不同刚度约束对能量桩应力和位移的影响研究     

王成龙  刘汉龙  孔纲强  吴宏伟  李建斌 《岩土力学》2018,39(11):4261-4268

能量桩是一种在传递上部建筑荷载的同时获取地热能源的新技术,其实际工作过程中,热荷载会引起桩体的膨胀或收缩,而桩顶建筑和桩底持力层则会对桩体变形产生约束,进一步影响桩体的应力和位移,但是目前对该问题的研究却十分有限。基于模型试验和数值模拟方法,对桩顶和桩底不同约束条件下两种埋管形式（单U和W型）的桩体位移和热应力进行了分析,并进一步探讨了位移零点随桩顶和桩底约束条件的变化规律。研究结果表明,随着桩顶上部荷载约束刚度的增大,桩体位移零点上移,桩体热应力随着深度增大而减小;随着桩端土体约束刚度的增大,桩体位移零点下移,桩体热应力随着深度增大而增大;相较于无外荷载,工作荷载作用下位移零点上移。  相似文献   

膨胀土地基中隧道施工对群桩影响研究     

马少坤  WONG K S  吕虎  吴宏伟  赵乃峰 《岩土力学》2013,34(11):3055-3060

在膨胀土地基中进行隧道对群桩影响的三维离心模型试验研究,目标地层损失比为2%,着重研究引起的地基沉降槽、桩的附加沉降、附加弯矩、轴力的变化规律。试验得出：隧道开挖沉降槽空间效应明显;隧道开挖从-0.75D至1.25D时,桩附加沉降呈线性增长,隧道开挖至1.25D以后,桩依然沉降明显。前桩与后桩沉降值不同,桩帽会出现倾斜;前桩上部出现负附加弯矩而下部出现正附加弯矩,而后桩仅在下部出现正附加弯矩;前桩附加弯矩最大值出现在隧道轴线附近,且比后桩附加弯矩大得多;前桩附加轴力随着隧道的开挖而增加,且每步最大值在隧道轴线附近。后桩的轴力也随隧道的开挖而增加,但每步最大值出现在桩顶附近。  相似文献   

地下水开采引起的次压缩对隧道长期沉降的影响     

刘国彬  李青  吴宏伟 《岩土力学》2012,33(12):3729-3735

软土地区盾构隧道建成后往往伴随有明显的长期沉降,较大的隧道沉降会严重影响地铁系统的运营及安全。然而,目前对于软土地区隧道长期沉降机制的认识尚不明确。以上海地区地铁盾构隧道1999－2007年间的隧道沉降为例,通过室内试验及现场监测对引起隧道长期沉降的因素,特别对地下水开采引起的软土及砂土层次压缩进行了研究。结果表明,第4含水砂层具有明显的次压缩特性,抽取地下水引起的第4含水层的压缩,特别是其次压缩变形,是引起隧道长期沉降的主要原因之一。因此,严格控制该承压含水层地下水开采是目前缓解上海地铁隧道长期沉降的主要措施。  相似文献   

ICE‐MARGINAL SEDIMENT DELIVERY TO THE SURFACE OF A HIGH‐ARCTIC GLACIER: AUSTRE BRØGGERBREEN,SVALBARD     

PHILIP R. PORTER  GEIR VATNE  FELIX NG  TRISTRAM D.L. IRVINE‐FYNN 《Geografiska Annaler: Series A, Physical Geography》2010,92(4):437-449

Enhanced delivery of water‐saturated, ice‐marginal sediments to the glacier surface is a response to glacier thinning that has the potential to increase both levels of sediment transfer through the glacier hydrological system and total basin sediment yields. Preliminary observations made during summer 2007 at Austre Brøggerbreen, Svalbard, confirm that ice‐marginal debris flows in the upper reaches of the glacier are actively delivering sediments to the glacier surface, which may then be flushed into the glacier's hydrological system. During a four‐day observation period, several stochastic pulses in water turbidity were observed at a single portal where solely supra‐ and englacial drainage emerge at the glacier margin. The erratic suspended sediment fluxes were hypothesized to originate from ice‐marginal sources. Quantitative analysis of continuous turbidity and discharge data confirm that discharge is not driving these turbidity pulses and, combined with observational data, that the most likely origin is the delivery of water‐saturated sediments to the glacier surface from ice‐marginal, debris flows with subsequent transfer to the portal via the glacial drainage system. These observations illustrate the potential importance of the paraglacial component to the overall sediment cascade of deglaciating basins and highlight the need for careful interpretation of turbidity records, where stochastic pulses in turbidity may be attributed to sources and processes other than ice‐marginal sediment inputs.  相似文献