Exsolution and Phase Diagrams Lecture 11. Alkali Feldspar Exsolution ‘Microcline’ - an alkali feldspar in which Na- and K-rich bands have formed perpendicular.

Slides:



Advertisements
Similar presentations
The thermodynamics of phase transformations
Advertisements

Thermobarometry Lecture 12. We now have enough thermodynamics to put it to some real use: calculating the temperatures and pressures at which mineral.
MSEG 803 Equilibria in Material Systems 12: Solution Theory
Complex Phase Diagram construction using Free Energy vs. Composition Curves Author: Kartikay Agarwal Shrey Singh 10D D UG sophomore year.
Solutions Lecture 6. Clapeyron Equation Consider two phases - graphite & diamond–of one component, C. Under what conditions does one change into the other?
Lecture 13: Phase diagrams 2 PHYS 430/603 material Laszlo Takacs UMBC Department of Physics.
Activities in Non-Ideal Solutions
Lecture 18Multicomponent Phase Equilibrium1 Thermodynamics of Solutions Let’s consider forming a solution. Start with X A moles of pure A and X B moles.
Crystal-Melt Equilibria in Magmatic Systems Learning Objectives: –How are crystal-melt equilibria displayed graphically as phase diagrams? –What are the.
CHAPTER 8 Phase Diagrams 8-1.
Congruent and Incongruent Melting
Chapter 6 Interpretation of Phase Diagrams Phase diagrams summarize in graphical form the ranges of temperature (or pressure) and composition over which.
Chapter 14-Part VII Applications of VLLE.
Lecture 7 (9/27/2006) Crystal Chemistry Part 6: Phase Diagrams.
Phase diagram Need to represent how mineral reactions at equilibrium vary with P and T.
The Advanced Chemical Engineering Thermodynamics The retrospect of the science and the thermodynamics Q&A -1- 9/16/2005(1) Ji-Sheng Chang.
Melt-crystal equilibrium 1 l Magma at composition X (30% Ca, 70% Na) cools  first crystal bytownite (73% Ca, 27% Na) l This shifts the composition of.
Solution thermodynamics theory—Part IV
Mineral Stability What controls when and where a particular mineral forms? Commonly referred to as “Rock cycle” Rock cycle: Mineralogical changes that.
Notation convention Let G' stand for total free energy and in a similar fashion S', V', H', etc. Then we will let = G'/n represent the free energy per.
Lecture 9 Phase Diagrams 8-1.
(Earth Science Teachers’ Association)
Microstructure and Phase Transformations in Multicomponent Systems
Lecture 12: Phase diagrams PHYS 430/603 material Laszlo Takacs UMBC Department of Physics.
Phase equilibrium Plan 1.Phase equilibrium. Gibb’s phase rule. 2.Diagram of the state for a one component system 2.Diagram of the state for a one component.
The Phase Rule and its application. Thermodynamics A system: Some portion of the universe that you wish to study The surroundings: The adjacent part of.
Thermobarometry Lecture 12. We now have enough thermodynamics to put it to some real use: calculating the temperatures and pressures at which mineral.
Phases, Components, Species & Solutions Lecture 5.
Partial Molar Quantities and the Chemical Potential Lecture 6.
Geol 2312 Igneous and Metamorphic Petrology
Redox in Magmatic Systems Activities in Non-Ideal Solutions Lecture 10.
47.1 Ternary Phase Diagrams In ternary systems involving 3 components the Gibb’s phase rule predicts a maximum of: F = C - P + 2 = = 4 degrees.
The Phase Rule and its application
CHEE 311J.S. Parent1 4. Chemical Potential in Mixtures When we add dn moles of a component to n moles of itself, we will observe (?) a change in Gibbs.
 Thermodynamics?  Therma (heat) + Dynamics (study of the causes of motion and changes in motion)  Heat = energy (1 st law?)  Wiki: the branch of physical.
Solution thermodynamics theory—Part IV
10.5 Liquid and Solid Standard States
8. Solute (1) / Solvent (2) Systems 12.7 SVNA
Chapter 17 Stability of minerals. Introduction Kinetics (the rate of reactions): Kinetics (the rate of reactions): –Reaction rates slow down on cooling.
And now, THERMODYNAMICS!. Thermodynamics need not be so hard if you think of it as heat and chemical “flow” between “phases”.
Exsolution and Phase Diagrams Lecture 11. Alkali Feldspar Exsolution ‘Microcline’ - an alkali feldspar in which Na- and K-rich bands have formed perpendicular.
Lecture 4 Phase Diagram.
Solution thermodynamics theory—Part III
Gibbs-Duhem and the Chemical Potential of Ideal Solutions
Topic Name : Solid solution
Geol 2312 Igneous and Metamorphic Petrology
Phase Diagrams 8-1.
EQUILIBRIUM & STABILITY, LIQUID-LIQUID EQUILIBRIUM,
Solution of Thermodynamics: Theory and applications
Solutions and Thermobarometry
Geol 2312 Igneous and Metamorphic Petrology
Composition as a Variable (Two Component System)
Lecture 49 More on Phase Transition, binary system
Phase Diagrams Liquid a b Anorthite + Liquid T C Diopside + Anorthite
15 CHAPTER Chemical and Phase Equilibrium.
Hemin Hasary MSc. Pharmaceutical sciences
Chapter 4 Revision.
CHAPTER 8 Phase Diagrams 1.
CHAPTER 8 Phase Diagrams 1.
The effect of applied pressure on vapor pressure
Thermodynamic Properties
WCB/McGraw-Hill © The McGraw-Hill Companies, Inc.,1998 Thermodynamics Çengel Boles Third Edition 15 CHAPTER Chemical and Phase Equilibrium.
CHAPTER 8 Phase Diagrams 1.
Working with Phase Diagrams
Phase diagrams of pure substances
S. M. Joshi College, Hadapsar Welcome T. Y. B. Sc
The Phase Rule.
Phase Diagram.
Three component systems
The simplest picture of the atomic structure of metallic crystals is one of spherical ions closely packed and existing in a ‘sea’ of conduction electrons.
Presentation transcript:

Exsolution and Phase Diagrams Lecture 11

Alkali Feldspar Exsolution ‘Microcline’ - an alkali feldspar in which Na- and K-rich bands have formed perpendicular to the twinning direction. This leads to this cross-hatched or fabric-like texture under crossed polarizers.

G-bar–X and Exsolution We can use G-bar–X diagrams to predict when exsolution will occur. Our rule is that the stable configuration is the one with the lowest free energy. A solution is stable so long as its free energy is lower than that of a physical mixture. Gets tricky because the phases in the mixture can be solutions themselves.

Inflection Points At 800˚C, ∆G real defines a continuously concave upward path, while at lower temperatures, such as 600˚C (Figure 4.1), inflections occur and there is a region where ∆G real is concave downward. All this suggests we can use calculus to predict exsolution. Inflection points occur when curves go from convex to concave (and visa versa). What property does a function have at these points? Second derivative is 0. Albite-Orthoclase

Inflection Points Second derivative is: First term on r.h.s. is always positive (concave up). Inflection will occur when

Spinodal Actual solubility gap can be less than predicted because an increase is free energy is required to begin the exsolution process.

Phase Diagrams Phase diagrams illustrate stability of phases or assemblages of phases as a function of two or more thermodynamic variables (such as P, T, X, V). Lines mark boundaries where one assemblage reacts to form the other (∆G r =0).

Thermodynamics of Melting Melting occurs when free energy of melting, ∆G m, is 0 (and only when it is 0). This occurs when: ∆G m = ∆H m –T∆S m Hence: Assuming ∆S and ∆H are independent of T: where T i,m is the freezing point of pure i, T is the freezing point of the solution, and the activity is the activity of i in the liquid phase. T-X phase diagram for the system anorthite-diopside.

Computing an Approximate Phase Diagram We assume the liquid is an ideal solution (a i = X i ) and compute over the range of X i

Constructing T-X phase diagrams from G-bar–X diagrams We can use thermodynamic data to predict phase stability, in this case as a function of temperature and composition

Phase Rule and Phase Diagrams Phase rule: ƒ = c – ϕ + 2; c = 2 for a binary system. Accordingly, we have ƒ = 4 – ϕ and: PhasesFree compositional variables Univariant ϕ = 3; 2 solids + liquid, 2 liquids + solid 3 solids or liquids0 Divariant ϕ = 2; 1 solid + 1 liquid, 2 solids, 2 liquids0 Trivariant ϕ = 1; 1 solid or 1 liquid1 G-bar-X diagram for a trivariant, one-phase system exhibiting complete solid solution. Need to specify P, T, and X to completely describe the system. Trivariant System

Divariant Systems We need to specify both T and P (G-bar–X relevant only to that T and P). Two phases coexist on a plane in T–P–X space. G-bar-X diagrams for different divariant systems o (a) Liquid solution plus pure solid o (b) Liquid solution plus solid solution o (c) Two pure solids o (d) Limited solid solution (limited liquid solution would be the same) The free energy of the system as a whole is that of a mechanical mixture of phases – described by straight line through or tangent to free energies of individual phases. We deduce compositions of solutions by drawing tangents between curves (or points) for phases.

Univariant Systems One degree of freedom. o We specify only P or T. o Three phases in binary system can coexist along a line (not a plane) in P-T-X space. o only at one T, once we specify P (and visa versa). Compositions of solutions are determined by drawing tangents.

Plagioclase Solution Unlike alkali feldspar, Na-Ca feldspar (plagioclase) forms a complete solid (and liquid) solution. Let’s construct the melting phase diagram from thermodynamics. For simplicity, we assume both liquid and solid solutions are ideal.

Plagioclase Solution Condition for equilibrium: o e.g. Chemical potential is Combining these: o standard states are the pure end member solids and liquids.

Plagioclase Solution The l.h.s. is simply ∆G m for the pure component: rearranging Since X An = 1 - X Ab error in book: Ab on lhs should be An

Plagioclase Solution From: Solving for mole fraction of Ab in the liquid: The mole fraction of any component of any phase in this system can be predicted from the thermodynamic properties of the end-members. In the ideal case, as here, it simply depends on ∆G m and T. In a non-ideal case, it would depend on G excess as well. Computing the equation above (and a similar one for the solid), we can compute the phase diagram.