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笔者根据对广州双燕岗住宅区边坡支护的施工实践,获得了先进的锚杆施工技术。本文详细阐述了边坡支护预应力锚杆的原理、工程作用、锚杆设计及锚杆施工工艺,为承担边坡和基坑支护锚杆工程提供了技术保证。 相似文献
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结合四海香大厦基坑支护工程，介绍钻孔灌注桩连续墙支护、锚杆、锚喷网支护和降水井等工程的施工技术与方法，并介绍基坑周边建筑物沉降的控制方法及承压水的处理方法。 相似文献
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桩锚支护结构体系是将护坡桩与土层锚杆相结合的一种支护方法,安全经济的特点使它广泛应用于边坡和深基坑支护工程中,但在超深基坑中的应用仍在探索中。在凤城国贸超深基坑工程中,根椐场地的工程地质条件、水文地质条件,充分考虑到周边条件,通过分析论证不同的基坑支护方案,选择技术上可行、经济上合理、整体性能好、同时便于基坑支护开挖及后续施工的桩锚支护体系。然后对基坑支护结构进行了土压力计算、灌注桩设计、锚杆设计、稳定性的验算,并通过后期变形观测,验证桩锚支护型式对于此超深基坑是安全经济适用可行的。 相似文献
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苏州地区地层多为粉质粘土夹粉土,含水量较大,呈软塑至流塑状态,对深基坑支护极为不利。苏州世茂运河城深基坑支护工程选用护坡桩＋土层锚杆方案。锚杆设计为三层,间距为1.5m,承载力分别为250、280和220kN,有效锚固段长度分别为13、14.4和14m,杆体选用1860级75mm钢铰线。每层锚杆施工完成后,均进行了验收试验。试验结果表明,各层锚杆的承载力完全满足设计要求,而且安全储备很大,证明锚杆在软塑土层中的应用是可行的。 相似文献
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深层搅拌桩，碎石注浆桩，参应力锚杆，岩体喷锚和压力注浆5种施工工艺在一个深基坑支护工程中综合应用，降低了工程造价，保证了基坑支护系统的安全性，可靠性，并取得成功，概述以上几种施工方法的设计，施工概况及主要技术措施。 相似文献
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以某地下连续墙斜锚杆支护工程施工为例，介绍了斜锚杆桩的施工工艺，主要包括：斜锚杆的设计；施工设备的选择及机具设计；灌浆锚杆的施工工艺等。 相似文献
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结合深圳市星海阁办公楼的工程实例,从周边环境对深基坑支护的特殊要求及复杂的地质条件出发,论述了采用土钉与锚杆联合支护形式的依据.介绍了在深基坑支护施工中采取的具体措施后期效果.同时分析了这种联合支护结构形式的力学特点,通过将两者联合使用,可实现锚杆支护结构水平侧移小和土钉支护结构受力合理的优点.且土钉与锚杆联合支护,使得上部锚杆和中下部的土钉墙两者形成了统一的受力整体,共同抵抗荷载和变形. 相似文献
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上层水泥浆预应力锚杆广泛应用于上层基础加固。锚杆头部主要作用是将拉杆的力传递给建筑物，易于掌握。水泥浆团结体对拉杆的握裹力大小取决于水泥浆质量及拉杆表面的清洁程度与凸凹程度。此类传力方式锚杆没有充分发挥钢筋拉杆的应力，造成锚固段深部上层抗剪应力的浪费，减小锚杆抗拔力。倒拉式锚杆则克服了上述缺点。水泥浆团结体与上层间的作用力对锚杆的极限抗拔力起决定作用，它的大小决定于水泥浆团结体凸体对上层的剪切应力和相对平滑的水泥浆团结体对土层的摩擦阻力。土层蠕变作用限定了锚杆安全系数的取值范围。锚固段要求设置在非重力土楔范围以外的稳定区域。 相似文献
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锚固岩质边坡具有良好的抗震效果,为深入了解其地震动响应机制,系统梳理了地震荷载下锚固岩质边坡动力响应的国内外研究文献,论述了地震作用下岩质边坡-锚固结构体系动力特性、锚固岩质边坡动力稳定性及其动力响应影响因素.基于现有研究成果,未来可进一步分析强震或频发微震等不同地震荷载形式下的锚固岩质边坡动力演化模式;借助基于演化模式的锚固岩质边坡地质力学模型,明晰地震荷载传递规律、锚固结构力学演化特征与锚固岩质边坡动力响应特性,综合揭示岩质边坡-锚固结构体系地震动耦联作用机理;开展具有大塑性变形能力的新型抗震锚固结构设计关键技术的创新、集成与标准化,并建立新型抗震锚固结构关键技术应用示范区. 相似文献
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Data for the Waimea Plains, New Zealand indicate that the lower confined groundwater aquifer is hydraulically homogeneous and that shallow groundwater levels inland are affected mostly by anthropogenic processes, while those near the coast are affected more by sea level variation. Analysis of long-term data for New Zealand indicates that sea level has increased continuously, but trends are not spatially uniform. Results from non-parametric trend analysis show that rising trends for groundwater levels are predominant in the shallow aquifer both inland on the Waimea Plains and, for recent years, near the coast, while decreasing trends are evident in the underlying confined aquifer near the coast. Groundwater level change in the shallow aquifer appears to be more affected by climate change than the lower confined aquifer. Correlation analysis indicated that groundwater levels are more affected by rainfall during the rainy season than the dry season and more influenced by rainfall inland than near the coast. Groundwater level declines in the lower confined aquifer near the coast, which has its major recharge area inland in the catchment, may be substantially affected by groundwater abstraction in inland areas as well as sea level variation, but there are little evidences of seawater intrusion. Meanwhile, groundwater recharge over the catchment area has great influence on rising groundwater levels in the shallow aquifer and its recharge is estimated to be 417.8 mm/year using chloride concentrations of precipitation and groundwater. 相似文献
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东营凹陷古近系沙四上亚段地层大规模发育典型的湖相滩坝砂体,并获得大量油气发现。作者从固体与流体相互作用的产物——胶结物和次生孔隙入手,结合盆地的演化和断层的演化阶段,来定量半定量地恢复储集层中流体性质的变化以及对储集层物性的影响。根据流体来源和持续时间,可以把固体—流体作用过程划分为5个阶段: 初始流体作用阶段、围岩流体作用阶段、外来流体作用阶段、排烃流体作用阶段和排烃后流体作用阶段。根据滩坝砂体的分带性和次生孔隙形成机理,总体可分为砾质滩坝酸性流体主控次生孔隙发育带、近岸滩坝酸碱流体共同作用次生孔隙发育带和远岸滩坝—中央共振带滩坝碱性流体主控次生孔隙发育带,并进行了平面上次生孔隙成因的推测。 相似文献
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基于过程模拟的地下水污染预警是基于包气带和饱和带过程模拟的耦合实现的,且融合了涵盖整个地下水系统的四个预警指标。选取浑河冲洪积扇的李官堡水源地为例,基于Hydrus-1D和Visual Modflow分别进行包气带过程模拟和饱和带过程模拟,针对潜层和承压层的复杂程度分别制定了各自的预警临界值;经分析可知,随着时间的推移,地表污染物持续进入到地下水中,污染晕范围不断扩大,地下水中最大浓度值和水源井浓度值也持续增加,且承压含水层的预警级别要高于潜水含水层;同时基于潜层和承压层中污染物最大浓度值与时间分别近似呈线性关系和指数关系可进行长时间尺度的预警;并提出了零级预警区和一级预警区管理措施以监测和预防为主,二级预警区、三级预警区和四级预警区管理措施以控制和监测为主。 相似文献
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Simulation experiment of sedimentary process and sedimentary architecture of alluvial fan under the control of normal faults 
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下载免费PDF全文 Normal fault structures are widely developed in basins and orogenic belts,which control the accommodation space and the distribution of sediments and thus affecting the morphology of alluvial fans. A flume tank experiment was carried to simulate and clarify the control of normal faults on the sedimentary process and internal architecture of alluvial fans.The results show that the large amount of sediments carried by debris flow tend to be unloaded near the hanging wall of faults and are subsequently reworked by traction current,which result in a triangular distributary gravel bar grows vertically on fault plane with the tip pointing to the source area. When the hydrodynamic force is strong,debris flow goes across distributary gravel bar and forms over-bar lobe at the tail of the distributary gravel bar. When the hydrodynamic force is weak,debris flow forms fault plane-dominated lobe along fault plane and is located on both sides of the distributary gravel bar. Under the control of normal faults and the barrier of distributary gravel bar,the unloading process of sediments varies greatly at different positions on the surface of alluvial fan. The particle size varies greatly among different facies,with coarsest grains developed on the fans of hanging wall,finer grained on over-bar lobe and finest sediments on fault plane-dominated lobe. The development process of alluvial fan can be divided into three stages,according to the sandbody thickness and fault throw of distributary gravel bar. The fault throw also affects the sedimentary architecture of alluvial fan,with larger the fault throw generating larger the accommodation space of hanging wall,longer development time of distributary gravel bar and more complex of the superposition pattern of the sand bodies inside the fan. The internal architecture of alluvial fan that is controlled by normal faults includes longitudinal sandbar,distributary gravel bar and debris flow lobe in the profile vertical perpendicular to the sediment source direction from the proximal to the distal end. Along sediment longitudinal section,composite channel,superimposed distributary gravel bar complex and superimposed bodies of multi-phased lobes are dominant facies. 相似文献
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陆源碎屑与湖相碳酸盐混合沉积在渤海海域古近系普遍发育,已经成为重要的油气勘探目标.基于90余口已钻井,结合地震、测井以及相关分析化验资料,以渤海海域古近系钻遇的混合沉积为研究对象,开展了沉积特征与成因背景分析,建立了混合沉积发育模式.研究表明:渤海古近系混合沉积发育近岸混积扇、近岸混积滩坝、远岸混积滩坝3种沉积相、7种沉积亚相和14种沉积微相.近岸混积扇以发育混积沟道为典型特征,岩性为含生屑的砂砾岩或中粗砂岩,为陡坡扇三角洲环境短源水道废弃后与生物碎屑间歇性间互沉积;近岸混积滩坝,为近源搬运沉积的陆源碎屑与盆内碎屑之间的混合沉积,典型沉积特征为发育高陆源碎屑含量的各种粒屑滩或坝;远岸混积滩坝为典型的以富含生物碎屑为主的混合沉积,陆源碎屑含量低,一般为盆内低隆或孤立潜山之上原地生长生物与少量供给的陆源碎屑发生的混合沉积.混合沉积发育模式和规模受古气候与古水体环境、古构造与水动力、陆源碎屑物质供给、古地貌条件等共同控制,其中古地貌特征起主导作用.混合沉积发育模式的建立,对混积型储层预测和油气勘探具有重要意义. 相似文献