(1) NONEQUILIBRIUM
SOLIDIFICATION
Group:
material | transformations
There
is no old definition
NEW DEFINITION
Nonequilibrium conditions vary
widely from process to process, from manufacturer to manufacturer for a given
process, and from day-to-day (and batch to batch within a day) for a specific
process performed by a specific manufacturer. There are literally an infinite
number of ways in which conditions can differ from equilibrium. and only one
way there can be equilibrium. To take into account the effects of
nonequilibrium is not simple, and the best that can be done is to model some
cases as boundary (or bounding) conditions. Because, as engineers, you will
spend much of your working life dealing with nonequilibrium, we will look at
one example of how nonequilibrium results in different microstructure during
the solidification of a single-phase alloy now.
So, let us reconsider the case
of nonequilibrium solidification of a single-phase alloy in an isomorphous binary
system to see how the microstructure that develops differs from equilibrium.
Figure 13.18. Cooling from the
melt will occur too fast for equilibrium to prevail during the process of
solidification. The boundary conditions that will be imposed (because
nonequilibrium always requires some statement or assumption about the bounding
conditions) are:
(1) complete mechanical stirring of
the liquid will assure uniform composition throughout the volume of liquid
present (i.e., we are not relying on diffusion of atoms in the liquid to keep
the composition uniform) and
(2) there will be no time for any
diffusion in the solid state, so the composition of solid at every stage of its
formation will remain unchanged. In many references on solidification in
general, and welding in particular, this set of boundary conditions is known as
Case 2 (with equilibrium solidification being known as Case 1).
·
Above
the equilibrium liquidus temperature. Tliquidus entire volume of
material is liquid L of composition Co for an alloy of composition Co.
·
Upon
reaching T1, just below Tliquidus, the first equiaxed particles (or
grains) of solid of composition Cs, begin to form randomly
throughout the volume of liquid I. under homogeneous nucleation. Because not
all of the solute B dissolved in the L at Co can be accommodated in
the new solid (i.e., Cs, < C0), the excess solute B
rejected into the liquid at the S–L interface is assumed (here) to be
immediately mechanically mixed through the entire liquid, raising its
composition slightly above Co to CL1.
·
As
the temperatures continues to fall farther below Tliquidus say to T2
the new solid that forms on the outside of all of the original particles of
solid, along with some additional new particles of solid, has composition Cs2’
which is higher in solute B than Cs, as the result of it
having been formed from liquid containing more solute B than Co.
Because there is assumed to be no diffusion in the solid state, this new layer
of Cs: forms over the earlier particles of Cs1. resulting
in a cored structure. Rejection of solute B as this new layer of solid forms
raises the composition of the liquid L to CL2—everywhere due to
instantaneous mechanical stirring.
·
The
average composition of particles or grains of the solid formed to this point
(i.e., between Tliquidus and T2} is not Cs2
however, because the cores of the particles or grains contain less solute R
than Cs2, (i.e., Cs1 in this case). Hence, the average
solute composition of all of the solid formed to this point lies somewhere
between Cs1 and Cs2 depending on the slopes of the
liquidus and solidus lines and on the relative volume fractions of each in the
particles or grains. indicated here by an X.
·
Upon
reaching the equilibrium solidus temperature. Tliquidus, at which
solidification would be completed under equilibrium, here called T3, the new
solid forming from liquid (as an outer layer on all previously formed grains,
as well as forming some new grains by further nucleation) with the composition
CL3, has the composition Cs, = Co. Once again,
the average composition of all of the solid formed to this point (i.e., to T3)
lies between Cs2 and Cs, = Co, here shown by
the X at T3
·
Because
the total composition of all of the solid formed has not reached C0
(the composition of the starting liquid L), the material or mass balance is not
correct and, thus, solidification cannot actually be completed. For
solidification to be completed, the average composition of the solid (grains)
must be Co.
·
By
extending the average solid composition line (shown bold and dashed) until it
crosses the composition line at Co, it can be seen that
solidification under these nonequilibrium conditions is not actually completed
until the temperature reaches T4. At T4, the composition of the last solid
layer formed is Cs4 having formed from highly solute-enriched CL4.
The consequences of such
nonequilibrium solidification of an alloy are: ( I) resulting grain structure
(actually, dendritic structure in real castings or welds) will be cored, with
varying composition (and, thus, properties) from solute-lean regions near the
grain centers to highly solute-enriched at grain boundaries, often with weak or
brittle grain boundary regions; (2) solidification well below the equilibrium
solidus tem-perature, typically 50 to a couple of hundred degrees C (90 to
several hundred degrees F) for real alloys, depending on their melting ranges:
and (3) unexpected remelting (upon reheating in service, for example) at grain
boundaries. Unfortunately, such microsegregation of solute during
nonequilibrium solidification is a natural consequence of solute redistribution
and is largely unavoidable. There are, in fact, additional complications with
nonequilibrium, because deviation from equilibrium shifts transformation
temperatures (i.e., phase boundary lines) on equilibrium phase diagrams.
Nonequi-librium heating shifts transformation temperatures upward, more for
faster heating rates, whereas nonequilibrium cooling shifts transformations
downward, more for faster cooling rates. The effects of cooling are generally
greater than the effects of heating, because it is easier to cool rapidly than
to heat rapidly. Shifting phase transformations require phase boundary lines to
change in slope and extend into the normally adjoin-ing phase region, thereby
shifting the compositions of the phases that form also. In rare cases, extreme
nonequilibrium solidification can result in nonequilibrium metastable phase formation,
but this is rare. Not so during nonequilibritun solid-state transformations,
however.
(Robert
W. Messler, The Essence of Materials for Engineers, pg.391-393)
No comments:
Post a Comment