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671.
为研究筋土界面特性及节点突起对格栅加筋性能的影响,采用三维离散元方法,通过副颗粒的引入从构造上对节点处突起进行了模拟,并对含节点突起的三向土工格栅拉拔过程进行了仿真分析,系统研究了筋-土界面剪胀效应,揭示了宏观强度发展与细观组构演化的内在关联,明确了节点突起对格栅工作性能的改善。研究结果表明,傅里叶系数曲线与拉拔力曲线偏离较大,综合考虑法向接触力幅值与各向异性程度的组构演化系数更能准确反映宏观强度的发展;节点突起调整了纵肋内力分布,允许筋-土间发生较大程度的相对位移,更有助于材料性能的充分发挥。研究成果可为从细观角度优化格栅加筋性能提供参考。 相似文献
672.
AbstractThe suction anchor becomes more popular for offshore oil and gas industry in deeper water. For suction anchor–soil interaction, the prediction of hydraulic conductivity of porous materials is a long-standing problem in offshore engineering. To investigate the hydraulic characteristics, an upward seepage flow through saturated sands is considered in this study. A numerical approach, which is able to describe the fluid–particle interaction at particle scale, has been employed to analyse fluid flow in sands. This approach is constructed by adopting a coupled discrete element method and computational fluid dynamic approach (CFD-DEM numerical model). The coupled CFD-DEM approach is first benchmarked by a classic geomechanics problem where analytical solutions are available, and then employed to investigate the characteristics of upward seepage flow in coarse sand columns. Through numerical modelling, the predicted relation between hydraulic gradient and flow velocity is obtained and it is compared with the classical analytical correlation. The effect of several bulk and micromechanical parameters including packing porosity, particle size combination and inter-particle rolling resistance on the flow characteristics is numerically examined. The results show that the particle polydispersity and packing porosity have significant effect on the hydraulic conductivity in the seepage flow. The introduction of inter-particle rolling resistance can change initial packing structure of particle assembly in some extent rather than the hydraulic conductivity from the particle shape effect perspective. A further development of numerical model, in which the effect of non-spherical particles on the seepage flow, will be carried out later. 相似文献
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675.
山东,既发育着崮群、海岸等具有山东特色的岩溶地貌形态,也发育着泉群、长垣状山体、干谷等中国北方及温带岩溶地貌的典型形态,还发育着洞穴群、漏斗、洼地、峡谷等常见的岩溶地貌形态;它们以寒武系和奥陶系为主的可溶性地层为物质基础,或呈线状,或呈面状,或呈点状分布于众多规模、形态不一,且彼此独立的岩溶孤岛内,是崮群、泉群、洞穴群和海岸等岩溶地貌的典型集中发育区,是展现崮、泉自然美景最杰出的代表地之一。同时在对区域地质地理背景进行分析和研究的基础上,按区域气候特征将山东岩溶地貌划分为半干旱、半湿润、海岸性3类暖温带岩溶地貌区,并系统研究和探讨了山东岩溶"离散型孤岛式"的形成演化过程,认为它是一个能充分展现中国北方及全球温带岩溶地貌复杂演化过程和规律的杰出范例。 相似文献
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677.
多层四流球谐函数算法的构建及在大气辐射传输模式中的应用 总被引:1,自引:0,他引:1
为了在不大幅度增加计算成本的情况下提高大气辐射传输计算的精度,利用单层四流球谐函数结合多层二流累加法,构造了可用于多层大气的四流球谐函数算法。为了比较与其他辐射传输算法的差异,引入48流离散纵坐标算法作为比较标准,Eddington 近似、四流离散纵坐标算法作为比较对象。在真实大气廓线条件下,计算了晴空和有云大气顶向上辐射通量、地表向下辐射通量以及加热率廓线。得出以下结论:在晴空情况下,与作为标准的48流离散纵坐标法相比,Eddington 近似、四流离散纵坐标法和新构造的四流球谐函数方法加热率绝对误差都小于0?3 K/d;向上、向下辐射通量的相对误差分别小于1%和0?6%。这表明在晴空情况下,3种算法对加热率的计算精度差别不大;对辐射通量的计算精度,两种四流近似算法比传统的 Eddington 近似更为精确。在有云情况下,与48流离散纵坐标法相比,四流球谐函数和四流离散纵坐标法计算的云顶加热率相对误差小于1%,而 Eddington 近似计算的云顶加热率相对误差大于5%。结果表明:新构造的四流球谐函数算法可用于大气辐射传输模式,在不大幅度增加计算成本的同时,提高了晴空大气的整体辐射计算精度和有云大气辐射加热率的计算精度。 相似文献
678.
Discrete Element Analysis of Huangtupo Landslide 总被引:5,自引:0,他引:5
On the basis of the deep geology and the geological structure of Huangtupo landslide,and ancient landslide in the reservoir of the Three Gorges,the geo-environmental model of the landslide is es-tablished to analyze quantitatively the sliding mechanism by using the discrete element method.It is con-cluded that interbedding structure of soft and hard formation consists of the main geological background,which induced the arching of the formation under gravity.Stability analysis of different loadings shows that the ground building weight on the middle slope may restrain the extension of shear sliding zone be-low,but may activate the foot area which will reduce the safety factor of the front. 相似文献
679.
Wind‐blown sand movement, considered as a particle‐laden two‐phase flow, was simulated by a new numerical code developed in the present study. The discrete element method was employed to model the contact force between sand particles. Large eddy simulation was used to solve the turbulent atmospheric boundary layer. Motions of sand particles were traced in the Lagrangian frame. Within the near‐surface region of the atmospheric boundary layer, interparticle collisions will significantly alter the velocity of sand. The sand phase is quite dense in this region, and its feedback force on fluid motion cannot be ignored. By considering the interparticle collision and two‐phase interaction, four‐way coupling was achieved in the numerical code. Profiles of sand velocity from the simulations were in good agreement with experimental measurements. The mass flux shows an exponential decay and is comparable to reported experimental and field measurements. The turbulence intensities and shear stress of sand particles were estimated from particle root‐mean‐square velocities. Distributions of slip velocity and feedback force were analysed to reveal the interactions between sand particles and the continuous fluid phase. 相似文献
680.
筒型基础安装过程中,筒内的负压作用会导致土塞现象的出现。以试验模型为基础建立可变形离散元计算模型,通过VC++编制的程序SPSAⅡ对筒型基础负压沉贯中土塞的生成过程进行可视化模拟计算。考虑渗流力、筒壁内外摩擦阻力和筒内负压吸力作为土塞产生的主要外荷载,分别模拟渤海地区3种典型土(黏土、粉土和砂土)的情况。其中,粉土情况下。程序的收敛速度最快,黏土情况下,土塞的计算高度最接近试验测量值,数值计算结果表明该计算方法作为筒型基础施工前筒内土塞高度的预测方法是可行的。 相似文献