T型管中冷热流体混合过程热波动大涡模拟

在FLUENT平台上,运用大涡模拟湍流模型及Smagorinsky-Lilly亚格子模型,对T型混合结构中的温度波动进行了模拟.获得了分别用于描述时均温度和温度波动强度的无量纲时均温度和无量纲均方根温度.分析了用于热疲劳分析和生命周期评价关键参数,即温度波动的功率谱密度函数.对不同条件下的混合过程进行了模拟,分析不同Reynolds数Re和Richardson数Ri对混合过程和热波动的影响.     

流体饱和多孔介质中波传播问题的有限元分析

采用基于混合物理论的多孔介质模型,给出流体饱和两相多孔介质波动问题的有限元分析方法·　采用罚方法导出的有限元动力方程,时间积分可采用显式和隐式积分两种方案·　用编制的有限元程序分析了一维柱体在跃阶载荷和脉冲载荷作用下的波传播问题,得到该两种瞬态载荷作用下固体和流体相位移、速度以及固体相有效应力和孔隙压力随时间的变化关系,并对波的传播现象进行了分析·　所得结果与理论相吻合·     

多孔介质平板通道发展传热中非局部热平衡时的温度分布特征

研究了多孔介质平板通道中,Darcy流体发展传热强迫对流非局部热平衡下,固相骨架和孔隙流体的温度分布特征．考虑流体流动方向的热传导以及固相和流相相互作用的粘性耗散,根据非局部热平衡的两能量方程模型,得到了常壁温度时多孔介质固相骨架温度和孔隙流体温度的解析解．证明了当两相间的热交换系数趋于无穷大时,两能量方程的温度解趋于局部热平衡时一能量方程的温度解．针对不同的无量纲参数,给出了固相和流相的温度分布状态,通过参数研究,揭示了非局部热平衡强迫对流时温度对无量纲参数的依赖关系．     

相互作用的Brinkman-Forchheimer方程组与Darcy方程组的结构稳定性

研究了在R³中有界区域内的多孔介质中相互作用的Brinkman-Forchheimer流体与Darcy流体方程组解的结构稳定性,假设在Ω₁中流体速度较慢,满足BrinkmanForchheimer方程组,而在Ω₂中,饱和流体满足Darcy方程组.借助于温度的四阶范数估计以及Sobolev不等式,构造能量表达式,推出该表达式所满足的微分不等式,积分得到了相互作用Brinkman-Forchheimer与Darcy流体方程组的解对Brinkman系数的连续依赖性结果.     

多孔介质中两相不可压缩流体的时间局部网格加密有限差分格式

引入Charent压力变量,对于多孔介质中两相不可压缩流体的非混溶驱动问题,其模型表现为耦合的非线性偏微分方程组,一个是压力方程,另一个为饱和度方程．文中考虑一维问题且假定达西速度“已知,建立了在时间上进行局部加密的有限差分格式,给出了饱和度的最大模误差估计．最后给出了数值算例．     

流体饱和多孔隙介质波动方程小波有限差分法

研究流体饱和多孔隙介质中波动方程的数值模拟．针对求解二维弹性波方程问题,提出小波有限差分法．该方法综合了小波多分辨分析计算灵活、计算效率高特性和有限差分易于实现的优点．数值模拟的结果显示,此方法对于求解流体饱和多孔隙介质方程的数值模拟是有效稳定的．     

混合微通道中不稳定的广义Couette流

在一个平行板通道中,部分充满了均匀的多孔介质,部分为纯流体的流动区,对其微通道中完全发展的不稳定层流进行了数值分析,流动由其中一块板的运动和压力梯度所引起.多孔介质区域的流动,采用扩展的Brinkman模型,即Darcy模型,纯净流动区域的流动,采用Stokes方程.还对稳定的完全发展流进行了理论分析,给出了分界面速度、边界板处的速度和表面摩擦的闭式解.通过数值计算发现,稳定完全发展流的闭式解,和不稳定流动的数值解,在所有时间点上得到很好地吻合.     

多孔介质热弥散系数的分形模型北大核心CSCD

热弥散系数是与流体的物性和多孔介质结构有关的,表征多孔介质传热传质强弱的重要参数.该文建立了分形多孔介质的孔喉结构模型,研究了在孔喉结构处流体由湍流状态变为层流状态的局部水头损失和速度弥散效应,在考虑微观孔喉结构和速度弥散效应的影响下,推导了热弥散系数关系式.研究表明,热弥散系数与孔喉比、孔喉结构个数和迂曲分形维数成正比,与孔隙率和面积分形维数成反比.进一步研究发现,孔喉比在1~150范围内对速度弥散效应有显著影响,流体在孔喉结构处存在局部水头损失,导致速度弥散效应增强,热弥散系数增大.     

外形任意的多孔介质轴对称物体中充满非Newton幂律流体时的自然对流

在一个轴对称、外形任意的多孔介质二维体中,充满了有屈服应力的非Newton幂律流体时,数值分析其自由对流及其传热/传质问题．利用相似变换,将边界层控制方程及其边界条件变换为无量纲形式,然后用有限差分法求解该方程组．所研究的参数为流变常数、浮力比和Lewis数．给出并讨论了典型的速度、温度及浓度曲线．发现屈服应力参数值和非Newton流体的幂律指数对结果有着显著的影响．     

微极流体薄膜层通过以滑移速度移动的可渗透无限平板时流体特性变化和热辐射对流动和热传导的影响

微极流体薄膜层通过按滑移速度移动的可渗透无限竖直平板时,研究热辐射对混合对流薄膜层流动和热传导的影响.假定流体粘度和热传导率变化是温度的一个函数.对一些典型的可变参数值,应用Chebyshev谱方法,数值求解流动的控制方程.将所得结果与已发表文献的结果进行比较,结果是一致的.绘出并讨论了可变参数对速度、微旋转速度、温度分布曲线、表面摩擦因数和Nusselt数的影响.     

Stochastic modelling of the heat and moisture transfer in a porous medium

A multi-phase and multi-component flow model with inherent stochastic terms is derived and is used to study the heat and moisture transfer in a fibrous porous medium. The materials’ porosity, velocity derived from Darcy’s law and ambient temperature at the external boundary are treated as white Gaussian noises. An effective multistep implicit splitting finite difference method (FDM) is adopted to solve the strongly coupled non-linear water, energy, vapour and air equations. The existence of a unique solution is analysed through the Lipschitz, monotonicity, growth, hemicontinuity and coercivity conditions. The notion of better thermal comfort arises from the results, as fluctuations are seen to dissipate on approaching the inner boundary (human body). Also, attention is drawn to the significance of considering all necessary uncertain variables in the system of equations. Four scenarios are considered in order to investigate the degree of contribution of the fluctuating terms. Clearly, ignoring certain vital stochastic elements can influence the results. Consequently, a combination of the stochastic porosity, velocity and ambient temperature incorporated into the same multi-phase and multi-component flow model is expected to provide more realistic results.     

Magnetohydrodynamic non-Darcy mixed convection heat transfer from a vertical heated plate embedded in a porous medium with variable porosity

A numerical model is developed to study magnetohydrodynamics (MHD) mixed convection from a heated vertical plate embedded in a Newtonian fluid saturated sparsely packed porous medium by considering the variation of permeability, porosity and thermal conductivity. The boundary layer flow in the porous medium is governed by Forchheimer–Brinkman extended Darcy model. The conservation equations that govern the problem are reduced to a system of non-linear ordinary differential equations by using similarity transformations. Because of non-linearity, the governing equations are solved numerically. The effects of magnetic field on velocity and temperature distributions are studied in detail by considering uniform permeability (UP) and variable permeability (VP) of the porous medium and the results are discussed graphically. Besides, skin friction and Nusselt number are also computed for various physical parameters governing the problem under consideration. It is found that the inertial parameter has a significant influence in increasing the flow field and the rate of heat transfer for variable permeability case. The important finding of the present work is that the magnetic field has considerable effects on the boundary layer velocity and on the rate of heat transfer for variable permeability of the porous medium. Further, the results obtained under the limiting conditions were found to be in good agreement with the existing ones.     

放/吸热流体在两个充满多孔材料的竖直平行板之间作不稳定的自然对流

在一个由两块无限竖直平行板组成的管道中,充满着多孔的介质材料,使用Darcy模型(Brinkman模型的推广)的动量方程,连同能量方程,计算不可压缩、粘性、放/吸热流体在该管道中的不稳定自然对流,即Couette流动.流动是由于边界平板有不对称的加热,以及作加速运动所引起.选用合理的无量纲参数,对控制方程进行简化,通过Laplace变换进行解析求解,得到闭式的速度和温度分布曲线解,随后导出表面摩擦力和传热率.发现在竖直管道中的不同剖面,流体的流动及温度分布曲线随着时间而增加,且在运动平板附近更高.特别是,流体的速度和温度随着平板间距的增加而增加,但是,表面摩擦力和热传导率随着平板间距的增加而减小.     

Gas injection into a moist porous medium with the formation of a gas hydrate

The model problem of the formation of a gas hydrate when a gas is injected into a porous medium, filled in the initial state with a gas and water, is considered in the one-dimensional approximation. A detailed pattern of the seepage flow with phase transitions for different modes of gas injection is obtained. Three seepage modes in a porous medium are possible, which differ qualitatively in the temperature and hydrate saturation fields. At low boundary pressures no hydrate is formed and the temperature distribution increases monotonically. As the boundary pressure increases, when the corresponding values of the pressure and temperature on the phase diagram lie in the region of gas-hydrate stability (below the equilibrium curve), a purely frontal pattern of hydrate formation is obtained with a monotonic temperature distribution. When the boundary pressure is increased further, an extended region of hydrate formation appears with a convex temperature profile, where, depending on the values of the boundary pressure, the hydrate saturation may be continuous (at high boundary pressures) or change abruptly at lower boundary pressures.     

Analytical solutions for movement of cold water thermal front in a heterogeneous geothermal reservoir

In the present study an analytical model has been presented to describe the transient temperature distribution and advancement of the thermal front generated due to the reinjection of heat depleted water in a heterogeneous geothermal reservoir. One dimensional heat transport equation in porous media with advection and longitudinal heat conduction has been solved analytically using Laplace transform technique in a semi infinite medium. The heterogeneity of the porous medium is expressed by the spatial variation of the flow velocity and the longitudinal effective thermal conductivity of the medium. A simpler solution is also derived afterwards neglecting the longitudinal conduction depending on the situation where the contribution to the transient heat transport phenomenon in the porous media is negligible. Solution for a homogeneous aquifer with constant values of the rock and fluid parameters is also derived with an aim to compare the results with that of the heterogeneous one. The effect of some of the parameters involved, on the transient heat transport phenomenon is assessed by observing the variation of the results with different magnitudes of those parameters. Results prove the heterogeneity of the medium, the flow velocity and the longitudinal conductivity to have great influence and porosity to have negligible effect on the transient temperature distribution.     

Effects of Hall current and heat transfer on rotating flow of a second grade fluid through a porous medium

The effects of Hall current and heat transfer on the rotating flow of a second grade fluid past a porous plate with variable suction are examined. The medium considered is porous and suction and external flow velocities vary periodically. The plate is assumed to be at a higher temperature than the fluid. The influences of the Hall parameter and porosity of the medium have been seen and discussed on the velocity and temperature profiles. Moreover, these influences have also been seen on the drag and lateral stress. Finally, the obtained solutions are also compared with the previous studies in the literature and found quite agreement.     

Flow in a porous medium induced by torsional oscillation of a disk near its surface

Torsional oscillation of an infinite disk in a viscous liquid bounded by a porous medium fully saturated with the liquid has been discussed. It is assumed that the flow between the disk and the porous medium is governed by Navier-Stokes equation and that in the porous medium by Brinkman equation. Flows in the two regions are matched at the interface by assuming that the velocity and stress components are continuous at it. It is found that the depth of penetration of the flow in the porous medium is proportional to the square root of the permeability of the medium. The oscillation of the disk induces a steady radial-axial flow in both the regions in such a way that there is a steady axial flow of the fluid from the porous medium to the free flow region i.e. the fluid is expelled out from the porous medium. The steady flow in the porous medium increases with the increase of the permeability of the medium and with the decrease of the distance between the oscillating disk and porous surface.     

Homogenization of a two‐phase incompressible fluid in crossflow filtration through a porous medium

We study the homogenization of a slow viscous two‐phase incompressible flow in a domain consisting of a free fluid domain, a porous medium, and the interface between them. We take into account the capillary forces on the fluid‐fluid interfaces. We construct boundary layers describing the flow at the interface between the free fluid and the porous medium. We derive a macroscopic model with a viscous two‐phase fluid in the free domain, a coupled Darcy law connecting two‐phase velocities in the porous medium, and boundary conditions at the permeable interface between the free fluid domain and the porous medium.     

Reflection of acoustic waves in a cylindrical channel from the perforated part

The reflection and transmission of harmonic waves and waves of finite duration through the boundary of the perforated part of a cylindrical channel (a lined borehole), filled with a fluid and surrounded by a permeable porous medium, is investigated. A model of the plane time-varying fluid flow in the cylindrical channel in a quasi-one-dimensional approximation and of the seepage absorption of the fluid in the porous medium surrounding the channel is presented. The effect of the collector characteristics of the porous medium surrounding the channel and the quality of the perforation (the length of the perforation channels) on the evolution of the waves when they are reflected from the boundary of the perforated part of the wall are investigated.