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    Lesson 16

    Su ested ReadinChapter 3 in Waseda, pp. 67-75

    Ch. 6 B.D. Cullity and S.R. Stock, Elements of X-ray Diffraction, 3 rd Edition, Prentice-Hall (2001)

    409

    . - . . . , , .Ch. 7 Pecharsky and Zavalij, Fundamentals of Powder Diffraction and Structural Characterization of

    Materials, 2 nd Edition, Springer (2009)

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    10-6

    Wavelengthin nm

    Frequency incycles per second

    Visible Light: ~6000 X-rays : ~0.5 2.5 Electrons : ~0.05

    1020

    One an strom 10-1

    Gamma raysViolet

    Indigo

    nm

    450

    400

    1015 One micrometer

    One nanometer 1

    UltravioletX-rays

    Visible Light

    Blue

    Green

    Yellow

    550500

    1010One centimeter

    104 Infrared Orange

    Red700

    650

    One kilometer

    One meter 109

    Broadcast band

    Short radio waves 750

    EM Radiation105

    1014 Long radio waves Self-propagatingwaves with

    410

    Spectrum of electromagnetic (EM) radiation as afunction of frequency (s -1) and wavelength (nm).

    electric and magnetic

    components

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    Properties of Electromagnetic Waves

    y

    ec r cField E

    particles of energycalled photons .

    x

    Beam of EMradiation

    Pro a ationPhotons interact withelectrons.

    z

    Magnetic

    direction

    Thus they can be e

    hc E h photon of energy

    .

    346.626 10h

    Planck's constant J s frequency of the wave

    411

    83.00 10c

    speed of light m/s wavelength of radiation

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    Scattering of EM Radiation by Crystals For a material to yield a diffraction pattern,

    d . This limits us to usin :. Neutrons

    X-rays

    X-ray scattering (i.e., absorption + re-emission): Elastic (little or no energy loss diffraction peak)

    Inelastic ener loss no diffraction eak

    412

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    Laues Equations When scattering occurs there is a change in the path of the

    incident radiation.Diffracted

    n

    n n

    path difference between incident andscattered beams where is an inte er

    S

    beam

    (cos cos ) ( ) x o oa a S hS o

    (cos cos ) ( ) y o

    z

    o

    ooc c l S S S oIncident

    a[ , , are integers]h k l

    Constructive interference occurs when all three equations

    beam

    413

    .

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    Braggs Law

    A C

    d

    B

    path difference 2 sin B BC d For constructive interference n

    2 sind nd

    d

    4142 sin (or 2 sin )hkl n

    d n d

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    Braggs Law

    A C

    d

    B

    path difference 2 sin B BC d For constructive interference n

    2 sind nd

    d

    4152 sin (or 2 sin )hkl n

    d n d

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    Braggs Law

    ragg s aw can e expresse n vec or orm:hkl *2sino hkl S S d

    *d

    S o-S o

    S -S o

    *hkl

    hkl d d Incidentbeam

    Diffracted

    Thus: Trace of (hkl )

    reflecting plane* * * *o d ha kb l S S c

    eam

    This tells us that constructive interference occurs when

    S S o coincides with the reciprocal lattice vector of thereflecting planes.

    416

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    Laues Equations and the Reciprocal Lattice e can represent t e aue equat on grap ca y.

    This is similar to Ewalds sphere. * od S S

    For diffraction to be

    (13)

    S . .

    law satisfied) S must

    end on a reciprocal S (00) (10)

    (01)

    (11)

    2

    a ce po n .

    Points satisfying this criteria

    Reflecting sphere

    represent planes that are orientedfor diffraction

    Braggs law, which describes diffraction in terms of scalars, isgenerally used for convenience. 417

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    Diffractedbeam

    *h l

    ok d

    S S

    (13)

    S

    RADIUS = 2 S o /

    oS

    (00) (10)

    (01) (11)

    (10)

    INCIDENTBEAM To

    satisfyraggs

    2

    raggslaw

    *oS d S sphere

    *

    2 sin1 2sin

    n d

    418

    hkl d n

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    Reciprocal Lattice

    from all diffractionvectors (i.e., g ) for acrystal definespossible Braggreflections.

    Points that intersect

    b*c*the reflecting spherewill satisfy Braggs

    law.000

    Incidentbeam

    a* Changes inwavelength ( )changes the circle

    ,to diffraction.However, we generallydo not change .

    419

    000

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    Reciprocal Lattice

    orientation of theincident beam relativeto the crystal changesthe orientation of thereciprocal lattice,reflecting sphere, and

    .

    Chan e will eventuall

    000

    Incidentbeam

    yield a condition wherediffraction is possible.

    We mentioned this afew lectures ago.

    420

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    X-ray Diffractometer X-ray source is generally

    fixed.Focal circle

    Rotate sample andDetector Source

    e ec or o a us .

    Rotates onfocal circle

    Fixed

    our Bruker D8 and PhilipsMPD, the source and

    2

    Sample

    e ec or move w e esample remainsstationary.

    421

    -

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    Diffraction Directions

    combining Braggs law with the interplanar spacinge uations for a cr stals.

    Cubic:

    2

    2 2 2 22

    2 sin

    sin

    d

    h k l

    2 2 2

    2 21 h k l

    d a

    This equation predicts, for a particular incident anda particular cubic crystal of unit cell size a , all of the

    422

    possible Bragg angles for the diffracting planes ( hkl )

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    Diffraction Directions contd Example:

    planes in a cubic crystal?

    Solution:2

    2 2 2 2111 2 2sin 1 1 14 4a a

    h k l

    423

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    Diffraction Directions What about other systems?

    Tetragonal:

    2 2 2 22

    2 2 2

    2 sinsin

    4

    d h k l

    a a c

    2 2 21 h k l

    d a c

    22 2 1For 111 , sin

    Solution: must know c and a . Will be one eak.

    a a c

    424 What about {110}? Ive intentionally given you a family here

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    Sphere

    Cone Debye

    Ring

    2*hkl d

    S

    In powder diffraction you

    Beam S o

    S

    generate an in inite num er orandomly oriented, but identical,reciprocal lattice vectors. Detector

    placed on the surface of Ewaldssphere.

    The roduce owder diffraction

    * 1* hkl hkl

    R g d d

    425

    cones at different Bragg angles

    (see the next slide). Adapted from Vitalij K. Pecharsky and Peter Y. Zavalij, Fundamentals

    of Powder Diffraction and Structural Characterization of Materials, Kluwer Academic Publishers (2005)

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    Ewaldssphere

    * 1hkl

    hkl

    d d

    Incident SoBeam

    Fi ure 8.2

    426

    Adapted from Vitalij K. Pecharsky and Peter Y. Zavalij, Fundamentals of Powder Diffractionand Structural Characterization of Materials, 2 nd Edition, Kluwer Academic Publishers

    (2009), p. 154.

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    Diffraction vector cone Diffraction cone

    Ewald sphere

    /S

    hkl

    X-ray2

    * 1hkl

    hkl

    d d

    2 /oS

    /S

    hkl

    430Diffraction cone and diffraction vector cone illustrated on the Ewald sphere. Adapted from B.B. He, Two-Dimensional X-ray Diffraction, Wiley (2009), p. 20.

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    (a) (b)

    2 1

    2 2

    Increasing 2

    2 1

    2 22 3

    (c) (d)

    431

    X-ray diffraction patterns: (a) from single crystal, (b) Laue diffraction pattern from single crystal, (c)diffraction cones from polycrystalline solid, and (d) diffraction frame from a polycrystalline solid. (a)and (c) from B.B. He,Two-Dimensional X-ray Diffraction , Wiley (2009), p. 22. (d) from PhotonicScience (http://photonic-science.co.uk ).

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    Incidentelectrons

    Ewald sphere

    Figure 2.11 Formation of a single crystal diffraction pattern in transmission electron microscopy.The short wavelength of electrons makes the Ewald sphere flat. Thus, the array of reciprocal lattice

    432

    po n s n a rec proca p ane ouc es e sp ere sur ace an genera es a rac on pa ern on escreen. Adapted from Y. Leng , Materials Characterization, Wiley (2008), p. 55.

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    Linedetector

    In a linear diffraction pattern,the detector scans through anarc that intersects each Debye

    cone at a sin le oint.

    Figure 8.4This gives the appearance of a

    discrete diffraction peak.

    433

    Adapted from Vitalij K. Pecharsky and Peter Y. Zavalij, Fundamentals of PowderDiffraction and Structural Characterization of Materials, 2 nd Edition, Kluwer

    Academic Publishers (2009), p. 156.