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Solidification, Crystallization

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Title: Solidification, Crystallization


1
Solidification, Crystallization Glass Transition
  • Crystallization versus Formation of Glass
  • Parameters related to the formation of glass ?
    Effect of cooling rate ? Glass transition
    temperature
  • Structure of Glasses ? Radial distribution
    function

2
Glasses and Amorphous Materials
  • The word glass and amorphous material can be
    interchangeably used in most circumstances?
    though there is a small technical difference
    (which we will consider later).
  • Based on atomic structure it is one of the 3
    fundamental states of matter. In glasses the
    atoms do not have long range order (LRO), though
    they may have short range order (SRO).
  • The SRO could be very different from that
    encountered in crystals (even the crystals formed
    out of the same composition). E.g. one may find
    local icosahedral clusters.
  • In a simplistic picture, glass can be thought of
    as a time snapshot of the liquid.
  • Typically glasses have a higher free-volume as
    compared to the crystal (the preferred crystal
    structure that the material is expected to form
    for a given T P).
  • Concepts like Lattice and motif thus cannot be
    used in glasses. This automatically implies that
    many of the properties of a glasses will be
    drastically different as compared to the
    corresponding crystal (thought he composition may
    be identical and the density not very different).
    For example, dislocations (in the usual sense)
    cannot be defined in glasses and hence the
    plastic deformation of glasses have to take place
    by other mechanisms (e.g. shear banding).

Matter
STATE / VISCOSITY
One kind of glass is the window pane glass, but
glasses come in many forms (based on bonding,
etc.). Many of these glasses are not transparent.
SOLID
GAS
LIQUID
LIQUID CRYSTALS
STRUCTURE
AMORPHOUS
QUASICRYSTALS
CRYSTALS
3
  • It is assumed that glasses are metastable and
    there exists at least one crystal structure which
    has a lower Gibbs free energy (at constant, T,P).
    This implies if sufficient activation energy is
    provided (usually by heating), then glasses will
    tend to crystallize. At low temperatures the
    glass in frozen in a disordered state and may
    remain so for a long time (e.g. glass used in the
    window panes are not expected to crystallize in
    geological time scales).
  • On heating glasses (see page on heating of
    glass more on this) they tend to crystallize.
    This process occurs by nucleation and growth of
    crystallites in the amorphous matrix. Many
    materials like long chain (and branched) polymers
    are difficult to crystallize completely (more on
    this soon). As we shall see soon, in some
    circumstances a partially crystallized
    microstructure can give us better properties.
  • Many different kinds of materials can be obtained
    in the amorphous state. These include polymers,
    inorganic materials, organic materials, metals
    and alloys, semiconductors, etc. In fact if we
    look around us, most of the materials we see
    (like wood, building walls, etc.) are not fully
    crystalline.
  • From the above it is clear that the term
    amorphous (which is based on atomic level
    structure) is used for a wide class of materials
    and based on the specifics of the material
    involved, the properties will be varied. As
    expected, polymeric glasses will have poor
    tolerance to heat, while inorganic glasses may
    withstand high temperatures.

4
Formation of Glass
  • Certain materials are easy glass formers (e.g.
    silicates, long chain polymers, etc.), which
    others are difficult to amorphize (e.g. pure
    metals, simple alloys, etc.).
  • Glasses can be synthesized in many ways. Three
    typical ways are listed below.
  • 1) From the vapour state? By condensing the
    vapour of the material onto a cold substrate.
  • 2) From the liquid state? Quenching from the
    melt (usually fast cooling from the molten
    state). The rate of quenching required depends on
    the material (and parameters to be discussed
    soon). To amorphize certain alloys cooling rates
    of the order of 106 K/s needs to be employed,
    while certain special alloys and silicate
    materials can be slowly cooled to get glass (even
    1 K/s).
  • 3) In the solid state? By severely deforming the
    crystals (say a polycrystal) amorphous state can
    be obtained. Ball milling has been one of the
    popular examples for this method (for alloys).

5
Glass Forming Ability Resistance to
Crystallization
  • Glass Formation Ability (GFA) should be
    differentiated with Resistance to Crystallization
    (RTC) also called Glass Stability (GS). GFA is in
    the cooling direction (i.e. how slowly can I
    cool to still get a glass?), while RTC is in the
    heating direction (i.e. to how high a
    temperature can I heat and still retain a
    glass?). Many parameters have been developed to
    characterize materials with respect to GFA and
    RTC.
  • Crystallization is favoured by high enthalpy of
    fusion (?Hfusion) and a low viscocity (?). ? The
    critical Gibbs free energy for the nucleation of
    a crystal is related to the enthalpy of fusion as
    in the equation below. Large ?Hfusion implies a
    lower ?Gcrystallization, which further implies
    ease of crystallization. ? An embryo becomes a
    nucleus by jump of atom across the interface from
    liquid to crystal. This requires a activation
    enthalpy (?Hd). The activation enthalpy is
    related to the log of viscosity. This implies
    that a lower viscosity allows for easier atomic
    jumps, which in turn favours crystallization.

Click here to revise concepts on nucleation
6
  • Metals (in molten state) with a high enthalpy of
    fusion (10 kJ/mole) and low viscosity (1-10
    poise) are difficult to amorphize. Pure metals
    (like Al, Cu) are virtually impossible to
    amorphize by quenching from the liquid state.
    Some alloys (one popular brand name is Metglas?)
    can be cooled at a high cooling rate (using
    processes like melt-spinning or splat quenching)
    of 106 K/s to obtain a foil of amorphous
    material. one popular commercial composition of
    metallic glass is Metglas? is Fe 85 wt., Si 10
    wt., B 5 wt..
  • Needless to say one dimension of the sample will
    have to be thin for fast heat extraction (which
    implies that we end up with foils).
  • Inorganic glasses on the other hand, with low
    ?Hfusion and high viscosity are easily
    amorphized. In fact some oxides may have to be
    added promote crystallization. E.g. Borosilicate
    glass 81 SiO2, 13 B2O3, 4 Na2O/K2O, 2 Al2O3
    softening point of 820?C.

High ? (10-15) kJ / mole
Low
? ?Hfusion
Thermodynamic
Silicates
Metals
Crystallization favoured by
High ? (1000) Poise
Low ? (1-10) Poise
? ?Hd ?? Log Viscosity (?)
Kinetic
Enthalpy of activation for diffusion across the
interface
Very fast cooling rates 106 K/s are used for the
amorphization of alloys
Easily amorphized
Difficult to amorphize metals
7
  • In contrast to metals silicates, borates and
    phosphates tend to form glasses
  • Due to high cation-cation repulsion these
    materials have open structures
  • In silicates the difference in total bond energy
    between periodic and aperiodic array is small
    (bond energy is primarily determined by the first
    neighbours of the central cation within the unit)

8
Measures of Glass Forming Ability (GFA)
  • There are many parameters used to characterize
    the glass forming ability of a material. Most
    important of these are Critical Cooling Rate
    (qcr) and Critical Diameter (dcr).
  • These two parameters are related to one another

9
Heating of Glass
  • As pointed out before, a glass will tend to
    crystallize on heating.
  • If crystallization does not intervene, then
    glasses will slowly soften (i.e. the viscosity
    will decrease) and will begin to flow. This is
    what enables glow blowing operations, wherein
    silicate glass is heated and blown to form
    bottles. This is what we observe when we heat wax
    candles.
  • This implies that glasses do not have a well
    defined melting point like crystals.
  • The crystallization of glass can be studied by
    using Differential Scanning Calorimetry (DSC). In
    DSC a sample is heated at a constant rate (say 20
    ?C/min) and hence the origin of the word
    scanning. The heat absorbed or evolved (with
    respect to a reference pan and hence called
    differential) is measured as a function of
    temperature. Typical plot in the next page.
  • In a DSC plot (where Y axis is exothermic) (i)
    glass transition appears as a step, (more about
    glass transition later)(ii) crystallization(s)
    as exothermic peak(s) and (iii) melting as a
    endothermic valley. More than one
    crystallization peaks may be observed if more
    than one type of crystal forms during the heating.

10
  • Materials which show glass transition (as
    indicated in the DSC plot) are called glasses and
    those which do not are referred to as Amorphous
    materials. In amorphous materials it is assumed
    that crystallization masks the glass transition
    (the presumed reason as to why we do not observe
    glass transition).
  • The temperature interval between Tg and Tx
    (Tx?Tg) is called the supercooled liquid region.
    The properties of the material below Tg will be
    different (often drastically) from that above.

Crystal
Supercooled liquid region
Glass
Tg
Tx
Tg
Tg
Amorphous solid
Glass
Glass
Glass
Cool liquid
Cool liquid
Crystal
Heat Amorphous solid
Crystal
Heat glass
Tx
Tx
Often metallic glasses crystallize first (in a
viewpoint before Tg) Hence the glass transition
temperature in heating is masked by
crystallization (hence not observed
experimentally)
11
  • DSC is a versatile tool to study phase
    transformations.
  • By using various scanning rates (temperature
    scanned per unit time, K/s or ?C/min) in
    conjunction with the Kissinger analysis the
    activation energy for the phase transformations
    can be determined.
  • The crystallization temperature (Tx) and glass
    transition temperature (Tg) are determined from
    the DSC plot as shown in the figure.
  • The crystallization process is exothermic (as the
    system is going from a higher internal energy
    amorphous structure to a lower energy crystal),
    while the melting process is endothermic (energy
    has to be supplied to break the bonds in a
    crystal and to cause melting). The glass
    transition is step-like in the DSC plot.

Differential Scanning Calorimetry (DSC)
Glass transition step
Note crystallization peak(exothermic)
Material gives out heat during crystallization
Note melting valley(endothermic)
Material absorbs heat to melt (the latent heat)
Sample heated at constant rate
12
Glass Transition
  • We have seen as to how glass transition is
    indicated in a DSC plot. But, typically glass
    transition is understood first in the cooling
    direction.
  • When a liquid is cooled slowly and its volume is
    plotted as a function of the temperature, there
    is a sudden shrinkage at the melting point when
    crystallization takes place.
  • On the other hand if crystallization is avoided
    and the material is freezes into a glass.

Liquid
All materials would amorphize on cooling unless
crystallization intervenes
Slow change in volume
Sudden shrinkage in volume during crystallization
Instead of V we can plot other extensivethermodyn
amic quantities (i.e. they all show same
behvaiour) ? S, H, E
Glass
Volume ?
Crystal
Tm
Tg
T ?
Glass transition temperature
13
Change in slope
Volume ?
T ?
Tf
Fictive temperature (temperature at which glass
is metastable if quenched instantaneously to this
temperature) ? can be taken as Tg
14
Effect of rate of cooling
As more time for atoms to arrange in closer
packedconfiguration
Volume ?
Slower cooling
Lower volume
T ?
Slower cooling
Higher density
Lower Tg
15
  • On crystallization the viscosity abruptly
    changes from 100 ? 1020 Pa s
  • A solid can be defined a material with a
    viscosity gt 1012 Poise

If the glass crystallizes on heating (at Tx),
before Tm then ?T Tx ? Tg is a measure of the
glass formability. The region between Tg and Tx
is the supercooled liquid region in this case.
Crystal
Glass
Log (viscosity) ?
Supercooledliquid
Liquid
T ?
Tm
Tg
16
Glass transition temperature of various types of
glasses
  • Note that there are elemental, alloy and compound
    glasses. Boding varies from covalent to Van der
    Waals type. Glass transition temperature ranges
    from low values (65 K) to high values (1430 K).

Material Bonding Tg (K)
SiO2 Covalent 1430
Pd0.4Ni0.4P0.2 Metallic 580
BeF2 Ionic 570
Polystyrene mixed 370
Se 310
H2O Hydrogen 140
As2S3 Covalent 470
Isopentane Van der Waals 65
R. Zallen, Physics of Amorphous Solids, John
Wiley and Sons, 1983.
17
Glass-ceramic (pyroceram)
  • A composite material of glass and ceramic
    (crystals) can have better thermal and mechanical
    properties (especially spalling resistance).
  • But glass itself is easier to form (shape into
    desired geometry).

Heterogenous nucleating agents (e.g. TiO2) added
(dissolved) to molten glass
Shaping of material in glassy state
TiO2 is precipitated as fine particles
Held at temperature of maximum nucleation rate (I)
Heated to temperature of maximum growth rate
18
  • Even at the end of the heat treatment the
    material is not fully crystalline
  • Fine crystals are embedded in a glassy matrix
  • Crystal size 0.1 ?m (typical grain size in a
    metal 10 ?m)
  • Ultrafine grain size ? good mechanical properties
    and thermal shock resistance
  • Cookware made of pyroceram can be heated directly
    on flame.

19
Radial Distribution Function
  • In crystals interatomic distances are well
    defined. In a CCP crystal the distances are
    a?2/2, a, a?6/2, a?2, etc. These vectors are
    shown in the figure below.
  • In glasses this is not so. The minimum approach
    distance is (r1 r2), however the distances
    after that are not discrete. Hence we have to
    come up with measures as to how the distribution
    of atoms varies from a given reference atom. One
    such measure is the Radial Distribution Funtion.
  • For a distribution of atoms the Radial
    Distribution Function (g(r), RDF), describes how
    density varies as a function of distance from a
    reference atom. This reference atom could be any
    atom, as there are no preferred sites in a glass
    and things average out due to the randomness of
    atomic positions.
  • RDF is a measure of the probability of finding an
    atom at a distance of r in a spherical shell,
    relative to that for an ideal gas (i.e. the
    probability is normalized w.r.t. to an ideal
    gas).
  • Fourier transform of the RDF is related to the
    structure factor.

Can also be defined for molecules, etc. RDF
is closely related to the Pair Correlation
Function
20
RDF continued
  • RDF (g(r)) is defined as in the formula below.
  • ? ? number density- number of atoms/volume
  • n ? number of atoms in the volume between r (r
    dr)

Note that the discrete peaks found in the case of
crystals has become diffuse
21
(No Transcript)
22
Solidification and Crystallization
23
Metals
? ?Hfusion
High ? (10-15) kJ / mole
Thermodynamic
Crystallization favoured by
Low ? (1-10) Poise
? ?Hd ?? Log Viscosity (?)
Kinetic
Enthalpy of activation for diffusion across the
interface
Difficult to amorphize metals
Very fast cooling rates 106 K/s are used for the
amorphization of usual alloys ? splat cooling,
melt-spinning.
24
Silicates
? ?Hfusion
low
Thermodynamic
Crystallization favoured by
High ? (1000) Poise
? ?Hd ?? Log Viscosity (?)
Kinetic
Enthalpy of activation for diffusion across the
interface
Easily amorphized
Certain oxides can be added to silica to promote
crystallization
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