- 134 Views
- Uploaded on
- Presentation posted in: General

Binary Phase Diagrams

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.

- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -

Binary Phase Diagrams

GLY 4200

Fall, 2012

- Binary diagrams have two components
- We therefore usually choose to plot both T (temperature) and X (composition) with pressure held constant
- P-X (T fixed) or P-T (X fixed) are also possible

- Binary solid solution - olivine, plagioclase feldspar
- Binary eutectic with congruent melting - potassium feldspar - silica
- Binary peritectic and eutectic with solid to solid conversion - leucite - Potassium feldspar - silica
- Binary minimum melting point - potassium feldspar - albite
- Binary minimum melting point with solvus - potassium feldspar - albite

- f = c - p + 2 = 2 - p + 2 = 4 - p
- If two phases are present, there are two degrees of freedom (both T and X)
- If three phases are present, there is one degree of freedom (either T or X)

- Plagioclase Feldspar series, 39% of the earth’s crust

- How many degrees of freedom are present at points 1,2, and 3?

- Two immiscible components: such as CaAl2Si2O8 (calcic plagioclase) and FeMgSiO4 (olivine) plotted along the horizontal axis, OR olivine (isolated tetrahedra) and pyroxene (single chain tetrahedra), which are immiscible because they have different crystal structures
- One variable, temperature, plotted along the vertical axis.
- Pressure is held constant at 1 atmosphere.
- Three phases, crystal A, crystal B, and melt.
- Complete miscibility of the melt (magma)

- The system remains in equilibrium throughout its history, so that all reactions can take place and everything can come to stability
- Everything in the original melt remains in communication throughout the crystallization process

- The previous case is an example of congruent melting
- Congruent melting means melting of a substance directly to a liquid that is of the same composition as the solid

- Melting accompanied by decomposition or by reaction with the liquid, so that one solid phase is converted into another
- Melting to give a liquid different in composition from the original solid
- One example occurs in the forsterite-quartz system

- L = Liquid
- Fo is fosterite
- En is enstatite
- Qtz is quartz

- MgSiO3 + SiO2 = Mg2SiO4
- En + Qtz = Fo

- Two liquid phases are present on the right side of the diagram

- C = 65 weight% β

- Solid phase B starts to form with a composition of 96 weight% β

- C1 = 58 weight% β and C2 = 92 weight% β

- Fraction of solid b = (65 - 58) / (92 - 58) = 20 weight%
- Fraction of liquid = (92 - 65) / (92 - 58) = 80 weight%

- C3 = 48 weight% β
- C4 = 87 weight% β

- Fraction of solid with composition C4 = (65 - 48) / (87 - 48) = 44 weight%.
- Fraction of liquid at eutectic = 56 weight%

- C5 = 9 weight% β and C6 = 91 weight% β

- Fraction of solid with composition C6 = (65 - 9) / (91 - 9) = 68 weight%
- Fraction of solid with composition C5 = (91 - 65) / (91 - 9) = 32 weight%

- With increased pressure, from 1 atm to 7 kbar, En changes from incongruent to congruent melting behavior
- The field of liquid immiscibility, the 2L field on the 1 atm diagram, disappears at slightly elevated pressures and is no longer evident in the 3 kbar diagram.

- Points on the edge have only two components

- Note that the scales are plotted increasing in a CCW directions

- Ternary diagrams can be used to plot any three things

- Another use of ternary diagrams

- Sample ternary diagram

Silica

0

100

90

10

80

20

70

30

60

40

% Silica ↑

% Kalsilite ↓

50

50

60

40

70

30

80

20

90

10

0

100

90

80

70

60

50

40

30

20

10

0

100

Nepheline

Kalsilite

← % Nepheline