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1.
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   

2.
A. Papo 《Rheologica Acta》1988,27(3):320-325
Shear stress and shear rate data obtained for gypsum plaster pastes were correlated by means of different rheological models. The pastes were prepared from a commercial calcium sulfate hemihydrate at various water/plaster ratios ranging from 100/150 to 100/190. The tests were performed at 25°C using a rotating coaxial cylinder viscosimeter. The measurements were accomplished by applying a step-wise decreasing shear rate sequence. Discrimination among the models was made: (1) on the basis of the fitting goodness; (2) by checking the physical meaning of the calculated parameters; (3) on the basis of the stability of the parameters and of their prediction capacity beyond the limits of the experimental data. In the light of above, the Casson model seemed to be most effective for application to gypsum plaster pastes. K Consistency - n Power-law index - N Number of experimental data - P Number of parameters - Shear rate (s–1) - 0 Viscosity (Pa · s) - d Dispersing medium viscosity (Pa · s) - p Plastic viscosity (Pa · s) - Viscosity at zero shear rate (Pa · s) - Viscosity at infinite shear rate (Pa · s) - [] Intrinsic viscosity - 2 Variance - Shear stress (Pa) - 0 Yield stress (Pa) - Solid volume fraction - m Maximum solid volume fraction  相似文献   

3.
Normal forms for random diffeomorphisms   总被引:1,自引:0,他引:1  
Given a dynamical system (,, ,) and a random diffeomorphism (): d d with fixed point at x=0. The normal form problem is to construct a smooth near-identity nonlinear random coordinate transformation h() to make the random diffeomorphism ()=h()–1() h() as simple as possible, preferably linear. The linearization D(, 0)=:A() generates a matrix cocycle for which the multiplicative ergodic theorem holds, providing us with stochastic analogues of eigenvalues (Lyapunov exponents) and eigenspaces. Now the development runs pretty much parallel to the deterministic one, the difference being that the appearance of turns all problems into infinite-dimensional ones. In particular, the range of the homological operator is in general not closed, making the conceptof-normal form necessary. The stochastic versions of resonance and averaging are developed. The case of simple Lyapunov spectrum is treated in detail.  相似文献   

4.
The behavior of supersonic mixing layers under three conditions has been examined by schlieren photography and laser Doppler velocimetry. In the schlieren photographs, some large-scale, repetitive patterns were observed within the mixing layer; however, these structures do not appear to dominate the mixing layer character under the present flow conditions. It was found that higher levels of secondary freestream turbulence did not increase the peak turbulence intensity observed within the mixing layer, but slightly increased the growth rate. Higher levels of freestream turbulence also reduced the axial distance required for development of the mean velocity. At higher convective Mach numbers, the mixing layer growth rate was found to be smaller than that of an incompressible mixing layer at the same velocity and freestream density ratio. The increase in convective Mach number also caused a decrease in the turbulence intensity ( u/U).List of symbols a speed of sound - b total mixing layer thickness between U 1 – 0.1 U and U 2 + 0.1 U - f normalized third moment of u-velocity, f u3/(U)3 - g normalized triple product of u2 , g u2/(U)3 - h normalized triple product of u 2, h u 2/(U)3 - l u axial distance for similarity in the mean velocity - l u axial distance for similarity in the turbulence intensity - M Mach number - M c convective Mach number (for 1 = 2), M c (U 1U 2)/(a 1 + a 2) - P static pressure - r freestream velocity ratio, r U 2/U 1 - Re unit Reynolds number, Re U/ - s freestream density ratio, s 2/1 - T t total temperature - u instantaneous streamwise velocity - u deviation of u-velocity, uuU - U local mean streamwise velocity - U 1 primary freestream velocity - U 2 secondary freestream velocity - average of freestream velocities, (U 1 + U 2)/2 - U freestream velocity difference, U U 1U 2 - instantaneous transverse velocity - v deviation of -velocity, V - V local mean transverse velocity - x streamwise coordinate - y transverse coordinate - y 0 transverse location of the mixing layer centerline - ensemble average - ratio of specific heats - boundary layer thickness (y-location at 99.5% of free-stream velocity) - similarity coordinate, (yy 0)/b - compressible boundary layer momentum thickness - viscosity - density - standard deviation - dimensionless velocity, (UU 2)/U - 1 primary stream - 2 secondary stream A version of this paper was presented at the 11th Symposium on Turbulence, October 17–19, 1988, University of Missouri-Rolla  相似文献   

5.
A lattice gas algorithm is proposed for the simulation of water flow in the unsaturated zone. Microscopic dynamics of a two-dimensional model system are defined. Up to four fluid particles occupy the sites of a square lattice. At each time step, the particles are sent to neighbouring sites according to probabilistic rules which depend on the permeability and the potential but not on the input velocities of the particles. On the macroscopic scale, the flow is described by a diffusion term and a Darcy term. Several extensions including higher dimension are discussed.List of Symbols c (n) constant in the definition of the rejection probabilityP forn = 1,2,3 particles at a site 0 c (n) 1 - D diffusion constant - D vertical extent of the system, measured in cells - E i vector connecting a site to its neighbour in directioni - i direction of a nearest neighbour site,i = 1,..., 4 - j direction of a nearest neighbour site,j = 1,..., 4 - j mass transport (fluid flow),j = v - j x x-component of the flowj - k(x) spatial dependence of the permeability, user defined under the constraint 0 k 1 - k () the part of the permeability which depends on the degree of saturation (seek) - k (n) (x) effective permeability at a sitex that holdsn particles - L horizontal extent of the system, measured in cells - l mac macroscopic length scale, e.g. one meter - l mic microscopic length scale (one lattice constant) - m integer number of time steps - n (x) number of particles at the lattice sitex - N A total number of particles on all A-sites - P probability for rejection of a randomly selected direction or set of directions - p arithmetic mean of the probability for a site to receive a particle from a particular neighbour (the average is taken over the four neighbours) - p i (n) probability that one out ofn particles at a site is sent in directioni - p ij (2) probability that the two particles at a site are sent in directionsi andj - t time - t mac macroscopic time scale, e.g. one day - t mic microscopic time scale (one time step) - v fluid velocity - x space vector, mostly two-dimensional:x = (x, y) - x horizontal component ofx - y vertical component ofx - quotient of microscopic and macroscopic time scales,t mic /t mac - quotient of microscopic and macroscopic length scales,l mic /l mac - i p + i is the probability that a particle is received from the neighbour atx +E i - K(X, ) effective permeability,k =k(x)k () - correlation length - degree of saturation, used synonymously with density (homogeneous porosity) - 0 value of a homogeneous particle density - ø(x) external potential (user defined), ø = gr + mat - ø(x) arithmetic mean of the external potential at the four sites surroundingx - ø i external potential at the sitex +E i - total potential, = ø + den - gr(x) gravitational potential - mat(x) matrix potential - den() density-dependent potential - n potential depending on the occupation number - (n) (x) probability that sitex is occupied byn particles - 0 (n) (n) in a system with homogeneous particle density - mac macroscopic - mic microscopic  相似文献   

6.
This paper presents a new formulation for the laminar free convection from an arbitrarily inclined isothermal plate to fluids of any Prandtl number between 0.001 and infinity. A novel inclination parameter is proposed such that all cases of the horizontal, inclined and vertical plates can be described by a single set of transformed equations. Moreover, the self-similar equations for the limiting cases of the horizontal and vertical plates are recovered from the transformed equations by setting=0 and=1, respectively. Heated upward-facing plates with positive and negative inclination angles are investigated. A very accurate correlation equation of the local Nusselt number is developed for arbitrary inclination angle and for 0.001 Pr .
Wärmeübertragung bei freier Konvektion an einer isothermen Platte mit beliebiger Neigung
Zusammenfasssung Diese Untersuchung stellt eine neue Formulierung der laminaren freien Konvektion von Flüssigkeiten mit einer Prandtl-Zahl zwischen 0,001 und unendlich an einer beliebig schräggestellten isothermen Platte dar. Ein neuer Neigungsparameter wird eingeführt, so daß alle Fälle der horizontalen, geneigten oder vertikalen Platte von einem einzigen Satz transformierter Gleichungen beschrieben werden können. Die unabhängigen Gleichungen für die beiden Fälle der horizontalen and vertikalen Platte wurden für=0 und=1 aus den transformierten Gleichungen wieder abgeleitet. Es wurden erwärmte aufwärtsgerichtete Platten mit positiven und negativen Neigungswinkeln untersucht. Eine sehr genaue Gleichung wurde für die lokale Nusselt-Zahl bei beliebigen Neigungswinkeln und für 0,001 Pr entwickelt.

Nomenclature C p specific heat - f reduced stream function - g gravitational acceleration - Gr local Grashof number,g(T w T w ) x3/v2 - h local heat transfer coefficient - k thermal conductivity - n constant exponent - Nu local Nusselt number,hx/k - p pressure - Pr Prandtl number, v/ - Ra local Rayleigh number,g(T w T )J x3/v - T fluid temperature - T w wall temperature - T temperature of ambient fluid - u velocity component in x-direction - v velocity component in y-direction - x coordinate parallel to the plate - y coordinate normal to the plate Greek symbols thermal diffusivity - thermal expansion coefficient - (Ra¦sin¦)1/4/( Ra cos()1/5 - pseudo-similarity variable, (y/) - dimensionless temperature, (TT )/(T wT ) - ( Ra cos)1/5+(Rasin)1/4 - v kinematic viscosity - 1/[1 +(Ra cos)1/5/( Ra¦sin)1/4] - density of fluid - Pr/(1+Pr) - w wall shear stress - angle of plate inclination measured from the horizontal - stream function - dimensionless dynamic pressure  相似文献   

7.
Laminar mixed convection over a horizontal plate with uniform wall temperature or uniform wall heat flux is analyzed by introducing proper buoyancy parameters and transformation variables for fluids of any Prandtl number between 0.001 and 10,000. Both cases of buoyancy assisting and opposing flow conditions are investigated. For the buoyancy-assisting case, the obtained numerical results are very accurate over the entire range of mixed convection intensity from pure forced convection limit to pure free convection limit. For the buoyancy-opposing case, solutions are obtained from the forced convection limit to the point of breakdown.
Mischkonvektion an einer horizontalen Platte für Fluide mit beliebiger Prandtl-Zahl
Zusammenfassung Es wurde laminare Mischkonvektion an einer horizontalen Platte mit einheitlicher Wandtemperatur oder einheitlicher Wandwärmestromdichte bei Einführung zweckmäßiger Auftriebsparameter und Transformationsvariablen für Fluide mit beliebiger Prandtl-Zahl zwischen 0,001 und 10 000 untersucht. Es wurden die Fälle der Strömung entgegen und in Richtung der Auftriebskraft untersucht. Für den Fall der Strömung in Richtung der Auftriebskraft wurden sehr genaue numerische Ergebnisse für den gesamten Bereich der gemischten Konvektion von rein erzwungener Konvektion bis zu rein freier Konvektion erhalten. Für den Fall der Strömung entgegen der Auftriebsrichtung wurden Lösungen für erzwungene Konvektion bis zum Umkehrpunkt erhalten.

Nomenclature C f local friction coefficient - f reduced stream function - g gravitational acceleration - Gr local Grashof number for UWT,g (T w T )x 3/ 2 - Gr* local Grashof number for UHF,g q w x 4/k 2 - m =10 for UWT; and =6 for UHF - n =5 for UWT; and =3 for UHF - Nu local Nusselt number - p pressure - Pr Prandtl number,/ - q w wall heat flux - Ra local Rayleigh number for UWT,Gr Pr - Ra* local Rayleigh number for UHF,Gr*Pr - Re local Reynolds number,u x/ - T fluid temperature - T w wall temperature - T free-stream temperature - u velocity component inx-direction - u free-stream velocity - v velocity component iny-direction - x coordinate parallel to the plate - y coordinate normal to the plate Greek symbols thermal diffusivity - thermal expansion coefficient - =0 for UWT; and =1 for UHF - buoyancy parameter, =( Ra)1/5/( Re)1/2 for UWT; and =( Ra*)1/6/( Re)1/2 for UHF - pseudo-similarity variable, (y/x) - dimensionless temperature, =(TT )/(T w T ) for UWT; and =(TT )/(q w x/k) for UHF - =[( Re)1/2+( Ra)1/5] for UWT; and =[( Re)1/2+( Ra*)1/6] for UHF - dynamic viscosity - kinematic viscosity - /(1+) - dimensionless pressure - density - Pr/(1+Pr) - w wall shear stress,(u/y) y=0 - stream function - Pr/(1+Pr)1/3  相似文献   

8.
Mathematical results are derived for the schlieren and shadowgraph contrast variation due to the refraction of light rays passing through two-dimensional compressible vortices with viscous cores. Both standard and small-disturbance solutions are obtained. It is shown that schlieren and shadowgraph produce substantially different contrast profiles. Further, the shadowgraph contrast variation is shown to be very sensitive to the vortex velocity profile and is also dependent on the location of the peak peripheral velocity (viscous core radius). The computed results are compared to actual contrast measurements made for rotor tip vortices using the shadowgraph flow visualization technique. The work helps to clarify the relationships between the observed contrast and the structure of vortical structures in density gradient based flow visualization experiments.Nomenclature a Unobstructed height of schlieren light source in cutoff plane, m - c Blade chord, m - f Focal length of schlieren focusing mirror, m - C T Rotor thrust coefficient, T/( 2 R 4) - I Image screen illumination, Lm/m 2 - l Distance from vortex to shadowgraph screen, m - n b Number of blades - p Pressure,N/m 2 - p Ambient pressure, N/m 2 - r, , z Cylindrical coordinate system - r c Vortex core radius, m - Non-dimensional radial coordinate, (r/r c ) - R Rotor radius, m - Tangential velocity, m/s - Specific heat ratio of air - Circulation (strength of vortex), m 2/s - Non-dimensional quantity, 2 82p r c 2 - Refractive index of fluid medium - 0 Refractive index of fluid medium at reference conditions - Gladstone-Dale constant, m 3/kg - Density, kg/m 3 - Density at ambient conditions, kg/m 3 - Non-dimensional density, (/ ) - Rotor solidity, (n b c/ R) - Rotor rotational frequency, rad/s  相似文献   

9.
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   

10.
Certain steady yawed magnetogasdynamic flows, in which the magnetic field is everywhere parallel to the velocity field, are related to certain reduced three-dimensional compressible gas flows having zero magnetic field. Under a restriction, the reduced flows are linked, by certain reciprocal relations, to a four parameter class of plane gas flows. In the instance of constant entropy an approximation method is suggested for obtaining magnetogasdynamic flows from the corresponding plane, irrotational gasdynamic flows and examples are given.

Nomenclature

magnetogasdynamic flow variables H magnetic intensity - q fluid velocity - fluid density - p pressure - s entropy - Q t, H t component of q, H in the x–y plane - w , h component of q, H perpendicular to the x–y plane reduced gasdynamic flow factor of proportionality - q* fluid velocity - * fluid density - p* pressure - Q t * =u*î+v*, w* components of q* - l arbitrary constant - A v Alfvén speed - Q t, , p fluid velocity, density, pressure of the reciprocal gas dynamic flow - L, n, k, arbitrary constants - , velocity potential, stream function - angle made by Q t, Q t * , and V with the x-axis - adiabatic gas constant - a 2=(–1)/2 constant - M Mach number - W constant value of w* - E approximate constant value of g(p) - * modified potential function - modified velocity coordinate - +i - complex potential of the irrotational flow - B arbitrary constant - V incompressible flow velocity - V modified fluid velocity - X p, Y p points on the profile  相似文献   

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