Lecture13-Fingerprinting of Xrd Result

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    Fingerprinting..

    Advantages: relatively quick and easy, can be non-destructive

    Problems:

    need reliable standards - new phases will not be in thePDF

    some things in the database are rubbish! often need other (chemical) information to narrow down

    searches not very sensitive - can hide up to 10% impurities

    (depending on relative weights see later) problems frompreferred orientation, etc. not much good for organics, organometallics.

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    Preferred Orientation

    Remember: we rely on a randomorientation of crystallites. When crystals are platey or needle-shaped (acicular) they

    will pack in a non-random fashion, preferentially exposingsome planes to the incident radiation.

    This can also happen if asample is packed down,or a thin film, etc.

    Brushite plates, SEM by Anna Fotheringham

    Thus some diffraction

    peaks will be enhanced

    relative to others.

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    Preferred OrientationIntensity mismatchdue to using single crystal

    So e.g. all (n00) peaks may be enhanced

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    Uses: different structures

    20 30 40 50 60 70

    53816-ICSD

    Lambd a: 1.54 178 Magnif: 1 .0 FWHM: 0.200

    Space grp: F m -3 m Direct cell: 5.6400 5.6400 5.640 0 90.00 90.00 90.00

    20 30 40 50 60 70

    53825-ICSD

    Lambd a: 1.54 178 Magnif: 1 .0 FWHM: 0.200

    Space grp: F m -3 m Direct cell: 6.2800 6.2800 6.280 0 90.00 90.00 90.00

    NaCl

    KCl

    Even if two structures are thesame (and they are chemicallysimilar) differences can beobserved:

    Peak positions (unit cell changes)and relative intensities (atoms)

    There is another major pointhere:

    K+and Cl-are isoelectronic

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    Uses: different structures

    BUT, sometimes you cantreally see any changes onvisual inspection

    This often happens in open

    structures where there is space

    for change of light atoms

    Zeolite A

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    Uses: polymorphs

    Differentpolymorphs willhave different

    powder patternse.g. Zn S

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    Uses: polymorphs

    K3SO4F: tetragonal & cubic forms

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    Peak Broadening

    In an X-ray diffraction pattern, peak width depends on the instrument

    radiation not pure monochromatic

    Heisenberg uncertainty principle

    focussing geometry

    the sample

    - a crystalline substance gives rise to sharp lines,whereas a truly amorphous material gives a broadhump.

    What happens between the two?

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    Peak Broadening

    If crystal size < 0.2 m, then peak broadening occurs

    At

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    Peak Broadening

    We can calculate the average size of the crystalsfrom the broadening:

    BcosB

    9.0t

    Scherrer formula

    t is the thickness of the crystal, the wavelength, BtheBragg angle.

    B is the line broadening, by reference to a standard, so

    that 2S

    2

    M

    2BBB

    where BSis the halfwidth of the standard material inradians. (A normal halfwidth is around 0.1o)

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    Peak Broadening

    Halfwidth: Full width at half-maximum - FWHM

    This can be different in different directions (anisotropic),so by noting which peaks are broadened we can also inferthe shape of the crystals.

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    Uses: particle size determination

    Here we see particle size increasing with temperature

    0

    50

    100

    150

    200

    15 20 25 30 35 40 45 50 55 60

    20 /o

    30oC

    1050oC

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    Particle size determination: ExamplePeak at 28.2 2with FWHM of 0.36 2

    Standard material has FWHM of 0.16 2

    = CuK= 1.540

    0.36 = 0.36 x /180 = 0.0063 rad (Bm)

    0.16 = 0.16 x /180 = 0.0028 rad (Bs)

    B = 0.0056 rad

    t = 255 = 0.0255 m

    1.14cos0056.0540.19.0

    t

    BcosB

    9.0

    t

    2

    S

    2

    M

    2BBB

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    Particle size determinaton

    An estimate, rather than an absolute value - also will bedominated by smallest particles.

    Good for indication of trends.

    A useful complement to other measurements suchas surface area, electron microscopy etc.

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    Amorphous / micro-crystalline?

    It can be difficult to distinguish between anamorphous material and a crystalline samplewith very small particle size.

    BUT the idea of such a small size crystal being

    crystalline doesnt make sense!5nm = 50 = e.g. 10 unit cellsIs this sufficient for longrange order??

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    Unit cell refinementAs the peak positions reflect the unit cell

    dimensions, it is an easy task to refine theunit cell.

    2d sin= and e.g. 1d

    h

    a

    k

    b

    l

    c2

    2

    2

    2

    2

    2

    2

    Thus if we can assign hkl values to each peak, we cangain accurate values for the unit cell

    2

    calcobs ddWe minimise the difference, e.g.

    This is known as least squares refinement. We will

    come back to this later.

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    Variable temperature/pressure

    Need special apparatus

    Here (see previous) we could follow a phase transition aswe heated the sample upfollowing the change in unit cell

    parameters. J. M .S. Skakle, J. G. Fletcher, A. R. West, Dalton 1996 2497

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    BaTiO3T/P

    S. A. Hayward, S. A. T. Redfern, H. J. Stone, M. G. Tucker,K. R. Whittle, W. G. Marshall, Z. Krist. (2005) 220735.

    T. Ishidate, PRL (1997) 78 2397

    Variable pressure hard to do: neutron diffraction (later)

    Much of these data actually from dielectric measurements.

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    Uses: more advanced

    Structure refinementthe Rietveld method

    A refinementtechnique, not determination

    Whole-pattern fitting - not just the Bragg reflections

    Needs a MODEL - pattern calculated from model, comparedpoint-by-point with observed pattern.

    Originally developed (1967,1969) for use with neutron data- good reproducible peak shapes1977 - first report of application to X-ray data

    Hugo Rietveld,

    b1932

    http://home.wxs.nl/~rietv025/

    http://home.wxs.nl/~rietv025/http://home.wxs.nl/~rietv025/
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    Uses: Rietveld Refinement

    x y z

    Ca/Ce 0.3333 0.6667 -0.0038(18)

    Ce 0.2337(4) -0.0108 0.25

    Si 0.403(3) 0.380(3) 0.25

    O1 0.316(4) 0.467(4) 0.25

    O2 0.597(5) 0.467(4) 0.25

    O3 0.340(2) 0.252(3) 0.071(3)

    O4 0 0 0.25

    Here there was a similarity

    between the powder patternof this phase and anexisting onealso chemicalcomposition similar.

    J. M. S. Skakle, C. L. Dickson, F. P. Glasser, Powder Diffraction (2000) 15, 234-238

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    21/222Th Degrees

    605040302010

    1,600

    1,400

    1,200

    1,000

    800600

    400

    200

    0

    -200

    -400

    HA 80.18 %

    b-TCP 19.82 %

    Uses: more advanced

    Quantitative phase analysis (how much of each)

    Nave approach - relative intensity of peak maxima?- Consider mixture of Ba,Si,O- Ba component would scatter more than Si component

    (e.g. Ba2SiO4c.f. SiO2)

    Thus uses Rietveldmethod and takesinto account relativescattering from eachcrystalline phase

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    Summary

    Many different uses for powder X-ray diffraction!

    Fingerprinting: identifying phases, distinguishingsimilar materials, identifying polymorphs, (followingchemical reactions)

    Indication of particle size from peak broadening

    Unit cell refinement

    Variable temperature/pressure measurements Crystal structure refinement

    Quantitative analysis