高压储氢系统泄漏爆炸事故的动力学演化

为研究燃料氢气泄漏、爆炸的特性和规律,预防高压储氢系统中氢气泄漏爆炸事故发生,以加氢站为背景,数值仿真45 MPa高压储罐氢气泄漏并引发爆炸事故,分析泄漏爆炸动力学性质以及爆炸波在非均匀氢气浓度中的传播机制。同时,基于泄漏爆炸事故演化的力学机理,开展氢气泄漏爆炸动态风险分析,针对氢气不同泄漏量,建立泄漏扩散形成的气云体积、气云爆炸产生的冲击波与空间x,z方向上危害距离之间关系。研究结果表明：氢气泄漏过程中,气云氢气浓度变化与流场雷诺数具有较好一致性;氢气扩散受到高压储氢罐周围装置影响,流场中氢气浓度分布不均匀;当发生燃烧爆炸事故时,冲击波参数和湍动能变化梯度大;得到复杂布局区域冲击波超压峰值与比例距离之间关系式,其相比于理论方法更精细、计算结果更准确。研究结果可为降低高压储氢系统泄漏爆炸事故后果、采取有效防护措施提供一定依据。     

波浪与抛石潜堤相互作用的MPS法数值模型研究

为了研究波浪与抛石潜堤相互作用过程中大自由表面变形和堤内渗流等强非线性紊流运动问题,利用改进的MPS法,建立了模拟波浪与抛石潜堤相互作用的MPS法数值计算模型。模型将抛石潜堤假定为均质多孔介质,采用Drew的二相流运动方程描述多孔介质内外的流体运动;通过在动量方程中增加非线性阻力项,并引入亚粒子尺度紊流模型,模拟波浪与可渗结构物相互作用过程中的紊流运动。选取“U”型管中多孔介质内渗流过程和孤立波与可渗潜堤相互作用两个典型的渗流问题,通过将数值计算结果与理论解和实测值的对比分析,对所提出的MPS法紊流渗流模型的模拟精度进行验证。结果表明：基于改进的MPS法构建的垂向二维紊流渗流模型可以很好地再现 “U”型管中多孔介质内渗流以及波浪作用下可渗潜堤内外的复杂流场,显著缓解流-固界面处的压力震荡与粒子分布不均匀问题,实现了较高的模拟精度。     

贯通巷道风流流场数值模拟若干关键问题研究

根据计算流体力学基本理论,利用计算流体动力学(CFD)软件Fluent,运用三维k-ε湍流模型对贯通型巷道风流流场数值模拟中风流入口、出口位置对巷道风流流场分布的影响、湍动能k及湍动能耗散率ε的取值对模拟结果的影响等进行考察。通过研究确定模拟巷道的流体力学入口长度,确定模拟巷道出口位置;湍动能k及湍动能耗散率ε的取值对入口附近流动还没有充分发展区域拟解算的结果影响较大,而对流动充分发展的区域影响较小。将数值模拟风速值与理论计算风速值进行对比,模拟结果与计算结果非常一致,验证了数值模拟方法的正确性,为研究贯通型巷道风流传质过程、瓦斯运移规律及通风排污效率等提供了理论基础。     

Mixing Processes in Geophysical and Astrophysical Flows – A Conference Report

The Third ERCOFTAC conference on `Mixing in Geophysical and Astrophysical Flows' was held at the University of Sheffield over the period 12–14 April 2000. The meeting attracted over forty participants from ten different countries. Some delegates had travelled from as far as U.S.A., Venezuela, Australia, Russia and Sweden to attend the conference. Nine invited papers were presented along with twenty-seven contributed oral presentations and six posters. The main topics discussed included stratified and rotating flows, gravity waves, turbulence and mixing. The presentations are summarised in this report, which aims to provide a broad account of current topics of interest related to mixing processes in geophysical and astrophysical flows.     

Experimental Study of the Criteria of Flow Laminarization in Two-Dimensional Dense Gas Plumes

Laminarization of flow in a two-dimensional dense gas plume was experimentally investigated in this study. The plume was created by releasing CO₂ through a ground-level line source into a simulated turbulent boundary layer over an aerodynamically rough surface in a meteorological wind tunnel. The bulk Richardson number (Ri_*), based on negative plume buoyancy, plume thickness, and friction velocity, was varied over a wide range so that the effects of stable stratification on plume laminarization could be observed. A variety of ambient wind speeds as well as three different sizes of roughness arrays were used so that possible effects of roughness Reynolds number (Re_*) on plume laminarization could also be identified. Both flow visualization methods and quantitative measurements of velocity and intermittency of turbulence were used to provide quantitative assessments of plume laminarization.Flow visualization provided an overall picture of how the plume was affected by the negative buoyancy. With increasing Ri_*, both the plume depth and the vertical mixing were significantly suppressed, while upstream propagation of the plume from the source was enhanced. The most important feature of the flow revealed by visualization was the laminarization of flow in the lower part of the plume, which appeared to be closely related to both Ri_* and Re_*.Measurements within the simulated dense gas plumes revealed the influence of the stable stratification on mean velocity and turbulence intensity profiles. Both the mean velocity and turbulence intensity were significantly reduced near the surface; and these reductions systematically depended on Ri_*. The roughness Reynolds number also had considerable influence on the mean flow and turbulence structure of the dense gas plumes.An intermittency analysis technique was developed and applied to the digitized instantaneous velocity signals. It not only confirmed the general flow picture within the dense plume indicated by the flow visualization, but also clearly demonstrated the changes of flow regime with variations in Ri_* and Re_*. Most importantly, based on this intermittency analysis, simple criteria for characterizing different flow regimes are formulated; these may be useful in predicting when plume laminarization might occur.     

Clustering of aerosols in atmospheric turbulent flow

A mechanism of formation of small-scale inhomogeneities in spatial distributions of aerosols and droplets associated with clustering instability in the atmospheric turbulent flow is discussed. The particle clustering is a consequence of a spontaneous breakdown of their homogeneous space distribution due to the clustering instability, and is caused by a combined effect of the particle inertia and a finite correlation time of the turbulent velocity field. In this paper a theoretical approach proposed in Elperin et al. (2002) Phys Rev E 66:036302 is further developed and applied to investigate the mechanisms of formation of small-scale aerosol inhomogeneities in the atmospheric turbulent flow. The theory of the particle clustering instability is extended to the case when the particle Stokes time is larger than the Kolmogorov time scale, but is much smaller than the correlation time at the integral scale of turbulence. We determined the criterion of the clustering instability for the Stokes number larger than 1. We discussed applications of the analyzed effects to the dynamics of aerosols and droplets in the atmospheric turbulent flow.     

采用大涡PIV研究Taylor-Couette流及其对混凝过程的影响

采用大涡PIV方法对Taylor-Couette流场的湍动能及湍动能耗散率进行了估算,并利用数值模拟对其进行验证,结合絮凝实验,综合对比速度矢量、湍动能分布、湍动能耗散率分布及对应流场中混凝过程的絮体图像,探究了湍动能与湍动能耗散率对絮凝效能的影响.结果表明,大涡PIV法与数值模拟在雷诺数较高的情况下有较好的一致性,且雷诺数越大一致性越好.在Taylor-Couette涡流场中,随着雷诺数的增大,湍动能与湍动能耗散率数值不断增大,且在流场中的分布由规律有序到紊乱最终趋于各向均匀一致.而混凝过程中湍动能与湍动能耗散率的数值大小及其在流场中的空间分布情况,均对产生絮体的大小和浊度去除率有较大影响.     

亚微涡旋的混凝作用研究

以粒子图像速度场仪(PIV)测得了Taylor-Couette反应器旋转内筒和固定外筒间的环隙流场图像.所得图像表明环隙间存在亚微尺度的涡旋.同时实验研究了在Taylor-Couette反应器环隙间不同涡旋形态下聚合氯化铝(PAC)对高岭土悬浊液的混凝效能.结果表明,在波涡流(WVF)形态范围内混凝效能达到了最大(50%以上),这可归因于涡的闭合特性及其随时间的膨胀和收缩.但在波涡流形态范围以外得到的混凝效能相对较低,可归因于相互连通的非闭合涡特性.     

用二阶闭合理论确定的大气扩散系数的分析

本文分析了作者以前得到的一种扩散系数的某些结果,认为这种扩散系数解释了垂直湍流和风切变的联合作用使水平扩散增大的实验观测结果;建立了与雷诺应力间的函数关系,在简化情况下,与泰勒理论得到的结论类似。在边界层低层,湍流扩散系数与粘性系数是不相等的,有时会有较大差别。     

影响静电收尘效率的紊流掺混系数的研究

根据紊流传质原理，在Ｎａｖｉｅｒ－Ｓｔｏｃｋｅｓ和Ｓｈａｕｇｈｎｅｓｓｙ方程的基础上从理论上定量地分析了紊流掺混系数以及对静电收尘效率的影响。该分析结果不仅反应了Ｓｅｌｆ和Ｇ等人的观测结果，而且与Ｒｉｅｈｌｅ等人所做的小型电除尘器的除尘效率测试结果基本一致。