泥水平衡盾构顶推力非线性动力学分析与应用研究     

耿哲  李树忱  赵世森  张靖宇 《岩土力学》2018,39(Z1):469-476

泥水平衡盾构开挖过程中常遇到盾构顶推力难以确定且波动复杂的问题。针对该问题,对盾构推进过程中所受阻力进行系统的分析,确定了阻力的组成部分和计算方法,改进了盾壳与周围土体间摩擦力的计算公式。分析泥水平衡盾构推进系统的组成和工作原理,基于盾构推力的静力学模型建立了单自由度动力学模型,根据能量守恒原理建立了系统的平衡微分方程,推导出盾构推力的非线性动力学公式。基于上述公式,分析了盾构推力的变化趋势和波动规律,确定了液压油缸的最佳行程距离。通过与武汉地铁8号线越江隧道长江穿越段盾构顶进推力的实测数据对比分析,验证了提出公式能够正确计算管片衬砌所受的动态顶推载荷,对衬砌结构内力分析具有重要意义。  相似文献   

Late Neoproterozoic adakitic magmatism of the eastern Arabian Nubian Shield     

《地学前缘(英文版)》2019,10(6):1981-1992

Late Neoproterozoic adakitic magmatism within the Eastern Arabian Nubian Shield has been dated at633.2±9.0 Ma(2σ).These magnas intrude the forearc Ad Dawadimi Basin,which is composed of metapelitic schists and greywacke along with ophiolitic melanges of boninitic affinity which underwent inversion and deformation by~620 Ma.This adakitic magmatism,while intruding parts of the Ad Dawadimi Basin,predates this deformation,but is possibly coincident with basin closure.As adakitic magmatism requires melting of an amphibolite or eclogitic source,empirical and experimental constraints require anomalously hot supra-subduction zone mantle.Considering that this magmatism immediately predates basin inversion,these magmas possibly pinpoint the timing of the slab breaking,marking the terminal stages of arc magmatism,terrane accretion and the influx of hot oceanic asthenospheric mantle.This influx of hot asthenospheric mantle may also be responsible for postcolltsional A-type magmatism.  相似文献   

Geochemical Constraints of the Ediacaran Volcano-Sedimentary Succession of the Sa’al Metamorphic Complex at Wadi Zaghra, South Sinai, Egypt     

SAMUEL D. Michael  MOUSSA E. Hilmy  AZER K. Mokhles  SADEK GHABRIAL Doris 《《地质学报》英文版》2019,93(1):50-73

The volcano-sedimentary succession around Wadi Zaghra in Sinai, at the northernmost segment of the Arabian Nubian Shield, comprises volcanic rocks interbedded with rather immature sediments. The succession is dominated by intermediate to silicic volcanics of medium-to high-K calc-alkaline affinity. It is divided into two units, the lower unit includes intermediate rocks and dacites interbedded with graywackes, semi-pelites and pelites and topped by polymict conglomerates. This unit is subjected to folding and regional metamorphism(up to garnet zone) and is intruded by quartz diorite-granodiorite inducing, locally, low-pressure contact thermal metamorphism. The unmetamorphosed upper unit encompasses acid volcanics intercalated with litharenite, sublitharenite and minor arenite. The rhyolites of this unit pertain to the highly fractionated granites and are characterized by an agpaitic index(NK/A) ranging from 0.87 to 0.96. They may reflect either extensive interaction of subduction-related magmas with the continental crust or a change in the tectonic regime. The present lithological and geochemical characteristics of the studied sediments together with available zircon ages indicate rather distal provenance of their detritus. This detritus comprises fluvial-alluvial sediments accumulated in the intermontane basins, which are half-grabens or tilted fault blocks. The tectonic setting of the depositional basins is active continental margin and continental island arcs. Geochemical patterns of the Zaghra volcano-sedimentary succession indicate their correlation with the Dokhan Volcanics-Hammamat Clastics sequence of the Eastern Desert of Egypt. Also, the Zaghra volcanics display geochemical similarities with those exposed in Sinai, at the Rutig, Ferani and Iqna Shar'a areas. The Zaghra succession is dated as Ediacaran but is not related either to the ensimatic island arc assemblage or to the rift-related assemblage formed during the early stages of the break-up of Rodinia as previously thought.  相似文献   

隔离桩及盾构近接施工对高铁桩基的影响分析     

李雪  周顺华  王培鑫  李晓龙 《岩土力学》2015,36(Z1):235-240

针对饱和砂土地区盾构隧道超近接高铁桥墩摩擦桩的工程问题,采用钻孔灌注桩及高压旋喷桩组合隔断隧桩间位移。分别对钻孔灌注桩、高压旋喷桩及盾构上下行线近接高铁桥梁桩基引起的高铁桩基的变形及变位开展现场试验,对现场实测数据及规律进行分析。结果表明,钻孔灌注桩施工使高铁桥墩产生沉降,占施工过程最大沉降量的 75%～125%;高压旋喷桩施工导致桥墩产生隆起,占施工过程最大沉降量的-50%,旋喷桩施工完成后将持续一段时间;盾构施工对高铁桥墩竖向变形产生影响,距离高铁桩基越近影响越大,同时累计沉降跟盾构施工控制有较大关系。  相似文献   

盾构近距离下穿引起已建地铁隧道纵向变形理论研究   总被引：2，自引：0，他引：2  

张琼方  林存刚  丁智  夏唐代  单华峰 《岩土力学》2015,36(Z1):568-572

盾构下穿会引起邻近已建隧道附加应力的变化,使已建隧道产生变形,对已建隧道的结构和运营安全造成一定的影响。基于明德林（Mindlin）解,经数值积分可以计算出盾构产生的刀盘附加推力q、盾壳摩擦力f及同步注浆附加压力p作用下所引起的已建隧道轴线处的附加应力。同时,利用镜像法算出在土体损失作用下已建隧道轴线处的附加应力,再将已建隧道视为温克勒（Winkler）地基梁,应用Winkler地基梁理论即可算出上述4个参数作用下已建隧道的变形,根据盾构穿越的不同工况,将上述参数作用下的变形进行叠加得到已建隧道总变形。通过杭州4号线盾构隧道下穿1号线隧道的工程实例将理论计算结果与实测结果对比分析,证明了该方法的有效性。  相似文献   

挤压地层双护盾TBM围岩变形及应力场特征研究     

程建龙  杨圣奇  潘玉丛  田文岭  赵维生 《岩土力学》2016,37(Z1):371-380

为研究挤压地层双护盾隧道掘进机（TBM）作用下围岩变形及应力场特征,采用FLAC3D建立了完整模型,并详细阐述了隧道掘进机（TBM）施工过程中的模拟方法,重点分析了隧洞纵横断面内围岩位移场、应力场、塑性区特征。模拟结果表明,两腰下部范围内的围岩与TBM护盾发生接触并产生挤压,拱顶并未接触;受刀盘与护盾连接处的尺寸高差和前后护盾的锥度影响导致仰拱围岩内出现3次加卸载,仰拱内部环向应力和径向应力均大于拱顶和两腰,而且其主应力方向与径向线斜交,受扰动剧烈,但仰拱下方70°范围内的围岩基本处于弹性状态;横向断面内围岩塑性区自上而下逐渐减小,且距掌子面越远塑性区范围越大,但后盾塑性区范围变化不大。  相似文献   

软土地层盾构隧道结构整体抬升实践     

朱瑶宏  夏汉庸  胡志飞 《岩土力学》2016,37(Z2):543-551

软土地层盾构施工易沉降过大导致轴线偏差,出现调坡困难,甚至影响后期列车运行速度,注浆抬升是轴线偏差治理的一种方法。宁波轨道交通某区间在施工过程中因对地层变化理解不彻底,导致沉降过大,调坡困难,为了不造成结构破坏,不影响工程工期,使隧道线型得到改善,对隧道结构整体抬升进行了实践。通过对地质情况分析,结构验算,注浆工艺研究,提出了下部注浆,内部支撑,实时监控,即时调整的思路,在注浆过程及时调整浆液。经过精细化管理,该区间最大稳定抬升量达3 cm。工程实践表明,注浆工艺和内部支撑对抬升阶段通用环管片结构安全起到重要作用,浆液的选择对后期稳定非常重要。该工程探索了软土地层盾构隧道不均匀沉降治理、控制措施,可为其他盾构隧道沉降治理提供参考和抬升设计提供依据。  相似文献   

考虑黏度时变性的水泥浆液盾构壁后注浆扩散规律及管片压力模型的试验研究   总被引：3，自引：0，他引：3  

刘健  张载松  韩烨  吴星 《岩土力学》2015,36(2):361-368

对水泥浆液黏度时变性进行了试验研究,证实了工程常用水灰比范围内水泥浆液服从宾汉姆流体特性;不同水灰比浆液黏度均随注浆时间增大而大幅度增加。根据试验结果,考虑注浆过程中水泥浆液黏度随时间的变化,对盾构壁后注浆水泥浆液的扩散规律及因注浆而造成的管片压力进行了推导及分析。计算表明：相同注浆时间条件下,水泥浆液扩散半径及注浆对管片产生的压力值均随注浆压力的增大而增大。考虑浆液黏度时变性后,扩散半径、注浆对管片压力值等均较不考虑浆液时变性时减小,且随注浆压力的增大,浆液黏度变化对管片压力值的影响更加明显。相同注浆压力条件下,浆液扩散半径及对管片产生的压力值均随注浆时间的增长而增加,但注浆前期增长速度较快,而后逐渐减缓。研究成果对于盾构壁后注浆工艺选择及参数设计具有较大的指导意义。  相似文献   

Provenance and Tectonic Setting of the Metasedimentary Rocks of the Neoproterozoic Adola Belt of Southern Ethiopia     

Bisrat Yibas   《Gondwana Research》1999,2(3):377

The Metasedimentary rocks from the Adola metamorphic belt has been analysed for major, minor, and trace elements, including REEs, in order to investigate the provenance and tectonic setting of these rocks.On the basis of filed work, petrographic data and major element geochemistry the Adola sedimentary rocks are essentially greywackes with subordinate lithic arenite. Among the 27 samples analysed, only two samples are quartz arenite with SiO₂ values above 89%. CaO-Na₂O-K₂O diagrams showed that most sample cluster around the average plots of granites and granodiorites. In order to determine the tectonic setting and provenance of the rocks, the samples are plotted on various binary and ternary diagrams. The plots on Fe₂O₃T+MgO versus TiO₂, K₂O/Na₂O, Al₂O₃/SiO₂ and Al₂O₃/(CaO+Na₂O) plots show that the Adola sediments have Oceanic Island Arc(OIC), Continental Island Arc(CIA), Active Continental Margin(ACM) and Passive Margin(PM) characteristics. Most samples, however, show island arc affinity. Only two samples (the quartz arenites) fall in the Passive Margin (PM) field.The trace element characteristics of these rocks discriminate the rocks only into oceanic and continental arc fields. The relatively high abundance of the transition metals, mainly Co, Ni, Cr and the low concentration of TiO₂ correlates well with the previously determined geochemical affinity of the basic rocks of Adola suggesting the dominance of the low- Ti oceanic tholeiites and even boninites in the source region.The REE patterns show three distinct groupings; a)With strong LREE enrichment, flat HREE and with out Eu anomaly, shows similar patterns with that of the oceanic island arc rocks; b) samples with strong Light REE enrichment, flat HREE pattern and strong negative Eu anomaly showing similar patterns to the Andean type andesites, probably derived from granitic gneisses and are affiliated to Active Continental Margin settings; c) this group is represented by a single plot having an enriched LREE pattern, flat HREE pattern and strong positive Eu anomaly. It is most likely that this pattern is related to a high normative plagioclase content due to local accumulation of feldspar during sedimentation rather than representing excessive Eu content of the precursor rock. The REE pattern represented by this sample is roughly similar to that of the Devonian greywackes of Australia.In conclusion, the use of geochemical characteristics of the sediments coupled with the geological information from the area strengthens the suprasubduction zone (SSZ) ophiolitic tectonic setting interpretation suggested (Yibas 1993) for the Adola belt. The trace element plots and their absolute abundance, and the REE patterns strongly constrain the tectonic setting and the provenance of the metasediments to an arc related setting.  相似文献   

盾构施工纵向地表沉降分析及基于延迟差分方程的动态预报     

张书丰  孙树林  姜志强 《岩土力学》2008,29(1):182-186

结合南京地铁某盾构施工区间,对纵向地表沉降进行了理论分析,提出了盾构掘进对纵向地表的影响范围,总结了盾构推进不同阶段引起地表沉降量占总沉降量的百分比。针对引起地表沉降因素的复杂性和不稳定性,将纵向地表沉降视为随机过程,基于延迟差分方程建立模型进行动态预报,并与实测数据进行比较。结果表明,该方法具有较高的准确性。  相似文献