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Nucleation and crystallization

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Title: Nucleation and crystallization


1
Nucleation and crystallization
2
Forming crystals
  • From solutions, melts, vapors
  • From disordered and random to ordered
  • Halite crystals demo

3
Halite
  • Solution with Na and Cl-
  • Finally super saturated, solid precipitates ion
    by ion

4
Halite
  • Evaporation rate impacts crystal size
  • Can force precipitation with evaporation, drop in
    T, drop in P
  • Same from melts

5
Stability of minerals
  • Stable
  • Unstable
  • metastable

6
Gibbs free energy (G)
  • Comparison of G tells you which mineral is more
    stable
  • Stable minerals have lowest ?G at specific T and P

7
Nucleation
  • Appropriate atoms must find each other,
    chemically bond, form a nucleus of a crystal
  • Then nucleus progressively grows adding more
    atoms to surface

8
Nucleation
  • Atoms constantly bumping into each other forming
    embryos
  • Some embryos will by chance have correct
    composition and structure

9
Nucleation
  • Embryos try to reach size-critical radius
  • Whether a mineral will grow depends on Gibbs Free
    energy

10
Nucleation
  • Embryos dont form at exact equilibrium T
  • To nudge growth, you need to undercool (like
    activation energy)
  • To no undercooling
  • T1 low undercooling
  • T3 large undercooling

11
Nucleation
  • Small undercooling, slow cooling (magma in
    crust), less nuclei but larger crystals
  • Large undercooling, fast cooling (volcanic
    rocks), more nuclei but small crystal size

12
Nucleation
  • Rate of nucleation and growth as function of T
    below melting T

13
Crystal growth
  • If nucleus is to survive, grows fast enough to
    reduce surface energy and therefore solubility
  • Single large crystal more stable than many small
    ones
  • Perfect shaped crystal more stable than irregular
    one

14
Crystal growth
  • Once nuclei stable, need to add atoms
  • Atoms stable with lowest surface area
  • Where is energetically best place to put new
    atoms?

15
Rate of growth
  • Calcite in lab 14.8 ?m/day - 6 cm in 11.26 years
  • Plag in magma chamber can be 10,000 years for 1
    cm
  • Calcareous concretions in se rocks 5 cm in 1.7
    Ma

16
Rate of growth
  • 1700 lbs!!

17
Rate of growth
  • What is the face that had fastest growth?

18
Rates of growth
  • Hypothetical crystal all faces grow at same rate
  • Realistic crystal and 110 grows faster

19
Rates of growth
  • Halite growth
  • 111 face is layers of Na and Cl
  • Strong attraction of next layer because of
    charges
  • Fast growth
  • 001 face equal Na and Cl, neutral charge, slow
    growth

20
Growth rate and crystal shape
  • Shape of zircon as function of growth rate and
    melt chemistry

21
Growth rate and crystal shape
  • Shape of plag as function of growth rate and melt
    chemistry

22
Growth rate and crystal shape
  • What tectonic environment would you find these
    each in assuming plag forming in a basalt during
    cooling

23
Other issues impacting crystal size and shape
  • Room to grow

24
Other issues impacting crystal size and shape
  • fluids
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