Growth II Twinning, defects, and polymorphism Jon Price ongratula - - PowerPoint PPT Presentation

growth ii
SMART_READER_LITE
LIVE PREVIEW

Growth II Twinning, defects, and polymorphism Jon Price ongratula - - PowerPoint PPT Presentation

Growth II Twinning, defects, and polymorphism Jon Price ongratula on i twins! Rational, symmetrical intergrowth of structures This raises the internal energy hromi ontac Growth twins - free growth


slide-1
SLIDE 1

Growth II

Twinning, defects, and polymorphism

Jon Price

slide-2
SLIDE 2
  • ngratulaon…i twins!

Rational, symmetrical intergrowth of structures This raises the internal energy

  • Growth twins - free growth accidents, where

a lattice becomes offset during nucleation

  • Transformation twins - movement of parts of

the lattice when internal symmetry changes

  • These may be contact (planar face) or

penetration (throughgoing) twins.

  • Gliding twins - offsets in the lattice as a strain

(in response to a stress). Polysynthetic

hromi ontac

  • win

tauroli

  • eneaon twin
slide-3
SLIDE 3
slide-4
SLIDE 4

Common Twin Laws Triclinic

Albite twinning: plagioclase feldspars (CaAl,NaSi)AlSi2O8 commonly show b-axis perpendicular polysynthetic twinning Pericline twinning: microcline, KAlSi3O8 , develops twining around the [010] axis when it transforms from a monoclinic structure X-polar photomicrograph by K. Hollocher, Union

http://open-adit.com

slide-5
SLIDE 5

Common Twin Laws Monoclinic

Manebach twinning: orthoclase, KAlSi3O8 , contact twin. Very common. Formed from accidental growth. Carlsbad twinning: orthoclase and sanidine, KAlSi3O8 , develop penetration twining around the [001]. Formed from accidental growth. Baveno twinning: orthoclase, KAlSi3O8 , develops contact twin during accidental growth.

http://open-adit.com

slide-6
SLIDE 6

Common Twin Laws Monoclinic

Swallow tail twinning: gypsum, CaSO4 2H2O , develops contact twin during accidental growth. Most are cyclical contacts

  • n {011}. Rutile (TiO2) and

cassiterite (SnO2) are examples.

Tetragonal

http://open-adit.com

slide-7
SLIDE 7

Common Twin Laws Hexagonal

Calcite twinning: Common contact twins are {0001} and rhombohedron. The right from can also can be stress Induced. Brazil twinning and daupine twinning: Penetration quartz twins resulting from transformation.

http://open-adit.com

slide-8
SLIDE 8

Common Twin Laws Isometric

Spinel twinning: contact twin parallel to an

  • ctahedron common to spinel (MgAl2O4)

Iron cross twin: Pyrite (FeS2), 2/m class, may have pentration twinning

  • f the forms with appearant 3A4

symmetry.

http://open-adit.com

slide-9
SLIDE 9

Defects

Missing atoms (vacancies) Impurities Edge dislocations Screw dislocations Interlayered structures Twins

slide-10
SLIDE 10

Non-stoichiometric atoms Schottky defect

Image from Perkins, 1998

slide-11
SLIDE 11

Frenkle defect Edge defect

Image from Perkins, 1998

slide-12
SLIDE 12

Edge defect Screw dislocation AFM image of growth spiral on graphite along [001]. MIT STM image of PtNi alloy edge defects Michael Schmid,

IAP/TU Wien

slide-13
SLIDE 13

Importance of defects

Incorporation of non-stoichiometric elements (non substitution) Color Incorporation of foreign materials inclusions Can produce diagnostic characteristics Twinning in feldspar

slide-14
SLIDE 14

Energy Minimization

Everything explained in the course thus far is the result

  • f energy minimization!

Examples?

In nature, energy is the only commodity.

slide-15
SLIDE 15

Energy Minimization - a system will assume a state of minimum energy. Parameterizing energy - the Gibb’s Free Energy equation

G = E + PV - TS

E is a measurement of lattice energy, or the sum

  • f bond energy

P is pressure V is molar volume T is temp S is entropy note: E + PV = H

slide-16
SLIDE 16

So Free Energy is dependent

  • n:
  • 1. The nature of the bonding
  • 2. Pressure
  • 3. Temperature
  • 4. Degree of disorder
slide-17
SLIDE 17

The Carbon System

Graphite - steep dG/dP Diamond - higher initial G, shallow dG/dP

slide-18
SLIDE 18

Image modified from Zoltai and Stout, 1984

Diamond’s excited state

slide-19
SLIDE 19

Poly morph - µ many forms

These abound in Earth Materials and can be of great use in pinning down the conditions at which the mineral formed.

slide-20
SLIDE 20

Why can we observe graphite and diamond at the same time? There is a place where both phases share the same G, but at room T, this is ~14 kbar!

slide-21
SLIDE 21

At P = 5 kbar

slide-22
SLIDE 22

Image from Pauling, 1970

slide-23
SLIDE 23

Phase Diagram

Recall that as you go into the Earth, both P and T increase These two variables control phase stability of compositions in the earth. On the left is a map for phases of carbon

slide-24
SLIDE 24

Reconstruction vs. displacement

Displacement requires less transition energy because lattices are just “tweaked” Reconstruction requires substantial excess energy to move things to new configuration

slide-25
SLIDE 25

Polymorphs

slide-26
SLIDE 26

From Blackburn & Dennen, 1998

slide-27
SLIDE 27

Silica Polymorphs

slide-28
SLIDE 28

More ‘morphs

CaCO3 AlSiO5

slide-29
SLIDE 29

Order-disorder

Reorganization of atoms into more ordered arrangements Decrease in T produces higher order

G = E + PV - TS

Change in structure accompanies change in order.

slide-30
SLIDE 30

Alkali Feldspar Order-disorder

M T T

slide-31
SLIDE 31

Polytypism

Polymorphs that differ only in the stacking of identical, two-dimensional sheets or layers. Cell dimensions parallel to sheets are identical Spacing between sheets is related by multiples .

slide-32
SLIDE 32
  • 1. Increasing P results in structures with

high densities and large CN are favored

  • 2. Increasing T favors low density and CN
  • 3. High-T modifications often has highest

symmetry

slide-33
SLIDE 33

In summary - Polymorphism is a reconfiguration of chemical components in response to changing energy. Polymorphs therefore have the same composition but differing structures.