phase rule from rutstein
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8/3/2019 Phase Rule From Rutstein
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And now, THERMODYNAMICS!And now, THERMODYNAMICS!
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Thermodynamics need not be so hard if you think of it asThermodynamics need not be so hard if you think of it as
heat and chemical ³flow´ between ³phases´.heat and chemical ³flow´ between ³phases´.
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Derivation of Phase RuleDerivation of Phase Rule
Let¶s do a ³bookLet¶s do a ³book--keeping´ exercisekeeping´ exercise
and evaluate the number of and evaluate the number of
minerals (phases) that can cominerals (phases) that can co--existexist
in a chemical system under certainin a chemical system under certain
P,T conditions.P,T conditions.
(Derivation adapted from Prince, 1967,(Derivation adapted from Prince, 1967,
Alloy Phase Equilibria)Alloy Phase Equilibria)
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F F = C= C -- P + 2P + 2F = # degrees of freedom, or..F = # degrees of freedom, or..
The number of The number of intensiveintensive
parameters that must beparameters that must be
specified in order to completelyspecified in order to completely
determine the systemdetermine the system
What does this MEAN?What does this MEAN?
The Gibbs Phase RuleThe Gibbs Phase Rule
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F=
F= CC -- PP + 2+ 2
P = # of phasesP = # of phases
phases arephases are mechanicallymechanically
separableseparable constituentsconstituents
The Phase RuleThe Phase Rule--P & CP & C
C =C = minimum #minimum # of componentsof components
(the # of chemical constituents(the # of chemical constituentsthat must be specified in order tothat must be specified in order to
define all phases)define all phases)
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The Phase RuleThe Phase Rule--´2´´2´
F = CF = C -- P +P + 22
2 = the number of 2 = the number of intensiveintensive
parametersparameters
Usually = 2 for Usually = 2 for TemperatureTemperature andand
PressurePressure and this is especiallyand this is especially
useful for geologistsuseful for geologists
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Derivation of Phase RuleDerivation of Phase Rulea balancing of a balancing of
FIXED PARAMETERSFIXED PARAMETERSandand
SYSTEM VARIABLESSYSTEM VARIABLES
??which means???????which means?????
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HOW MANY VARIABLES AREHOW MANY VARIABLES ARE
THERE IN A CHEMICALTHERE IN A CHEMICALSYSTEM?SYSTEM?
Simplistically, ³3´,Simplistically, ³3´,
Pressure, Temperature, Composition,Pressure, Temperature, Composition,
BUT, for more than one phase, what isBUT, for more than one phase, what isthe TOTAL number of variables?the TOTAL number of variables?
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AssignAssign
CC components betweencomponents between PP phasesphases
For each Phase, composition is definedFor each Phase, composition is defined
byby (C(C--1)1) concentration terms.concentration terms.
For ALL Phases in the system,For ALL Phases in the system, P(CP(C--1)1) ==
the number of concentration terms.the number of concentration terms.
Can also vary Pressure & Temperature,Can also vary Pressure & Temperature,
or P + T, which =or P + T, which = 22 more variables.more variables.
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Therefore,Therefore,
the TOTAL NUMBER OF the TOTAL NUMBER OF
VARIABLES =VARIABLES =
P(CP(C--1) +21) +2
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NOW, LET¶S EXAMINENOW, LET¶S EXAMINE
HOW MANY FACTORSHOW MANY FACTORS
EXIST THAT FULLYEXIST THAT FULLY
DESCRIBE THEDESCRIBE THE
SYSTEM and ARESYSTEM and ARE
³FIXED´ BY THE SET³FIXED´ BY THE SETFACTORS.FACTORS.
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Since the system is inSince the system is in
equilibrium,equilibrium, BY DEFINITIONBY DEFINITION, we, we
have already implicitly definedhave already implicitly defined
some of the variables.some of the variables.
µµ = chemical potential or = chemical potential or
chemical flux or energychemical flux or energybetween two minerals.between two minerals.
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So, if system is ³in equilibrium´,So, if system is ³in equilibrium´,
and if there isand if there is NO NET CHANGENO NET CHANGE ininthe net ³amounts´ of chemicalsthe net ³amounts´ of chemicalsmoving between phases that are inmoving between phases that are indynamic equilibrium,dynamic equilibrium,
(e.g., NO NET MOVEMENT or (e.g., NO NET MOVEMENT or
CHEMICAL CHANGE, PLUS ORCHEMICAL CHANGE, PLUS ORMINUS BETWEEN PHASES),MINUS BETWEEN PHASES), thenthen
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AAµµ == AAµµ == AAµµ«.. =«.. = AAµµ
BBµµ == BBµµ == BBµµ«.. =«.. = BBµµ
CCµµ == CCµµ == CCµµ«.. =«.. = CCµµ
The chemical potential or the chemical fluxThe chemical potential or the chemical flux
of a given chemical must be the same in allof a given chemical must be the same in allphases coexisting at equilibriumphases coexisting at equilibrium--No NETNo NETChange!Change!
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So,So,
AAµµ == AAµµ && AAµµ == AAµµ
and, they yieldand, they yield
AAµµ == AAµµ
and then,and then,
TWO independent equations determine theTWO independent equations determine the
equilibrium between 3 phases for EACHequilibrium between 3 phases for EACH
Component.Component.
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For EACH Component,For EACH Component,
there are:there are:
(P(P--1)1) independent equationsindependent equations
relating the chemicalrelating the chemical
potential,potential, µµ, of that, of that
component incomponent in ALLALL of theof thePhases.Phases.
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For theFor the GENERALGENERAL case of Pcase of P
phases and C components,phases and C components,
There areThere are
C(PC(P--1)1) independent equations.independent equations.
Thus, weThus, we ³FIX´ C(P³FIX´ C(P--1)1)
variablesvariables when we stipulate thatwhen we stipulate thatthe system is in equilibriumthe system is in equilibrium..
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Now, the number of Now, the number of
independent variables or independent variables or the total number of the total number of
variations which can bevariations which can be
made independently =made independently =
the total number of the total number of
variables, less those thatvariables, less those thatare automatically fixed.are automatically fixed.
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F= number of ³Freedom´ factorsF= number of ³Freedom´ factors
F= [P(C
F= [P(C--1) +2]1) +2] ± ± [C(P[C(P--1)]1)]
TOTALTOTAL AUTOMATICALLYAUTOMATICALLY
FIXEDFIXED
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The variance of a system or theThe variance of a system or the
Degrees of Freedom =Degrees of Freedom =
F= CF= C--P +2P +2
Which is calledWhich is called
the Gibb¶s Phase Rule.the Gibb¶s Phase Rule.
For a ´dry´ system w/ no vapor,For a ´dry´ system w/ no vapor,
F =CF =C--P +1P +1
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The Goldschmidt MineralogicalThe Goldschmidt Mineralogical
Phase RulePhase Rule
What is the likelihood of What is the likelihood of
being on a specificbeing on a specificreaction curve in Preaction curve in P--TT
space or being inspace or being in
³general´ P³general´ P--T space,T space,
where P & T are variables?where P & T are variables?
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The Phase Rule in MetamorphicThe Phase Rule in Metamorphic
SystemsSystems
If F If F uu 2 (at least P & T are variables)2 (at least P & T are variables)which is the most common situation,which is the most common situation,then the phase rule may be adjustedthen the phase rule may be adjusted
accordingly:accordingly:F = CF = C -- P + 2, and P = CP + 2, and P = C
PP ee CC which iswhich is Goldschmidt¶sGoldschmidt¶s³Mineralogical Phase Rule´³Mineralogical Phase Rule´when solid solutions andwhen solid solutions andsystem is ´open´ andsystem is ´open´ andcomponents are ³mobile´.components are ³mobile´.
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Consider each of the following three scenarios for Consider each of the following three scenarios for PP--T space for the aluminoT space for the alumino--silicate polymorphs:silicate polymorphs:
C = 1C = 1
P= 1P= 1 commoncommon
P= 2P= 2 rarerare
P= 3P= 3 only at theonly at the
specific Pspecific P--TT
conditions of theconditions of the
invariant pointinvariant point
(~ 0.37 GPa and(~ 0.37 GPa and500500ooC)C)
Calculated P-T phase diagram for
the system Al2SiO5. Winter, 2001
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³Problems´ in real Rock Systems³Problems´ in real Rock Systems
Equilibrium has not been attainedEquilibrium has not been attained
The phase rule applies only toThe phase rule applies only to
systems at equilibrium, and theresystems at equilibrium, and therecould be any number of mineralscould be any number of minerals
coexisting if equilibrium iscoexisting if equilibrium is notnot
attainedattained
We didn¶t chooseWe didn¶t choose the number the number of of
components correctlycomponents correctly
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Choosing the number of Choosing the number of
components correctlycomponents correctly
Components that substitute for each other Components that substitute for each other
Adding a component such as NaAlSiAdding a component such as NaAlSi33OO88
(albite) to the 1(albite) to the 1--C anorthite system wouldC anorthite system would
dissolve in the anorthite structure, resultingdissolve in the anorthite structure, resultingin ain a single solidsingle solid--solution mineralsolution mineral (plagioclase)(plagioclase)
below the solidusbelow the solidus
Fe and Mn commonly substitute for MgFe and Mn commonly substitute for Mg
Al may substitute for SiAl may substitute for Si
Na may substitute for KNa may substitute for K
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Correct number of components:Correct number of components:
³Perfectly mobile´ components³Perfectly mobile´ components
Mobile components are either a freely mobileMobile components are either a freely mobile
fluid component or a component thatfluid component or a component that
dissolves readily in a fluid phase and can bedissolves readily in a fluid phase and can be
transported easily.transported easily.
The chemical activity of such components isThe chemical activity of such components is
commonly controlled by factorscommonly controlled by factors externalexternal toto
the local rock systemthe local rock system
They are commonly ignored in deriving C for They are commonly ignored in deriving C for
most rock systemsmost rock systems