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软岩高边坡预应力锚索抗滑桩的设计计算 总被引:3,自引:1,他引:3
目前已提出了多种预应力错索抗滑桩的设计计算方法,例如按Winkler弹怀地基梁的方法、错索与桩的协调变形的方法等.由于软弱岩体的变形特征,结构与岩体的相互作用机理较为复杂,这些方法难以直接应用于软岩高边坡工程,需要加以分析改进.应该分析预应力锚索抗滑桩的施工顺序、实际受力条件、锚索预应力的主要控制因素等,分阶段进行计算,这样得出的计算结果才有可能与实际情况一致.在充分吸取现有计算方法优点的基础上,提出了改进的方法.通过实际工程的计算,得出了较为符合实际情况的结果. 相似文献
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三峡库岸城区滑坡治理与沿江公路建设一体化模式--以重庆万州清泉路滑坡为例 总被引:5,自引:0,他引:5
三峡库岸城区滑坡90%属于由第四纪松散土体组成的散体滑坡,滑坡区属于城区重要组成部分,降雨及三峡库水位降落是此类滑坡孕发的动力因素。本文以重庆万州清泉路滑坡为例,基于库岸城区滑坡防治原则,构建了实用的滑坡治理与沿江路建设一体化模式,推导了抗滑桩的内力计算方法;详细分析了一体化模式的结构组成及受力特性。研究成果对于三峡库区城区滑坡的治理与开发利用具有较强的指导借鉴作用。 相似文献
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通过填方边坡下覆软弱地基处理采用水泥土搅拌桩和袋装砂井联合法进行处理的案例得出填方边坡软基处理效果较好,地基土体强度可以迅速提高,同时经过水泥土搅拌桩处理填方边坡的地基,能够使得高填方边坡的地基的稳定性大大提高。 相似文献
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通过工程实例,介绍了长螺旋钻孔在CFG桩施工中存在的由于钻门打不开而造成堵管或爆管,憋钻和卡钻,断桩、缩径和桩身缺陷等事故及采取的防治措施。 相似文献
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磨刀溪岩石滑坡由于人工开挖、在支挡不当的情况下产生并逐步扩大。对此,着重采用了工程地质力学法对该滑坡进行了分析,明确了该滑坡为一切层滑坡,其发生发展与岩层的结构面关系密切。在此基础上以推力传递系数法及地基系数等为理论,确定以一排抗滑桩及一排锚索抗滑桩进行支挡,并在下排桩前采用锚索框架对桩前岩土体进行加固,以确保抗滑桩的锚固段不松弛变形,同时结合疏排水的措施对该滑坡予以彻底治理,从实践看最后一次的治理取得了成功。同时分析了前面几次失败的治理经历,从中总结了很多有益的经验和教训,并从治理实践中证明了该滑坡治理措施的合理性和有效性,值得同类工程借鉴。 相似文献
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采用工程地质钻探、物探、地质测绘及室内试验等技术方法探讨飞鹅山Ⅲ号滑坡形成机理与防治技术。结果表明:1)滑坡体主要岩性为泥质粉砂岩,飞鹅山滑坡属于新形成的深层中型牵引式滑坡,在平面上呈圈椅状。2)滑坡属于双层滑面滑坡,主滑面以中型深层滑坡为主,主滑体上部发育中型中厚层滑坡。3)滑坡产生的原因为:(1)泥质粉砂岩倾向与坡向基本一致,且岩层倾角为中等倾角;(2)人工开挖使坡脚形成高陡临空面,抗滑力大为降低;(3)雨水沿层面及节理裂隙入渗至坡体深部,大大增加岩土体容重,同时泥质粉砂岩遇水软化,抗剪强度显著降低。4)结合该滑坡区地质环境条件,采用坡面削坡+锚杆(索)+格构梁+双排预应力锚拉抗滑桩+三维网植草绿化+截排水+毛石挡墙的综合治理方法进行防治,监测结果显示该滑坡变形及位移已得到有效控制,整治效果良好。 相似文献
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Seismotectonics of the Cyprian Arc 总被引:1,自引:0,他引:1
Shimon Wdowinski Zvi Ben-Avraham Ronald Arvidsson Goran Ekström 《Geophysical Journal International》2006,164(1):176-181
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In the decades since World War II, large-scale ecological changes have affected fishing communities across the northern Atlantic. Substantial declines hit their historically important resources, most notably the Atlantic cod. Such declines were often accompanied by increases in other, previously less exploited, species. Interactions between fishing pressure and environmental variation have driven ecological change. Ecological changes in turn reshaped the fisheries, contributing to altered demographic profiles of fisheries-dependent communities. Many places lost population, especially through out-migration of young adults. Broad social forces also contributed to these trends, but the timing and geographical details of population changes often correspond to specific fisheries/ecological events. 相似文献
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Double-planed deep seismic zone and upper-mantle structure in the Northeastern Japan Arc 总被引:6,自引:0,他引:6
Summary. The ScSp wave converted from the ScS wave at the boundary between the descending lithospheric slab and the mantle above it was clearly observed from a nearby deep earthquake with magnitude 7.7 at some stations of the seismic network of Tohoku University which covers the Tohoku District, the northeastern part of Honshu, Japan. By applying the three-dimensional seismic-ray tracing method, the location of this boundary was determined from the difference in arrival time between the ScS and ScSp waves. The result shows that the upper boundary of the descending slab lies exactly on the upper plane of the double-planed deep seismic zone found in the Northeastern Japan Arc.
There is an additional evidence that the boundary is located on the upper plane of the double-planed deep seismic zone. The hypocentre distribution of intermediate-depth earthquakes located by the small-scale seismic-array observation is extremely different from that obtained by the relatively large-scale seismic network. The discrepancy in the distribution of hypocentres of the same earthquake independently located is well explained by the inclined lithospheric slab model derived from the difference in arrival time between the ScS and ScSp waves.
The earthquakes with reverse faulting or with down-dip compressional stresses occur at the upper boundary of the descending slab. Within the descending slab, the earthquakes with down-dip extensional stresses also occur in a very narrow zone from 30 to 40 km below the dipping boundary in the depth range from 50 to about 200 km, and these shocks form the lower plane of the double-planed deep seismic zone. 相似文献
There is an additional evidence that the boundary is located on the upper plane of the double-planed deep seismic zone. The hypocentre distribution of intermediate-depth earthquakes located by the small-scale seismic-array observation is extremely different from that obtained by the relatively large-scale seismic network. The discrepancy in the distribution of hypocentres of the same earthquake independently located is well explained by the inclined lithospheric slab model derived from the difference in arrival time between the ScS and ScSp waves.
The earthquakes with reverse faulting or with down-dip compressional stresses occur at the upper boundary of the descending slab. Within the descending slab, the earthquakes with down-dip extensional stresses also occur in a very narrow zone from 30 to 40 km below the dipping boundary in the depth range from 50 to about 200 km, and these shocks form the lower plane of the double-planed deep seismic zone. 相似文献
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Ch. Hollenstein A. Geiger H.-G. Kahle G. Veis 《Geophysical Journal International》2006,164(1):182-191
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Yoshio Fukao 《Geophysical Journal International》1977,50(3):621-642
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Upper Mantle Velocity Structure Estimated From Ps-Converted Wave Beneath the North-Eastern Japan Arc 总被引:2,自引:0,他引:2
Toru Matsuzawa Norihito Umino Akira Hasegawa Akio Takagi 《Geophysical Journal International》1986,86(3):767-787
Summary. The upper boundary of the descending oceanic plate is located by using PS -waves (converted from P to S at the boundary) in the Tohoku District, the north-eastern part of Honshu, Japan. the observed PS-P time data are well explained by a two-layered oceanic plate model composed of a thin low-velocity upper layer whose thickness is less than 10 km and a thick high-velocity lower layer; the upper and lower layers respectively have 6 per cent lower and 6 per cent higher velocity than the overriding mantle. the estimated location of the upper boundary is just above the upper seismic plane of the double-planed deep seismic zone. This result indicates that events in the upper seismic plane, at least in the depth range from 60 to 150 km, occur within the thin low-velocity layer on the surface of the oceanic plate. 相似文献
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