crystal chemistry 1
TRANSCRIPT
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CRYSTAL CHEMISTRY
Wh i l h i ? Reading:
• description and classification of crystals
b di iti t t l ti hi
What is crystal chemistry? Reading: West 7, 8
• bonding; composition-structure relationships
• the conditions in which particular type of crystal structure is observed
• structure property relations• structure-property relations
Common ways to describe crystals:Common ways to describe crystals:
• unit cell approach (specify size, shape and atomic positions)
• close-packing approach (good for metals alloys ionic structures covalent• close-packing approach (good for metals, alloys, ionic structures, covalent
networks, molecular and supermolecular solids)
• space-filling polyhedron approachspace g po y ed o app oac
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CLOSE-PACKED CRYSTAL STRUCTURESConsider the close-packing of incompressible (hard) spheres:Consider the close-packing of incompressible (hard) spheres:
In 2D, regular close-packing requires an hexagonal array (HCP)
Most efficient wayto pack spheres of single size
• 6 nearest neighbors
Coordination number (CN): 6
In 3D, regular close-packing involves stacking 2D HCP arrays
CCP
Regular(crystalline)
ki
Irregularpacking
packing
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HEXAGONAL CLOSE-PACKED STRUCTUREAn HCP crystal is a close-packed structure with the stacking sequence ABABABAn HCP crystal is a close-packed structure with the stacking sequence ...ABABAB...
To construct:1st layer: 2D HCP array (layer A)2 d l HCP l i h h h l d i l i i i 1 t l (B)2nd layer: HCP layer with each sphere placed in alternate interstices in 1st layer (B)3rd layer: HCP layer positioned directly above 1st layer (repeat of layer A)
…ABABABAB…
AA
B
A B A AHCP is two interpenetrating simple hexagonal lattices displaced by a1/3 + a2/3 + a3/2
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HCP STRUCTURE• not a Bravais latticenot a avais lattice
Orientation alternateswith each layerwith each layer
• each sphere touches 12 equidistant nearest neighbors (CN = 12)
Six in plane, six out-of-plane
• structure has maximum packing fraction possible for single-sized spheres (0.74)p g f p f g p ( )
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HCP STRUCTURE
• unit cell is a simple hexagonal lattice with a two-point basis
(0 0 0)a
• ideal ratio c/a of 8 / 3 1.633(0,0,0)
(2/3,1/3,1/2)a• {0002} planes are close packed
Plan view• ranks in importance with FCC and BCCBravais lattices
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HCP STRUCTURE
• about 30 elements crystallize in the HCP form
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CUBIC CLOSE-PACKED STRUCTUREA CCP crystal is a close-packed structure with the stacking sequence ABCABCA CCP crystal is a close-packed structure with the stacking sequence ...ABCABC...
To construct:1st layer: 2D HCP array (layer A)2 d l HCP l i h h h l d i l i i i 1 t l (B)2nd layer: HCP layer with each sphere placed in alternate interstices in 1st layer (B)3rd layer: HCP layer placed in the other set of interstitial depressions (squares, C)4th layer: repeats the 1st layer (A)
ABCABCABC…ABCABCABC…
stacking gof HCP layers
along body diagonals
A B CIt t t th t th CCP t t i j tIt turns out that the CCP structure is just
the FCC Bravais lattice!71
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CCP STRUCTURE• CN = 12 packing fraction 0 74• CN = 12, packing fraction 0.74
• {111} planes are close packed
• 4 atoms in unit cell
Plan viewPlan view
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• most common are HCP and CCP
CLOSE-PACKED STRUCTURESmost common a e C and CC
• an infinite # of alternative stacking sequences exist
Example: silicon carbide has over 250 polytypese.g., 6H-SiC
stacking sequence …ABCACB…
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STACKING FAULTSStacking faults are one or two layer interruptions in the stacking sequence that
destroy lattice periodicity
e.g., an <110> projection of an FCC lattice:
ABCA
ABC
B
[111]-
missing lA
BCAB
BCABC
[001]-[110]-
[110] planeof atoms
perfect FCCABCABCABC
faulted FCCABCBCABC
C C[110]
The stacking fault is an example of a planar defect2• stacking fault energy γ ~100 mJ m-2
• results also in perpendicular linear defects called dislocations74
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EXAMPLE InAs nanowires - <110> projection
Caroff, P. et al. Nature Nanotechnology 4, 50 - 55 (2009) 75
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• CCP and HCP have very similar lattice energiesy g• no clear cut trends
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Nature 353, 147 - 149 (12 Sep 1991)
G A (CC )Rare Gases: Ne, He, Ar, Kr, Xe (CCP)77
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gold nanocrystalsX. M. Lin
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ANOTHER VIEW OF CLOSE PACKING
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. It was reviewed by a panel of 12 referees; the panel reported in 2003 after 4 years ofreviewed by a panel of 12 referees; the panel reported in 2003, after 4 years of work, that it was “99% certain” of the correctness of the proof, but couldn’t verify the correctness of all of the computer calculations. Hales and Ferguson (his student) received the Fulkerson Prize for outstanding papers in the area of(his student) received the Fulkerson Prize for outstanding papers in the area of discrete mathematics in 2009.
http://en.wikipedia.org/wiki/Kepler_conjecture80
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PACKING FRACTIONSThe fraction of the total crystal volume that is occupied by spheres
CCP (and HCP)2aradius
The fraction of the total crystal volume that is occupied by spheres
3
3atoms
4 24 ( )3 4 2 0.7405
6VV
a
fractiona
2a
4radius
cell 6V a2a
a 74%
34 ( )a
BCC3
4aradius
SC
3
( )3 2 0.5236fraction
a
34 32 ( )3 4 0 6802
a
fraction
4
52%33 4 0.6802fraction
a
68%52%
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b f / i ll
DENSITY CALCULATION
1atomsm nAV N V
n: number of atoms/unit cellA: atomic mass
VC: volume of the unit cellcell A CV N V
VC: volume of the unit cell
NA: Avogadro’s number (6.023×1023 atoms/mole)
Calculate the density of copper.
RCu = 0.128 nm, Crystal structure: FCC, ACu= 63.5 g/mole
n = 4 atoms/cell, 3 3 3(2 2 ) 16 2CV a R R , ( )C
38 3 23
(4)(63.5) 8.89 /[16 2(1.28 10 ) (6.023 10 )]
g cm
[16 2(1.28 10 ) (6.023 10 )]
8.96 g/cm3 in the literature83
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INTERSTICIAL SITES IN CP STRUCTURESA large number of ionic structures can be regarded as built of CP layers of anionsA large number of ionic structures can be regarded as built of CP layers of anions
with the cations placed in interstitial sites
for every anion, there is 1 Octahedral site and 2 Tetrahedral sitesy ,
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Octahedral holesOctahedral holes
di tdi tcoordinates:coordinates:½00½000½00½00½00½000½ 00½ ½½½ ½½½
= O site
cavities have <100>cavities have <100>i t tii t tiorientationorientation
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Tetrahedral holes in CCPTetrahedral holes in CCP TT++ sites:sites:+ + ¾¼¼ ¾¼¼ ¼¾¼¼¾¼¼¼¾¼¼¾¾¾¾¾¾¾
TT-- sites:sites:¼¼¼¼¼¼¼¼¼¼¼¼¾¾¼¾¾¼¼¾¾¼¾¾¾¼¾¾¼¾
cavities have <111> orientationcavities have <111> orientation86
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Holes in HCPHoles in HCP
O sites:O sites:O sites:O sites:2/3,1/3,1/42/3,1/3,1/42/3,1/3,3/4 2/3,1/3,3/4 , ,, ,
TT++ sites:sites:1/3 2/3 1/81/3 2/3 1/8
(1/3,2/3,1/2)
1/3,2/3,1/81/3,2/3,1/80,0,5/8 0,0,5/8
(0,0,0) TT-- sites:sites:0,0,3/80,0,3/8a2
a1
, ,, ,1/3,2/3,7/8 1/3,2/3,7/8
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LOCATION OF OCTAHEDRAL HOLES
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LOCATION OF TETRAHEDRAL HOLES
(3/8 of a unit cell directly above/below each anion)
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SIZE OF OCTAHEDRAL CAVITYOnly cations smaller than the diameter of the cavity can fit y y
without forcing the anion lattice to expand
2 2a r r
from cell edge
M ti
2 2M Xa r r
from face diagonalM = cationX = anion 2 2 Xa r
.The cation radius must be< 41% of the anion radius90
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SIZE OF TETRAHEDRAL CAVITYThe tetrahedral holes are twice asThe tetrahedral holes are twice as
numerous but six times smaller in volume
The cation radius must be< 23% of the anion radius91
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EUTACTIC STRUCTURESStructures in which the arrangement of ions is the same as in a close packed arrayStructures in which the arrangement of ions is the same as in a close packed array
but the ions are not necessarily touching
Within certain loose limits (given by the radius ratio rules), cations too large to fit in the interstices can be accommodated by an
expansion of the anion arrayexpansion of the anion array
• anions don’t like to touch anyway
• modern techniques show that, in many cases, anions (cations) are not as large (small) as previously thoughtg ( ) p y g
• we still describe eutactic structures as CCP or HCP lattices with ions in some fraction of the interstitial siteswith ions in some fraction of the interstitial sites
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CRYSTALS THAT CAN BE DESCRIBED IN TERMS OF INTERSTITIAL FILLING OF ATERMS OF INTERSTITIAL FILLING OF A
CLOSE-PACKED STRUCTURE
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SOME EUTACTIC CRYSTAL STRUCTURESVariables:Variables:
1) anion layer stacking sequence: CCP or HCP array?2) occupancy of interstitial sites
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NaCl (ROCK SALT, HALITE) STRUCTURE(CCP 100% O t H l Fill d)(CCP, 100% Oct. Holes Filled)
Space Group = Fm3mLattice = FCCBasis = Cl (0,0,0), Na (½,½,½)
Coordination = 6, 6Cation Coord. → OctahedronAnion Coord → OctahedronAnion Coord. → OctahedronConnectivity → Edge sharing octahedra
with faces parallel to {111}4 NaCl in unit cell 96
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POLYHEDRAL REPRESENTATION• shows the topology and indicates interstitial sites• shows the topology and indicates interstitial sites• tetrahedra and octahedra are the most common shapes
Rock Salt:
• Array of edge sharing NaCl6 octahedra
h h d h ll d
Rock Salt:
• Each octahedron shares all 12 edges
• Tetrahedral interstices
Galena (PbS) 97
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ROCK SALT - OCCURANCE
• Very common (inc. 'ionics', 'covalents' & 'intermetallics' )
lk l h l ( l ) • Most alkali halides (CsCl, CsBr, CsI excepted)
• Most oxides / chalcogenides of alkaline earths
M n nit id s bid s h d id s ( Z N TiC N H)• Many nitrides, carbides, hydrides (e.g. ZrN, TiC, NaH)
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COMPLEX ION VARIANT OF ROCK SALT
• space group = Pa3
• sulfur dimers oriented along <111>
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(CCP T H l Fill d)
ZINC BLENDE (ZnS, SPHALERITE)(CCP, T+ Holes Filled)
Space Group = F43mLattice = FCCB i S (0 0 0) Z (¼ ¼ ¼)Basis = S (0,0,0), Zn (¼,¼,¼)
Coordination = 4, 4Cation Coord. → TetrahedronAnion Coord. → TetrahedronConnectivity → Corner sharing Tetra.4 ZnS in unit cell 100
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ZINC BLENDE GaAs
• bonding is less ionic than in rock salt
• common for Be, Zn, Cd, Hg chalcogenides (i.e., ZnS, ZnSe, ZnTe)
• common for III-V compounds (B, Al, Ga, In with N, P, As, Sb)
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DIAMOND STRUCTURES h l it b t ith id ti l t i ll itiSame as sphalerite, but with identical atoms in all positions
Space Group = F43mLattice = FCCB i C (0 0 0) C (¼ ¼ ¼)Basis = C (0,0,0), C (¼,¼,¼)
Coordination = 4Connectivity → Corner sharing Tetra.y g8 C atoms per unit cell
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FLUORITE (CaF2) & ANTIFLUORITE (Na2O)Fluorite : CCP of Ca2+, 100% Tetra. Holes Filled with F-
Anti-fluorite : cation and anion positions are reversed
Ca2+
Space Group = Fm3m
Lattice = FCCBasis = Ca2+ (0 0 0) F- (¼ ¼ ¼) & (¾ ¾ ¾)Basis = Ca2+ (0,0,0), F (¼,¼,¼) & (¾,¾,¾)
Coordination = 8, 4 (fluorite)Cation Coord. → CubicAnion Coord. → TetrahedralConnectivity → Edge sharing FCa4 tetrahedra or edge sharing CaF8 cubes4 CaF2 in unit cell 103
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ALTERNATIVE REPRESENTATIONS
Ca2+
Displacing the unit cell by ¼ of a body diagonal emphasizes the cubic cation coordination:
F-
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FLUORITE / ANTIFLUORITE
Ca2+
• origin of the term “fluorescence” (Stokes, 1852)
• fluorite common for fluorides of large,divalent cations and oxides of largetetravalent cations (M2+F and M4+O )tetravalent cations (M F2 and M O2)
• antifluorite common foroxides/chalcogenides of alkali earths (M2O)
CaF2
oxides/chalcogenides of alkali ea ths ( 2O)
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FLUORESCENT MINERALS
http://en.wikipedia.org/wiki/Fluorescence= fluorite 106
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COMPARING NaCl, ZnS, Na2O
NaCl ZnS Na2O
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Li3Bi EXAMPLE
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NiAs STRUCTURE(HCP, 100% Oct. Holes Filled)
2
Space Group = P63/mmcLattice = Primitive hexagonalBasis = As (0,0,0) & (2/3,1/3,1/2)
Ni (1/3,2/3,1/4) & (1/3,2/3,3/4)Coordination = 6, 6Cation Coord. → OctahedronAnion Coord → Trigonal prismAnion Coord. → Trigonal prismConnectivity → Edge/face sharing Oct.
or edge-sharing trigonal prisms2 NiAs in unit cell 110
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Alternative unit cell with Ni at the origin:
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•Transition metals withNiAs
Transition metals withchalcogens, As, Sb, Bi e.g. Ti(S,Se,Te); Cr(S,Se,Te,Sb); ( , , , )Ni(S,Se,Te,As,Sb,Sn)
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WURTZITE (ZnS) STRUCTURE(HCP T H l Fill d)(HCP, T+ Holes Filled)
Space Group = P63mcLattice = Primitive hexagonalB i S (0 0 0) & (2/3 1/3 1/2)Basis = S (0,0,0) & (2/3,1/3,1/2)
Zn (0,0,5/8) & (2/3,1/3,1/8)Coordination = 4, 4Cation Coord. → TetrahedronAnion Coord. → TetrahedronConnectivity → Corner sharing Tetra.2 ZnS in unit cell 113
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ZnO
Projections perpendicular to close-packed planes
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Very different next-nearest neighbor coordinations & beyond
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HCP VERSION OF CaF2?N t t k ith ll T t it (T d T ) fill d i HCPNo structures are known with all Tetra. sites (T+ and T-) filled in HCP- i.e. there is no HCP analogue of the Fluorite /Anti-Fluorite structure
Why?
The T+ and T- interstitial sites above and below a layer of close-packed spheres in HCP are too close to each HCP are too close to each other (distance = 0.25c) to tolerate the coulombic repulsion generated by filling with like-charged ions.
Face-linking is unfavorable117
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RUTILE STRUCTURE (TiO2)(distorted HCP, 50% Oct. Holes Filled)( , )
Ti O
Space Group = P4 /mnm
(0,0,0)
Space Group = P42/mnm
Lattice = Primitive tetragonalBasis = Ti (0,0,0) & (½,½,½)O (0 3 0 3 0) (0 7 0 7 0) (0 8 0 2 0 5) (0 2 0 8 0 5)O (0.3,0.3,0), (0.7,0.7,0), (0.8,0.2,0.5), (0.2,0.8,0.5)Coordination = 6, 3Cation Coord. → OctahedralAnion Coord. → Trigonal planarConnectivity → chains of edge-sharing Oct.
along axis, linked by vertices2 TiO2 per unit cell 118
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ANATASE STRUCTURE (TiO2)(di t t d CCP 50% O t H l Fill d)(distorted CCP, 50% Oct. Holes Filled)
a = 3.776 Åb 3 776 Å
Volume anatase TiO2 cell: 136.25 Å3
b = 3.776 Åc = 9.486 Å
Ti O
2 rutile TiO2 cell: 62.07 Å3
Space Group = I41/amd
Lattice = body-centered tetragonal
Coordination = 6, 3Cation Coord. → OctahedralAnion Coord. → Trigonal planarConnectivity chains of edge sharing OctConnectivity → chains of edge-sharing Oct.
along axis, linked by vertices and edges4 TiO2 per unit cell 119
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RUTILE AND ANATASE
chains of edge sharing oct.,linked at corners
greater density of edge sharing→ a bit less stablelinked at corners → a bit less stable
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CdI2 STRUCTURE(HCP ith Cd i O t H l f lt t l )(HCP, with Cd in Oct. Holes of alternate layers)
A layered crystal
Cd
I
Space Group = P3m1Lattice = Primitive trigonalB i Cd (0 0 0)Basis = Cd (0,0,0)
I (2/3,1/3,1/4) & (1/3,2/3,3/4)Coordination = 6, 3Cation Coord. → OctahedronAnion Coord. → Trigonal pyramidConnectivity → sheets of edge-sharing Oct.1 CdI2 per unit cell 121
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Alternative unit cell with Cd at the origin:the origin:
CdI6 units NiAs6 units6 6
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CdI2 - OCCURANCE
• Iodides of moderately polarizing cations; bromides andchlorides of strongly polarizing cations; f g y p g ;
e.g. PbI2, FeBr2, VCl2
• Hydroxides of many divalent cations e.g. (Mg,Ni)(OH)2
• Di-chalcogenides of many quadrivalent cations TiS Z S C Te.g. TiS2, ZrSe2, CoTe2
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CdCl2 STRUCTUREThe CCP analogue of CdI2
(CCP, with Cd in Oct. Holes of alternate layers along [111])
Space Group = R32/m
CdCl6 octahedra
Chlorides of moderately polarizing cationse.g. MgCl2, MnCl2
Di-sulfides of quadrivalent cations e.g. TaS2, NbS2 (CdI2 form as well) 124
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Formula Type and fraction of sites occupied CCP HCP
AB All octahedral NaClRock Salt
NiAsNickel Arsenide
Half tetrahedral(T+ or T-)
ZnSZinc Blende
ZnSWurtzite
N O A ti Fl itA2B All tetrahedral Na2O Anti-FluoriteCaF2 Fluorite not known
A3BAll octahedral& t t h d l Li3Bi not knownA3B & tetrahedral Li3Bi not known
AB2
Half octahedral (Alternate layers
full/empty)CdCl2 (Cadmium Chloride) CdI2 (Cadmium Iodide)
full/empty)
Half octahedral(Ordered
framework arrangement)
TiO2 (Anatase) CaCl2TiO2 (Rutile)
arrangement)
AB3
Third octahedral Alternate layers
2/3 full/emptyYCl3 BiI3 125
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PEROVSKITE STRUCTURE ABO3 (CaTiO3)(CCP of Ca & O , 25% Oct. Holes Filled by Ti)
B C llA-Cell
Space Group = Pm3mLattice = Primitive cubicB i Ti (0 0 0) C (½ ½ ½)
An extremely important class of ABX3compounds:
B-Cell
Basis = Ti (0,0,0), Ca (½,½,½), O (½,0,0), (0,1/2 ,0) & (0,0,½)
Coordination = Ca-12 ; Ti-6; O-6Ca Coord. → Cuboctahedron
compounds:MagnetoresistanceFerroelectricityMultiferroics
dTi Coord. → OctahedronO Coord. → distorted octahedron (4 Ca, 2 Ti)1 CaTiO3 per unit cell
SuperconductivityCatalysis (fuel cells)Spin transport 126
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PEROVSKITE CONNECTIVITY
B-Cell
3D network of corner-sharing octahedra
Network of face-sharing cuboctahedraoctahedra cuboctahedra
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Perovskites: the most widely studied oxide structurePerovskites: the most widely studied oxide structure
• Wide range of chemistries possible- thousands of examples knownthousands of examples known
• Cubic, tetragonal, and orthorhombic symmetries are common
- high Tc cuprate superconductorsColossal Magneto Resistance (La SrMnO )
Unique properties of perovskites
- Colossal Magneto-Resistance (La,SrMnO3)- fast ion conduction (Li+, O2-), batteries, fuel cells- mixed electronic/ionic conduction, fuel cells- oxidation/reduction catalystsoxidation/reduction catalysts- ferroelectric / piezoelectric ceramics (BaTiO3, Pb(ZrTi)O3)- important mineral structure in lower mantle (MgSiO3, pyroxene)- frequency filters for wireless communications : Ba(Zn1/3Ta2/3)O3q y ( 1/3 2/3) 3
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Perovskite Structure: ABX3AX
Tolerance factor (t):
A Xr r2( )
A X
B X
tr r
B
t Effect Likely structureA-Cell
t Effect Likely structure
> 1 A cation too large to fit in interstices
Hexagonal perovskite
0.9 - 1.0 ideal Cubic perovskite
0.71 - 0.9 A cation too small Orthorhombic perovskiteperovskite
< 0.71 A cation same size as B cation Possible close packed lattice 129
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PEROVSKITESMost perovskites contain distorted octahedra and are not cubic These distortions giveMost perovskites contain distorted octahedra and are not cubic. These distortions give
perovskites a rich physics.
symmetry at 25°CBaTiO3: Ba2+ r = 1.56 Å
Ti4+ r = 0.68 ÅO2- r = 1.26 Å
t = 1.03 - tetragonal
symmetry at 25 C
O r 1.26 Å
KNbO3: K+ 1.65 ÅNb5+ 0.78 Å
t = 1.01 - orthorhombic
LiNbO3: Li+ 1.06 ÅNb5+ 0.78 Å
t = 0.81 – trigonal
LiNbO3 : ferroelectricity, Pockels effect, piezoelectricity, photoelasticity, nonlinear optical polarizabilitynonlinear optical polarizability
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Reading: West 15
C m-2
V m-1V m 1
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DI- , PARA- , AND FERROELECTRICSdipole moment: p = qd = αEresponse of atom to applied E field
P E
dipole moment: p = qd = αEpolarization: P = Σp/V
p pp
P = ε0χeEP : polarization (C/m2)ε0: vacuum permittivity – 8.85 x 10-12 C2 N-1 m-2
l b l ( l )p χe: electric susceptibility (unitless)E : electric field (V/m, or N/C)
p
dielectric polarization paraelectric polarization ferroelectric polarization
• linear: P = ε χ E • nonlinear • residual (zero field) polarization• linear: P = ε0χeE
• no P without E
• nonlinear
• no P without E
• residual (zero-field) polarization• reversible direction of residual P• very large susceptibilities
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WHY IS BaTiO3 FERROELECTRIC
ferroelectric phase transition~0.1 Å displacement
> 120°C cubic, not FE< 120°C tetragonal, FE
transition occurs at the Curie temperature, Tc
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con
stan
t εr = χe+ 1
diel
ectr
ic
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FERROELECTRIC HYSTERESIS LOOPS
saturation polarization, Psremnant polarization, PR
dipoles aligned “up”
coercive field Ecoercive field, EC
dipoles aligned “down”
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ORDERED ELECTRIC DIPOLE PHASES
ferroelectric (BaTiO3) • parallel ordering below Tc
antiferroelectric (PbZrO3)• antiparallel ordering below T• antiparallel ordering below Tc
• E field can induceferroelectric state
ferrielectric (Bi4Ti3O12)ferrielectric (Bi4Ti3O12)• net spontaneous polarization in only certain direction(s)
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CURIE TEMPERATUREThermal energy destroys the ordered electric dipole state The temperature aboveThermal energy destroys the ordered electric dipole state. The temperature above
which this order-disorder phase transition occurs is the Curie temperature, Tc.
Above Tc, the material is often paraelectric.
orderedF / AF
randomizedorientation
PNote: These curves Pomit the “spikes” in Pat Tc
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PHASE DIAGRAMS
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K2NiF4 STRUCTURE (La2CuO4) Many “complex” structures are composed of simple familiar building blocks
Doped La2CuO4 was the first (1986) High-Tc Superconducting Oxide (Tc ~ 40 K)B d & Müll d d N b l P i
Many complex structures are composed of simple, familiar building blocks. The high-Tc copper oxide superconductors are an example.
Bednorz & Müller were awarded a Nobel PrizeLa2CuO4 may be viewed as if constructed from an ABAB... arrangement of Perovskite cells - known as an AB Perovskite!
B
A
B
2 La2CuO4 per unit cell 140
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ALTERNATE VIEWS OF La2CuO4
We may view the structure as based on:y1. Sheets of elongated CuO6 octahedra, sharing only vertices 2. Layered networks of CuO4
6-, connected only by La3+ ions 141
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COMMON STRUCTURAL FORM
Cations formFCC with O2-FCC with O2
interstitials
• Common structural motif of vertex-linked CuO4 squares• This motif occurs in all the high-T superconducting copper oxides • This motif occurs in all the high-TC superconducting copper oxides • The structures differ in the structure of the 'filling' in the 'sandwich‘of copper oxide layers - known as Intergrowth Structures 142
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YBa2Cu3O7: THE 1,2,3 SUPERCONDUCTOR• the first material to superconduct at LN2 temperature, Tc > 77 K• YBa2Cu3O7 can be viewed as an Oxygen-Deficient Perovskite
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T t p s f C sit s:
POLYHEDRAL REPRESENTATION OF YBCOTwo types of Cu sites: 1) Layers of CuO5 square pyramids2) Chains of vertex-linked CuO4 squares
CuO2BaOBaOCuOBaOCuOCuO2YCuO2
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SPINEL STRUCTURE AB2O4 (MgAl2O4) (CCP, Mg in 1/8th of Tetra. Holes and Al in 50% of Oct. Holes)
a = 8.08 Å
Space Group = Fd3m
• extremely flexible structure, adoptedby over 100 compounds
Lattice = FCCCoordination = Mg-4; Al-6; O-4Mg Coord. → TetrahedronAl Coord. → Octahedron
• normal spinel: 8 A in Tetra., 16 B in Oct.
• inverse spinel: 8 A in Oct., 8 B in Oct. and Al Coord. OctahedronConnectivity → chains of Edge-sharing AlO6
octahedra, linked by MgO 4 tetra.8 MgAl2O4 per unit cell (56 atoms)
8 B in Tetra.• intermediate cations distributions also
occur. 145
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SPINELS - OCCURANCEAluminium spinels: Aluminium spinels:
Spinel – MgAl2O4, after which this class of minerals is namedGahnite - ZnAl2O4H i F Al OHercynite - FeAl2O4
Iron spinels: Magnetite - Fe3O4Franklinite - (Fe,Mn,Zn)(Fe,Mn)2O4Franklinite (Fe,Mn,Zn)(Fe,Mn)2O4Ulvöspinel - TiFe2O4Jacobsite - MnFe2O4Trevorite - NiFe2O4
Ch i s i ls: Chromium spinels: Chromite - FeCr2O4Magnesiochromite - MgCr2O4
Others with the spinel structure: pUlvöspinel - Fe2TiO4Ringwoodite - Mg2SiO4, an abundant olivine polymorph within the Earth's mantle from about 520 to 660 km mantle from about 520 to 660 km depth, and a rare mineral in meteorites 147
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CRYSTAL FIELD STABILIZATION ENERGYIn transition metal compounds d electron effects such as crystal field In transition metal compounds, d electron effects such as crystal field stabilization energy (CFSE) can be important in determining structure.
crystal field splitting diagrams
e.g. MF2 compounds (high spin rutile)
crystal field splitting diagrams
Δoct =
Δtetra =
No CFSE
Δtetra = (4/9)Δoct
CFSEoct = (0.4 × #t2g – 0.6 × #eg) Δoct
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CATION SITE PREFERENCES IN SPINELSThe larger CFSE of metal ions in octahedral sites is sometimes an important
f d l ( l )
Normal - [A]tet[B2]octO4 Inverse - [B]tet[A,B]octO4
factor in determining spinel structures (normal vs inverse).
γ = fraction of A in oct. sitesγ = 0 is normal, γ = 1 is inverse
In the absence of CFSE effects: 2,3 spinels tend to be normal (MgAl2O4)4,2 spinels tend to be inverse (TiMg2O4)
l E f h f ll In 2,3 spinels, CFSE favors the following: 1) Chromium spinels (Cr3+) are normal2) Magnetite (Fe3O4) is inverse b/c 2) Magnetite (Fe3O4) is inverse b/c
Fe3+ has zero CFSE, while Fe2+ prefers oct. 3) Mn3O4 is normal b/c Mn2+ has no CFSE 149
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CORUNDUM STRUCTURE (α-Al2O3)(HCP 2/3 f O t H l fill d)(HCP, 2/3 of Oct. Holes filled)
Space Group = R3c
Lattice = Primitive trigonal
Coordination = 6, 4Cation Coord → OctahedronCation Coord. → OctahedronAnion Coord. → distorted tetrahedronConnectivity → edge, face-sharing Oct.6 Al2O3 per unit cell
• Ruby (Cr), sapphire (Fe, Ti, Cr), Fe2O3
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