山体尾流对烟羽扩散影响的风洞实验

本文以中性模拟的相似参数为判据,用四种不同的方法探测组合山体的流场.根据探测结果,探讨了尾流的结构并进行了较细致的区划.指出复杂地形的摩擦速度(u~*)在近地层不为常数.文中还讨论了尾流中扩散参数的变化及烟羽轴线下倾角分布,指出用修正的高斯烟羽模式描述尾流浓度场的可行性.风洞的实验结果与现场实验结果基本一致.     

Flow and dispersion of pollutants within two-dimensional valleys

Wind tunnel experiments and a theoretical model concerning the flow structure and pollutant diffusion over two-dimensional valleys of varying aspect ratio are described and compared. Three model valleys were used, having small, medium, and steep slopes. Measurements of mean and turbulent velocity fields were made upstream, within and downwind of each of these valleys. Concentration distributions were measured downwind of tracer sources placed at an array of locations within each of the valleys. The data are displayed as maps of terrain amplification factors, defined as the ratios of maximum ground-level concentrations in the presence of the valleys to the maxima observed from sources of the same height located in flat terrain. Maps are also provided showing the distance to locations of the maximum ground-level concentrations. The concentration patterns are interpreted in terms of the detailed flow structure measured in the valleys. These data were also compared with results of a mathematical model for treating flow and dispersion over two-dimensional complex terrain. This model used the wind tunnel measurements to generate mean flow fields and eddy diffusivities, and these were applied in the numerical solution of the diffusion equation. Measured concentration fields were predicted reasonably well by this model for the valley of small slope and somewhat less well for the valley of medium slope. Because flow separation was observed within the steepest valley, the model was not applied in this case.     

Wind field and dispersion in a built-up area—A comparison between field measurements and wind tunnel data

The dispersion of accidentally released gases from sources near the ground in built-up areas is determined by the complex flow conditions around the buildings. Wind tunnel experiments must be performed to obtain detailed information on the diffusion of pollutants. In order to show that the wind tunnel results are transferable to nature, parallel measurements in a wind tunnel and for prototype conditions of wind direction, wind velocity, and gas dispersion have been carried out in an industrial plant. The results show excellent agreement of model and prototype for properly scaled conditions.     

A new wind tunnel technique for investigating gas diffusion behind a structure

We predicted the diffusion of exhaust gas without thermal buoyancy from the top of a structure in down-wash under the influence of a structure by means of wind tunnel. We reproduced a wind directional fluctuation σ_A of about 10° in a wind tunnel.The present experimental method and experimental results are introduced here. Wind directional fluctuation was simulated by means of turntable equipment which rotated the model according to probability of wind direction in the field. In measuring concentration, NH₃ as tracer gas was used and a sampling method was adopted. The tracer gas was continuously sampled while rotating the model. As a result the sampled gas concentration was integrated with the weight according to the probability of each wind direction.We compared results of this wind tunnel experiment with the field test and the reliability of this prediction method was confirmed.     

河谷型城市风场及污染物扩散的CFD数值仿真

为研究河谷型城市地形及其引起的风场和污染物扩散的复杂问题,利用CFD（计算流体力学）方法和复杂地形网格生成技术,建立河谷型城市风场及大气污染分布的数值仿真模型,实现CFD方法在复杂地形空气运动和污染物扩散方面的应用.分别使用LES（large eddy simulation）模型和mixture模型研究兰州市地面风场特征和污染物扩散形态,计算得到的污染物分布结果与实测结果分布一致.结果表明:复杂地形对空气运动的影响很大,如风速因山体屏障作用会呈现带状分布特征,山体后侧易出现弱风区域;同时,风场会密切影响污染物扩散,决定了污染物扩散形态,如幅散能够影响污染物扩散范围及污染水平.而给定西北风条件下,如地面以上10 m、风速为5 m/s、不受地形阻挡情况下,工业区污染物浓度被稀释10倍,约扩散2.2 km;山体阻挡会抑制污染物纵向扩散,表现在山体阻挡情况下污染物稀释100倍时的扩散长度约为相对平坦区域的1/3.此外,不同的入口风向会引起空气运动与山体相互作用发生变化,进而会使得地面风速、局部风场存在差异,造成污染物扩散及分布形态差异.研究显示,CFD方法可行,模型可靠,可以用来研究地形对风场和污染物扩散的影响.      

Fluid modeling applied to atmospheric diffusion in complex terrain

Wind-tunnel and towing-tank studies conducted over the past 10 years at the U.S. Environmental Protection Agency's Fluid Modeling Facility (FMF) of flow and diffusion in complex terrain are reviewed. A primary impetus for this work was EPA's Complex Terrain Model Development Program (CTMDP)—designed to develop reliable atmospheric dispersion models applicable to large pollutant sources in complex terrain, with primary emphasis on plume impaction during night-time stable conditions. The FMF interacted closely with the model developers participating in the CTMDP and provided support in various ways through the conduct of a wide range of laboratory studies. Work at the FMF prior to the inception of the program provided the basic framework for the model—the dividing-streamline concept— and the focal point around which the field program was designed. At the beginning of the program, the FMF provided direct support as an aid to planning the details and strategies of the field experiments and testing the limits of applicability of the dividing-streamline concept. Later work included exercises of ‘filling in the gaps’ in the field data, furthering the understanding of the physical mechanisms important to plume impaction in complex terrain and in stably stratified flows in general, testing various modeling assumptions, providing data for ‘calibration’ of various modeling parameters, and testing the ability of the laboratory models to simulate full-scale conditions. Simultaneously, the FMF responded to the needs of the regulatory arm of EPA, the Office of Air Quality Planning and Standards (OAQPS), by providing guidance concerning expected terrain effects and by conducting demonstration studies. These latter studies were concerned primarily with simulation of diffusion in the neutral atmospheric boundary layer. Finally, several supplemental studies were conducted, broadening and expanding upon the specific requests of the model developers and the OAQPS. The highlights of the FMF complex-terrain research work are described herein.     

复杂地形机械湍流扩散的粒子随机行走模拟

应用粒子随机行走模拟方法模拟了高架点源在中性情况下在复杂地形上的排放,并将模拟结果与风洞实验进行了比较,二者能较好地吻合。虽然将该方法用于复杂地形大气扩散计算在技术上不存在什么困难,但是在确定模式基本参数等方面,还应该慎重考虑。      

桃花江核电厂冷却塔对近场流动影响的风洞试验研究

采用雷诺数自准准则作为动力相似的判据,对冷却塔等建筑物及周围复杂地形进行风洞模拟.风洞实验采用1:1500的缩比模型,通过模拟实验,研究桃花江核电厂厂址冷却塔等建筑物及山体对厂址近场流场、放射性核素迁移扩散的影响,获得厂址近场大气扩散特征.实验表明:山体(建筑物)的存在引起流场的空气动力学畸变,越过山体(建筑物)各测点...     

Mesoscale meteorological modelling for Hong Kong-application of the MC2 model

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建筑物尾流区气流与污染物扩散的数值计算

采用了细网格非静力能量闭合边界层模式和随机游动模拟方法建立了一套分析建筑物尾流流场和污染物扩散的数值模拟系统．作为应用研究的例子，在对某城市地下交通隧道排废气的风井塔尾流区流场和浓度场进行风洞流体物理实验的基础上，利用所建的模拟系统对风井塔尾流区气流和污染物扩散特征进行研究．结果表明，所建的模拟系统的模拟结果与风洞试验的结果吻合较好，对一些小尺度带有明显湍流不均匀性的流场和局地空气污染物散布的情况有较好的模拟效果和良好的应用前景．     

Simulation analysis of environmental risk accident and management of high-sulfur gas field development in complex terrain

Environmental risk of high sulfur gas field exploitation has become one of the hot spots of environmental management studies. Severe gas H₂S blowout accidents in recent years have shown that poor understanding and estimates of the poisonous gas movement could lead to dangerous evacuation delays. It is important to evaluate the real concentration of H₂S, especially in complex terrain. Traditional experiential models are not valid in the case of rough terrain, especially in low-lying areas where the gas accumulates. This study, using high sulfur content gas field of Sichuan “Pu Guang gas field” as study object and adopting objective diagnosis of wind field of land following coordinate three dimensions, applied Lagrangian Puff Model and breaking up technique of puffs to simulate the H₂S diffusion condition of blowout accidents produced in the high sulfur content gas field of complex terrain area. The results showed that the H₂S distribution did not occur mainly in low wind direction, and due to the obstruction of the mountain’s body, it accumulated in front of mountain on produced turn over, flowed around submitted jumping type distribution. The mountain waist near the hilltop and low hollow river valley site rapture points simulating contrast showed that the higher the rapture point, the better the diffusing condition of pollutant, the distribution of risk sensitive point decided piping rupture environmental risk size combining the H₂S diffusion result and residential area dispersing in the study area, synthetic judge located in the high rapture point environmental risk was smaller than the low hollow point, thus it was suggested to carryout laying of lining build of equal high line of higher terrain. According to simulation results, the environmental risk management measures aimed at putting down adverse effects were worked out.     

城市中心街道交通隧道废气排放模拟

利用风洞试验、模式预测和现场监测的方法,对某城市中心街道交通隧道汽车废气的扩散特征作了模拟研究。结果表明,环境中汽车尾气污染程度与隧道中汽车行驶工况、车流量、气象条件（温度、风速、风向）等诸多因素有关。随着环境风速减小或环境气温升高,隧道外废气浓度显著增加。隧道出口至离出口90m处的引道范围是污染物高浓度区域,但废气排放对引道两侧离地面较高的匝道影响较小。对模式预测结果和风洞测量结果、现场监测结果作了比较,一致性良好     

Study on the wind field and pollutant dispersion in street canyons using a stable numerical method

A stable finite element method for the time dependent Navier-Stokes equations was used for studying the wind flow and pollutant dispersion within street canyons. A three-step fractional method was used to solve the velocity field and the pressure field separately from the governing equations. The Streamline Upwind Petrov-Galerkin(SUPG) method was used to get stable numerical results. Numerical oscillation was minimized and satisfactory results can be obtained for flows at high Reynolds numbers. Simulating the flow over a square cylinder within a wide range of Reynolds numbers validates the wind field model. The Strouhal numbers obtained from the numerical simulation had a good agreement with those obtained from experiment. The wind field model developed in the present study is applied to simulate more complex flow phenomena in street canyons with two different building configurations. The results indicated that the flow at rooftop of buildings might not be assumed parallel to the ground as some numerical modelers did. A counter-clockwise rotating vortex may be found in street canyons with an inflow from the left to right. In addition, increasing building height can increase velocity fluctuations in the street canyon under certain circumstances, which facilitate pollutant dispersion. At high Reynolds numbers, the flow regimes in street canyons do not change with inflow velocity.     

榆中县城大气污染物扩散的观测实验与数值模拟

结合榆中县外场观测实验资料,利用计算流体动力学CFD (Fluent)软件对榆中县城区的流场和污染物扩散形态及规律进行了模拟研究.根据实际测量数据,利用Gambit软件建立了榆中县城区的三维城市建筑模型,导入Fluent进行模拟计算,对模拟结果与观测数据进行了对比分析,结果显示Fluent对流场和污染物扩散的模拟具有较好的一致性;具体而言,对风向、风速的模拟值与观测值的总体相似系数分别为0.876和0.843,对0.5m和27m高度处污染物模拟值和观测值的相关系数分别为0.71和0.72.因此,Fluent软件可用于城市污染扩散的模拟研究,也可以根据其模拟结果指导空气质量检测点的布设.     

有限体积法软件在天然气处理厂含硫气体三维扩散模拟中的应用

应用基于流体动力学原理的CFD方法,用有限体积法软件进行了某天然气处理厂脱硫塔泄漏后在复杂三维地形的仿真扩散模拟,计算结果能够较真实地反映气体扩散过程受三维复杂地形和风速的影响情况,为定量风险评价和企业安全生产管理提供技术支撑。     

海岸地区三维风场与污染物输送扩散模式

首先建立了一个复杂地形条件下的中尺度三维边界层预报模式,模拟研究了局地海陆风环流条件下的三维风场。并将其输出直接作为一个三维欧拉数值模式的输入,以模拟沿海地区海陆风演变过程中,空气污染物(SO_2)浓度的时空分布。为更接近实际,还专门建立了一个只需少量常规气象资料输入的背景风诊断模式。较好地完成了这三个模式间的联接。实例模拟计算的结果表明,此联接模式是行之有效的。     

汽车环境风洞地面区域流场数值仿真

目的 探究汽车环境风洞地面区域流场规律,获取风洞边界层抽吸装置的最佳抽吸率和底盘测功机对风洞地面区域边界层厚度、风速、总压和静压的影响规律,并比较MRF法和旋转壁面法对底盘测功机转毂转动模拟的精度。方法 运用计算流体动力学方法对汽车环境风洞流场进行数值仿真计算。结果 边界层抽吸装置对应于喷口风速120 km/h时的最佳抽吸率为0.048。底盘测功机区域总压呈现下降趋势。相比于存在底盘测功机,汽车环境风洞无底盘测功机时,底盘测功机区域内相同位置的边界层厚度会增加1.28～12.22 mm。在前转毂的前侧、上侧、后侧和后转毂的上侧和后侧会有一个高风速区域,区域内风速比设定风速高1%～4%,与无底盘测功机相比,区域内静压值低0.32～46.02 Pa。在前后转毂前侧和后侧与地面相连接的凹部会有一个低风速区域,区域内风速比设定风速低1%～5%,与无底盘测功机相比,区域内静压值高0.08～49.34 Pa。底盘测功机转毂的转动会使附近区域的地面边界层厚度变大。在前转毂前侧,采用旋转壁面法进行模拟比MRF法地面边界层厚度增加近8 mm,而在其他位置,2种模拟方法对边界层厚度的模拟差别在1.5 mm...     

Simulation of dispersion in moderately complex terrain—Part C. A dispersion model for operational use

An operational dispersion model for use in areas with complex terrain is presented. The model uses mean and turbulence quantities simulated with the fluid dynamic model presented in Part A. A large number of wind and turbulence fields are simulated with the fluid dynamic model. These simulations are put into a database and can be used in the calculations of dispersion with the operational model. To get relevant meteorological data for the model a Doppler sodar and a 10 m high mast with a temperature profile and wind and wind direction at one level are used. The model calculates a trajectory for the plume centerline from the simulated wind field, and approximates the concentration field with a bi-Gaussian distribution. For convective conditions the mixing height and the surface heat flux, used as input for the model, are being determined from the sodar measurements through relations related to the temperature structure parameter C_T² and the standard deviation of the vertical velocity. The horizontal and vertical standard deviations for the plume are determined by using the simulated turbulence quantities from the dynamic model and Eulerian velocity spectra. Simulations with the model is compared with dispersion measurements performed in an area in the southern Sweden, the Vänersborg-Trollhättan region. The geographical area is characterized by topographical features on the meso-γ-scale, i.e. 2–20 km. Thus there are forested hills, a relatively flat agricultural area and an extended lake area within the model domain. The terrain height relief is typically 80 m. The simulations show, in general, good agreement with the measured data both for unstable and stable stratifications.     

Building wake dispersion at an Arctic industrial site: Field tracer observations and plume model evaluations

Ten multi-hour atmospheric dispersion SF₆ tracer experiments were conducted during October and November of 1987 near a large oil gathering facility in the Prudhoe Bay, Alaska, oilfield reservation. The purpose of this study was to investigate dispersion under arctic conditions and in situations where building-generated airflow disturbances dominate downwind distributions of ground level pollutant concentrations. This was accomplished with a network of micrometeorological instruments, portable syringe tracer samplers, continuous tracer analyzers, and infrared visualization of near source plume behavior.Atmospheric stability and wind speed profiles at this arctic site are influenced by the smooth (surface roughness = 0.03 cm), snow covered tundra surface which receives negligible levels of solar isolation in winter. The dispersion of pollutants emitted from sources within the oil gathering facility, however, is dominated by the influence of nearby buildings when high winds generate elevated ground level concentrations. An order of magnitude increase in maximum ground level concentration was observed as wind speeds increased from 5 to 8 m s⁻¹ and another order of magnitude increase was observed as winds increased from 8 to 16 m s⁻¹. Variation in maximum concentrations was also observed with changes in wind direction. Vertical plume diffusion (σ_z) near the buildings was a factor of 2–3 greater than that observed in open terrain and was dependent on both wind speed and the projected building width and location of nearby buildings. Wind tunnel tracer distributions for east winds agree with field observations but also indicate that a significant increase in plume downwash occurs with other wind directions. Concentration distributions were calculated using several versions of the Industrial Source Complex (ISC) model. Model estimates of ground level concentrations were within a factor of three depending on wind direction. The model predictions are extremely sensitive to the ratio of plume height to vertical plume diffusion which is significantly influenced by a complex aerodynamic wake in the field.