1. Transport Equations and Flux Laws Basic concepts and ideas 1.A concept model of Diffusion 2.The transient Diffusion Equation 3.Examples of Diffusion Fluxes 4.The Advection-Diffusion Equation

2. A concept model for Diffusion Imagine “social” particles particles arranged and oscillating laterally on a lattice A given particle can only interact with its two nearest neighbors. the particle is determined to fit in and tries over time to take on the attributes of its neighbors –lets assume that there is a minimum time for the particle to achieve full social equilibrium. (based on the neighboring particle attributes at the beginning of the time step) L P R As an equation Attribute of P at new time old new We can use this equation to advance the evolution of the attributes at a point in time.

3. One example would be an initial top hat distribution (a set of red particles isolated in a sea of white particles) Red Intensity Particles in middle loose intensity particles at edge increase in intensity As we move from left to right in the domain How does the intensity of the red in the particles change

4. Another example is when the dye of the left most particle is continuously topped up to retain its intensity while the initial state of the other particles is white Fixed red Fixed white Time Approaches A steady state

5. L P R old new We can rewrite our equation as

6. Aside Assume (i) particles oscillate in a range +/- ½ of the lattice spacing (ii) that in a unit time the particle moves a unit distance with equal probability of going left of right (until it reaches its oscillation limit it which case its direction is reversed), and (iii) particles only have To meet once to come in “equilibrium” Simulation shows that when the particles are 2 units apart The expected meeting (equilibrium) time is 8 units 4 units apart The expected meeting (equilibrium) time is 32 units 8 units apart The expected meeting (equilibrium) time is 128 units So we can write Where  is a proportionality constant (m 2 /s) In this way

7. L P R old new We can rewrite our equation as Further in a more general setting we can check in on the progress of our solution at time steps Arriving at the update equation

8. L P R We can write this equation as Captures interaction between particle at point P and particle at point R

9. L P R If the interactions occur faster on the left that the right we can adjust the value of the diffusivities That is write Where If our particles were molecules we would expect very rapid times and short distances

10. The transient diffusion equation where Is the x component of flux (quantity/area/time) In an isotropic material

11. So we see that we will have a movement of quantity down a potential gradient In the model developed here we get the flow of quantity without macroscopic movement of the medium The molecules (particles) vibrate but the medium does not “flow” EXAMPLES Diffusion of a Chemical Species Diffusion of heatDiffusion of ground water Fick’s LawFourier’s LawDarcy’s Law (medium fixed porous media) Potential  : Molar Concentration C [moles/m 3 ] Potential  : Temperature [K] Potential  : head [m] Transported quantity: mass (moles) Transported quantity: heat (joules) [J] Transported quantity Volume [m 3 ] Flux: [moles/m 2 -s] Flux: [J/m 2 -s] Flux: [m 3 /m 2 -s] Coefficient: D [m 2 /s]-mass diffusivity Coefficient: K [J/m-s-K]-thermal conductivity Coefficient: k [m/s] –hydraulic conductivity [quantity/area-time] In a general 3-D field The diffusive flux in an ISOTROPIC material is

12. The advective flux C = C red C = 0 A fluid is moving down a pipe with velocity u. At time t the fluid to the left of a point x contains an immiscible (incapable of being mixed without separation of phases) dye at a concentration Cred. As the dye front moves through the box of length  x its average concentration increases from C = 0 to C= C red. u x xx What is the rate [moles/time] per unit area of dye entering the box q u = [moles/area-time] In general—the advective flux of a given quantity at a point in a flowing medium is a vector obtained by multiplying the velocity vector with the scalar [quantity/area-time] Mass Transport  C [moles/m 3 ] Heat Transport c—specific heat [J/kg-K] May which to write heat diffusive term as Diffusivity m 2 /s

13. n Total Flow across a surface element Consider a surface element of area dA and normal n in a flowing material which contains conserved scalar quantity The Total flux at any point on the surface will be And the total quantity crossing the surface in the Opposite direction to the normal n is [quantity/ time] n q Resolution of q in across Surface depends on surface orientation

14. Slope of  in direction of normal Diffusive flux in opposite direction To normal -u.n Advective flux In opposite direction To normal u n u n Direction of normal will control value of flux across surface. E.g. advection flux Addendum u n u n Max advec flux Zero Advec flux

15. Conservation Balance—Steady State No Source u(x,t) n Now consider a FIXED Arbitrary control volume located in A flowing material (velocity u) If there is no accumulation (steady state) or Generation or dissipation (Source/Sink) The net flow rate of a given quantity INTO the Volume has to be zero What goes in has to come out In math using the definition of the general flux By the divergence theorem But since volume V is chosen arbitrarily the argument in the integral must be identically zero At all points in the domain—leading to the general steady state diffusion-advection transport equation