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双语推荐:孔隙水压力

碎石桩是一种常用的地基处理方式,其振动挤密施工会对桩周土产生一定程度的扰动效应,但现有关于碎石桩振动扰动效应的研究较少.通过埋设孔隙水压力计、土压力盒、测斜管,并结合静力触探试验,研究了碎石桩施工过程中桩周土中的孔隙水压力、土压力、深层平位移和强度变化规律.研究结果表明:碎石桩施工时会在桩周土中产生较大的孔隙水压力和深层平位移,随着孔隙水压力的消散,桩周土中的附加有效应力增加,土体的强度得到一定程度的改善.
Stone column is commonly used in foundation treatment. Till now,there is little research about the construction influence of stone column. The pore water pressure,earth pressure,deep horizontal deformation and strength during construction process of surrounding soil were respectively measured by piezometers ,pressure transducers,inclinometers and CPT. The field test results show that there were large pore water pressure and deep horizontal deformation due to stone column construction. The effective stress and strength of surrounding soil increased with the dispassion of pore water pressure.

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为解决压力合算和分算的争议,从理论上证明粘性土土合算在某些情况下的合理性,基于微观层面分析了土中孔隙及土中的类型及特征,研究了土共同作用的微观机理,建立了临界重度方程及估算公式,给出了粘性土传递孔隙水压力的判别公式;选取不同地区粘性土,进行重力失试验,试验结果表明:试验值与公式计算值差异很小,试验验证了公式的合理性.综合机理分析及试验成果,证实了对于现有基坑工程中所涉及的粘性土,其孔隙中仍然存在可流动的孔隙水,一般都能传递孔隙水压力,压力应当区别对待.
In order to resolve controversy of separate and combined calculation of water and earth pressures and to theoretically prove that combined calculation of water and earth pressure of clay is reasonable under some circumstances. The formation character of pores in the clay,the existence mode of pore water, the analysis of micro-mechanism of interaction of water and clay is established. The equation and estimating formula of critical density is defined to discriminate whether compact clay can transfer pore water pressure;The gravity dehydration test was studied by selecting different local clay, and the test result shows the slight differences between the results of test and estimated value, and the test verification of the formula rationality.The conclusion that clay is related to existing foundation pit project can generally transfer pore water pressure based on the studies above.

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在自主研制的孔隙介质热--应力耦合有限元程序中引入Taron等提出的颗粒聚集体的压力溶解模型,针对一个假设的实验室尺度且位于非饱和石英颗粒聚集岩体中的高放废物地质处置模型,拟定两种计算工况:(1)孔隙率和渗透系数是压力溶解的函数;(2)孔隙率和渗透系数均为常数,进行4 a处置时段的数值模拟,考察了岩体中的温度、颗粒界面膜及孔隙中的溶质浓度、迁移和沉淀质量、孔隙率及渗透系数、孔隙水压力、地下流速和应力的变化、分布情况。研究结果表明:工况1计算终了时,压力溶解使得孔隙率和渗透系数分别下降到初始值的43%~54%、4.4%~9.1%。在核废料释热温度场的作用下,工况1、2中的负孔隙水压力分别为初始值的1.00~1.25倍、1.00~1.10倍,前者表现了压力溶解的明显影响;两种工况的岩体中的应力量值及分布基本相同。
The model of pressure solution for granular aggregates established by Taron et al is introduced into the FEM code for analysis of thermo-hydro-mechanical coupling in porous media developed by the first author. Aiming at a hypothetical model for nuclear waste disposal in an unsaturated quartz aggregate rock mass with a laboratory scale, two computational conditions are designed: (1) the porosity and the permeability of rock mass are functions of the pressure solution; (2) the porosity and the permeability are constants, then the corresponding numerical simulations for a disposal period of 4 years are carried out; and the states of temperatures, solute concentrations in the intergranular fluid film and at the pore space, removal and precipitation masses, porosities and permeabilities, pore pressures, flow velocities and stresses in the rock mass are investigated. The results show:at the end of the calculation in case 1, pressure solution makes the porosities and the permeabilities decrea

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针对宁波海相淤泥质软土开展现场模爆试验,获得了不同装药量和埋深条件下软土的孔隙水压力、冲击压力及温度的时程分布和演化规律,揭示了爆炸作用下软土中渗流、应力和温度的耦合现象。试验结果表明:随着药量增大,超静孔隙水压力峰值增大,爆炸后数分钟内孔隙水压力消散较快,随后变慢。爆炸后,软土中冲击波向弹性波转化存在一个分界压力,这个分界压力与介质性质有关系,尤其是含气量。温度在软土介质中具有一定的传导时间和上升时间,且在软土介质中的上升较空气中慢。最后,利用相关理论开展计算,并与实测结果进行了对比分析。研究结果可以为沿海软土地区地下人防工程设计及地基压密处理提供参考。
An in-situ simulated explosion test was carried out at a site with Ningbo marine silt soft soil.The time history distribution and evolution laws of pore water pressure,shock pressure and temperature under the conditions of different explosive quantities and buried depth were obtained. The test results revealed that there exist coupling phenomena of seepage,stress and temperature;the peak of super-static pore water pressure increases with increase in explosive quantity and the dissipation of pore water pressure is relatively quick within early minutes after explosion and then it decreases;there is a dividing line pressure which means a pressure for shock wave to be converted into elastic wave and it is related to soil''s character,especially,its air content;the explosion temperature has a certain conduction time and rise time in soft soil,and it rises more slowly in soft soil than it does in the air.Finally,relevant theories were used to compute the pressure and temperature.Th

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为揭示不同埋深岩溶陷落柱在承压水压力和压实程度2种影响因素作用下的突机理,利用改进的变质量破碎岩石渗流试验系统,进行了考虑颗粒迁移的破碎泥岩变质量渗流试验,得出渗流突变历时、突出物质量、突出物质量变化率及孔隙度变化率等在渗透压力和初始孔隙度共同作用下的变化规律。研究表明:1)在渗流初始阶段,渗透压力和流量稳定;渗流突变时,渗透压力和流量均发生剧变,变化幅度与试样的突出物质量和孔隙结构调整情况有关。2)随初始孔隙度增大、渗透压力增加,突历时变短,突出物质量增大,二者均可由渗透压力和初始孔隙度表示为对数函数,突出物质量变化率和孔隙度变化率均变快,可用指数函数拟合。3)随着渗透压力增大,突历时、突出物的质量、突出物质量变化率和孔隙度变化率受初始孔隙度的影响逐渐减弱。
In order to study the water inrush mechanism of Karst collapse column in different depths with coupled underground water pressure and compaction degree, a modified variable mass seepage experiment system on broken rock was used to conduct variable mass seepage experiments for broken mudstone considering particle migration. The duration time of seepage burst, weight of gushed particle, change rate of gushed particle weight and change rate of porosity were recorded and calculated, and the change rules under seepage pressure and initial porosity were obtained. It shows that in the initial seep-age stage, seepage pressure and flow are stable, they change rapidly when seepage burst happens, and the change range is related to weight of gushing particle and the process of pore structure adjusting. With the initial porosity and seepage pressure increasing, the duration time of seepage burst gets shorter,weight of gushed particle gets larger, and these two parameters are fitted by logarithmic f

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针对小浪底大坝心墙内部某些监测点孔隙水压力持续偏高的情况,通过对坝体多年渗透压力监测资料分析,建立渗透压力与库位、降雨、温度及时效之间的相关模型,分析心墙渗透压力的变化规律及原因,计算库位、降雨、温度及时效对渗透压力的影响。分析结果表明:测点P115、P116及P117渗透压力随库位变化明显,且渗透压力变化与库位变化规律一致;测点P124和P125渗透压力基本保持稳定,对库位变化不敏感,各测点土体固结时间长,孔隙水压力消退缓慢。各影响要素中,库位对渗透压力影响较大,降雨、温度及时效分量对渗透压力的影响较小。
For the case of pore water pressure continued high in some monitoring points of the internal core wall of the Xiaolangdi dam,this paper analyzed the monitoring data of osmotic pressure of the dam,establishes statistical models about osmotic pressure and water level,rain-fall,temperature and aging,analyzed the change rules and causes of the osmotic pressure of the core wall and calculated the impact of these component on the osmotic pressure. The results shows that osmotic pressure in measuring points P115,P116 and P117 changes significantly with water level and osmotic pressure change is consistent with the change rule of reservoir water level;the osmotic pressure values in meas-urement points P124 and P125 remain stable,which is not sensitive to change with the water level,the soil in each measuring point consoli-dates with long time and pore water pressure subsides slowly. Among these influential elements,the reservoir water level has greater impact on the osmotic pressure

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半直立式圆筒护岸是一种新式港口工程结构,结合其在大连某工护岸工程中的应用,进行了半直立式圆筒护岸地基的加载试验,通过实测土压力、沉降、平位移及孔隙水压力,分析了半直立式圆筒护岸地基的沉降及平位移变化特点,并进一步研究了其不均匀沉降的发展过程.试验结果表明:半直立式圆筒护岸沉降及平位移对护岸荷载分级、每级荷载加载量、加载历时及两级荷载之间的间隔时间较为敏感,其中护岸后方最后一级不对称加载对圆筒结构的不均匀沉降影响最大,孔隙水压力变化主要受每级加载量、加载历时及潮汐作用影响,而圆筒安装及第一级荷载施加后,孔隙水压力产生较大的波动.
@@@@Semi-vertical cylindrical revetment is a new port engineering structure. Field load tests on a semi-vertical cylindrical revetment is carried out based on its application of a hydraulic revetment in Dalian. The earth pressure, foundation settlement, horizontal movement and pore water pressure of the semi-vertical cylindrical revetment are monitored. The settlement and horizontal movement of foundation of the semi-vertical cylindrical revetment are analyzed, and its non-uniform settlement is further studied. The monitoring results indicate that the sensitive factors affecting the settlement of the semi-vertical cylindrical revetment are loading stage, loading intensity, loading duration and loading intervals. The final unsymmetrical loading behind the revetment has the greatest impact on the non-uniform settlement of cylindrical structure. The variation of pore water pressure is mainly affected by each loading, loading duration and tidal action. When the cylindrical structure is ins

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针对当前压力计算中很少考虑土自身性质对其影响的研究现状,以自制试验槽为研究工具,通过使用3种不同渗透性土样进行的支挡结构上压力测试研究,对比了压力实测值和由压力分算、压力合算得到的理论计算值,分析了孔隙水压力和土压力的变化规律。由试验结果可以得到,由压力合算得到结果偏小,但在一定条件下尚可以接受,在发生主动位移情况下墙后土体会产生负超孔压,渗透系数影响着负超孔压的消散和孔隙水压力的传递程度,并进一步影响支挡结构上压力的分布情况。由试验结果推知,当土体渗透系数小到一定程度时,压力合算的方法是合理的。
For the current status of research that it rarely considers the impact of the nature of soil when calculating water and earth pressures, using self-made testing tank as research tool through measurement study by using three types of soil samples with various permeability coefficients, the measured water and earth pressures are compared with the theoretical values obtained by water and earth pressures calculated separately and together method; and the variation laws of pore water pressure and earth pressure are analyzed. The experimental results show that the values obtained by water and earth pressures calculating together method is lower than measured values; but still acceptable under certain conditions. Accompanied by active displacements, it generates negative exceed pore pressure in soil behind wall. Dissipation of negative exceed pore water and transfer of pore water pressure are both affected by permeability of soils which further affect the distribution of water and earth press
为了研究静力触探试验及沉桩扩孔等工程问题,基于修正剑桥模型,推导了不排条件下球孔扩张问题的半解析解。将扩张球孔周围土体分为临界状态区、塑性区以及弹性区三个区域。弹性区内,利用弹性理论得到应力和孔隙水压力的解答;临界状态区及塑性区内,利用相关联的流动法则、拉格朗日分析法建立了关于应力的一阶非线性常微分方程组,以弹塑性界面处的应力分量作为初值,求解微分方程组可得到应力和孔隙水压力的解答。研究结果表明:各向同性超固结比对扩孔压力、土体应力、超孔隙水压力以及塑性区范围均具有显著影响,且扩孔过程中土体剪切模量并非常量,其随扩孔半径、各向同性超固结比的变化而变化;同时通过与已有解答进行比较,对本文方法的可靠性进行了验证。
An exact semi?analytical solution in the undrained cavity expansion can be obtained on the basis of the MCC model to research the cone penetration test and the pile driving. The field around the cavity can be divided into three zones: critical zone, plastic deformation zone and elastic deformation zone. In the elastic zone, an analytical solution for the distributions of stress and excess pore pressure is deduced according to the elastic theory. In the critical and plastic zone, a set of first?order nonlinear ordinary differential equations concerning stress can be obtained according to the associated flow rule and the lagrangian analysis method. The stressss and pore pore pressure can be solved as an initial value problem starting at the elastic?plastic boundary. The results show that the isotropic over consolidation ratio has a significant influence on the stresses and the excess pore pressure.The shear modulus vary significantly with the cavity radius and the isotropic ove

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为进一步研究复合桩加固液化土地基机理,制备未加固、碎石桩与钢管桩、泥土桩与钢管桩复合加固三种地基模型,模拟地震荷载,进行振动台试验。通过数据采集系统采集三种模型数据,整理出地基在振动过程中不同埋深处的超静孔隙水压力时程曲线和土压力时程曲线。结果表明:未加固、泥土桩与钢管桩复合加固模型超静孔隙水压力增长到峰值7 kPa 左右,保持不变到试验结束,碎石桩与钢管桩复合加固达到峰值为5 kPa 左右,试验结束时减小到2.5 kPa 左右,其中碎石桩起到消散超静孔隙水压力的作用;未加固、泥土桩与钢管桩复合加固的土压力达到峰值105 kPa 左右,之后减小了35 kPa 左右;碎石桩与钢管桩复合加固地基模型土压力值与峰值相等为110 kPa 左右,土体强度较高,复合地基承载能力较大。表明采用碎石桩与钢管桩复合加固不仅有效的抵抗土体液化,而且还提高了复合地基的承载能力,为碎石桩与刚性桩复合加固液化土在实际工程中的推广应用起到参考作用。
In order to study the mechanism of using composite pile to reinforce liquescent soil foun-dation, three models, including un-reinforced foundation, foundation reinforced by gravel pile and steel pipe pile, foundation reinforced by cement pile and steel pipe pile were prepared, and simula-ted seismic load was applied by the shaking table test. Pressure-time curve of excess pore water in different depth and pressure-time curve of earth in different depth were sorted out from the data col-lected by the data acquisition system in the three models during the vibration of foundations. The test results show that the pressure of excess pore water of the un-reinforced and foundation reinforced by cement pile and steel pipe pile was increased to the peak around 7 kPa and the pressure remained 7 kPa until the end of the test. The pressure of excess pore water of the foundation reinforced by gravel pile and steel pipe pile was increased to the peak around 5 kPa and it was reduced to about 2. 5 kPa

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