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Enggineering Material Coordination No

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    Atomic Packing Factor

    Atomic Packing Factor (APF) is defined as the

    volume of atoms within the unit cell divided by

    the volume of the unit cell.

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    Crystal Structure 3

    1-CUBIC CRYSTAL SYSTEM

    In the unit cell on the left, the atoms at the corners are cut

    because only a portion (in this case 1/8) belongs to that cell.

    The rest of the atom belongs to neighboring cells.

    Coordinatination number of simple cubic is 6.

    a- Simple Cubic (SC)

    a

    bc

    http://www.kings.edu/~chemlab/vrml/simcubun.wrl
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    a- Simple Cubic (SC)

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    Crystal Structure 6

    Atomic Packing Factor of SC

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    Crystal Structure 7

    b-Body Centered Cubic (BCC)

    BCC has eight nearest neighbors.

    Each atom is in contact with itsneighbors only along the body-

    diagonal directions.

    Many metals (Fe,Li,Na..etc),

    including the alkalis and severaltransition elements choose the

    BCC structure.

    a

    b c

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    +Body Centred Cubic (BCC) Lattice Sphere Motif

    =

    Body Centred Cubic Crystal

    Unit cell of the BCC lattice

    Atom at (, , )

    Atom at (0, 0, 0)

    Space filling model

    Central atom is coloured differently for better visibility

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    Crystal Structure 9

    0.68=V

    V=APF

    cellunit

    atomsBCC

    2 (0,433a)

    Atomic Packing Factor of BCC

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    Crystal Structure 10

    c- Face Centered Cubic (FCC)

    There are atoms at the corners of the unit cell and at the center ofeach face.

    Face centered cubic has 4 atoms so its non primitive cell.

    Many of common metals (Cu,Ni,Pb..etc) crystallize in FCCstructure.

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    +Face Centred Cubic (FCC) Lattice Sphere Motif

    =

    Cubic Close Packed Crystal

    (Sometimes casually called the FCC crystal)

    Atom at (, , 0)

    Atom at (0, 0, 0)

    Unit cell of the FCC lattice

    Space filling model

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    Crystal Structure 12

    4 (0,353a)

    0.68=V

    V=APF

    cellunit

    atomsBCCFCC

    0,74

    Atomic Packing Factor of FCC

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    Crystal Structure 13

    2 - HEXAGONAL SYSTEM

    A crystal system in which three equal coplanar axes

    intersect at an angle of 60 , and a perpendicular to the

    others, is of a different length.

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    Both FCC and HCP structures are close packedAPF = 0.74.

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    VOLUME, PLANAR, AND LINEAR DENSITY

    Volume density --

    Planar density --

    Linear Atomic density --

    celltvolume/uni

    cellmass/unit==metalofdensityVolume

    v

    planeofareaselected

    dintersectecentersatom#==densityatomicPlanar

    p

    lineoflengthselected

    dintersectediametersatom#==densityatomicLinear

    l

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    BCC FCC HCP

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    LINEAR & PLANAR DENSITIES

    Linear density (LD) = number ofatoms centered on a direction vector/ length of direction vector LD (110) = 2 atoms/(4R) = 1/(2R)

    Planar density (PD) = number ofatoms centered on a plane / area ofplane PD (110) = 2 atoms / [(4R)(2R2)] =

    2 atoms / (8R22) = 1/(4R22) LD and PD are important

    considerations during deformationand slip; planes tend to slip or

    slide along planes with high PDalong directions with high LD

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    THEORETICAL DENSITY,

    Density = mass/volume

    mass = number of atoms per unit cell * mass of each atom

    mass of each atom = atomic weight/avogadros number

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    Why?

    Metalshave... close-packing

    (metallic bonding)

    large atomic mass

    Ceramicshave... less dense packing

    (covalent bonding)

    often lighter elements

    Polymershave... poor packing

    (often amorphous)

    lighter elements (C,H,O)

    Compositeshave... intermediate values Data from Table B1, Callister 6e.

    DENSITIES OF MATERIAL CLASSES

    metals> ceramic s> polymer s

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    Someengineering applications require single crystals:

    --diamond single

    crystals for abrasives--turbine blades

    Single crystal: when the periodic and repeated arrangement

    of atoms is perfect and extends throughout the entirety of the

    specimen

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    POLYCRYSTALLINE MATERIALS

    Nuclei form during solidification, each of which grows into crystals

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    No crystal has 100% flawless structure

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    Crystal defects

    Defects can affect

    Strength

    Conductivity

    Deformation style

    Color

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    Crystal DefectsSteel spheres:

    a) Regular packed array with 3 pointdefects

    b) Pointand line defects

    c) Mosaic(or domains) separated by

    defect boundaries

    Fig 3.50 of Klein

    and Hurlbut, Manual

    of Mineralogy,

    John Wiley and Sons

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    Point defects

    Higher density of defects at higher T

    Defects represent disorder - disorder

    favored at higher T Point defects

    Vacant sites

    Atoms out of correct position Extraneous atoms

    Substituted atoms

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    Crystal Defects

    1. Point Defectsa) Schottky(vacancy) - seen with steel balls

    in last frame

    a) Need to maintain charge balance!

    b) Impurity

    Foreign ion replacesnormal one

    Foreign ion is added (interstitial)

    Both combined

    a. Schottky defect

    b. Interstitial (impurity) defect

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    Line defects

    Crystal deformation controlled by crystalstructure

    Planes/locations are favored fordeformation based on bond strength

    Bond breakage doesnt happen throughoutentire structure simultaneously

    Lump in carpet

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    Crystal Defects2. Line Defects

    d) Edge dislocation

    Migration aids ductile deformation

    Fig 10-4 of

    Bloss,

    Crystallography

    and Crystal

    Chemistry.

    MSA

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    Crystal Defects

    2. Line Defectse) Screw dislocation (aids mineral growth)

    Fig 10-5 of

    Bloss,

    Crystallography

    and Crystal

    Chemistry.

    MSA

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    Planar defects

    Mismatch of the crystal structure across a

    surface

    Officially grain boundaries count as planardefect

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    Crystal Defects3. Plane Defects

    f) Domainstructure (antiphasedomains)

    Has short-range but not long-range order

    Fig 10-2 of Bloss, Crystallography and Crystal Chemistry. MSA

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    Crystal Defects

    3. Plane Defects

    g) Stacking faults

    Common in clays and low-T disequilibrium

    A - B - C layers may be various clay types (illite, smectite, etc.)

    ABCABCABCABABCABC

    AAAAAABAAAAAAA

    ABABABABABCABABAB

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    Line Defects

    Dislocations

    Missing half plane A Defect

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    Missing half planeA Defect

    An extra half plane

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    An extra half plane

    or a missing half plane

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    What kind of

    defect is this?

    A line defect?

    Or a planar defect?

    An extra half plane

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    An extra half plane

    or a missing half plane

    Edge

    Dislocation

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    This is a line defectcalled an

    EDGE DISLOCATION

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    1 2 3 4 5 6 7 8 9

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    1 2 3 4 5 6 7 8 9

    1 2 3 4 5 6 7 8 9

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    1 2 3 4 5 6 7 8 9

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    1 2 3 4 5 6 7 8 9

    1 2 3 4 5 6 7 8 9

    slipno slip

    boundary = edge dislocation

    Slip planeb

    Burgers vector

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    Slip plane

    slip no slip

    dislocation

    b

    t

    Dislocation: slip/no slip

    boundary

    b: Burgers vectormagnitude and

    direction of the slip

    t: unit vector tangent

    to the dislocation line

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    Dislocation Line:

    A dislocation line is the boundary between slip and no

    slip regions of a crystal

    Burgers vector:

    The magnitude and the direction of the slip is

    represented by a vector bcalled the Burgers vector,

    Line vector

    A unit vector ttangent to the dislocation line is called a

    tangent vector or the line vector.

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    In general, there can be any angle between the Burgers

    vector b(magnitude and the direction of slip) and the

    line vector t (unit vector tangent to the dislocationline)

    b t Edge dislocation

    b t Screw dislocation

    Mixed dislocationb t, b t

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    b

    t

    b || t

    1 23

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    If b || t

    Then parallel planes to the dislocation line lose their

    distinct identity and become one continuous spiral ramp

    Hence the name SCREW DISLOCATION


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