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1.
We report non-equilibrium molecular dynamics simulations of rigid and non-rigid dumbbell fluids to determine the contribution of internal degrees of freedom to strain-rate-dependent shear viscosity. The model adopted for non-rigid molecules is a modification of the finitely extensible nonlinear elastic (FENE) dumbbell commonly used in kinetic theories of polymer solutions. We consider model polymer melts — that is, fluids composed of rigid dumbbells and of FENE dumbbells. We report the steady-state stress tensor and the transient stress response to an applied Couerte strain field for several strain rates. We find that the rheological properties of the rigid and FENE dumbbells are qualitatively and quantitatively similar. (The only exception to this is the zero strain rate shear viscosity.) Except at high strain rates, the average conformation of the FENE dumbbells in a Couette strain field is found to be very similar to that of FENE dumbbells in the absence of strain. The theological properties of the two dumbbell fluids are compared to those of a corresponding fluid of spheres which is shown to be the most non-Newtonian of the three fluids considered.Symbol Definition b dimensionless time constant relating vibration to other forms of motion - F force on center of mass of dumbbell - F i force on bead i of dumbbell - F force between center of masses of dumbbells and - F ij force between beads i and j - h vector connecting bead to center of mass of dumbbell - H dimensionless spring constant for dumbbells, in units of / 2 - I moment of inertia of dumbbell - J general current induced by applied field - k B Boltzmann's constant - L angular momentum - m mass of bead, (= m/2) - M mass of dumbbell, g - N number of dumbbells in simulation cell - P translational momentum of center of mass of dumbbell - P pressure tensor - P xy xy component of pressure tensor - Q separation of beads in dumbbell - Q eq equilibrium extension of FENE dumbbell and fixed extension of rigid dumbbell - Q 0 maximum extension of dumbbell - r ij vector connecting beads i and j - r position vector of center of mass dumbbell - R vector connecting centers of mass of two dumbbells - t time - t * dimensionless time, in units of m/ - T * dimensionless temperature, in units of /k - u potential energy - u velocity vector of flow field - u x x component of velocity vector - V volume of simulation cell - X general applied field - strain rate, s–1 - * dimensionless shear rate, in units of /m 2 - general transport property - Lennard-Jones potential well depth - friction factor for Gaussian thermostat - shear viscosity, g/cms - * dimensionless shear viscosity, in units of m/ 2 - * dimensionless number density, in units of –3 - Lennard-Jones separation of minimum energy - relaxation time of a fluid - angular velocity of dumbbell - orientation angle of dumbbell   相似文献   

2.
The objective of this paper is to present an overview of the fundamental equations governing transport phenomena in compressible reservoirs. A general mathematical model is presented for important thermo-mechanical processes operative in a reservoir. Such a formulation includes equations governing multiphase fluid (gas-water-hydrocarbon) flow, energy transport, and reservoir skeleton deformation. The model allows phase changes due to gas solubility. Furthermore, Terzaghi's concept of effective stress and stress-strain relations are incorporated into the general model. The functional relations among various model parameters which cause the nonlinearity of the system of equations are explained within the context of reservoir engineering principles. Simplified equations and appropriate boundary conditions have also been presented for various cases. It has been demonstrated that various well-known equations such as Jacob, Terzaghi, Buckley-Leverett, Richards, solute transport, black-oil, and Biot equations are simplifications of the compositional model.Notation List B reservoir thickness - B formation volume factor of phase - Ci mass of component i dissolved per total volume of solution - C i mass fraction of component i in phase - C heat capacity of phase at constant volume - Cp heat capacity of phase at constant pressure - D i hydrodynamic dispersion coefficient of component i in phase - DMTf thermal liquid diffusivity for fluid f - F = F(x, y, z, t) defines the boundary surface - fp fractional flow of phase - g gravitational acceleration - Hp enthalpy per unit mass of phase - Jp volumetric flux of phase - krf relative permeability to fluid f - k0 absolute permeability of the medium - Mp i mass of component i in phase - n porosity - N rate of accretion - Pf pressure in fluid f - pca capillary pressure between phases and =p-p - Ri rate of mass transfer of component i from phase to phase - Ri source source rate of component i within phase - S saturation of phase - s gas solubility - T temperature - t time - U displacement vector - u velocity in the x-direction - v velocity in the y-direction - V volume of phase - Vs velocity of soil solids - Wi body force in coordinate direction i - x horizontal coordinate - z vertical coordinate Greek Letters p volumetric coefficient of compressibility - T volumetric coefficient of thermal expansion - ij Kronecker delta - volumetric strain - m thermal conductivity of the whole matrix - internal energy per unit mass of phase - gf suction head - density of phase - ij tensor of total stresses - ij tensor of effective stresses - volumetric content of phase - f viscosity of fluid f  相似文献   

3.
Two thermodynamical models of pseudoelastic behaviour of shape memory alloys have been formulated. The first corresponds to the ideal reversible case. The second takes into account the hysteresis loop characteristic of this shape memory alloys.Two totally independent techniques are used during a loading-unloading tensile test to determine the whole set of model parameters, namely resistivity and infrared thermography measurements. In the ideal case, there is no difficulty in identifying parameters.Infrared thermography measurements are well adapted for observing the phase transformation thermal effects.Notations 1 austenite 2 martensite - () Macroscopic infinitesimal strain tensor of phase - (2) f Traceless strain tensor associated with the formation of martensite phase - Macroscopic infiniesimal strain tensor - Macroscopic infinitesimal strain tensor deviator - f Trace - Equivalent strain - pe Macroscopic pseudoelastic strain tensor - x Distortion due to parent (austenite =1)product (martensite =2) phase transformation (traceless symmetric second order tensor) - M Total mass of a system - M() Total mass of phase - V Total volume of a system - V() Total volume of phase - z=M(2)/M Weight fraction of martensite - 1-z=M(1)/M Weight fraction of austenite - u 0 * () Specific internal energy of phase (=1,2) - s 0 * () Specific internal entropy of phase - Specific configurational energy - Specific configurational entropy - 0 f (T) Driving force for temperature-induced martensitic transformation at stress free state ( 0 f T) = T *Ts *) - Kirchhoff stress tensor - Kirchhoff stress tensor deviator - Equivalent stress - Cauchy stress tensor - Mass density - K Bulk moduli (K 0=K) - L Elastic moduli tensor (order 4) - E Young modulus - Energetic shear (0 = ) - Poisson coefficient - M s o (M F o ) Martensite start (finish) temperature at stress free state - A s o (A F o ) Austenite start (finish) temperature at stress free state - C v Specific heat at constant volume - k Conductivity - Pseudoelastic strain obtained in tensile test after complete phase transformation (AM) (unidimensional test) - 0 Thermal expansion tensor - r Resistivity - 1MPa 106 N/m 2 - () Specific free energy of phase - n Specific free energy at non equilibrium (R model) - n eq Specific free energy at equilibrium (R model) - n v Volumic part of eq - Specific free energy at non equilibrium (R L model) - conf Specific coherency energy (R L model) - c Specific free energy at constrained equilibria (R L model) - it (T) Coherency term (R L model)  相似文献   

4.
The problem of hypersonic flow over a flat delta plate with a high sweepback anglex at angles of attack close to /2 is solved using a numerical algorithm based on transition to the conical solution. The existence of conical flow at /2 with the velocity vector directed towards the apex of the plate is established. Values ofC p/sin2 and the thickness of the shock layer in the plane of symmetry of the plate are given as functions of the hypersonic similarity parameterk=tan tanx. A comparison of the calculated and experimental data shows that they are in good agreement.Translated from Izvestiya Rossiiskoi Akademii Nauk, Mekhanika Zhidkosti i Gaza, No.5, pp. 183–185, September–October, 1992.  相似文献   

5.
In this paper we continue previous studies of the closure problem for two-phase flow in homogeneous porous media, and we show how the closure problem can be transformed to a pair of Stokes-like boundary-value problems in terms of pressures that have units of length and velocities that have units of length squared. These are essentially geometrical boundary value problems that are used to calculate the four permeability tensors that appear in the volume averaged Stokes' equations. To determine the geometry associated with the closure problem, one needs to solve the physical problem; however, the closure problem can be solved using the same algorithm used to solve the physical problem, thus the entire procedure can be accomplished with a single numerical code.Nomenclature a a vector that maps V onto , m-1. - A a tensor that maps V onto . - A area of the - interface contained within the macroscopic region, m2. - A area of the -phase entrances and exits contained within the macroscopic region, m2. - A area of the - interface contained within the averaging volume, m2. - A area of the -phase entrances and exits contained within the averaging volume, m2. - Bo Bond number (= (=(–)g2/). - Ca capillary number (= v/). - g gravitational acceleration, m/s2. - H mean curvature, m-1. - I unit tensor. - permeability tensor for the -phase, m2. - viscous drag tensor that maps V onto V. - * dominant permeability tensor that maps onto v , m2. - * coupling permeability tensor that maps onto v , m2. - characteristic length scale for the -phase, m. - l characteristic length scale representing both and , m. - L characteristic length scale for volume averaged quantities, m. - n unit normal vector directed from the -phase toward the -phase. - n unit normal vector representing both n and n . - n unit normal vector representing both n and n . - P pressure in the -phase, N/m2. - p superficial average pressure in the -phase, N/m2. - p intrinsic average pressure in the -phase, N/m2. - p p , spatial deviation pressure for the -phase, N/m2. - r 0 radius of the averaging volume, m. - r position vector, m. - t time, s. - v fluid velocity in the -phase, m/s. - v superficial average velocity in the -phase, m/s. - v intrinsic average velocity in the -phase, m/s. - v v , spatial deviation velocity in the -phase, m/s. - V volume of the -phase contained within the averaging volmue, m3. - averaging volume, m3. Greek Symbols V /, volume fraction of the -phase. - viscosity of the -phase, Ns/m2. - density of the -phase, kg/m3. - surface tension, N/m. - (v +v T ), viscous stress tensor for the -phase, N/m2.  相似文献   

6.
The paper presents an exact analysis of the dispersion of a passive contaminant in a viscous fluid flowing in a parallel plate channel driven by a uniform pressure gradient. The channel rotates about an axis perpendicular to its walls with a uniform angular velocity resulting in a secondary flow. Using a generalized dispersion model which is valid for all time, we evaluate the longitudinal dispersion coefficientsK i (i=1, 2, ...) as functions of time. It is shown thatK 1=0 andK 3,K 4, ... decay rapidly in comparison withK 2. ButK 2 decreases with increasing (the dimensionless rotation parameter) for values of upto approximately =2.2. ThereafterK 2 increases with further increase in and its value gets saturated for large values of (say, 500) and does not change any further with increase in . A physical explanation of this anomalous behaviour ofK 2 is given.
Instationäre konvektive Diffusion in einem rotierenden Parallelplattenkanal
Zusammenfassung In dieser Untersuchung wird eine exakte Analyse der Ausbreitung eines passiven Kontaminierungsstoffes in einer zähen Flüssigkeit gegeben, die, befördert durch einen gleichförmigen Druckgradienten, in einem Parallelplattenkanal strömt. Der Kanal rotiert mit gleichförmiger Winkelgeschwindigkeit um eine zu seinen Wänden senkrechte Achse, wodurch sich eine Sekundärströmung ausbildet. Unter Verwendung eines generalisierten, für alle Zeiten gültigen Dispersionsmodells werden die longitudinalen DispersionskoeffizientenK i (i=1, 2, ...) als Funktionen der Zeit ermittelt. Es wird gezeigt, daßK 1=0 gilt und dieK 3,K 4, ... gegenüberK 2 schnell abnehmen.K 2 nimmt ab, wenn , der dimensionslose Rotationsparameter, bis etwa zum Wert 2,2 ansteigt. Danach wächstK 2 mit bis auf einem Endwert an, der etwa ab =500 erreicht wird. Dieses anomale Verhalten vonK 2 findet eine physikalische Erklärung.

List of symbols C solute concentration - D molecular diffusivity - K i longitudinal dispersion coefficients - 2L depth of the channel - P 0 dimensionless pressure gradient along main flow - Pe Péclet number - q velocity vector - Q x,Q y mass flux along the main flow and the secondary flow directions - dimensionless average velocity along the main flow direction - (x, y, z) Cartesian co-ordinates Greek symbols dimensionless rotation parameter - the inclination of side walls withx-axis - kinematic viscosity - fluid density - dimensionless time - angular velocity of the channel - dimensionless distance along the main flow direction - dimensionless distance along the vertical direction - dimensionless solute concentration - integral of the dispersion coefficientK 2() over a time interval  相似文献   

7.
We consider singularly perturbed systems , such that=f(, o, 0). o m , has a heteroclinic orbitu(t). We construct a bifurcation functionG(, ) such that the singular system has a heteroclinic orbit if and only ifG(, )=0 has a solution=(). We also apply this result to recover some theorems that have been proved using different approaches.  相似文献   

8.
A study has been made of the flow formed in a supersonic nozzle when gas is blown in a transverse jet into an expanding supersonic flow. Measurements were made of the total and static pressures of the flow at several sections of the nozzle. It was established that, depending on the relative flow rate = mj/(mj+ m0) of the blown gas (mjand m0 are the flow rates of the blown gas and the main flow, respectively), there exist two flow regimes with different dependences of the Mach number of the flow. At small , the experimental flow parameters correspond satisfactorily to the parameters calculated in a one-dimensional model with a narrow mixing layer near the blowing section. Agreement was observed at flow rates less than a certain *, this critical value being determined in the model as the flow rate at which the flow after mixing becomes sonic. In the experiments at large flow rates of the blown gas, * < < 1, the value of M for the flow hardly depends on and corresponds to the calculated value of M for a supersonic flow having the velocity of sound near the blowing section. A scheme is proposed for calculating the flow in a nozzle with transverse blowing in the supersonic part; it describes satisfactorily the experimental results in the complete range of blown-gas-main-flow flow rate ratios (0 1) over the complete length of the nozzle.Translated from Izvestiya Akademii Nauk SSSR, Mekhanika Zhidkosti i Gaza, No. 3, pp. 188–192, May–June, 1984.  相似文献   

9.
Summary The subject of this article is the thermodynamics of perfect elastic-plastic materials undergoing unidimensional, but not necessarily isothermal, deformations. The first and second laws of thermodynamics are employed in a form in which only the following quantities appear: the temperature , the elastic strain e, the plastic strain p, the elastic modulus (gq), the yield strain (gq), the heat capacity (e, p,), the latent elastic heat e(e, p, ), and the latent plastic heat p(e, p, ). Relations among the response functions , , , e, and p are derived, and it is shown that a set of these relations gives a necessary and sufficient condition for compliance with the laws of thermodynamics. Some observations are made about the existence and uniqueness of energy and entropy as functions of state.Dedicated to Clifford Truesdell on the occasion of his 60th birthdayThis research was supported by the U.S. National Science Foundation.  相似文献   

10.
We consider the parametrized family of equations tt ,u- xx u-au+u 2 2 u=O,x(0,L), with Dirichlet boundary conditions. This equation has finite-dimensional invariant manifolds of solutions. Studying the reduced equation to a four-dimensional manifold, we prove the existence of transversal homoclinic orbits to periodic solutions and of invariant sets with chaotic dynamics, provided that =2, 3, 4,.... For =1 we prove the existence of infinitely many first integrals pairwise in involution.  相似文献   

11.
Lack of regularity of local minimizers for convex functionals with non-standard growth conditions is considered. It is shown that for every >0 there exists a function aC() such that the functional admits a local minimizer uW1,p() whose set of non-Lebesgue points is a closed set with dim()>Np–, and where 1<p<N<N+<q<+.  相似文献   

12.
The wedge subjected to tractions: a paradox resolved   总被引:4,自引:0,他引:4  
The classical two-dimensional solution provided by Lévy for the stress distribution in an elastic wedge, loaded by a uniform pressure on one face, becomes infinite when the opening angle 2 of the wedge satisfies the equation tan 2 = 2. Such pathological behavior prompted the investigation in this paper of the stresses and displacements that are induced by tractions of O(r ) as r0. The key point is to choose an Airy stress function which generates stresses capable of accommodating unrestricted loading. Fortunately conditions can be derived which pre-determine the form of the necessary Airy stress function. The results show that inhomogeneous boundary conditions can induce stresses of O(r ), O(r ln r), or O(r ln2 r) as r0, depending on which conditions are satisfied. The stress function used by Williams is sufficient only if the induced stress and displacement behavior is of the power type. The wedge loaded by uniform antisymmetric shear tractions is shown in this paper to exhibit stresses of O(ln r) as r0 for the half-plane or crack geometry. At the critical opening angle 2, uniform antisymmetric normal and symmetric shear tractions also induce the above type of stress singularity. No anticipating such stresses, Lévy used an insufficiently general Airy stress function that led to the observed pathological behavior at 2.  相似文献   

13.
The molecular theory of Doi has been used as a framework to characterize the rheological behavior of polymeric liquid crystals at the low deformation rates for which it was derived, and an appropriate extension for high deformation rates is presented. The essential physics behind the Doi formulation has, however, been retained in its entirety. The resulting four-parameter equation enables prediction of the shearing behavior at low and high deformation rates, of the stress in extensional flows, of the isotropic-anisotropic phase transition and of the molecular orientation. Extensional data over nearly three decades of elongation rate (10–2–101) and shearing data over six decades of shear rate (10–2–104) have been correlated using this analysis. Experimental data are presented for both homogeneous and inhomogeneous shearing stress fields. For the latter, a 20-fold range of capillary tube diameters has been employed and no effects of system geometry or the inhomogeneity of the flow-field are observed. Such an independence of the rheological properties from these effects does not occur for low molecular weight liquid crystals and this is, perhaps, the first time this has been reported for polymeric lyotropic liquid crystals; the physical basis for this major difference is discussed briefly. A Semi-empirical constant in eq. (18), N/m2 - c rod concentration, rods/m3 - c * critical rod concentration at which the isotropic phase becomes unstable, rods/m3 - C interaction potential in the Doi theory defined in eq. (3) - d rod diameter, m - D semi-empirical constant in eq. (19), s–1 - D r lumped rotational diffusivity defined in eq. (4), s–1 - rotational diffusivity of rods in a concentrated (liquid crystalline) system, s–1 - D ro rotational diffusivity of a dilute solution of rods, s–1 - f distribution function defining rod orientation - F tensorial term in the Doi theory defined in eq. (7) (or eq. (19)), s–1 - G tensorial term in the Doi theory defined in eq. (8) - K B Boltzmann constant, 1.38 × 10–23 J/K-molecule - L rod length, m - S scalar order parameter - S tensor order parameter defined in eq. (5) - t time, s - T absolute temperature, K - u unit vector describing the orientation of an individual rod - rate of change ofu due to macroscopic flow, s–1 - v fluid velocity vector, m/s - v velocity gradient tensor defined in eq. (9), s–1 - V mean field (aligning) potential defined in eq. (2) - x coordinate direction, m - Kronecker delta (= 0 if = 1 if = ) - r ratio of viscosity of suspension to that of the solvent at the same shear stress - s solvent viscosity, Pa · s - * viscosity at the critical concentrationc *, Pa · s - v 1, v2 numerical factors in eqs. (3) and (4), respectively - deviatoric stress tensor, N/m2 - volume fraction of rods - 0 constant in eq. (16) - * volume fraction of rods at the critical concentrationc * - average over the distribution functionf(u, t) (= d 2u f(u, t)) - gradient operator - d 2u integral over the surface of the sphere (|u| = 1)  相似文献   

14.
Summary Let denote the congruence of null geodesics associated with a given optical observer inV 4. We prove that determines a unique collection of vector fieldsM() ( =1, 2, 3) and (0) overV 4, satisfying a weak version of Killing's conditions.This allows a natural interpretation of these fields as the infinitesimal generators of spatial rotations and temporal translation relative to the given observer. We prove also that the definition of the fieldsM() and (0) is mathematically equivalent to the choice of a distinguished affine parameter f along the curves of, playing the role of a retarded distance from the observer.The relation between f and other possible definitions of distance is discussed.
Sommario Sia la congruenza di geodetiche nulle associata ad un osservatore ottico assegnato nello spazio-tempoV 4. Dimostriamo che determina un'unica collezione di campi vettorialiM() ( =1, 2, 3) e (0) inV 4 che soddisfano una versione in forma debole delle equazioni di Killing. Ciò suggerisce una naturale interpretazione di questi campi come generatori infinitesimi di rotazioni spaziali e traslazioni temporali relative all'osservatore assegnato. Dimostriamo anche che la definizione dei campiM(), (0) è matematicamente equivalente alla scelta di un parametro affine privilegiato f lungo le curve di, che gioca il ruolo di distanza ritardata dall'osservatore. Successivamente si esaminano i legami tra f ed altre possibili definizioni di distanza in grande.


Work performed in the sphere of activity of: Gruppo Nazionale per la Fisica Matematica del CNR.  相似文献   

15.
An analysis is developed for the laminar free convection from a vertical plate with uniformly distributed wall heat flux and a concentrated line thermal source embedded at the leading edge. We introduce a parameter=(1 +Q L/Qw)–1=(1 + RaL/Raw)–1 to describe the relative strength of the two thermal sources; and propose a unified buoyancy parameter=( RaL+ Raw)1/5 with=1/(1 +Pr –1) to properly scale the dependent and independent variables. The variables are so defined that the resulting nonsimilar boundary-layer equations can describe exactly the buoyancy-induced flow from the dual sources with any relative strength to fluids of any Prandtl number from very small values to infinity. These nonsimilar equations are readily reducible to the self-similar equations of an adiabatic wall plume for=0, and to those of free convection from uniform flux plate for=1. Rigorous finite-difference solutions for fluids of Pr from 0.001 to are obtained over the entire range of from 0 to 1. The effects of both relative source strength and Prandtl number on the velocity profiles, temperature profiles, and the variations of wall temperature, are clearly illustrated.
Freie Konvektion an einer vertikalen Platte mit einer konzentrierten und einer gleichmäßig verteilten Wärmequelle
Zusammenfassung Für die freie Konvektion an einer vertikalen Platte mit einer gleichmäßig verteilten Wandwärmestromdichte und einer in der Vorderkante eingebetteten linienförmigen Wärmequelle wird eine Berechnungsmethode entwickelt. Zur Beschreibung der relativen Stärke der beiden Wärmequellen führen wir einen Parameter=(1 + QL/Qw)–1=(1 + RaL/Raw)–1 ein und schlagen einen vereinheitlichten Auftriebsparameter=( Ra L+ Ra w)1/5 mit=1/(1 +Pr –1 für die Skalierung der abhängigen und unabhängigen Variablen vor. Die Variablen werden so definiert, daß mit den sich ergebenden unabhängigen Grenzschichtgleichungen die von den beiden Wärmequellen beliebiger Stärke verursachte Auftriebsströmung von Fluiden beliebiger Prandtl-Zahl genau beschrieben werden kann. Diese unabhängigen Gleichungen können ohne weiteres auf die selbstähnlichen Gleichungen für den Fall einer lokalen Wärmezufuhr an einer sonst adiabatischen Wand für=0 und jenen der freien konvektion an einer Platte mit einheitlichem Wärmestrom für=1 zurückgeführt werden. Für Fluide mit der Prandtl-Zahl zwischen 0,001 und Unendlich werden nach der strengen finite Differenzen-Methode Lösungen im Bereich von zwischen 0 und 1 erhalten. Der jeweilige Einfluß der relativen Quellenstärke und der Prandtl-Zahl auf die Geschwindigkeits- und Temperaturprofile sowie die Veränderung der Wandtemperatur werden deutlich dargestellt.

Nomenclature C f friction coefficient - C p specific heat - f reduced stream function - g gravitational acceleration - k thermal conductivity - L width of the plate - Nu local Nusselt number - Pr Prandtl number - q w wall heat flux - Q L heat generated by the line source - Q w heat released by the uniform-flux wall from 0 tox, q w Lx - Ra L local Rayleigh number, g T L * x 3/( ) - Ra w local Rayleigh number,g T w * w 3/( ) - T fluid temperature - T temperature of ambient fluid - T L * characteristic temperature of the line source,Q L/(C p L) - T w * characteristic temperature of the uniform flux wall, =q w x/k=Q w /(C p L) - u velocity component in then-direction - U0 dimensionless velocity,u/(/x) Ra L 2/5 - U 1 dimensionless velocity,u/(/x) Ra w 2/5 - velocity component in they-direction - x coordinate parallel to the plate - y coordinate normal to the plate - thermal diffusivity - thermal expansion coefficient - pseudo-similarity variable,(y/x) - dimensionless temperature, (T–T )/(T L * +T w * ) - 0 dimensionless temperature, (Ral)1/5 (T–T )/T L * - 1 dimensionless temperature, (Raw)Raw)1/5 (T–T )/T w * - (Ra L+Raw)1/5 - kinematic viscosity - (1 +Ra L/Raw)–1=(1 +T L * /T w * )–1=(1 + QL/Qw)–1 - density - Pr/(1 +Pr) - w wall shear stress - stream function  相似文献   

16.
The stability of stationary traveling waves of the first and second families with respect to infinitesimal perturbations of arbitrary wavelength is subjected to a detailed numerical investigation. The existence of a unique region of stability of the first family is established for wave numbers (1, 1) corresponding to the optimal wave regime. There are several regions of stability of the second family ( k , k),k=2,3,..., lying close to the local flow rate maxima. In the regions of instability the growth rates of perturbations of the first family are several times greater than for the second family. This difference increases with increase in the Reynolds number. The calculations make it possible to explain a number of experimental observations.Translated from Izvestiya Akademii Nauk SSSR, Mekhanika Zhidkosti i Gaza, No. 3, pp. 33–41, May–June, 1989.The authors are grateful to V. Ya. Shkadov for his constant interest, and to A. G. Kulikovskii, A. A. Barmin and their seminar participants for useful discussions and suggestions.  相似文献   

17.
We consider infiltration into a soil that is assumed to have hydraulic conductivity of the form K = K = Kseh and water content of the form = K – r. Here h denotes capillary pressure head while Ks, , and r represent soil specific parameters. These assumptions linearize the flow equation and permit a closed form solution that displays the roles of all the parameters appearing in the hydraulic function K and . We assume Ks and r to be known. A measurement of diffusivity fixes the product of and resulting in a parameter identification problem for one parameter. We show that this parameter identification problem, in some cases, has a unique solution. We also show that, in some cases, this parameter identification problem can have multiple solutions, or no solution. In addition it is shown that solutions to the parameter identification problem can be very sensitive to small changes in the problem data.  相似文献   

18.
The wedge subjected to tractions: a paradox re-examined   总被引:2,自引:0,他引:2  
The classical two-dimensional solution for the stress distribution in an elastic wedge loaded by a uniform pressure on one side of the wedge becomes infinite when the wedge angle 2 satisfies the equation tan 235-1. This paradox was resolved recently by Dempsey who obtained a solution which is bounded at 235-2. However, for not equal but very close to 235-3, the classical solution can still be very large as approaches 235-4. In this paper we re-examine the paradox. We obtain a solution which remains bounded as approaches 235-5 and reproduces Dempsey's solution in the limit 235-6. At 235-7 the stress distribution contains a (ln r) term for general loadings. The (ln r) term disappears under a special loading and the stresses are bounded for all r. Moreover, the solution is not unique. In other words, for the wedge angle 235-8 under a special loading, infinitely many solutions exist for which the stresses are bounded for all r. We also obtain solutions which are bounded and approach Dempsey's solutions when 2= and 2. Again, under a special loading infinitely many solutions exist for which the stresses are bounded for all r. Care has been exercised in this paper to present the solutions in a form in which the terms r - and ln r are replaced by R -gl and ln R where R=r/r 0is the dimensionless radial distance and r 0 is an arbitrary constant having the dimension of length.  相似文献   

19.
The aim of this article is to study the quasistatic evolution of a three-dimensional elastic-perfectly plastic solid which satisfies the Prandtl-Reuss law. The evolution of the field of stresses -which solves a time dependent variational inequality — and that of the field of displacements u, have been described in previous works [15], [26], [35], [36], [37] but it was not shown there that and u satisfy indeed the Prandtl-Reuss constitutive law. In this article we find and u in a class of functions which are sufficiently regular for the Prandtl-Reuss law to make sense and we prove that and u satisfy the constitutive law. This result is attained by considering the elastic-perfectly plastic model as the limit of a family of elastic-visco-plastic models like those of Norton and Hoff. The Norton-Hoff type models which we introduce depend on a viscosity parameter > 0; we study the perturbed models (i.e. > 0 fixed) and then we pass to the limit 0.Dedicated to James Serrin on the occasion of his 60th Birthday  相似文献   

20.
Simplified nonlinear governing differential equations proposed by Berger for static cases and extended by Nash and Modeer for dynamic cases are used to analyse the title problem. Steady-state harmonic oscillations are assumed and the time variable is eliminated by a Kantorovich averaging method. The enclosure or comparison theorem of Collatz is then applied to the reduced equations to obtain the upper and lower bounds for the fundamental nonlinear frequency of simply-supported rectangular plates with linearly varying thickness. The fundamental eigenvalues are given for several taper and aspect ratios.Nomenclature a, b dimensions of plates - A i series coefficients - D Eh 3/12(1– 2) flexural rigidity - D 0 Eh 0 3 /12(1– 2) - E Young's modulus - h thickness, h 0(1+x) - h 0 thickness parameter - N x , N y stress resultants in the X and Y directions - N (N x +N y )/(1+) - P 1, P 2, ... parameters - Q 1, Q 2, ... parameters - R[X, (A/h 0)2] bounding function - t time - u, v in-plane displacements - lateral deflections of plate - X=x/a dimensionless co-ordinate - x, y rectangular co-ordinates - y n (X) series related to - thickness taper ratio - parameter in the neighbourhood of - error-function associated with differential equation - eigenvalue relating to frequency - Poisson's ra-tio - plate material specific weight - (X) function related to plate deflection - (X) admissible functions - circular frequency  相似文献   

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