久人人爽人人爽人人片va| 成人鲁丝片一二三区免费| 精品福利观看| 国产精品日韩av在线免费观看| 乱系列少妇在线播放| 欧美+日韩+精品| 日韩精品有码人妻一区| 在现免费观看毛片| 国产精品一区二区三区四区免费观看 | 长腿黑丝高跟| 久久99热6这里只有精品| 国产精品乱码一区二三区的特点| 久久亚洲精品不卡| 亚洲成人久久爱视频| 国产在线男女| 精品一区二区免费观看| 久久精品国产亚洲网站| 一区二区三区激情视频| 亚洲七黄色美女视频| 天堂影院成人在线观看| 日韩人妻高清精品专区| 亚洲五月天丁香| 成人美女网站在线观看视频| 国产不卡一卡二| 成年人黄色毛片网站| 午夜日韩欧美国产| 香蕉av资源在线| 成人无遮挡网站| 精品国内亚洲2022精品成人| 18禁黄网站禁片免费观看直播| 美女xxoo啪啪120秒动态图| 热99re8久久精品国产| 少妇熟女aⅴ在线视频| 欧美日韩精品成人综合77777| 久久久久九九精品影院| 中文资源天堂在线| avwww免费| 亚洲四区av| 欧美日本视频| 久久久久久久久大av| 麻豆成人午夜福利视频| 国内精品一区二区在线观看| АⅤ资源中文在线天堂| 国产精品伦人一区二区| 三级国产精品欧美在线观看| 成人午夜高清在线视频| 久久精品国产鲁丝片午夜精品 | 成人鲁丝片一二三区免费| 欧美日韩综合久久久久久 | av在线老鸭窝| 精华霜和精华液先用哪个| 91久久精品国产一区二区成人| 国产精品永久免费网站| 午夜影院日韩av| 欧美xxxx黑人xx丫x性爽| 欧美潮喷喷水| 99久久精品热视频| 精品无人区乱码1区二区| 亚洲精品一卡2卡三卡4卡5卡| 麻豆国产97在线/欧美| 99久国产av精品| 全区人妻精品视频| 亚洲国产欧美人成| 蜜桃久久精品国产亚洲av| 国产一级毛片七仙女欲春2| 91久久精品国产一区二区三区| 精品久久久久久成人av| 91久久精品电影网| 俺也久久电影网| 午夜免费男女啪啪视频观看 | 99riav亚洲国产免费| 午夜视频国产福利| 深夜精品福利| 亚洲久久久久久中文字幕| ponron亚洲| 国产精品久久久久久av不卡| 搡老熟女国产l中国老女人| 99久久中文字幕三级久久日本| 国产精品国产高清国产av| 成人国产麻豆网| 久99久视频精品免费| 一个人看视频在线观看www免费| 深夜精品福利| 直男gayav资源| 嫩草影视91久久| 亚洲五月天丁香| 在线国产一区二区在线| 国产欧美日韩精品亚洲av| 午夜福利成人在线免费观看| 午夜福利高清视频| 久久天躁狠狠躁夜夜2o2o| 亚洲中文日韩欧美视频| 日韩欧美一区二区三区在线观看| 日本撒尿小便嘘嘘汇集6| 亚洲中文字幕日韩| 免费观看人在逋| 久久久精品大字幕| 日韩精品有码人妻一区| 男人狂女人下面高潮的视频| 欧美+亚洲+日韩+国产| 国模一区二区三区四区视频| 两性午夜刺激爽爽歪歪视频在线观看| 国国产精品蜜臀av免费| 国产色爽女视频免费观看| 亚洲自拍偷在线| 国产精华一区二区三区| 亚洲经典国产精华液单| 一夜夜www| 中文字幕久久专区| 色噜噜av男人的天堂激情| 男人的好看免费观看在线视频| 人人妻人人看人人澡| 男女做爰动态图高潮gif福利片| 在线免费十八禁| 成年版毛片免费区| 嫩草影院精品99| 级片在线观看| 成人三级黄色视频| 中文字幕精品亚洲无线码一区| 老熟妇乱子伦视频在线观看| 搡老妇女老女人老熟妇| 窝窝影院91人妻| 国产精品久久久久久精品电影| 久久久色成人| 在线观看免费视频日本深夜| 男女之事视频高清在线观看| 免费av观看视频| 五月玫瑰六月丁香| 色尼玛亚洲综合影院| 国产男靠女视频免费网站| 久久久色成人| 国产精品亚洲一级av第二区| 亚洲精品影视一区二区三区av| 国产精品亚洲美女久久久| 国产精品一及| 老司机午夜福利在线观看视频| 夜夜看夜夜爽夜夜摸| 噜噜噜噜噜久久久久久91| 九九爱精品视频在线观看| 日韩精品青青久久久久久| 最近最新免费中文字幕在线| 黄色一级大片看看| 天美传媒精品一区二区| 国产亚洲精品av在线| 99热网站在线观看| 亚洲av电影不卡..在线观看| 男女啪啪激烈高潮av片| 日本欧美国产在线视频| 日韩,欧美,国产一区二区三区 | 欧美日本视频| 一进一出好大好爽视频| 色尼玛亚洲综合影院| 欧美日本亚洲视频在线播放| 午夜精品在线福利| 国产亚洲精品久久久久久毛片| 露出奶头的视频| 亚洲天堂国产精品一区在线| 3wmmmm亚洲av在线观看| 一级av片app| 大型黄色视频在线免费观看| 午夜免费激情av| a级一级毛片免费在线观看| 久久99热这里只有精品18| 午夜老司机福利剧场| 日韩国内少妇激情av| 国产欧美日韩精品亚洲av| 九九爱精品视频在线观看| 亚洲欧美日韩无卡精品| 男女视频在线观看网站免费| 欧美精品啪啪一区二区三区| 一进一出好大好爽视频| 日韩欧美在线二视频| 人人妻人人澡欧美一区二区| 18禁黄网站禁片午夜丰满| 亚洲一区二区三区色噜噜| 淫秽高清视频在线观看| 欧美一级a爱片免费观看看| 黄片wwwwww| 女人被狂操c到高潮| 国产爱豆传媒在线观看| 别揉我奶头~嗯~啊~动态视频| 日本黄色视频三级网站网址| 免费观看人在逋| 日日夜夜操网爽| 亚洲av美国av| 99热这里只有是精品50| 日韩欧美精品v在线| 亚洲最大成人手机在线| 又紧又爽又黄一区二区| 亚洲欧美日韩卡通动漫| 成人高潮视频无遮挡免费网站| 国产精品日韩av在线免费观看| 老女人水多毛片| avwww免费| 欧美成人免费av一区二区三区| 大型黄色视频在线免费观看| 无人区码免费观看不卡| 国内少妇人妻偷人精品xxx网站| 男插女下体视频免费在线播放| 伊人久久精品亚洲午夜| 日本免费a在线| 99久久成人亚洲精品观看| 国产主播在线观看一区二区| 婷婷丁香在线五月| 亚洲真实伦在线观看| 春色校园在线视频观看| 精品不卡国产一区二区三区| 性插视频无遮挡在线免费观看| 欧美激情久久久久久爽电影| 亚洲七黄色美女视频| 国产免费男女视频| 久久6这里有精品| 国产精品99久久久久久久久| 欧美一区二区亚洲| 99久久精品一区二区三区| 亚洲自偷自拍三级| 十八禁国产超污无遮挡网站| 亚洲熟妇中文字幕五十中出| 婷婷丁香在线五月| 男女下面进入的视频免费午夜| 成人欧美大片| 精品人妻视频免费看| 乱系列少妇在线播放| 欧美一区二区精品小视频在线| 一个人观看的视频www高清免费观看| 亚洲国产精品合色在线| 亚洲国产精品成人综合色| 亚洲av中文字字幕乱码综合| 国产av不卡久久| 国产高清三级在线| 亚洲综合色惰| 久久人妻av系列| 久久精品国产清高在天天线| 又黄又爽又刺激的免费视频.| 久久精品国产清高在天天线| 成人美女网站在线观看视频| 麻豆国产97在线/欧美| 日日摸夜夜添夜夜添小说| 麻豆国产97在线/欧美| 成人欧美大片| 久久精品综合一区二区三区| 国产精品野战在线观看| 久久久久久国产a免费观看| 免费人成在线观看视频色| 国产av不卡久久| 久久国产精品人妻蜜桃| 美女黄网站色视频| 最近最新中文字幕大全电影3| 久久久成人免费电影| 99久久中文字幕三级久久日本| 精品久久久久久久久久久久久| 男女下面进入的视频免费午夜| 91麻豆av在线| 99久久精品热视频| 一本精品99久久精品77| 免费不卡的大黄色大毛片视频在线观看 | 精品日产1卡2卡| 中文亚洲av片在线观看爽| 日本免费a在线| 中文字幕久久专区| 黄片wwwwww| 中文字幕精品亚洲无线码一区| 久久精品人妻少妇| 国产日本99.免费观看| 午夜福利高清视频| 一级黄片播放器| 国产男靠女视频免费网站| 又爽又黄无遮挡网站| 国产真实伦视频高清在线观看 | 久久久久久大精品| a级一级毛片免费在线观看| a级毛片a级免费在线| 中文字幕av在线有码专区| 久久久久久大精品| 俄罗斯特黄特色一大片| 国产精品国产高清国产av| 亚洲aⅴ乱码一区二区在线播放| 一个人看的www免费观看视频| 最后的刺客免费高清国语| 成年女人看的毛片在线观看| 国产精品美女特级片免费视频播放器| 日韩欧美 国产精品| 真人一进一出gif抽搐免费| 亚洲电影在线观看av| 国产亚洲av嫩草精品影院| 国产精品久久久久久久电影| 久久久国产成人免费| 又粗又爽又猛毛片免费看| bbb黄色大片| 国产三级在线视频| 99久国产av精品| 国产伦精品一区二区三区视频9| 国产av一区在线观看免费| 久久久久久久久大av| 久久久久久久亚洲中文字幕| 丰满乱子伦码专区| 日韩国内少妇激情av| 一区二区三区四区激情视频 | 久久久久久久久久成人| 亚洲精华国产精华精| 亚洲第一区二区三区不卡| 熟女人妻精品中文字幕| 国产 一区精品| 精品99又大又爽又粗少妇毛片 | 国产激情偷乱视频一区二区| 欧美性猛交黑人性爽| 亚洲精华国产精华液的使用体验 | 五月玫瑰六月丁香| 免费一级毛片在线播放高清视频| 欧美性猛交黑人性爽| 韩国av一区二区三区四区| 精品免费久久久久久久清纯| 欧美人与善性xxx| 久久久久久久精品吃奶| 精品一区二区三区视频在线观看免费| 麻豆国产av国片精品| 日日啪夜夜撸| 欧美极品一区二区三区四区| 91麻豆精品激情在线观看国产| 国产在线精品亚洲第一网站| 琪琪午夜伦伦电影理论片6080| 亚洲午夜理论影院| 欧美zozozo另类| 变态另类成人亚洲欧美熟女| 国内精品宾馆在线| 亚洲精品一区av在线观看| 免费看av在线观看网站| 他把我摸到了高潮在线观看| 99久久精品一区二区三区| 在线观看美女被高潮喷水网站| 国产黄片美女视频| 午夜精品在线福利| 午夜影院日韩av| 九九爱精品视频在线观看| 五月玫瑰六月丁香| 欧美高清成人免费视频www| 我要搜黄色片| 亚洲精品一卡2卡三卡4卡5卡| 国产精品嫩草影院av在线观看 | 亚洲国产色片| 亚洲自拍偷在线| 亚洲avbb在线观看| 日韩欧美三级三区| 亚洲午夜理论影院| 色精品久久人妻99蜜桃| 在线观看av片永久免费下载| 欧美极品一区二区三区四区| 久久中文看片网| 国产伦精品一区二区三区四那| 制服丝袜大香蕉在线| 看免费成人av毛片| 午夜免费激情av| 亚洲中文字幕日韩| 很黄的视频免费| eeuss影院久久| 国产 一区 欧美 日韩| 琪琪午夜伦伦电影理论片6080| 午夜视频国产福利| 成人亚洲精品av一区二区| 婷婷六月久久综合丁香| 日韩大尺度精品在线看网址| 乱人视频在线观看| 免费av不卡在线播放| 乱系列少妇在线播放| 亚洲精品成人久久久久久| 日本一本二区三区精品| 久久久久久久午夜电影| 中文资源天堂在线| 少妇猛男粗大的猛烈进出视频 | 亚洲专区国产一区二区| 51国产日韩欧美| 精品久久久久久久久亚洲 | 亚洲狠狠婷婷综合久久图片| 婷婷亚洲欧美| 午夜精品在线福利| 久久国产乱子免费精品| 久久久精品大字幕| 国产精品女同一区二区软件 | 亚洲人与动物交配视频| 婷婷色综合大香蕉| 亚洲在线观看片| 免费大片18禁| 动漫黄色视频在线观看| 性欧美人与动物交配| 99久久精品热视频| 国产欧美日韩精品一区二区| 日韩av在线大香蕉| 午夜福利在线观看免费完整高清在 | 成年女人永久免费观看视频| 黄色配什么色好看| 国产精品一区www在线观看 | 免费在线观看日本一区| 久久6这里有精品| 12—13女人毛片做爰片一| 特大巨黑吊av在线直播| 亚洲自偷自拍三级| 日韩国内少妇激情av| 高清毛片免费观看视频网站| 又粗又爽又猛毛片免费看| 精品日产1卡2卡| 国产高清视频在线观看网站| 亚洲无线观看免费| 毛片女人毛片| 村上凉子中文字幕在线| 老女人水多毛片| 免费大片18禁| 亚洲一区二区三区色噜噜| 最新在线观看一区二区三区| 国产成年人精品一区二区| 日韩欧美在线乱码| 天天躁日日操中文字幕| 日韩欧美国产一区二区入口| 级片在线观看| 亚洲最大成人av| av福利片在线观看| 国产麻豆成人av免费视频| 久久精品国产自在天天线| av专区在线播放| 欧美zozozo另类| 国产免费一级a男人的天堂| 欧美日韩亚洲国产一区二区在线观看| 国产男人的电影天堂91| 少妇熟女aⅴ在线视频| 男人和女人高潮做爰伦理| 91av网一区二区| 又黄又爽又刺激的免费视频.| 搡老妇女老女人老熟妇| 国产视频一区二区在线看| 最新在线观看一区二区三区| 天堂动漫精品| 老熟妇乱子伦视频在线观看| 在线免费十八禁| 波多野结衣高清无吗| 啦啦啦啦在线视频资源| 亚洲熟妇中文字幕五十中出| 亚洲精华国产精华液的使用体验 | 久久精品国产清高在天天线| 伦精品一区二区三区| 成年人黄色毛片网站| 一a级毛片在线观看| 亚洲中文日韩欧美视频| 午夜免费激情av| 日本与韩国留学比较| 亚洲在线观看片| 免费人成视频x8x8入口观看| 国产乱人视频| 亚洲天堂国产精品一区在线| 听说在线观看完整版免费高清| 欧美最新免费一区二区三区| 午夜激情福利司机影院| 国产精品av视频在线免费观看| 小蜜桃在线观看免费完整版高清| 俺也久久电影网| 亚洲自拍偷在线| 成人美女网站在线观看视频| 欧美在线一区亚洲| 午夜福利在线在线| 乱码一卡2卡4卡精品| 亚洲av第一区精品v没综合| 999久久久精品免费观看国产| 精品久久久久久成人av| 久久精品综合一区二区三区| 亚洲av二区三区四区| 最新在线观看一区二区三区| 变态另类丝袜制服| 国产伦在线观看视频一区| 春色校园在线视频观看| 一a级毛片在线观看| 在线播放无遮挡| 99在线视频只有这里精品首页| 婷婷色综合大香蕉| 欧美高清成人免费视频www| 一本久久中文字幕| 国产精品无大码| 亚洲av中文字字幕乱码综合| videossex国产|