透水床面明渠湍流时空平均特征的大涡模拟与分析

基于大涡模拟数据,研究了理想粗糙透水床面明渠湍流的时空平均特性. 考虑到空间异构性,对比分析了不同位置的时空平均流速、雷诺剪应力、构造剪应力、脉动幅度的垂线分布. 结果表明:第一,顶层床面之上,空间异构性的影响较小,不同位置的双平均流速符合类似的对数分布,但由于透水床面影响,卡门常数较不透水床面小;在床面附近,空间异构性影响较大,不同位置的双平均流速分别符合线性分布与多项式分布;在透水河床内部,靠近底层球孔的双平均流速为上部球孔双平均流速的1.55 倍. 第二,床面之上,雷诺剪应力占总剪应力的95% 以上,占有主体地位;床面附近,紊动较大,构造剪应力不能忽略,其值大约占总剪应力的15%.由于流场的各向异性,纵向与垂向的脉动幅度有所差异.      

带滩槽地形的连续弯道中纵向流速横向分布解析

本文基于沿水深积分的动量方程,假定二次流项和弯道附加应力项沿横断面呈线性分布,提出了预测弯道垂线平均纵向流速的解析计算方法,进一步提出了河槽区和河滩区垂线平均纵向流速沿断面分布的求解模式,并将其应用于带滩槽地形的反向连续弯道水槽中.根据实测数据率定计算参数,该模式可计算不同出口水深条件下断面垂线平均纵向流速分布,计算结...     

不同高度柔性植被对坡面流水动力特性的影响

基于系列坡面流试验,研究了柔性植被的高度(4 cm,8 cm和15 cm)对坡面流水动力特性的影响.研究表明:覆盖率相同时,4 cm植被阻水效果最好,15cm最差,而该差异随着坡度增大而减小.4 cm和8 cm植被覆盖时,水流阻力系数随雷诺数增加先减小后增加,这是由于雷诺数较小时水流阻力主要以床面阻力为主,雷诺增大时主要以植被阻力为主.另外,通过染色剂法测得光滑床面平均流速修正系数为0.2～0.4,有植被覆盖床面为0.4～0.8,且修正系数随平均流速增大而增大.     

有限水深中二维湍流边界层的发展

有限水深中湍流边界层主要是指水流在重力作用下绕建筑物流动时的边界层现象。它区别于一般在无限流场中绕流物体的边界层。它的特点是具有自由表面,边界层有可能发展至全部水深,质量力不容忽视,受到外流流速变化的影响。本实验采用激光流速仪量测二维明渠水流沿程各断面的流速分布,根据实验结果,分析研究了有限水深、粗糙壁面条件下,二维湍流边界层的流速分布特征和厚度发展规律,以及孤立粗糙体对此二者的影响。      

基于颗粒离散元的沙纹演变大涡模拟研究

应用大涡模拟、"点球" 浸入边界法和基于"事件驱动" 模型和"弹簧-阻尼" 模型的颗粒离散元法, 数值模拟了明渠湍流中沙纹的演变. 通过对不同谢尔兹数下无沙纹床面的推移质输沙率进行计算, 并与经典输沙率公式进行对比, 验证了模型的精度和可靠性. 随后, 对明渠湍流中沙纹床面的演变过程进行了数值模拟, 计算了有沙纹床面的推移质输沙率、沙纹长度和高度、等效床面高度的最大值、最小值和平均值、沙纹形状阻力、体积流速随时间的变化曲线. 研究发现:初始平整的床面在较短的时间内(tU_b=h≈100) 发展出数条沙纹, 随后沙纹逐渐发展, 在tU_b=h为1 600~2 000 时, 沙纹发生合并. 在沙纹数量不变的条件下, 沙纹高度随时间近似呈线性增长, 而沙纹的长度的平均值却保持恒定. 随着沙纹高度的增大, 输沙率和体积流速逐渐降低, 沙纹形状阻力则逐渐增大;当沙纹发生合并时, 沙纹高度快速增加, 输沙率、体积流速和沙纹形状阻力也出现了大幅跳跃. 在同等的水流强度条件下, 有沙纹床面的输沙率小于平整床面的输沙率.      

不同交汇角度明渠交汇口三维水力特性的大涡模拟研究

采用气液两相流混合模型对不同交汇角度下等宽明渠交汇口三维水力特性进行了数值模拟研究。选取大涡模型(Large Eddy Model)封闭两相流时均方程,求解速度与压力耦合方程组时使用半隐式SIMPLE(Semi-Implicit Method for Pressure-Linked Equations)算法,模拟自由水面采用VOF(Volume of Fluid)法。将交汇角度为90°时采用大涡模型计算得到的纵向截面水面线和不同测线上的速度分布与文献中的试验结果相比较,两者吻合良好,且水面线高度误差在4.2%以内,由此可见大涡模型是模拟交汇口水力特性的有效方法。进而将大涡模型用于模拟交汇角度为30°、45°、60°的交汇口水流,得到交汇口处的水深变化及流场的分布规律,并定量分析了交汇口下游各横断面流速不均匀系数的分布规律。结果表明:在整体上交汇角度越大,交汇口各特征横断面流速不均匀系数越大,即水流流速分布越不均匀。     

辐流式沉淀池固液两相流力学特性数值模拟研究

利用Fluent软件,数值求解Mixture多相流模型,模拟了辐流式沉淀池内固液两相混合流场的水力特性。分析了辐流式沉淀池内污泥浓度场和流线分布随时间的变化,以及沉淀池内不同位置横断面上横向流速和纵向流速的分布规律。模拟结果表明:沉淀池内流线分布形式随时间变化较大,污泥浓度随时间的变化基本稳定;不同位置横断面上流速分布规律不同,越靠近挡板的位置,横断面的流速沿水深方向变化梯度越大,说明流场紊动较强;到沉淀池后部,横断面上流速分布较均匀,沿水深方向变化梯度也较小。     

定床弯道内水沙两相运动的数值模拟

在适体同位网格中采用非正交曲线坐标系下的三维k-ε-kp固液两相双流体湍流模型研究弯道内水流和悬浮泥沙运动,主要计算了试验室S型水槽内清水流动的三维流场、120°弯道内水沙两相流动中底沙与底流的运动轨迹以及S型水槽内水沙两相流动的两相流场和泥沙浓度场. 对于S型水槽内清水流动,数值结果与试验结果吻合良好. 120°弯道内水沙两相流动中固液两相的运动轨迹在弯道直线段基本重合,在弯道内泥沙轨迹逐步偏离水体轨迹,其偏离程度随泥沙粒径增大而增大. 从S型水槽内水沙两相流动计算结果中发现泥沙纵向流速在壁面附近比水流纵向速度大,在远离壁面区域比水流纵向速度小;弯道内泥沙横向流速比水流横向流速小;垂向流速在直线段和泥沙沉速相当,在弯道内受螺旋水流影响而变化;两相流速差别随泥沙粒径增大而变大;泥沙浓度呈现下浓上稀的分布,在弯道内横向断面上呈现凸岸大凹岸小的分布,泥沙浓度随泥沙粒径增大而减小.      

自由水跃区壁面阻力的研究

根据已有文献对附壁射流区流速分布和壁面阻力的试验成果,分析了自由水跃区断面流速分布和最大流速沿程分布规律;首次根据边界层的动量积分方程分析了水跃主体段的射流厚度、水跃区的壁面切应力系数、壁面阻力系数的变化规律;给出了边界层厚度、壁面局部阻力系数、壁面阻力系数、平均壁面阻力系数的计算方法,并将计算结果与已有文献的试验资料进行了比较。结果表明:由本文式(9)和式(26)得到的数据与文献中的试验数据吻合较好;在Fr1≥5.45时,式(29)的计算结果与试验较吻合,在Fr1?5.45时,其计算结果与试验偏差较大;采用本文公式(34)计算水跃的共轭水深,与文献所得结果的最大误差为3.643%。     

一种新的往复流试验平台及其泥沙冲刷试验研究

本文提出一种可以模拟潮流运动的自动化控制水槽。该水槽可以时控制往复流两端的水位,实现流的往复运动,并可以按计算机要求实现水位的稳定或渐变。本文同时利用该水槽进行了圆柱开桥墩周围的测试数据、照片为基础、分析了不同水流条件下圆柱形桥墩周围的床面冲刷情况。试验发现在桥墩附近,水流的旋滚运动及旋涡系是造成床面冲刷的主要原因,另外对于往复流情况,桥墩附近床面受到的冲刷比固定水位冲刷时要严重,也更为复杂 。     

Analytical solutions for transverse distributions of stream-wise velocity in turbulent flow in rectangular channel with partial vegetation

The theory of poroelasticity is introduced to study the hydraulic properties of the steady uniform turbulent flow in a partially vegetated rectangular channel. Plants are assumed as immovable media. The resistance caused by vegetation is expressed by the theory of poroelasticity. Considering the influence of a secondary flow, the momentum equation can be simplified. The momentum equation is nondimensionalized to obtain a smooth solution for the lateral distribution of the longitudinal velocity. To verify the model, an acoustic Doppler velocimeter (ADV) is used to measure the velocity field in a rectangular open channel partially with emergent artificial rigid vegetation. Comparisons between the measured data and the computed results show that the method can predict the transverse distributions of stream-wise velocities in turbulent flows in a rectangular channel with partial vegetation.     

Velocity distribution of flow with submerged flexible vegetations based on mixing-length approach

By choosing a PVC slice to simulate flexible vegetation, we carried out experiments in an open channel with submerged flexible vegetation. A 3D acoustic Doppler velocimeter （micro ADV） was used to measure local flow velocities and Reynolds stress. The results show that hydraulic characteristics in non-vegetation and vegetation layers are totally different. In a region above the vegetation, Reynolds stress distribution is linear, and the measured velocity profile is a classical logarithmic one. Based on the concept of new-riverbed, the river compression parameter representing the impact of vegetation on river is given, and a new assumption of mixing length expression is made. The formula for time-averaged velocity derived from the expression requires less parameters and simple calculation, and is useful in applications.     

Improvement of Acoustic Doppler Velocimetry in bubbly flow measurements as applied to river characterization for kinetic turbines

Acoustic Doppler Velocimetry (ADV) can measure flow velocities in three directions in experimental facilities and field applications. Based on the Doppler shift effect, ADV can accurately resolve the quasi-instantaneous flow field at frequencies of up to approximately 200 Hz. However, this technique is sensitive to operating conditions that can lead to contaminated signals containing large amplitude spikes, a disadvantage of ADV. Aliasing of the Doppler signal creates these spikes. Such a situation occurs when large particles intersect the sampling volume or acoustic waves. For example during the characterization of river velocities, sediments floating near the riverbed cause aliasing from particles, and more importantly, surface entrained air bubbles contaminate the ADV signal. Spikes due to air bubbles not only increase the standard deviation of the velocity, but also corrupt the autocorrelation and power spectra. As some of these spikes appear like velocity fluctuations, developing accurate despiking procedures is an important requirement during post-processing of ADV velocity measurements in bubbly flow applications. A new hybrid method is introduced which has advantages over conventional despiking methods such as the acceleration thresholding method and the phase-space thresholding method when using ADV in bubbly flow. ADV river velocity measurements near kinetic turbines demonstrate the proposed method. This method is applicable to other bubbly flow applications to characterize the liquid phase using ADV.     

Flow characteristics of rectangular open channels with compound vegetation roughness

An idealized parallel flow caused by a lateral bed roughness difference due to the partial vegetation across a channel is investigated. Similar to the flow in a compound channel, there are mixing layers adjacent to the interface between the vegetation and the non-vegetation lanes, and a lateral momentum exchange occurs between the slow-moving water in the former lane and the fast-moving water in the latter lane. Under a uniform flow condition, the three-dimensional (3D) instantaneous velocities of two cases with different discharges and water depths are measured with a 16MHz acoustic Doppler velocimeter (micro ADV). The longitudinal variation of the streamwise velocity and the vertical variation of the Reynolds stress are analyzed. A quadrant analysis is carried out to investigate the outward and inward interaction, ejection, and sweep phenomenon caused by the vegetation variation across the channel. The results show that the flow characteristics in the vegetation lane are similar to those in an open channel fully covered with submerged vegetation, and the flow characteristics in the smooth non-vegetation lane are similar to those in a free open channel. For the cases studied here, the width of the mixing region is about 10% of the channel width, and the mixing region is mainly on the non-vegetation half.     

Integrated numerical model for vegetated surface and saturated subsurface flow interaction

The construction of an integrated numerical model is presented in this paper to deal with the interactions between vegetated surface and saturated subsurface flows. A numerical model is built by integrating the previously developed quasi-three-dimensional (Q3D) vegetated surface flow model with a two-dimensional (2D) saturated groundwater flow model. The vegetated surface flow model is constructed by coupling the explicit finite volume solution of 2D shallow water equations (SWEs) with the implicit finite difference solution of Navier-Stokes equations (NSEs) for vertical velocity distribution. The subsurface model is based on the explicit finite volume solution of 2D saturated groundwater flow equations (SGFEs). The ground and vegetated surface water interaction is achieved by introducing source-sink terms into the continuity equations. Two solutions are tightly coupled in a single code. The integrated model is applied to four test cases, and the results are satisfactory.     

Two dimensional analytical solution for a partially vegetated compound channel flow

The theory of an eddy viscosity model is applied to the study of the flow in a compound channel which is partially vegetated. The governing equation is constituted by analyzing the longitudinal forces acting on the unit volume where the effect of the vegetation on the flow is considered as a drag force item, The compound channel is divided into 3 sub-regions in the transverse direction, and the coefficients in every region＇s differential equations were solved simultaneously. Thus, the analytical solution of the transverse distribution of the depth-averaged velocity for uniform flow in a partially vegetated compound channel was obtained. The results can be used to predict the transverse distribution of bed shear stress, which has an important effect on the transportation of sediment. By comparing the analytical results with the measured data, the analytical solution in this paper is shown to be sufficiently accurate to predict most hydraulic features for engineering design purposes.     

Dynamic coupling of fluid and structural mechanics for simulating particle motion and interaction in high speed compressible gas particle laden flow

In this work, structural finite element analyses of particles moving and interacting within high speed compressible flow are directly coupled to computational fluid dynamics and heat transfer analyses to provide more detailed and improved simulations of particle laden flow under these operating conditions. For a given solid material model, stresses and displacements throughout the solid body are determined with the particle–particle contact following an element to element local spring force model and local fluid induced forces directly calculated from the finite volume flow solution. Plasticity and particle deformation common in such a flow regime can be incorporated in a more rigorous manner than typical discrete element models where structural conditions are not directly modeled. Using the developed techniques, simulations of normal collisions between two 1 mm radius particles with initial particle velocities of 50–150 m/s are conducted with different levels of pressure driven gas flow moving normal to the initial particle motion for elastic and elastic–plastic with strain hardening based solid material models. In this manner, the relationships between the collision velocity, the material behavior models, and the fluid flow and the particle motion and deformation can be investigated. The elastic–plastic material behavior results in post collision velocities 16–50% of their pre-collision values while the elastic-based particle collisions nearly regained their initial velocity upon rebound. The elastic–plastic material models produce contact forces less than half of those for elastic collisions, longer contact times, and greater particle deformation. Fluid flow forces affect the particle motion even at high collision speeds regardless of the solid material behavior model. With the elastic models, the collision force varied little with the strength of the gas flow driver. For the elastic–plastic models, the larger particle deformation and the resulting increasingly asymmetric loading lead to growing differences in the collision force magnitudes and directions as the gas flow strength increased. The coupled finite volume flow and finite element structural analyses provide a capability to capture the interdependencies between the interaction of the particles, the particle deformation, the fluid flow and the particle motion.     

Particle imaging velocimetry of a wet aqueous foam with an underlying liquid film

 We investigate the utility of particle imaging velocimetry (PIV) for performing kinematic measurements in wet aqueous foam with a liquid film beneath it. The flow velocities are measured near the walls of a square cross-section horizontal duct. The flow velocities are useful for validating the rheological models. We show that there is a discrepancy between the velocity profiles in the wet foam and the Bingham plastic model of flow. The velocity measurements reveal a more complex flow pattern, which may be analysed following three different regimes: a plug flow, a shear flow in a vertical plane and a three-dimensional shear flow. The transition between the plug flow and the shear flows may be explained by a shear-induced migration of bubbles. Received: 25 April 2000 / Accepted: 26 February 2001     

Acoustic Doppler velocimeter-induced acoustic streaming and its implications for measurement

The acoustic Doppler velocimeter (ADV) is widely used for the characterization of fluid flow. Secondary flows (“acoustic streaming”) generated by the ADV’s acoustic pulses may affect the accuracy of measurements in experiments with small velocities. We assessed the impact of acoustic streaming on flow measurement using particle image velocimetry. The probes of two different ADVs were successively mounted in a tank of quiescent water. The probes’ ultrasound emitters were aligned with a laser light sheet. Observed flow was primarily in the axial direction, accelerating from the ultrasound emitter and peaking within centimeters of the velocimeter sampling volume before dropping off. We measured the dependence of acoustic streaming velocity on ADV configuration, finding that different settings induce streaming ranging from negligible to more than 2.0 cm s⁻¹. From these results, we describe cases where acoustic streaming affects velocity measurements and also cases where ADVs accurately measure their own acoustic streaming.