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In a supersaturated solid solution, precipitation may lead to the formation of grains or particles of a new phase. It is found that, after an
In a supersaturated solid solution, precipitation may lead to the formation of grains or particles of a new
phase. It is found that, after an initial stage of this process that involves nucleation, there is a second stage
in which the particles grow to much larger sizes. In the second stage the degree of supersaturation is slight,
and the rate of particle growth is controlled by diffusion. This coarsening of particles, called Ostwald
ripening, has important effects on the physicals properties of various alloys. An extensive analysis of the
kinetics of the second stage of this process was given by Lifshitz and Slyozov The objective here is
to derive one of their simpler results.
Consider a dilute solid solution consisting of components A and B with B the abundant species. The
particles being formed by precipitation are composed of pure B The densities of the particle and the
solution are the same. Because B is the abundant species, we do not need to consider its transport. We
only need to account for transport of species A Assume that at any given time the precipitate consists of
widely dispersed spherical particles of radius Rt Accordingly, it is sufficient to model one representative
particle, for which CA CAr t in the surrounding solution. Far from the particle the concentration of A
is constant at CAinfty A key aspect of this problem is that the concentration of A at the particle surface is
influenced by the interfacial energy and therefore depends on particle size. The relationship is:
CARt t CAinfty
Gamma
Rt
where the constant Gamma is proportional to the interfacial energy. It is the interfacial energy term that provides
the driving force for diffusion.
a Draw the physical system described in the problem. Since we are not modeling transport of B do not
show species B in the drawing. What is CA inside the particle? What is CA on the particle surface at
r Rt What is CA far away from the particle at r infty Indicate these on the drawing.
b Assume diffusion of A outside the particle is pseudosteady. Starting with the pseudosteady ODE and
boundary conditions, derive the pseudosteady concentration profile CAr t outside the particle. Note, the
ODE can be solved by direct integration.
c An expression for the growth rate dRdt of the particle can be derived from the interfacial conservation equation at the particle surface. Start from the general form of the interfacial conservation equation
considering only the r scalar components of all vectors
f CAv vI out f CAv vI in Rs
Here, f is the diffusive flux, v is the background flow velocity, CAv is the convective flux, vI is the interface
velocity, Rs is the surface generation rate of new A species, and the out and in subscripts indicate on
which side of the particle surface the quantities are evaluated on Note that some of the terms are zero and
that the diffusive flux f is specified by a constitutive equation Ficks law Use your pseudosteady state
profile from part b to obtain the expression for dRdtHint: Where would dRdt enter this interfacial
balance?
d Without solving for Rt what happens to R as t infty Considering this limit of dRdt what is the
ODE for Rt at very large times t
e By solving the ODE, show that, eventually, Rt t
While solving, you may assume that Rt
R but R cannot appear in the proportionality Rt t
f Define the process time tp as the characteristic time it takes the particle to grow an amount roughly equal
to its size, ieRR Starting with your equation for dRdt from part d use orderofmagnitude
reasoning to get tp
g We can define the diffusion time td as the characteristic time it takes for A to diffuse an amount roughly
equal to the particle size, ie td RD Using your estimate for the process time and this definition of
diffusion time, determine the conditions on R for the pseudosteady assumption to be valid.
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