Transport Processes
Transport Processes
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A1.18
comment(i) In an experiment, a finite amount of marker gas of diffusivity is released at time into an infinite tube in the neighbourhood of the origin . Starting from the one-dimensional diffusion equation for the concentration of marker gas,
use dimensional analysis to show that
for some dimensionless function of the similarity variable .
Write down the equation and boundary conditions satisfied by .
(ii) Consider the experiment of Part (i). Find and sketch your answer in the form of a plot of against at a few different times .
Calculate for a second experiment in which the concentration of marker gas at is instead raised to the value at and maintained at that value thereafter. Show that the total amount of marker gas released in this case becomes greater than after a time
Show further that, at much larger times than this, the concentration in the first experiment still remains greater than that in the second experiment for positions with .
[Hint: as
A3.16
comment(i) Viscous, incompressible fluid of viscosity flows steadily in the -direction in a uniform channel . The plane is fixed and the plane has constant -velocity . Neglecting gravity, derive from first principles the equations of motion of the fluid and show that the -component of the fluid velocity is and satisfies
where is the pressure in the fluid. Write down the boundary conditions on . Hence show that the volume flow rate is given by
(ii) A heavy rectangular body of width and infinite length (in the -direction) is pivoted about one edge at above a fixed rigid horizontal plane . The body has weight per unit length in the -direction, its centre of mass is distance from the pivot, and it is falling under gravity towards the fixed plane through a viscous, incompressible fluid. Let be the angle between the body and the plane. Explain the approximations of lubrication theory which permit equations (1) and (2) of Part (i) to apply to the flow in the gap between the two surfaces.
Deduce that, in the gap,
where . By taking moments about , deduce that is given by
where .
A4.19
comment(a) Solute diffuses and is advected in a moving fluid. Derive the transport equation and deduce that the solute concentration satisfies the advection-diffusion equation
where is the velocity field and the diffusivity. Write down the form this equation takes when , both and are unidirectional, in the -direction, and is a constant.
(b) A solution occupies the region , bounded by a semi-permeable membrane at across which fluid passes (by osmosis) with velocity
where is a positive constant, is a fixed uniform solute concentration in the region , and is the solute concentration in the fluid. The membrane does not allow solute to pass across , and the concentration at is a fixed value (where .
Write down the differential equation and boundary conditions to be satisfied by in a steady state. Make the equations non-dimensional by using the substitutions
and show that the concentration distribution is given by
where and should be defined, and is given by the transcendental equation
What is the dimensional fluid velocity , in terms of
(c) Show that if, instead of taking a finite value of , you had tried to take infinite, then you would have been unable to solve for unless , but in that case there would be no way of determining .
(d) Find asymptotic expansions for from equation in the following limits:
(i) For fixed, expand as a power series in , and equate coefficients to show that
(ii) For fixed, take logarithms, expand as a power series in , and show that
What is the limiting value of in the limits (i) and (ii)?
(e) Both the expansions in (d) break down when . To investigate the double limit , show that can be written as
where and is to be determined. Show that for , and for .
Briefly discuss the implication of your results for the problem raised in (c) above.
A1.18
comment(i) A solute occupying a domain has concentration and is created at a rate per unit volume; is the flux of solute per unit area; are position and time. Derive the transport equation
State Fick's Law of diffusion and hence write down the diffusion equation for for a case in which the solute flux occurs solely by diffusion, with diffusivity .
In a finite domain and the steady-state distribution of depend only on is equal to at and at . Find in the following two cases: (a) , (b) ,
where and are positive constants.
Show that there is no steady solution satisfying the boundary conditions if
(ii) For the problem of Part (i), consider the case , where and are positive constants. Calculate the steady-state solution, , assuming that for any integer .
Now let
where . Find the equations, boundary and initial conditions satisfied by . Solve the problem using separation of variables and show that
for some constants . Write down an integral expression for , show that
and comment on the behaviour of the solution for large times in the two cases and .
A3.16
comment(i) When a solid crystal grows into a supercooled infinite melt, latent heat must be removed from the interface by diffusion into the melt. Write down the equation and boundary conditions satisfied by the temperature in the melt, where is position and time, in terms of the following material properties: solid density , specific heat capacity , coefficient of latent heat per unit mass , thermal conductivity , melting temperature . You may assume that the densities of the melt and the solid are the same and that temperature in the melt far from the interface is , where is a positive constant.
A spherical crystal of radius grows into such a melt with . Use dimensional analysis to show that is proportional to .
(ii) Show that the above problem should have a similarity solution of the form
where is the radial coordinate in spherical polars and is the thermal diffusivity. Recalling that, for spherically symmetric , write down the equation and boundary conditions to be satisfied by . Hence show that the radius of the crystal is given by , where satisfies the equation
and .
Integrate the left hand side of this equation by parts, to give
Hence show that a solution with small must have , which is self-consistent if is large.
A4.19
commentA shallow layer of fluid of viscosity , density and depth lies on a rigid horizontal plane and is bounded by impermeable barriers at and . Gravity acts vertically and a wind above the layer causes a shear stress to be exerted on the upper surface in the direction. Surface tension is negligible compared to gravity.
(a) Assuming that the steady flow in the layer can be analysed using lubrication theory, show that the horizontal pressure gradient is given by and hence that
Show also that the fluid velocity at the surface is equal to , and sketch the velocity profile for .
(b) In the case in which is a constant, , and assuming that the difference between and its average value remains small compared with , show that
provided that
(c) Surfactant at surface concentration is added to the surface, so that now
where is a positive constant. The surfactant is advected by the surface fluid velocity and also experiences a surface diffusion with diffusivity . Write down the equation for conservation of surfactant, and hence show that
From equations (1), (2) and (3) deduce that
where is a constant. Assuming once more that , and that at , show further that
provided that
A1.18
comment(i) Material of thermal diffusivity occupies the semi-infinite region and is initially at uniform temperature . For time the temperature at is held at a constant value . Given that the temperature in satisfies the diffusion equation , write down the equation and the boundary and initial conditions satisfied by the dimensionless temperature .
Use dimensional analysis to show that the lengthscale of the region in which is significantly different from is proportional to . Hence show that this problem has a similarity solution
where .
What is the rate of heat input, , across the plane
(ii) Consider the same problem as in Part (i) except that the boundary condition at is replaced by one of constant rate of heat input . Show that satisfies the partial differential equation
and write down the boundary conditions on . Deduce that the problem has a similarity solution of the form
Derive the ordinary differential equation and boundary conditions satisfied by .
Differentiate this equation once to obtain
and solve for . Hence show that
Sketch the temperature distribution for various times , and calculate explicitly.
A3.16
comment(i) A layer of fluid of depth , density and viscosity sits on top of a rigid horizontal plane at . Gravity acts vertically and surface tension is negligible.
Assuming that the horizontal velocity component and pressure satisfy the lubrication equations
together with appropriate boundary conditions at and (which should be stated), show that satisfies the partial differential equation
where .
(ii) A two-dimensional blob of the above fluid has fixed area and time-varying width , such that
The blob spreads under gravity.
Use scaling arguments to show that, after an initial transient, is proportional to and is proportional to . Hence show that equation of Part (i) has a similarity solution of the form
and find the differential equation satisfied by .
Deduce that
where
Express in terms of the integral
A4.19
comment(a) A biological vessel is modelled two-dimensionally as a fluid-filled channel bounded by parallel plane walls , embedded in an infinite region of fluid-saturated tissue. In the tissue a solute has concentration , diffuses with diffusivity and is consumed by biological activity at a rate per unit volume, where and are constants. By considering the solute balance in a slice of tissue of infinitesimal thickness, show that
A steady concentration profile results from a flux , per unit area of wall, of solute from the channel into the tissue, where is a constant concentration of solute that is maintained in the channel and . Write down the boundary conditions satisfied by . Solve for and show that
where .
(b) Now let the solute be supplied by steady flow down the channel from one end, , with the channel taken to be semi-infinite in the -direction. The cross-sectionally averaged velocity in the channel varies due to a flux of fluid from the tissue to the channel (by osmosis) equal to per unit area. Neglect both the variation of across the channel and diffusion in the -direction.
By considering conservation of fluid, show that
and write down the corresponding equation derived from conservation of solute. Deduce that
where and .
Assuming that equation still holds, even though is now a function of as well as , show that satisfies the ordinary differential equation
Find scales and such that the dimensionless variables and satisfy
Derive the solution and find the constant .
To what values do and tend as ?
A1.18
comment(i) The diffusion equation for a spherically-symmetric concentration field is
where is the radial coordinate. Find and sketch the similarity solution to (1) which satisfies as and constant, assuming it to be of the form
where and are numbers to be found.
(ii) A two-dimensional piece of heat-conducting material occupies the region (in plane polar coordinates). The surfaces are maintained at a constant temperature ; at the surface the boundary condition on temperature is
where is a constant. Show that the temperature, which satisfies the steady heat conduction equation
is given by a Fourier series of the form
where are to be found.
In the limits and , show that
given that
Explain how, in these limits, you could have obtained this result much more simply.
A3.16
comment(i) Incompressible fluid of kinematic viscosity occupies a parallel-sided channel . The wall is moving parallel to itself, in the direction, with velocity , where is time and are real constants. The fluid velocity satisfies the equation
write down the boundary conditions satisfied by .
Assuming that
where , find the complex constants . Calculate the velocity (in real, not complex, form) in the limit .
(ii) Incompressible fluid of viscosity fills the narrow gap between the rigid plane , which moves parallel to itself in the -direction with constant speed , and the rigid wavy wall , which is at rest. The length-scale, , over which varies is much larger than a typical value, , of .
Assume that inertia is negligible, and therefore that the governing equations for the velocity field and the pressure are
Use scaling arguments to show that these equations reduce approximately to
Hence calculate the velocity , the flow rate
and the viscous shear stress exerted by the fluid on the plane wall,
in terms of and .
Now assume that , where and , and that is periodic in with wavelength . Show that
and calculate correct to . Does increasing the amplitude of the corrugation cause an increase or a decrease in the force required to move the plane at the chosen speed
A4.19
commentFluid flows in the -direction past the infinite plane with uniform but timedependent velocity , where is a positive function with timescale . A long region of the plane, , is heated and has temperature , where are constants ; the remainder of the plane is insulating . The fluid temperature far from the heated region is . A thermal boundary layer is formed over the heated region. The full advection-diffusion equation for temperature is
where is the thermal diffusivity. By considering the steady case , derive a scale for the thickness of the boundary layer, and explain why the term in (1) can be neglected if .
Neglecting , use the change of variables
to transform the governing equation to
Write down the boundary conditions to be satisfied by in the region .
In the case in which is slowly-varying, so , consider a solution for in the form
Explain why is independent of and .
Henceforth take . Calculate and show that
where satisfies the ordinary differential equation
State the boundary conditions on .
The heat transfer per unit length of the heated region is . Use the above results to show that the total rate of heat transfer is