Phase Diagrams II Notes

Week 7a – Phase Diagrams II

Phase Rule in Binary T-X Sections

The phase rule is defined as:
F+P=C+nF + P = C + n
Where:

  • CC = components
  • PP = phases
  • FF = degrees of freedom
  • nn or integer = intensive variables (Pressure) = 1

Therefore:
F=C+1PF = C + 1 - P
If F=2F = 2, then F=1F = 1

Tools for Phase Diagrams

  • Phase proportions = lever rule
  • Phase compositions = read from axis

Given a diagram with temperature (°C) on the y-axis and composition (A and B) on the x-axis, and regions for A, B, L (liquid), and AB+L (A and B + liquid):

To calculate phase proportions:

  • % solid = x<em>Lx</em>AB+xL100\frac{x<em>{L}}{x</em>{AB} + x_{L}} * 100
  • % liquid = x<em>ABx</em>AB+xL100\frac{x<em>{AB}}{x</em>{AB} + x_{L}} * 100

Where:

  • xmeltx_{melt} = composition of the melt
  • xsolidx_{solid} = composition of the solid
  • xABx_{AB} = composition of the solid phase
  • xLx_{L} = composition of the liquid phase

Binary Example: Equilibrium Crystallization

A phase diagram is presented with temperature (°C) on the y-axis and composition on the x-axis ranging from Mg2SiO4 (Fo) to SiO2 (Qz), with MgSiO3 (En) in between.

Regions include:

  • Fo + L (Forsterite + Liquid)
  • En + L (Enstatite + Liquid)
  • Qz + L (Quartz + Liquid)
  • Fo + En (Forsterite + Enstatite)
  • En + Qz (Enstatite + Quartz)
  • L (Liquid)

Binary Example: Fractional Crystallization

A phase diagram is presented with temperature (°C) on the y-axis and composition on the x-axis ranging from Mg2SiO4 (Fo) to SiO2 (Qz), with MgSiO3 (En) in between.

Regions include:

  • Fo + L (Forsterite + Liquid)
  • En + L (Enstatite + Liquid)
  • Qz + L (Quartz + Liquid)
  • Fo + En (Forsterite + Enstatite)
  • En + Qz (Enstatite + Quartz)
  • L (Liquid)

Compositions on Ternary Diagrams

  • Pure A plots at A.
  • Compositions with 50% A.
  • Same for other components, e.g. A20B50C30. A, B, and C are components of the ternary diagram.

Liquidus Projections

Key features:

  • Liquidus surface
  • Ternary eutectic
  • Binary eutectic
  • Ternary cotectic

Diagram shows regions:

  • X + Y
  • Y + Z
  • X + m
  • Y + m
  • Z + m
  • m + Y

Where X, Y, and Z are end-member components, and 'm' refers to the melt phase.

Equilibrium Crystallization

Crystallization path of A:

  • What phase crystallizes 1st?
  • Melt moves directly away from crystals.
  • Divariant curve → fixed bulk means follows it.
  • @ peritectic → which 3 phase triangle is the bulk in?
  • As in Fo-En-An cannot produce Qz

x<em>Lx</em>fo+xL100=\frac{x<em>{L}}{x</em>{fo} + x_{L}} * 100 = % liquid remaining

Where:

  • xLx_L = Composition of liquid.
  • xfox_{fo} = Composition of forsterite.

F=C+1PF = C + 1 - P

Equilibrium Crystallization (Continued)

Crystallization path of A:

  • What phase crystallizes 1st?
  • Melt moves directly away from crystals.
  • Divariant curve → fixed bulk means follows it.
  • Melt cannot produce any more fo, skips P.
  • Continues to eutectic.
  • Bulk in En-An-Qz triangle

xfo+enx_{fo+en}

Equilibrium Melting

Reverse of crystallization:

  • What 3 phase triangle?
  • First melt at relevant invariant (P).
  • Now proceeds along divariant until.
  • Co-aligned with Fo and bulk (as bulk in Fo field).

Fractional Crystallization

  • Imagine that the “effective bulk” keeps changing as crystals are removed.
  • The melt basically just keeps going downhill (it will always end at eutectic if only one is present).
  • But also - crystals are removed! So it doesn’t (always) follow divariants.

Fractional Crystallization & Lever Rule

  • The lever rule tells you about the cumulates

1 fo

x<em>Lx</em>fo\frac{x<em>{L}}{x</em>{fo}}

2, 3, 4 en. When 2 phases are crystallizing, take the tangent to divariant.
x<em>Lx</em>en\frac{x<em>{L}}{x</em>{en}}

en + an.

X<em>anX<em>{an}X</em>enX</em>{en}

xsolidx_{solid}

en + an
xLx_{L}

  • qz

Reading Resources

  • Chapter 2 Essentials of Igneous & Metamorphic Petrology (essential)
  • Chapter 8 Open Petrology (optional, a good resource!!)
  • Chapter 11 Principles of Igneous and Metamorphic Petrology (optional, more detail than required)

Practical 3: Ternary Phase Diagrams

  • Practice interpreting ternary phase diagrams [< 2 hours, finish in your own time].
  • Understand the difference between batch vs. fractional paths.
  • Apply the lever rule in a ternary system.
  • Ensure you know how to do this.