MTE 583_Class_1
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Transcript of MTE 583_Class_1
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READING Chapter 1 in DeGraef and McHenry, All;
ap er n e rae an c enry, pp. - . Chapter on bonding from your Introduction to Materials book.
REFERENCE: Chapter 1 in Rohrer
Prof. M.L. Weaver
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What do we mean by structure?What do we mean by structure?What do we mean by structure?What do we mean by structure? We are concerned with how to quantitatively describe
arranged at relevant length scales.
Prof. M.L. Weaver
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Structural Length Scales1 m1098
Radio
Electrons Neutrons Photonsnm
Can seen it w/ unaided eye.
1 mm
107
106Microwaves
totelescopes
methods)
Macro
Need a microscope to see it.
105
104Infrared
Microscopes
tronscatte
rin
EM,
SEM
)
Micro
1 m103
102UV
ge(v
ariousne
icationrange(
no
Visible
light
.
1 nm
101
100
rays
hods
pplicationra
Appl
ic
Na
size of an atom (~1 = 0.1 nm).10
-1
10-2
ays
X
Diffractionme
nAto
Prof. M.L. Weaver
FigureadaptedfromM.DeGraefandM.E.McHenry,StructureofMaterials,CambridgeUniversityPress,CambridgeUK(2007)p.5.
1 pm10-
10-4Gamma
Nuclear
Sub-atomic.
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What do we mean by structure?What do we mean by structure?What do we mean by structure?What do we mean by structure? Atomic structure. Atoms in a material are bound to
Metallic bonds
Covalent bonds
Secondar bonds
Atomic arran ements also rovide useful tructuraldescriptors.Crystalline structure
Prof. M.L. Weaver
Amorphous structure
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What do we mean by structure?What do we mean by structure?What do we mean by structure?What do we mean by structure? Microstructure: Arrangements of large groups of
.Phase/Crystal Morphology
Phase/Crystal Distribution
EtcStructural Feature Dimension(m)
10
Missing/extraatoms ~1010
Crystals(orderedatoms) 108 101
Prof. M.L. Weaver
Secondphase particles 108 104
Crystaltexturing >106
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Crystal Structure DescriptorsCrystal Structure DescriptorsCrystal Structure DescriptorsCrystal Structure Descriptors Forcrystalline materials, descriptors are based on the
theory ofcrystallography.
NaCl
rock salt
All atoms have the same average environment around
(green Cl- ; yellow Na+)
calcite
Prof. M.L. Weaver
them. This constitutes long-range order (LRO) which is
a major structure descriptor for crystals.
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NonNon--crystalline Structuralcrystalline StructuralNonNon--crystalline Structuralcrystalline Structural
If a material isnon-crystalline, it lacks spatial. ., .
Silica
glass
On a smaller length scale, the atoms may exhibit
http://www.pisces-press.com/C-Nav/images/silica%20glass-b.jpghttp://upload.wikimedia.org/wikipedia/commons/thumb/4/4b/Silica.svg/2000px-Silica.svg.png
Prof. M.L. Weaver
short-range order (SRO), which is a major
descriptor for the structure of glassy materials.
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Example of LRO and SROExample of LRO and SRO
From Prof. T. Scharf
University of North Texas
LRO SRO
-(amorphous) on singlecrystal Si wafer
Prof. M.L. Weaver
MFET 3450 14
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Materials are not perfectlyMaterials are not perfectly
ordered arra s of atom orordered arra s of atom or ionsionsPolycrystalline ZnO thin film
O2-
Zn2+
Planar stacking faults (2-D
area defect) denoted by
arrows
- An interfacial defect that exists withinabove hexagonal closed packed (HCP)stacking sequencedisruption in lattice.
Prof. M.L. Weaver
From Prof. T. Scharf
University of North Texas
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Materials are not perfectlyMaterials are not perfectly
ordered arra s of atom orordered arra s of atom or ionsionsPolycrystalline ZnO thin film
Zoom in on box from previous page:
. .
University of North Texas
-
line defect) denoted by
arrow
Prof. M.L. Weaver
16
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BondingBondingBondingBonding
The physical and chemical properties of materials arestrongly influenced by interatomic bonds. Thus they aren uence y e ou ermos va ence e ec rons.
Can we determine a materials structure from knowled eof chemical bonding?
NO!
Many examples in terms of structural state and bonding, e.g.,
TiCl2 (s) and TiCl4 (l)
Must be careful assigning particular types of bonds to agiven collection of atoms/ions.
Prof. M.L. Weaver
Cant just use stoichiometric formulas to predict material
structure.
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PropertiesPropertiesPropertiesProperties Refer to how a material responds to an external
. Isotropic non-directional
Tem erature
Gravity/mass
Etc n sotrop c rect ona
Stress
Elastic modulus
Electrical conductivity Etc
Prof. M.L. Weaver
rys a ograp y p ays a ro e. ymme ry.
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Symmetry ExampleSymmetry ExampleSymmetry ExampleSymmetry Example Consider the 2-D material illustrated to the right.
. .
Apply an electric field (E) alongx-axis. Generate acertain current density (j). x
y
Apply an electric field alongy-axis. Should generate the same
current density because structure is same inx
andy
directions. .
x xx xy xj E
E
Properties reflect
x xx xy xj E
E
structure. In this casethey are the same inxandy.
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Prof. M.L. Weaver