• <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 ?

    Landslide disaster prevention and mitigation through works in Hong Kong

    2013-10-19 06:56:50ChoiRaymondCheung
    關(guān)鍵詞:負(fù)責(zé)制責(zé)任制總經(jīng)理

    K.Y. Choi, Raymond W.M. Cheung

    Geotechnical Engineering Of fice, Civil Engineering and Development Department, The Government of the Hong Kong SAR, Hong Kong, China

    1. Introduction

    Hong Kong has a hilly terrain with little flat land; among the total land area of about 1100 km2, some 63% of the land is steeper than 15°and 30% steeper than 30°. Because of the intense urban development, a large number of man-made slopes are formed on hillsides in close proximity to buildings, roads and other facilities.These man-made slopes may be susceptible to landsliding during periods of high seasonal rainfall, which could be a serious hazard if not attended to. The situation was exacerbated by the lack of proper engineering standards in the design and construction of man-made slopes prior to the setting up of the Geotechnical Engineering Office(GEO, formerly known as the Geotechnical Control Office) in 1977 as a central body to regulate various aspects of slope safety in Hong Kong. Indeed, landslides have occurred regularly in Hong Kong over the past century, causing extensive socio-economic damage and loss of lives (CEDD, 2005). In the past 65 years since 1947, some 470 people have been killed by landslides in Hong Kong, mostly as a result of failures associated with man-made slopes. The notable incidents include two fatal landslides at Po Shan Road and Sau Mau Ping respectively on 18 June 1972 where a total of 138 people were killed, and another fatal landslide at Sau Mau Ping on 25 August 1976 where 18 people were killed (Fig. 1).

    Apart from man-made slopes, Hong Kong is faced with the insidious natural terrain landslide hazards. Based on a review of aerial photographs taken from 1924 to 2006, about 100,000 past landslides on natural terrain were identified (MFJV, 2007). In the severe rainstorm of 4 and 5 November 1993, over 800 landslides occurred on the natural terrain on Lantau Island. About 2400 natural terrain landslides occurred in West Lantau during another severe rainstorm of 7 June 2008. Whilst most of these natural terrain landslides occurred in relatively remote areas, some of them had affected existing facilities including buildings and roads. For example, a channelized debris flow was triggered by natural terrain landslides above Sham Tseng San Tsuen on 23 August 1999(Fig. 2).

    The channelized debris flow had travelled down the natural hillside and demolished several squatter structures at the foothill.One person was killed and another 13 persons were injured as a result of this incident (FMSWJV, 2005). Immediate emergency measures including closure of roads and evacuation of homes were implemented to ensure public safety. These incidents highlight the hazards arising from natural terrain landslides. With the growing demand for land to meet housing needs and other purposes, there is a trend to locate developments closer to areas of steep natural hillsides with a consequent increase in landslide risk.

    Fig. 1. The fatal landslides at Po Shan Road and Sau Mau Ping in the 1970s.

    Fig. 2. The 1999 natural terrain landslide at Sham Tseng San Tsuen.

    2. The Landslip Preventive Measures Programme from 1977 to 1994

    In the aftermath of the disastrous man-made slope failures in the 1970s, the Government embarked on a long-term slope retro fitting programme in 1977, known as the Landslip Preventive Measures (LPM) Programme, to deal with substandard man-made slopes. A catalogue of sizeable man-made slopes including cut slopes, fill slopes and retaining walls was compiled. Currently, there are about 60,000 man-made slopes registered in the New Slope Catalogue (Fig. 3). These slopes are mainly situated within developed areas or adjacent to traf fic routes over different geographical locations of Hong Kong.

    Fig. 3. Spatial distribution of the 60,000 man-made slopes in Hong Kong.

    Fig. 4. Distribution of slopes upgraded under the LPM Programme from 1977 to 2010.

    Initially, most of the slopes included in the LPM Programme were fill slopes affecting housing estates, schools and hospitals,mainly as a result of the two fatal landslides involving liquefaction of loose fill at Sau Mau Ping in 1972 and 1976, respectively. Since the mid-1980s, the proportion of soil cut slopes, rock cut slopes and retaining walls in the LPM Programme had increased. Up to 1994, a total of 620 slopes (Fig. 4) had been upgraded under the LPM Programme. In sum, the focus of the LPM Programme in this period, i.e. 1977-1994, was on treating man-made slopes affecting occupied buildings. The total expenditure involved was about HK$1200 million (Fig. 5).

    In general, there are four stages in the design and construction of slope upgrading works under the LPM Programme. These include:

    Fig. 5. Expenditure incurred under the LPM Programme from 1997 to 2010.

    (a) Stage 1 - Preliminary study consisting of a site reconnaissance to identify slopes that require a detailed study. Where signs of immediate and obvious danger are identified, urgent repair works would be initiated.

    (b) Stage 2 - Detailed study consisting of desk study, aerial photograph interpretation, site observations, stability analysis, and if necessary, ground investigation works to decide whether or not upgrading works are necessary. For private slopes, where there is primafacie evidence that the slope is dangerous or liable to become dangerous, a statutory repair order would be issued to the private owners concerned. This process is referred to as“safety screening”.

    (c) Stage 3 - Design of slope upgrading works to bring the slope up to the required safety standards.

    (d) Stage 4 - Construction of slope upgrading works including tender documentation, contract administration and site supervision.

    Fig. 6. The 1994 fatal landslide at Kwun Lung Lau.

    3. Acceleration of the LPM Programme from 1995 to 2010

    On 23 July 1994, a fatal landslide occurred below Block D of Kwun Lung Lau, Kennedy Town (Fig. 6). Five people were killed and another three people were injured during the incident. In addition, about 3900 residents were temporarily evacuated overnight.A comprehensive investigation into the cause of the landslide was subsequently carried out by the GEO. An international renowned geotechnical engineering expert was engaged by the Government to conduct an independent review of the investigation (GEO,2000a). A Select Committee was established by the Legislative Council in 1994 to inquire into matters related to the fatal landslide.Prompted by the Kwun Lung Lau landslide, the Government initiated a Slope Safety Review at the end of 1994 to examine the policy,legislation and resources related to the prevention of landslides in Hong Kong, and to recommend improvement measures.

    Following the investigation, inquiry and review, a number of recommendations to improve the slope safety system were made. One of the recommendations was to accelerate the LPM Programme. Following acceptance of the recommendations, the Government launched the 5-year Accelerated LPM Programme in April 1995. The target was to complete the upgrading works for about 800 substandard government man-made slopes and to carry out safety screening studies for 1500 private man-made slopes. To ensure that the most deserving slopes are selected for action under the Programme, a risk-based priority ranking system incorporating the results of quantitative risk assessment (QRA), and the experience and technical know-how in landslides accrued over the years was adopted (Wong, 2005). The risk-based priority ranking system takes account of both the likelihood of landslide and the consequence of the slope failure. A total score which reflects the risk of the slope is obtained by the product of instability score and consequence score. The instability score is determined by a number of factors including age of slope, level of geotechnical input during the formation of the slope, slope geometry, signs of distress, records of instability and other characteristics. The consequence score is determined by the type and proximity of the facilities affected, the probable scale of failure and the topography adjacent to the slope.

    Over the 5 years from 1995 to 2000, a total of 794 slopes were upgraded under the LPM Programme (Fig. 4). The total expenditure involved is about HK$ 2930 million (Fig. 5). At the end of the 5-year Accelerated LPM Programme, about 250 slopes were upgraded each year which is about five to six times the average productivity before 1995. It is worth noting that QRA has been applied at that time to evaluate and monitor the performance of the LPM Programme.An assessment made in 2000 found that the overall landslide risk posed by pre-1977 man-made slopes was reduced to 50% of the level existed in 1977 upon completion of the 5-year Accelerated LPM Programme (Cheung and Shiu, 2000).

    As part of the Government’s long-term strategy to improve slope safety in Hong Kong, the 10-year Extended LPM Programme was launched in 2000 upon completion of the 5-year Accelerated LPM Programme. The annual output under the 10-year Extended LPM Programme was to upgrade 250 government man-made slopes and to carry out safety-screening studies on 300 private man-made slopes. The aim was to reduce the landslide risk posed by pre-1977 man-made slopes to 25% of the level in 1977 (Cheng, 2011). The 10-year Extended LPM Programme was successfully completed in 2010, and this has brought about substantial improvement in the safety of slopes and a significant reduction in the number of fatal landslides in recent years.

    During the period from 1977 to 2010, about 4500 substandard government man-made slopes were upgraded under the LPM Programme (Fig. 4). The average number of slopes upgraded from 1977 to 1994 was about 35 per year and this had progressively increased to 250 per year during the 5-year Accelerated LPM Programme. The average number of slopes upgraded per year under the 10-year Extended LPM Programme had further increased to 300.

    The cumulative expenditure incurred under the LPM Programme from 1977 to 2010 was about HK$ 14 billion (Fig. 5). Before the 5-year Accelerated LPM Programme, the annual expenditure was about HK$ 60 million. Over the 5 years from 1995, the expenditure had increased geometrically until it reached the peak of about HK$ 900 million in 2000. In the next 10 years from 2000 to 2010,the average annual expenditure was about HK$ 950 million.

    Apart from LPM upgrading works, enhanced maintenance (EM)works, generally by means of prescriptive measures, were carried out on some 5000 selected old slopes maintained by various government departments who are responsible for maintaining these slopes. This also helps achieve quick improvement to the stability of old substandard slopes.

    Fig. 7. Landslide risk profile of Hong Kong.

    4. The post-2010 Landslip Prevention and MitigationProgramme

    With the introduction of geotechnical control and the implementation of the LPM Programme, the landslide risk has decreased progressively and reached the “As low as reasonably practicable” (ALARP) zone in 2010 (Fig. 7). However, there is no room for complacency. If investment in slope safety is not maintained, the landslide risk will increase with time due to slope deterioration and encroachment of urban development or redevelopment upon steep natural hillside. This would cause, in addition to risk to life,significant economic losses and social disruption as a result of road blockages and building evacuation due to landslides, thereby compromising public safety, sustainable development and Hong Kong’s reputation as a modern metropolitan city and tourist hub.

    The majority of the remaining landslide risk comes from about 15,000 man-made slopes with moderate risk affecting development and about 2700 natural hillside catchments (Fig. 8) with known hazards and close to existing buildings and important transport corridors. Therefore, the Government has implemented Landslip Prevention and Mitigation (LPMit) Programme since 2010 to dovetail with the 10-year extended LPM Programme. The strategy of the LPMit Programme is to contain this remaining landslide risk through rolling enhancement of man-made slopes and systematic mitigation of natural terrain landslide risk pursuant to the“react-to-known” hazard principle, i.e. to carry out studies and mitigation actions where significant hazards become evident. The annual target of the LPMit Programme is to complete the upgrading works for 150 substandard government slopes, carry out safety screening studies on 100 private slopes and carry out landslide risk mitigation works for 30 vulnerable natural hillside catchments from 2010 onwards.

    Fig. 8. Spatial distribution of the 2700 vulnerable natural hillside catchments.

    5. Technical advancement in man-made slope upgradingworks

    Slope upgrading works are substantial engineering works based on the principles of removal (e.g. cutting back the slope to reduce its gradient), reinforcement (e.g. strengthening slopes by installation of steel bars called soil nails), retention (i.e. supporting slopes with retaining structures), and replacement (e.g. excavating and reforming slopes with a denser surface soil layer). Combinations of different types of works may be used for upgrading man-made slopes. The design and construction practice for man-made slopes has evolved over time, as a result of the technical advancements made in respect of slope engineering and construction techniques.In particular, the findings of the systematic landslide investigation Programme initiated by the GEO since 1997 have contributed to achieving an improved understanding of the mechanisms and causes of slope failures. Areas for improvement in enhancing the slope engineering practice are identified, which are promulgated by Ho et al. (2002).

    Fig. 9. Stabilization of fill slopes.

    5.1. Fill slopes

    Substandard fill slopes, typically comprising loose fill materials,are susceptible to liquefaction when they become saturated and subjected to shearing. The conventional method of treating these fill slopes is to excavate and re-compact the top 3 m of loose fill to achieve 95% relative compaction (Fig. 9a). This is based on the recommendations made by the independent review panel for fill slopes, which was set up following the 1976 Sau Mau Ping landslide(HKG, 1977). Most of the fill slopes under LPM Programme were upgraded by means of this method because of its effectiveness and reliable performance in improving the stability of the fill slopes. A variant to this method, which entails the use of rock fill or cement stabilized soil in place of compacted soil fill to form the 3 m cap,has been adopted in some cases (Fig. 9b).

    Fig. 10. Upgrading of loose fill slopes using soil nails and grillage.

    5.2. Soil cut slopes

    Before 1990, the usual method of improving the stability of a substandard soil cut slope was by trimming back the slope to a gentler profile (Koirala and Tang, 1988). The major construction activity involved is excavation and removal of soil materials from the slope. Because no special engineering techniques are needed,the construction cost is relatively cheap and easy to implement.Vegetation is used as the slope surface cover in order to make the slope look as natural as possible. Where there is insufficient space at the crest to accommodate the cut back profile, structural supports such as hand dug caissons and retaining walls would be used to improve the stability of the slopes (Powell et al., 1990).

    Discussions on the reliability of the design of soil cut slopes were made in the 1980s (Malone, 1985). The profession recognized that there were uncertainties inherent in some of the important elements of a slope design such as the geological model, selection of slip surfaces, groundwater conditions and shear strength of the soil materials. Although the soil cut slopes are designed to the same factor of safety (FOS) derived from deterministic analysis, the reliability in terms of the probability of failure may vary significantly.Hence the mere demonstration of an adequate FOS carries with it no guarantee that the probability of failure is adequately low. It was necessary to improve the design of soil cut slopes that would give greater reliability and robustness for the same FOS.

    Soil nailing, which comprises high yield steel reinforcing bars installed into the ground by means of drilling and grouting, was introduced in Hong Kong in the mid-1980s. The process of soil nailing is not very susceptible to weather conditions and there is flexibility to position the soil nails to avoid existing trees. The technique is simple and versatile compared with other structural solutions, rendering it adaptable to the physical constraints commonly encountered in slope sites. In addition, because soil nails are usually installed at close spacing, they can reduce the vulnerability of the slope to undetected weak geological zones and unfavourable relict joints by binding the soil together to form an integral mass. That means the design of soil-nailed cut slopes is less sensitive to adverse ground conditions. Following documentation of the design approach and the construction practice by Watkins and Powell (1992), soil nailing has been accepted as a robust and economical engineering solution for improving the stability of soil cut slopes in Hong Kong. In order to improve the soil nailing technology and rationalize the design standards, a series of studies were conducted by the GEO in the early 2000s. This involved literature review, field tests, laboratory investigations, physical modelling,numerical modelling and analytical study (Figs. 11 and 12). The findings from these soil nails studies have led to the publication of a guide on soil nail design and construction (GEO, 2008). It enhances the technical know-how of local engineers in the technique.

    The use of soil nails in soil cut slopes has become increasingly popular. About 3400 and 2600 slopes have been upgraded using soil nails under the LPM Programme and EM Programme respectively up to 2010. Through theoretical studies and field observations, soil nailing is now recognized as a more robust and reliable scheme than cutting back in that the scheme is more resilient to local geological defects.

    Fig. 11. Numerical modelling of soil nails with different inclinations.

    (a) Set-up of a nailed-slope model in centrifuge test.

    Fig. 12. Centrifuge modelling of a soil-nailed slope.

    5.3. Retaining walls

    Most of the substandard retaining walls are old masonry walls constructed during the period from 1850 to 1950. A number of fatal landslide incidents involving masonry walls had occurred in the history of Hong Kong. In 1925, a masonry wall at Po Hing Fong on Hong Kong Island collapsed, demolishing seven houses and killing over 70 people. Most recently in 1994, the failure of a 100-year old masonry wall at Kwun Lung Lau claimed the lives of 5 persons (Fig. 6). These tragic incidents have highlighted the need for understanding the structure and behaviour of old masonry walls so that appropriate stabilization measures can be carried out to improve their stability.

    The assessment of stability of old masonry retaining walls is not simple because of their variable and non-monolithic construction.In order to tackle the problem, a comprehensive review on masonry retaining walls in Hong Kong, including the construction practice and structure of masonry walls, an examination of their structural behaviour, analyses of case histories of wall failures and suggestions on the approach to investigate stability of masonry walls, was carried out by Chan (1996). Further guidelines on the assessment of old masonry walls were given by GEO (2004) following a review of the lessons learnt from the Kwun Lung Lau landslide incident.

    A special feature found on many old masonry walls in Hong Kong is the presence of “wall trees”, which refer to trees growing from the open joints or crevices between stone blocks. These“wall trees” constitute an important landscape element in the community and should be preserved where at all possible in view of their special amenity value. A study on masonry walls with trees was carried out by Wong and Jim (2011). The study concluded that the roots of wall trees would not induce failure of masonry walls.They would occasionally cause displacement of masonry blocks at the wall crest but the roots would also strengthen the wall face by providing a form of mesh reinforcement. However, wall trees would affect the stability of masonry walls due to its surcharge effect and this should be considered in the stability assessment. The study also identified suitable methods of stabilizing old masonry walls. One of the methods is to use soil nailing, which has the bene fit of preserving both the existing wall trees and the original masonry facade (Fig. 13b). Other methods include the provision of conventional buttresses or flying buttresses in front of the masonry wall, and the construction of hand-dug caissons behind the wall.

    5.4. Rock cut slopes

    The stability of rock slopes is mainly controlled by the characteristics and orientations of discontinuities within the rock mass, as well as the groundwater conditions. Detailed engineering geological mapping is required for the investigation, design and construction of rock slope stabilization measures. Very often, the design of the necessary works can only be finalized during the construction stage when safe access for close inspection of the rock face has been made available and obscuring vegetation and surface covers have been removed. The common stabilization measures for use in rock cut slopes include scaling, buttresses, dentition, dowels and rock bolts, drainage provisions and mesh netting. The design and construction practice for upgrading existing rock cut slopes under the LPM Programme was described by Dubin et al. (1986).

    公司采用股份有限責(zé)任制,并根據(jù)公司發(fā)展特點(diǎn),初期采取直線制管理。后期根據(jù)公司發(fā)展?fàn)顩r進(jìn)行調(diào)整。公司所有權(quán)與經(jīng)營權(quán)分離,實(shí)行總經(jīng)理負(fù)責(zé)制。

    In the design of rock slope stabilization works, it is important to identify laterally persistent discontinuities such as sheeting joints which are conducive to large-scale rock slope failures. However,dislodgement of small rock blocks by way of rotation, sliding or ravelling may occur as a result of progressive deterioration and/or development of cleft water pressures within adversely oriented joints. Although the chance of direct impact by a small rock fall is not high, the consequence in the event of direct impact may be very serious given the nature of the material. Therefore, extreme care should be taken to ensure that minor but kinematically critical joints are not overlooked during the design process. Based on the key lessons learnt from studies of engineered rock cut slope failures and a review of the practice for the investigation and design of rock cut slopes, technical guidance on enhancement of rock slope engineering practice was promulgated by Yu et al.(2005).

    Fig. 13. Application of soil nailing technique in soil cut slopes and old masonry walls.

    6. Technical advancement in natural terrain mitigation works

    Natural terrain occupies an area of about 650 km2, which covers about 60% of the land area of Hong Kong. There is a high concentration of developments in Hong Kong mingled with man-made slopes and natural hillsides. The severe rainstorm of 7 June 2008 is a vivid reminder of the potential vulnerability of developments located close to natural terrain. To provide a dataset for planning of risk mitigation works, an inventory of hillside catchments with historical landslides that occurred close to existing buildings and important transport corridors has been compiled. The criteria are based on the proximity of the crown or toe of a landslide to an important facility. The inventory comprises about 2700 hillside catchments,scattered over different areas of Hong Kong (Fig. 8). A risk-based ranking system has been devised for establishing the priority of the 2700 hillside catchments for systematic follow-up action under the LPMit Programme.

    In Hong Kong, natural terrain hazards have been grouped into five main hazard types on the basis of the mechanism of transportation, the nature of displaced material and the topographic location. These include open hillside landslide, channelized debris flow, deep-seated failure, boulder fall and rock fall. A natural terrain hazard study is carried out to formulate the geological and geomorphological model for the hillside and evaluate the hazards involved.Three different approaches, namely FOS, QRA and design event,may be used either individually or in combination for evaluation of natural terrain hazards. In practice, the majority of natural terrain hazard assessments are carried out using the design event approach. The FOS approach is used only if it is pragmatic and cost-effective to stabilize the natural hillside. QRA, fairly involved and costly, is adopted if rigorous quantification of the landslide risk or cost-benefit analysis of alternative risk mitigation strategies is required for the natural terrain concerned. Regardless of the approach adopted, the large areal extent of the natural hillsides means that only limited ground investigation and testing can be carried out during the process of natural terrain hazard studies. Therefore, geological and geomorphological inputs based on site-specific observations should be provided to complement the investigation. Technical guidance on natural terrain hazard assessment is given by Ng et al. (2003).

    In the management of natural terrain risk under the LPMit Programme, the preferred approach is not to carry out extensive stabilization works to large areas of the natural hillside, which is impractical and environmentally damaging, but to mitigate the risk through the provision of defense measures to contain the landslide debris from the natural hillside above. In most cases, the defense measures adopted in Hong Kong consist of the provision of a concrete barrier at the toe of the natural hillside (Fig. 14). A review of the local and international natural terrain landslide risk mitigation strategy and practice was carried out by Shum and Lam (2011).As part of the review, a number of established techniques not commonly used in Hong Kong have also been examined. Some of these techniques including flexible debris-resisting barriers, transport channels and debris-straining structures would have potential applications to certain natural terrain landslide problems in Hong Kong.

    Fig. 14. Concrete barrier at the toe of a natural hillside.

    6.1. Debris mobility modelling

    One of the important factors affecting the design of defense works is debris mobility. This requires the use of dynamic analysis to assess the probable distance of debris runout and debris velocity of natural terrain landslides, based on continuum models which have been calibrated against field observations. These continuum models utilize the principles of conservation of mass,momentum and energy to describe the dynamic motion of landslide debris and incorporate a rheological model to represent the flow behaviour of the landslide debris. The findings of a study of the mobility of natural terrain landslides in Hong Kong by Ayotte and Hungr (1998) concluded that the frictional rheology and Voellmy rheology can be used to estimate the mobility of open hillside landslides and channelized debris flows (CDFs),respectively. A set of conservative material parameters for debris mobility analysis in Hong Kong, including the apparent friction angle for the frictional rheology and the apparent friction angle and turbulence coefficient for Voellmy rheology were recommended.

    However, the natural terrain landslides triggered by the 7 June 2008 rainstorm have provided plenty of additional information and data on debris movement. Back-analysis of selected CDF triggered by the 7 June 2008 rainstorm carried out by GEO showed that about 1% of the CDFs were more mobile than that predicted using the Voellmy parameters recommended by Ayotte and Hungr (1998).Based on findings of the back-analysis, supplementary guidelines on the assessment of mobility of CDFs are promulgated by GEO(2011).

    The GEO has developed its own two-dimensional (2D) dynamic modelling algorithm, based on a formulation and solution methodology similar to that adopted in the DAN model formulated by Hungr (1995). The GEO has also developed a three-dimensional(3D) landslide runout simulation model based on the Particle-in-Cell technique (Kwan and Sun, 2007). Both modelling algorithms have been used to back analyze CDFs and open hillslope failures(OHF) in Hong Kong. The development of 2D and 3D numerical modelling of debris movement has greatly enhanced the capability of assessing debris influence zones and design of the corresponding risk mitigation works.

    A benchmarking exercise on landslide debris mobility modelling was held in December 2007 in Hong Kong during the International Forum on Landslide Disaster Management (Hungr et al., 2007). It was participated by 13 groups of researchers and practitioners from different regions of the world including the GEO. A range of numerical models were used by the participants to complete the mobility analysis of selected benchmark cases. The outcome of this benchmarking exercise showed that the simulation results obtained by GEO’s 3D landslide runout simulation model were reasonably accurate compared with the corresponding analytical solutions, laboratory measurements and field observations. The results were also consistent with those determined from other numerical models by other participants,which would mean that the debris mobility modelling capability in Hong Kong is comparable to that in other technical leaders.

    6.2. Flexible debris-resisting barriers

    Flexible barriers, which are mainly formed of steel ring nets mounted between horizontal steel ropes spanning between steel posts and anchored into the ground, are one of the techniques that can be used to mitigate natural terrain landslides (Fig. 15a). The advantages of flexible barriers are that they are relatively easy to install on steep natural terrain, less visually obtrusive and have less environmental impact compared with reinforced concrete barriers.Whilst flexible barriers have been in use for over twenty years as a protective measure against boulder falls and rock falls, the application of flexible barriers for resisting the impact of natural terrain landslide debris is a relatively new concept.

    The design methodology for flexible rock fall barriers is based on an energy approach whereby a falling rock or boulder is stopped in one go by the barrier designed to absorb the kinetic energy carried by the rock or boulder. The design usually entails the use of proprietary flexible barrier systems with specific energy absorbing capacities that are verified by full scale field testing in accordance with the relevant national or international standards. The technology involved is relatively mature. In contrast to a rock fall, the impact of landslide debris hitting a flexible barrier is delivered as consecutive pulses due to the compressibility and mobility of the debris. Therefore, the design methodology for rock fall barriers is not applicable to the design of flexible barriers as a debris resisting structure. So far, there are no national or international standards for the design of flexible debris-resisting barriers. Suggestions on the design approaches for flexible debris-resisting barriers were prepared by Kwan and Cheung (2012) based on a review of the present state of knowledge, which would serve as a useful reference for the relevant practitioners. Fig. 15b shows the establishment of a numerical model for a flexible debris-resisting barrier using a commercial software LS-DYNA in conjunction with the suggested force design approach.

    Fig. 15. Flexible debris-resisting barrier.

    6.3. Managing public expectation

    Natural terrain mitigation works differ from slope upgrading works in that they would not stop the occurrence of landslides on the natural hillsides. Instead, they would only reduce the consequence of landslides. Muddy water and some debris could sometimes spill over to the roads and buildings they protect, which may still have to be closed temporarily for safety against risks remaining from the landslide scars. Furthermore, because of the variable nature of the natural terrain and the limitations in the current technology, the mitigation measures, which will contribute to reducing the consequence, may be overwhelmed under very severe or extreme rainstorms. Therefore, it is necessary to manage public expectation through public education so that the people of Hong Kong can be prepared for such situation.

    Fig. 16. Guidelines for planting on slopes.

    7. Landscaping to slopes

    It is government policy to make slopes look as natural as possible, blending them with their surroundings and minimizing their visual impact on the built environment. To pursue this policy, vegetation is used as slope surface cover in the upgrading of existing man-made slopes which are not steeper than 55°(Fig. 16). A hard surface cover such as chunam or shotcrete may be used for steeper slopes, but suitable landscape measures such as applying subdued colour, masonry facing and providing planter holes on the slope surface for screen planting are taken to minimize the visual impact(Fig. 17).

    For natural terrain mitigation works, the extent of mitigation works is minimized as far as practicable to reduce disturbance to the hillside and the environment. The existing vegetation, including trees and shrubs, is also preserved whereas possible during the construction of landslide risk mitigation measures. Landscape treatments such as vertical greening, screen planting and toe planters (Fig. 18) would be provided to minimize the visual impact of the mitigation works and blend them with their surrounding environment.

    Fig. 17. Landscaping to man-made slope with hard cover.

    In 2000, the GEO produced a set of technical guidelines on landscape treatment and bioengineering for man-made slopes and retaining walls (GEO, 2000b). A review of the technical guidelines was carried out in 2010 with a view to promulgating the latest best practice and expanding the scope to include landscape treatments for natural terrain mitigation works and landslide repairs.The review has culminated in the new GEO Publication No. 1/2011“Technical Guidelines on Landscape Treatment on Slopes” (GEO,

    2011).

    Fig. 18. Landscaping to natural terrain mitigation measures.

    Apart from slope appearance, we are mindful of the ecological impact of slope works. The GEO has put in effort to achieve ecological enhancement of slope works by using native species. A good example is the adoption of ecological planting in upgrading 24 man-made slopes along South Lantau Road between 2001 and 2004 (Fig. 19). Native species, either planted alone or when mixed with exotic species, would attract local wildlife including birds and insects which may act as seed dispersers to enrich the plant biodiversity. A bio-diversified vegetation cover is ecologically stable and hence more sustainable. Good practice on ecological planting for man-made slopes and engineering works for natural terrains with native species is given in GEO Publication No. 1/2011 (GEO,

    2011).

    Fig. 19. A success example to landscape the slopes along South Lantau Road.

    As part of the continuous improvement in landscape treatment of slopes, the GEO has been researching into the use of vegetation in slope works and experimenting with new techniques of providing erosion control measures and vegetation covers to steep slopes, with due regard to safety, cost, aesthetic quality, and longterm maintenance requirements. Since 2002, the GEO has set up a database called “Greening Methods on Slopes” to co-ordinate updates of the information on the different new greening techniques that have been tried on Government slopes. Studies have been undertaken to assess the performance of different greening techniques and to identify vegetation species that can successfully establish and self-sustain on steep slopes. In collaboration with the Kadoorie Farm and Botanic Garden, the GEO has carried out a planting trial of native small tree and shrub species on steep slopes.The results of the studies and the planting trial provide useful information for further research into the establishment of robust,cost-effective, and eco-friendly vegetation covers on man-made slopes. Further studies on the application of various vegetation species for greening of man-made slopes were completed in 2007 and 2011, respectively, which have expanded the range of suitable vegetation species for landscape use on man-made slopes.

    8. Conclusions

    Hong Kong is unique in the world in terms of its combination of high seasonal rainfall and close proximity of dense urban development to steep terrain. As a result, landslides are one of the common natural hazards in Hong Kong. Some of the past landslides had caused widespread damage and many casualties, together with significant economic losses and social disruption. Through sustained efforts to prevent landslide disasters by means of slope engineering works over the past 35 years, the overall landslide risk posed to the community of Hong Kong has been substantially reduced. This is corroborated by the declining trend of landslide fatality rate since 1977.

    Under the current LPMit Programme, about half of the funding resources will be allocated to natural terrain risk mitigation works.The philosophy and technology for dealing with man-made slope features and natural terrain landslide hazards differ significantly.The limited size of man-made slopes permits a level of ground investigation and testing sufficient for deterministic analysis and design. The technology is relatively well established. In contrast,natural terrain hazards studies require plenty of geological and geomorphological analyses with limited ground investigation and testing. The objective of mitigation works is to divert or contain landslide debris instead of preventing failure, which involves evaluation of debris movement down the slope and its interaction with the mitigation measures. The technology is still evolving. Further development work is being carried out in order to enhance the reliability, cost-effectiveness and buildability of natural terrain mitigation measures.

    Apart from keeping the slopes safe, it is necessary to make them look as natural as possible in order to create a safer and better living environment for the people of Hong Kong. Landscape design is treated as an essential part of the design of upgrading works for man-made slopes and natural terrain hazard mitigation works.Input by professional landscape architects is provided at the early stage of the design process to ensure that landscaping input is integrated with geotechnical input. Where appropriate, native species are used in the landscaping works in order to create a visually acceptable and ecological sustainable slope environment.

    Sustained development in Hong Kong requires continued vigilance and perennial attention in respect of landslide risk management. Notwithstanding this, absolute slope safety is not practical or achievable due to many uncertainties inherent in the variables including geological settings, properties of soil and rock,rainfall pattern and groundwater conditions. Hence, it is necessary to promote an accurate understanding of the nature of landslip danger in Hong Kong in order to enable the public to develop a realistic expectation for slope safety. This would reduce the likelihood of public over-reaction in future landslips and maintain community’s support and trust in the implementation of the landslip prevention and mitigation works.

    Acknowledgements

    This paper is published with the permission of the Head of the Geotechnical Engineering Office and the Director of Civil Engineering and Development, Government of the Hong Kong Special Administrative Region.

    Ayotte D, Hungr O. Runout analysis of debris flows and avalanches in Hong Kong.Hong Kong: Geotechnical Engineering Office, HKSAR Government; 1998.

    CEDD. When hillside collapse: a century of landslides in Hong Kong. Hong Kong:Civil Engineering and Development Department, HKSAR Government; 2005.

    Chan YC. Study of old masonry retaining walls in Hong Kong (GEO Report No. 31).Hong Kong: Geotechnical Engineering Office, HKSAR Government; 1996.

    Cheng PFK. Assessment of landslide risk posed by man-made slopes as of 2010 (Special Project Report No. SPR 1/2011). Geotechnical Engineering Office, HKSAR Government: Hong Kong; 2011.

    Cheung WM, Shiu YK. Assessment of global landslide risk posed by pre-1978 manmade slope features: risk reduction from 1977 to 2000 achieved by the LPM Programme (GEO Report No. 125). Hong Kong: Geotechnical Engineering Office,HKSAR Government; 2000.

    Dubin BI, Watkins AT, Chang DCH. Stabilisation of existing rock faces in urban areas of Hong Kong. In: Proceedings of the conference on rock engineering and excavation in an urban environment. Hong Kong: The Hong Kong Institution of Engineers; 1986. p. 155-71.

    FMSWJV. Report on the debris flow at Sham Tseng San Tsuen of 23 August 1999(GEO Report No. 181). Fugro Maunsell Scott Wilson Joint Venture. Hong Kong:Geotechnical Engineering Office. HKSAR Government; 2005.

    GEO. Guidelines for assessment of old masonry retaining walls in geotechnical studies and for action to be taken on private walls (GEO circular no. 33). Hong Kong:Geotechnical Engineering Office, HKSAR Government; 2004.

    GEO. Guide to soil nail design and construction (Geoguide 7). Hong Kong: Geotechnical Engineering Office, HKSAR Government; 2008.

    GEO. Report on the Kwun Lung Lau landslide of 21 July 1994 (GEO Report No.103). Hong Kong: N.R. Morgenstern & Geotechnical Engineering Office, HKSAR Government; 2000a.

    GEO. Technical guidelines on landscape treatment and bio-engineering for manmade slopes and retaining walls (GEO Publication No. 1/2000). Hong Kong:Geotechnical Engineering Office, HKSAR Government; 2000b.

    GEO. Technical guidelines on landscape treatment for slopes (GEO Publication No.1/2011). Hong Kong: Geotechnical Engineering Office, HKSAR Government;2011.

    HKG. Report on the slope failures at Sau Mau Ping. Hong Kong: Government of Hong Kong; 1977.

    HKIE. Soil nails in loose fill slopes (a preliminary study) - final report. Hong Kong:Geotechnical Division, The Hong Kong Institution of Engineers; 2003.

    Ho KKS, Sun HW, Hui THH. Enhancing the reliability and robustness of engineered slopes (GEO Report No. 139). Hong Kong: Geotechnical Engineering Office,HKSAR Government; 2002.

    Hungr O. A model for the runout analysis of rapid flow slides: debris flows and avalanches. Canadian Geotechnical Journal 1995;32(4):610-23.

    Hungr O, Morgenstern NR, Wong HN. Review of benchmarking exercise on landslide debris runout and mobility modeling. In: Proceedings of the 2007 international forum on landslide disaster management. Hong Kong: The Hong Kong Institution of Engineers; 2007. p. 755-812.

    Koirala NP, Tang KY. Design of landslip preventive works for cut slopes in Hong Kong.In: Proceedings of the fifth international symposium on landslides. Lausanne,Switzerland: A.A. Balkema; 1988. p. 933-8.

    Kwan JSH, Sun HW. Benchmarking exercise on landslide mobility modeling-runout analyses using 3dDMM. In: Proceedings of the 2007 international forum on landslide disaster management. Hong Kong: The Hong Kong Institution of Engineers;2007. p. 945-66.

    Kwan JSH, Cheung RWM. Suggestions on design approaches for flexible debrisresisting barriers (GEO Discussion Note 1/2012). In: Hong Kong: Geotechnical Engineering Office. HKSAR Government; 2012.

    Malone AW. The reliability of the design of cuttings in Hong Kong (GCO Discussion Note 5/85). In: Hong Kong: Geotechnical Engineering Office. HKSAR Government; 1985.

    MFJV. Final report on the compilation of the enhanced natural terrain landslide inventory. Hong Kong: Maunsell Fugro Joint Venture. HKSAR Government:Geotechnical Engineering Office; 2007.

    Ng KC, Parry S, King JP, Franks CAM, Shaw R. Guidelines for natural terrain hazard studies (GEO Report No. 138). Hong Kong: Geotechnical Engineering Office,HKSAR Government; 2003.

    Powell GE, Tang KW, Au-Yeung YS. The use of large diameter piles in landslip prevention in Hong Kong. In: Proceedings of the tenth Southeast Asian geotechnical conference; 1990. p. 197-202.

    Shum LKW, Lam AYT. Review of natural terrain landslide risk management practice and mitigation measures (GEO technical note 3/2011). Hong Kong: Geotechnical Engineering Office, HKSAR Government; 2011.

    Watkins AT, Powell GE. Soil nailing to existing slopes as landslip preventive works.Hong Kong: Hong Kong Engineer; 1992. p. 20-7.

    Wong CM, Jim CY. Study on masonry walls with trees (GEO Report No. 257). Hong Kong: Geotechnical Engineering Office, HKSAR Government; 2011.

    Wong HN. Landslide risk assessment for individual facilities. In: Proceedings of international conference on landslide risk management. Vancouver, Canada: Taylor& Francis Ltd.; 2005. p. 237-96.

    猜你喜歡
    負(fù)責(zé)制責(zé)任制總經(jīng)理
    黨建責(zé)任制要算好“兩本賬”——優(yōu)化國有企業(yè)黨建工作責(zé)任制考核體系研究
    糧食安全省長責(zé)任制順利“首考”
    用心做好產(chǎn)品 專訪Primare總經(jīng)理Slemen Algra先生
    向更前奔跑 向更廣尋找——訪Materialise公司中國區(qū)總經(jīng)理Kim Francois女士
    你會選哪個(gè)經(jīng)銷商
    DMG娛樂營銷總經(jīng)理徐衛(wèi)兵赴CIPRA演講
    主審法官責(zé)任制論析
    高?;鶎訉W(xué)院黨政共同負(fù)責(zé)制初探
    司法改革中合議庭負(fù)責(zé)制——走出“形合實(shí)獨(dú)”的困境
    讓主診醫(yī)師負(fù)責(zé)制健康運(yùn)作
    婷婷色综合www| 日本爱情动作片www.在线观看| 久久人人爽人人爽人人片va| 久久午夜福利片| 一本大道久久a久久精品| 又黄又粗又硬又大视频| 亚洲欧美清纯卡通| 午夜免费观看性视频| 18禁观看日本| 久久精品久久久久久久性| 夜夜骑夜夜射夜夜干| 亚洲国产精品一区三区| 国产日韩一区二区三区精品不卡| 视频中文字幕在线观看| 亚洲欧洲精品一区二区精品久久久 | av有码第一页| 欧美最新免费一区二区三区| 免费av不卡在线播放| 人体艺术视频欧美日本| 亚洲伊人久久精品综合| 午夜91福利影院| 久热久热在线精品观看| 国产成人精品福利久久| 一区在线观看完整版| 国产视频首页在线观看| 麻豆乱淫一区二区| 尾随美女入室| 久久久久久久久久久久大奶| 丰满乱子伦码专区| 国产日韩欧美视频二区| 亚洲性久久影院| 欧美xxⅹ黑人| 国产男人的电影天堂91| 国产 精品1| 在线观看一区二区三区激情| 亚洲成人av在线免费| 欧美日韩视频精品一区| 国产成人91sexporn| 国产午夜精品一二区理论片| 成年人免费黄色播放视频| 亚洲激情五月婷婷啪啪| 91国产中文字幕| 日韩不卡一区二区三区视频在线| 一本—道久久a久久精品蜜桃钙片| 国产亚洲午夜精品一区二区久久| 久久综合国产亚洲精品| 久久国产亚洲av麻豆专区| 天美传媒精品一区二区| 天美传媒精品一区二区| 91在线精品国自产拍蜜月| 国产成人a∨麻豆精品| 在线观看三级黄色| 国国产精品蜜臀av免费| 亚洲综合色网址| 99香蕉大伊视频| 2022亚洲国产成人精品| 在线看a的网站| 一级片免费观看大全| 国产福利在线免费观看视频| 制服丝袜香蕉在线| 天天躁夜夜躁狠狠久久av| 婷婷色麻豆天堂久久| 亚洲激情五月婷婷啪啪| 少妇人妻 视频| 日韩三级伦理在线观看| 国产成人免费观看mmmm| 夫妻午夜视频| 看免费av毛片| 久久午夜综合久久蜜桃| 国产精品久久久久久av不卡| 大片免费播放器 马上看| 人妻少妇偷人精品九色| 999精品在线视频| 欧美97在线视频| 欧美老熟妇乱子伦牲交| av天堂久久9| 亚洲,一卡二卡三卡| 国产免费一区二区三区四区乱码| av女优亚洲男人天堂| 好男人视频免费观看在线| 精品久久国产蜜桃| av又黄又爽大尺度在线免费看| 多毛熟女@视频| 看非洲黑人一级黄片| 中国三级夫妇交换| 91久久精品国产一区二区三区| 国产欧美另类精品又又久久亚洲欧美| 欧美少妇被猛烈插入视频| 一边亲一边摸免费视频| 91久久精品国产一区二区三区| 国产成人免费无遮挡视频| 久久精品国产综合久久久 | 久久婷婷青草| 熟女av电影| 女人久久www免费人成看片| 一区二区三区精品91| 亚洲欧洲国产日韩| 午夜免费鲁丝| 天天躁夜夜躁狠狠躁躁| 亚洲成人av在线免费| 最新中文字幕久久久久| 成人漫画全彩无遮挡| 建设人人有责人人尽责人人享有的| 蜜桃在线观看..| 超色免费av| 中国国产av一级| 久久99热6这里只有精品| 少妇的逼水好多| 日韩av在线免费看完整版不卡| 夫妻午夜视频| 欧美日韩亚洲高清精品| 黑丝袜美女国产一区| 美女国产视频在线观看| 水蜜桃什么品种好| 岛国毛片在线播放| 国产精品人妻久久久影院| 日本欧美国产在线视频| 人妻 亚洲 视频| 亚洲一区二区三区欧美精品| 国产日韩一区二区三区精品不卡| 欧美成人午夜免费资源| 日本黄大片高清| 免费久久久久久久精品成人欧美视频 | 97在线人人人人妻| 一级,二级,三级黄色视频| 黑人猛操日本美女一级片| 少妇人妻精品综合一区二区| 十八禁网站网址无遮挡| 亚洲国产av影院在线观看| 亚洲国产最新在线播放| 人妻 亚洲 视频| 亚洲精品自拍成人| 欧美日韩视频高清一区二区三区二| 亚洲美女搞黄在线观看| 人体艺术视频欧美日本| 国产精品欧美亚洲77777| 麻豆精品久久久久久蜜桃| 国产探花极品一区二区| 黑人高潮一二区| 国产成人aa在线观看| 国产毛片在线视频| 少妇人妻久久综合中文| 午夜激情av网站| 亚洲精品一二三| 亚洲精品乱码久久久久久按摩| 成人18禁高潮啪啪吃奶动态图| 婷婷成人精品国产| 中文字幕人妻丝袜制服| 一级片'在线观看视频| 少妇人妻精品综合一区二区| 成人亚洲精品一区在线观看| 午夜久久久在线观看| 99热6这里只有精品| 欧美激情国产日韩精品一区| 精品国产一区二区久久| 熟女人妻精品中文字幕| 国产成人精品福利久久| 国产精品三级大全| 日韩制服丝袜自拍偷拍| 欧美精品一区二区大全| 欧美日韩视频高清一区二区三区二| 熟妇人妻不卡中文字幕| 国产永久视频网站| 久久人人爽av亚洲精品天堂| 丝袜喷水一区| 国产精品成人在线| 国产在视频线精品| 高清视频免费观看一区二区| 亚洲精品乱久久久久久| 亚洲成人一二三区av| 久久精品人人爽人人爽视色| 欧美另类一区| 亚洲美女搞黄在线观看| freevideosex欧美| 国产深夜福利视频在线观看| 伊人亚洲综合成人网| 免费大片18禁| 亚洲国产毛片av蜜桃av| 如日韩欧美国产精品一区二区三区| 国产免费视频播放在线视频| 另类亚洲欧美激情| 99久久中文字幕三级久久日本| 日韩 亚洲 欧美在线| 久久精品国产亚洲av涩爱| 少妇人妻久久综合中文| 久久精品久久久久久久性| 人人妻人人澡人人爽人人夜夜| 在线观看三级黄色| 飞空精品影院首页| 亚洲精品aⅴ在线观看| 国产亚洲最大av| 丝袜在线中文字幕| 亚洲av欧美aⅴ国产| 黄色怎么调成土黄色| 国产在线一区二区三区精| 亚洲成色77777| 777米奇影视久久| 欧美成人午夜精品| 亚洲成色77777| 午夜激情久久久久久久| 女人被躁到高潮嗷嗷叫费观| 午夜福利在线观看免费完整高清在| 激情五月婷婷亚洲| 乱码一卡2卡4卡精品| 久久久久久久久久久久大奶| av卡一久久| 日韩一区二区视频免费看| 免费高清在线观看视频在线观看| 成人无遮挡网站| 一级爰片在线观看| 久久99蜜桃精品久久| av卡一久久| 日韩欧美一区视频在线观看| 日本色播在线视频| 亚洲欧美中文字幕日韩二区| 九草在线视频观看| www.熟女人妻精品国产 | 中国三级夫妇交换| 如何舔出高潮| 美女大奶头黄色视频| 啦啦啦视频在线资源免费观看| 国产淫语在线视频| 99久久中文字幕三级久久日本| 建设人人有责人人尽责人人享有的| 插逼视频在线观看| 久久97久久精品| 在线观看免费视频网站a站| 日本午夜av视频| 国产片特级美女逼逼视频| 亚洲中文av在线| 成人国产麻豆网| 国产成人免费无遮挡视频| 美女中出高潮动态图| 插逼视频在线观看| 欧美精品av麻豆av| 国产成人精品一,二区| 在线观看免费日韩欧美大片| 老熟妇乱子伦视频在线观看| 99国产综合亚洲精品| 精品第一国产精品| 色在线成人网| 中文字幕人妻熟女乱码| 欧美日韩瑟瑟在线播放| 亚洲中文av在线| 自拍欧美九色日韩亚洲蝌蚪91| 国产亚洲精品久久久久久毛片 | 亚洲午夜精品一区,二区,三区| 亚洲熟妇中文字幕五十中出 | 国产在视频线精品| 国产欧美日韩精品亚洲av| 大码成人一级视频| av线在线观看网站| 99riav亚洲国产免费| 亚洲成人手机| 亚洲第一青青草原| 欧美日韩亚洲国产一区二区在线观看 | 亚洲片人在线观看| 操美女的视频在线观看| 国产精品久久久久久精品古装| 51午夜福利影视在线观看| 看片在线看免费视频| av视频免费观看在线观看| x7x7x7水蜜桃| 国产高清视频在线播放一区| 人成视频在线观看免费观看| 中文字幕精品免费在线观看视频| 90打野战视频偷拍视频| 99精品在免费线老司机午夜| 亚洲av美国av| 在线播放国产精品三级| 久久精品熟女亚洲av麻豆精品| bbb黄色大片| 激情在线观看视频在线高清 | 亚洲自偷自拍图片 自拍| 久久精品熟女亚洲av麻豆精品| 久久精品国产亚洲av高清一级| 欧美黑人精品巨大| 中文字幕另类日韩欧美亚洲嫩草| 亚洲免费av在线视频| 真人做人爱边吃奶动态| 午夜两性在线视频| 欧美午夜高清在线| 一进一出抽搐动态| www日本在线高清视频| 亚洲av美国av| 国产国语露脸激情在线看| 老司机亚洲免费影院| 1024香蕉在线观看| 在线观看午夜福利视频| 精品少妇久久久久久888优播| 伊人久久大香线蕉亚洲五| 免费观看人在逋| svipshipincom国产片| 国产精品99久久99久久久不卡| 国产av一区二区精品久久| 男人的好看免费观看在线视频 | 精品一区二区三区四区五区乱码| 两性午夜刺激爽爽歪歪视频在线观看 | 久久热在线av| 国产高清视频在线播放一区| 国产精品一区二区在线观看99| 亚洲欧美激情综合另类| 又黄又爽又免费观看的视频| 精品人妻在线不人妻| 成人手机av| 在线国产一区二区在线| 啦啦啦免费观看视频1| 一级,二级,三级黄色视频| 黄色怎么调成土黄色| 人人妻,人人澡人人爽秒播| 日韩视频一区二区在线观看| 大片电影免费在线观看免费| 亚洲专区国产一区二区| www.999成人在线观看| 午夜老司机福利片| 色老头精品视频在线观看| 免费在线观看完整版高清| 亚洲熟女毛片儿| 国产欧美亚洲国产| 18禁美女被吸乳视频| 少妇的丰满在线观看| 亚洲精品一卡2卡三卡4卡5卡| 日本黄色日本黄色录像| 欧美黄色淫秽网站| 欧美日韩av久久| avwww免费| av福利片在线| 国产乱人伦免费视频| 国产一卡二卡三卡精品| 别揉我奶头~嗯~啊~动态视频| 热99国产精品久久久久久7| 一区福利在线观看| 欧美乱妇无乱码| 国产成人精品久久二区二区免费| 国产男靠女视频免费网站| 亚洲国产欧美一区二区综合| xxxhd国产人妻xxx| 国产又爽黄色视频| 精品福利永久在线观看| 国产日韩一区二区三区精品不卡| 新久久久久国产一级毛片| 视频在线观看一区二区三区| 成人精品一区二区免费| 午夜福利欧美成人| 国产色视频综合| 美女福利国产在线| 热99久久久久精品小说推荐| 很黄的视频免费| 美女国产高潮福利片在线看| 久久久久久久国产电影| 国产精品久久视频播放| 亚洲av成人一区二区三| av欧美777| 久久久国产成人免费| 又黄又爽又免费观看的视频| 岛国毛片在线播放| 亚洲综合色网址| 国产高清视频在线播放一区| 人成视频在线观看免费观看| 久久青草综合色| 在线观看免费视频网站a站| 视频区图区小说| 黄色成人免费大全| 午夜福利在线免费观看网站| 熟女少妇亚洲综合色aaa.| 午夜激情av网站| 1024香蕉在线观看| 首页视频小说图片口味搜索| 亚洲欧美日韩另类电影网站| 大陆偷拍与自拍| xxx96com| 黑人巨大精品欧美一区二区蜜桃| 国产成人精品无人区| e午夜精品久久久久久久| 免费人成视频x8x8入口观看| 黄色丝袜av网址大全| 999久久久国产精品视频| 啪啪无遮挡十八禁网站| 黑人欧美特级aaaaaa片| 无遮挡黄片免费观看| 日韩人妻精品一区2区三区| 亚洲av片天天在线观看| 别揉我奶头~嗯~啊~动态视频| 91精品国产国语对白视频| 免费少妇av软件| 中国美女看黄片| 亚洲在线自拍视频| 美女视频免费永久观看网站| 99精国产麻豆久久婷婷| 国产男女内射视频| 欧美成人午夜精品| 午夜免费成人在线视频| 黄片大片在线免费观看| 超碰成人久久| 国产精品九九99| 高清毛片免费观看视频网站 | 一级,二级,三级黄色视频| 亚洲avbb在线观看| 成人av一区二区三区在线看| av超薄肉色丝袜交足视频| 高清欧美精品videossex| 天天添夜夜摸| 日日摸夜夜添夜夜添小说| 亚洲熟妇熟女久久| 看免费av毛片| 国产一区二区激情短视频| 窝窝影院91人妻| 亚洲成av片中文字幕在线观看| 两个人看的免费小视频| 1024香蕉在线观看| 黄片播放在线免费| 99国产精品免费福利视频| 淫妇啪啪啪对白视频| 亚洲男人天堂网一区| 精品第一国产精品| 亚洲熟妇中文字幕五十中出 | 999久久久精品免费观看国产| 国产成人影院久久av| 少妇 在线观看| 久久精品91无色码中文字幕| 亚洲va日本ⅴa欧美va伊人久久| 少妇裸体淫交视频免费看高清 | 婷婷成人精品国产| 日本一区二区免费在线视频| 天天躁狠狠躁夜夜躁狠狠躁| 一级片'在线观看视频| 一区二区日韩欧美中文字幕| 美女 人体艺术 gogo| 黄色成人免费大全| 黄色视频,在线免费观看| 亚洲精品自拍成人| 欧美色视频一区免费| 成人三级做爰电影| 欧美精品亚洲一区二区| 午夜福利,免费看| √禁漫天堂资源中文www| 亚洲国产欧美日韩在线播放| av网站免费在线观看视频| 99久久99久久久精品蜜桃| 99re6热这里在线精品视频| 777米奇影视久久| 伊人久久大香线蕉亚洲五| 中文欧美无线码| 国产精品1区2区在线观看. | 18在线观看网站| 欧美性长视频在线观看| 女性生殖器流出的白浆| 国产片内射在线| 亚洲欧美色中文字幕在线| 国产精品秋霞免费鲁丝片| 999久久久精品免费观看国产| 最近最新免费中文字幕在线| 欧美乱码精品一区二区三区| 成年人免费黄色播放视频| 国产高清国产精品国产三级| 美女午夜性视频免费| 国产极品粉嫩免费观看在线| 亚洲中文字幕日韩| 亚洲精品国产区一区二| 亚洲九九香蕉| 18禁美女被吸乳视频| 国精品久久久久久国模美| 国产又爽黄色视频| 91国产中文字幕| 97人妻天天添夜夜摸| 久久精品国产亚洲av高清一级| 91精品国产国语对白视频| 亚洲精品一二三| 成人18禁在线播放| 天天躁狠狠躁夜夜躁狠狠躁| 在线观看免费午夜福利视频| 97人妻天天添夜夜摸| videosex国产| 丰满迷人的少妇在线观看| 国产不卡一卡二| 性少妇av在线| 精品福利观看| 国产有黄有色有爽视频| 国产激情欧美一区二区| 1024香蕉在线观看| 美女 人体艺术 gogo| 天堂俺去俺来也www色官网| 亚洲av熟女| 黑人操中国人逼视频| 美女高潮喷水抽搐中文字幕| 久久精品国产99精品国产亚洲性色 | 欧美性长视频在线观看| 久久精品国产清高在天天线| 亚洲综合色网址| 国产精品综合久久久久久久免费 | 岛国在线观看网站| 欧美午夜高清在线| 国产精品久久电影中文字幕 | cao死你这个sao货| 又黄又粗又硬又大视频| 精品久久久久久久毛片微露脸| 咕卡用的链子| 视频在线观看一区二区三区| 嫩草影视91久久| 美女扒开内裤让男人捅视频| 啦啦啦 在线观看视频| 老司机深夜福利视频在线观看| 国产成人影院久久av| 韩国精品一区二区三区| 欧美国产精品一级二级三级| 女性生殖器流出的白浆| 97人妻天天添夜夜摸| 欧美日韩福利视频一区二区| 欧美在线黄色| 免费在线观看日本一区| 满18在线观看网站| 女人被躁到高潮嗷嗷叫费观| 一级片'在线观看视频| 十八禁网站免费在线| 国产免费男女视频| 一边摸一边抽搐一进一小说 | www.精华液| 国产午夜精品久久久久久| 咕卡用的链子| 大香蕉久久成人网| 波多野结衣av一区二区av| xxx96com| 国产伦人伦偷精品视频| 欧美精品亚洲一区二区| 美女 人体艺术 gogo| 久久久精品免费免费高清| 久久国产亚洲av麻豆专区| 人成视频在线观看免费观看| 午夜精品国产一区二区电影| 国产精品免费大片| 国产欧美亚洲国产| 欧美日韩精品网址| 国产精品美女特级片免费视频播放器 | 欧美国产精品一级二级三级| 精品乱码久久久久久99久播| 99精品在免费线老司机午夜| 精品国产美女av久久久久小说| 亚洲av日韩在线播放| 人人妻人人添人人爽欧美一区卜| 国产一卡二卡三卡精品| 最近最新中文字幕大全电影3 | 久久亚洲精品不卡| 欧美大码av| 亚洲成av片中文字幕在线观看| 我的亚洲天堂| 久久久久精品人妻al黑| 啦啦啦在线免费观看视频4| 在线天堂中文资源库| 久久国产亚洲av麻豆专区| 一个人免费在线观看的高清视频| 精品久久久精品久久久| 中文字幕另类日韩欧美亚洲嫩草| 热99国产精品久久久久久7| 夜夜爽天天搞| 国产亚洲精品久久久久久毛片 | 天堂俺去俺来也www色官网| 成人黄色视频免费在线看| 久久人人97超碰香蕉20202| 免费不卡黄色视频| 欧美av亚洲av综合av国产av| 人妻久久中文字幕网| av视频免费观看在线观看| 淫妇啪啪啪对白视频| 日韩熟女老妇一区二区性免费视频| 久久精品国产综合久久久| 99精国产麻豆久久婷婷| 欧美乱色亚洲激情| 国产成人精品久久二区二区91| 午夜成年电影在线免费观看| 啦啦啦免费观看视频1| av片东京热男人的天堂| 在线国产一区二区在线| 90打野战视频偷拍视频| 99国产精品一区二区三区| tocl精华| 亚洲伊人色综图| 欧洲精品卡2卡3卡4卡5卡区| 人妻 亚洲 视频| 久久影院123| 精品久久久精品久久久| tube8黄色片| 久久香蕉激情| 下体分泌物呈黄色| 中亚洲国语对白在线视频| 亚洲 欧美一区二区三区| 91成年电影在线观看| 一本综合久久免费| 91精品三级在线观看| 少妇猛男粗大的猛烈进出视频| 午夜影院日韩av| 18禁黄网站禁片午夜丰满| 搡老岳熟女国产| 男女高潮啪啪啪动态图| 波多野结衣av一区二区av| 91精品三级在线观看| 欧美大码av| 女人被躁到高潮嗷嗷叫费观| 欧美黄色淫秽网站| 黄色女人牲交| 丰满迷人的少妇在线观看| av视频免费观看在线观看| 精品久久久久久久久久免费视频 | 中文字幕人妻丝袜一区二区| 色综合婷婷激情| 一二三四社区在线视频社区8| 国产高清国产精品国产三级| 伊人久久大香线蕉亚洲五| 香蕉丝袜av| 高清毛片免费观看视频网站 | 久久精品国产亚洲av高清一级| 亚洲专区国产一区二区| 叶爱在线成人免费视频播放| 中文亚洲av片在线观看爽 | 欧美日韩一级在线毛片| 国产野战对白在线观看|