Crystallography Flashcards

(97 cards)

1
Q

X-Ray Diffraction (XRD)

A
  • single crystal X-ray diffraction (SXD): analyses 1 crystal
  • powder X-ray diffraction (PXRD): analyses powders/bulk solids
    ~ millions of crystallites or amorphous (or in between i.e. poorly crystalline)
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2
Q

SXD

A

use just one crystal
- rotate in 3D (data is 3-dimensional)
- measure I(hkl): direct determination of crystal symmetry

determines crystal structure:
- unit cell
- symmetry
- atomic coordinaties
- atomic vibrations
- derived parameters: bond lengths (i.e. bond strength) and angles

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3
Q

PXRD

A

Bragg’s Law: nλ = 2dsinθ
scan 2θ and measure I

peak positions (2θ): unit cell parameters
peak heights/areas (intensity): structure and quantity

applications:
- qualitative analysis: diffraction pattern for a material is unique
- quantitative analysis: a mixture exhibits a diffraction pattern that is the sum of the diffraction pattern of each component, scaled by the amount present
- unit cell parameter refinement: 2θ values give crystal system and Bravais lattice

sample preparation:
1. fine powder (light grinding)
2. mounted: flat-plate holder/between thin foils/glass capillary
(glass capillary gives better intensity data, but difficult to fill without breaking)
3. measurement: accurate position (2θ) of Bragg peak requires good sample preparation

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4
Q

coordinate system: cartesian system in real space

A

3 mutually perpendicular axes with same unit length scale along each axes (Ångstroms, Å)
1Å = 10^-10 m (similar to sizes of atoms)

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5
Q

NaCl cartesian system

A
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6
Q

coordinate system: crystallographic system

A

3 non-planar vectors defining repeat of the lattice in 3-dimensional space
- vectors define size of the unit cell
- given by symbols 𝐚, 𝐛, 𝐜
- magnitude a, b, c
- inter-vector angles α, β, γ

position of an atom: 𝐫 = x𝐚 + y𝐛 + z𝐜

coordinates are fractions of a, b, c

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7
Q

NaCl crystallographic system

A
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8
Q

rationale for crystallographic xyz

A
  1. to identify common structural types
  2. to enable generation of coordinates of atoms within the unit cell
  3. to enable the calculation of the intensity of diffraction peaks
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9
Q

crystallographic system: describing crystal structure based on atoms WITHIN the unit cell

A

0 ≤ x < 1
0 ≤ y < 1
0 ≤ z < 1

exceptions
- conventional to put centres of mass of the molecule within the unit cell
- since molecules do not have sharp edges, some of the molecule may be outside the unit cell

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10
Q

rationale for cartesian system

A

best for calculating parameters of chemical interest: bond lengths, bond angles, torsion angles, intramolecular or intra-ionic distances

distance, r between two points S and O given by Pythagoras’ rule

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11
Q

rationale for crystallographic system

A

best for finding the coordinaes of symmetry related objects

  • mirror symmetry
  • rotation axes
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12
Q

mirror planes

A
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13
Q

rotation axis: twofold rotation of points in space by 180 degrees

A
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14
Q

rotation axis: threefold roation of points in space by 120 degrees

A

no need to use numbers like √3 as in a Cartesian system

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15
Q

interatomic distances

A

orthogonal axis systems: cubic, tetragonal, orthorhombic
X = xa
Y = yb
Z = zc

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16
Q

describing crystal structures: BaSO4

forms of description
- words
- visual images
- tables of crystallographic and chemical parameters

A

WORDS:
discrete Ba2+ cations and SO42- anions
- isolated and not linked

SO42- anions are tetrahedral
10 x O of SO42- anions lie within 3.2Å or Ba2+

TABLES OF CRYSTALLOGRAPHIC AND CHEMICAL PARAMETERS:
CIF files (Crystallographic Information File)
typically contain:
- unit cell parameters
- space group symmetry: symmetry operators
- coordinates of the atoms: derived bond lengths, angles and torsion angles
- atomic displacement parameters

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17
Q

atomic coordinates

A
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18
Q

symmetry operators

A

enable one to determine the coordinates of symmetry related atoms within a crystal structure (usually either in the unit cell or in an adjacent one)

a mirror plane perpendicular to c located at z=1/4 has the symmetry operator (x, y, 1/2-z)

so there is another O(3)’ at:

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19
Q

translational symmetry

A

symmetry operators may generate atom coordinates outside the unit cell

translational symmetry provides additional symmetry operators that allows the generation of atoms within the unit cell

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20
Q

additional translational symmetry may be provided by a centred lattice (so none for a P lattice)

A

these operators appy to every atoms within the cell

in NaCl, Cl- are at:
0,0,0
1/2,1/2,0
1,2, 0, 1/2
0, 1/2, 1/2

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21
Q

general position

A

substitution of O(3) coordinates into the symmetry operators will generate 8 symmetry-related atoms of type O(3) per unit cell
- 8 symmetry operators and 8 sets of coordinates: O(3) is said to be in a GENERAL POSITION within the unit cell

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22
Q

special position

A

when the number of atomic positions is less than the number of symmetry operators per unit cell
- atom is said to be in a SPECIAL POSITION
- i.e. its position is on a symmetry element

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23
Q

ionic solids: NaCl (halite) + NiAs

A

NaCl
- cubic close packed layers of Cl- with Na+ in all Oh holes
- 6:6 coordination

NiAs
- hexagonal close packed layers of As- with Na+ in all Oh holes
- 6:6 coordination

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24
Q

ionic solids: ZnS (zinc blende/sphalerite) + ZnO (wurtzite/zincite)

A

ZnS
- cubic close packed layers of S2- with Zn2+ in half of the Td holes
- 4:4 coodination

ZnO
- hexagonal close packed layers of O2- with Zn2+ in half of the Td holes

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25
ionic solids: Li2O (anti-fluorite strucure) + CaF2 (fluorite structure)
Li2O - cubic close-packed layers of O2- with Li+ in all Td holes - 4:8 coordination CaF2 - anion and cation sites are swapped with each other to give an 8:4 coordination - primitive cubic array of F- - cubic close-packed layers of Ca2+ with F- in all td holes
26
ionic solids: CdI2 + CdCl2
CdI2 - hexagonal close-packed (ABABAB) layers of I- with Cd2+ in Oh holes - but in alternate layers i.e. 100%, 0%, 100%, 0%... CdCl2 - cubic close-packed (ABCABC) layers of Cl- with Cd2+ in Oh holes - but in alternate layers
27
spinel AB2O4 structure
structure O2- anions with two types of cation A is normally 2+ B is normally 3+ face-centred cubic - close-packed layers of oxide anions can be seen when model is viewed perpendicular to body diagonal of cube (a 2D view) structure 1: - close-packed O2- anions - all Oh holes filled with cations structure 2: - close-packed O2- anions - half of Oh holes filled with cations structure 3: - close-packed O2- anions - all Td holes filled with cations structure 4: - close-packed O2- anions - 1/8 (12.5%) Td holes filled with cations structure 5: - close-packed O2- anions - half of Oh holes filled with cations - 1/8 (12.5%) Td holes filled with cations
28
inverse spinel B(AB)O4 structure
close-packed O2- anions (shown as 2x2x2 fcc cube) BUT 3+ cations on Td site 2+ and 3+ cations on Oh site (disordered)
29
eamples of AB2O4 and B(AB)O4 structure
A = 2+ cation B = 3+ cation NORMAL: spinel structure - MgAl2O4 - larger Mg2+ ion prefers tetrahedral geometry - smaller Al3+ ion prefers octahedral geometry INVERSE: spinel structure - CoFe2O4 - larger Co2+ ion prefers octahedral geometry - smaller Fe3+ ion swaps to tetrahedral geometry (whilst other stays octahedral)
30
close packing for more highly charged cations
close sphere packing works well for low charged cations (1+ and 2+) - not good for highly charged cations (Ti4+ or Si4+ - ionic with some covalency)
31
perovskite oxides (ABO3) parent compound: CaTiO3
sum charges ABO3 oxides: A + B = 6+ ABX3 (less common) halides A + B = 3+ examples: SrCoO3 NaMgF3 cubic, tetragonal, orthorhombic or monoclinic
32
importance of perovskites
ceramic high Tc superconductors YBa2Cu3O7-x perovskites of recent interest: MAPI Methyl Ammonium Lead (Pb) Iodide
33
perovskite ABO3 structure (ideal)
corner shared octahedrons of [BO6] units - form a primitive unit cell with a = 3.7 - 4.5 Å large cation A at the centre of the cube (1/2, 1/2, 1/2) smaller cation B is at (0,0,0) O2- anions are at (1/2, 0, 0), (0, 1/2, 0), and (0,0,1/2) can be viewed as cubic close packed layers of AO3 with B in 25% Oh holes
34
perovskite ABO3 structure (actual)
if A cation too small: cooperative rotations lower the symmetry - tilting of [BO6] octahedra - reduces distance between A site cation and O2- - O2- can get closer to A site - many tilt combinations possible other distortions caused by the B cation moving slightly off the centre of the O6 octahedron - results in interesting electrical and magentic properties
35
volume of unit cell
36
density
37
linking MO6 octahedra
simple corner-sharing octahedra: perovskite structure mixing corner-sharing with edge-sharing: several permutations possible -Anatase -Rutile -Brookite
38
Anatase
Tetragonal Bravais Lattice - TiO6 octahedra with both corner and edge sharing slice through structure parallel to c - within the slice, [TiO6] units are corner linked double slice through the structure parallel to c - slices are linked together along c via edge-shared [TiO6] units
39
consequences of vertex and 2D edge sharing in Anatase
- distorted internal angles within octahedron - coordination around O2- deviates from 120° Ti-O-Ti: 101.9° (×2), 156.2°
40
Rutile
Tetragonal Bravais Lattice - TiO6 octahedra with both corner and edge sharing slice through structure parallel to c - within the slice [TiO6] units are corner linked (but differently to Anatase) edge sharing occurs in 1D columns
41
consequences of vertex and 2D edge sharing in Rutile
- less distorted angles within octahedron - coordination around O2- has smaller deviation from 120° (compared to anatase) Ti-O-Ti: 130.6° (×2), 98.8.2° density comparison Rutile: 4.25 g cm-3 Anatase 3.89 g cm-3 Rutle is the thermodynamically stable form Anatise is the kinetic form
42
Brookite
Orthorhombic lattice - TiO6 octahedra with both corner and edge sharing
43
silica (SiO2) and silicates
tetrahedral [SiO4] group - either as a discrete anion, (SiO4)2- or as oxygen-linked tetrahedral neutral/anionic species -O-Si(-O-)2-O-Si(-O-)2-O-
44
crystalline quartz SiO2
common crystalline form of SiO2 its crystalline nature can be seen in PXRD pattern
45
quartz glass (silica) SiO2
tough clear solid with very high melting point (softens at > 950°C) no sharp diffraction peaks in PXRD pattern - indicates a purely amorphous (glassy) substance
46
SiO2 is polymorphic
multiple crystalline forms + an amorphous (glassy) form local structure is the same for all forms difference in the way the [SiO4] tetrahedra are linked random [SiO4] linking occurs when cooling from the liquid state - leads to a glass as evidenced by the lack of Bragg peak in PXRD pattern [SiO4] tetrahedra may be linked so as to lead to solids varying from high to low density
47
zeolites: low density SiO4 networks
[SiO4] or [AlO4]- tetrahedra (often simplified to [TO4]) T = Si or Al primary building unit: [TO4] unit linked via O bridging secondary building unit: T-O-T rings
48
Lowensteins' rule
Al-O-Al linkages in zeolitic frameworks are forbidden - all [AlO4]- must be linked to 4 [SiO4] units
49
Sodalite (SOD)
simplest zeolite framework structure Na8(Al6Si6O24)Cl2 [Si]/[Al] ratio is 1:1 cubic with a = 8.9 Å
50
Faujasite (FAU)
cubic, naturally occuring zeolite with a = 24.7 Å (Na2,Ca,Mg)3.5[Al7Si17O48].32(H2O) synthetic versions are known as zeolites X/Y X is where [Si]/[Al] = 2 to 3 Y is where [Si]/[Al] > 3
51
diffraction: scattering by a single atom
x-rays are scattered by electrons in an atom incoming x-ray photon acts as a plane wavelet as source is a long way from the sample scattered x-ray photon acts as a spherical wavelet
52
diffraction in 1-dimension
multiple slits: a 1-D optical diffraction grating optical grating: nλ = dsinθ n - order d - slit spacing if atoms are in a regular array, diffraction will occur if an appropriate wavelength source is used
53
diffraction in 2-dimension
2-D optical diffraction grating useful to demonstrate how symmetry information can be derived from a single image - inversion symmetry added during the process of diffraction - diffraction space unit cell vectors are in a different direction to real space ones when the unit cell angle is not 90 - diffraction space has natural origin (0,0,0) - small dimensions become big and vice versa (property of diffraction space: e.g. volume, V* = 1/V) - translational symmetry in 2-dimensional space due to a centred lattice leads to missing intensity spots in a systematic matter in 2-D diffractional space
54
inversion symmetry is added during the process of diffraction
(not exact when object itself has no inversion symmetry but very close to inversion symmetry) diffraction pattern contains a point of inversion in the absence of anomalous dispersion, even when this symmetry element is not present in the crystal structure
55
diffraction space unit cell vectors are in a different direction to real space ones when the unit cell angle is not 90°
diffraction space indicated with * b* perpendicular to a a* perpendicular to b c and c* are colinear and perpendicular to the plane of the screen unit cell angles that are 90° in the crystal will exhibit 90° angles in reciprocal space
56
diffraction and crystals
crystalline objects produce diffraction spots symmetry relationship between crystal (real) space and diffraction (reciprocal) space crystal space: 3-dimensional symmetry across all space diffraction space: 3-dimensional symmetry around a point (h,k,l = 0,0,0) amorphous objects (glasses) do not produce diffraction spots
57
single-crystal experiment
modern single-crystal x-ray diffractometer has 3 rotation axes (ω, κ (or χ), φ) rotate crystal in 3-dimensional space, plus a rotation axis 2θ for the detector orient the crystal with respect to the incident x-ray beam so as to satisfy Bragg's law by rotations about the different instrument axes - as the crystal is slowly rotates, the intensity of the diffracted x-rays is measured using an area detector 2θ value for every spot provides d spacing via Braggs law λ = 2d_hkl sinθ_hkl d-spacing relates to the 6 unit cell parameters: a, b, c α, β, γ
58
d-spacing for orthogonal symmetry
59
d-spacing for cubic symmetry
60
coordinate system for diffraction spots is defined in terms of 3 vectros
a* b* c* a* is perpendicular to b and c in the crystal b* is perpendicular to c and a in the crystal c* is perpendicular to a and b in the crystal the vector dot products are unity a.a* = 1 b.b* = 1 c.c* = 1 the diffraction coordinate space has a 'reciprocal' relationship to crystal coordinate space (hence, the name reciprocal space)
61
diffraction space coordinates: position of a point, d* on the lattice formed by the 3 vectors, a*, b*, c*
d* = ha* + kb* + lc* hkl correspond to the same Miller indices hkl of the lattice planes from which the diffraction intensity I(hkl) arises
62
diffraction space coordinates: if crystal axes (a,b,c) are orthogonal
diffraction space axes (a* ,b* ,c*) are orthogonal and in the same direction lengths of the axes are given by: a* = 1/a b* = 1/b c* = 1/c
63
diffraction space coordinates: length of d*
if cell angles are 90,
64
consider a unit cell with orthogonal axes
65
Fourier Transform links diffraction data to crystal structure
real space (crystal) → reciprocal space (diffraction) atoms → scattering factor unit cell and lattice → interference term atomic displacements → Debye-Waller factors
66
scattering of x-rays by atoms
x-rays interact strongly with the electrons in an atom (or ion) elastic interaction → diffraction absorption & re-emittance → fluorescence (loss of coherent scattering) elastic interaction is proportional to number of electrons (atomic number, Z) - scattering factor given by symbol, f
67
x-ray scattering factors, f (2θ)
electron density of atom has gaussian distribution fourier transform of the electron cloud corresponds to the X-ray form factor
68
intensity of diffraction I(hkl)
position of the atoms is determined by I(hkl) - peak maximum is the position of the peak at 2θ - position of the peaks, 2θ, determined by Bragg's Law peak area is the intensity of the peak I(hkl) peak has height H and width W (for powder diffracion) - I(hkl) ∝ H ∝ W intensity of the peak, I(hkl) is given by the 'Structure Factor' equation (symbol F(hkl))
69
I(hkl) ∝ IF(hkl)I^2
the proportionality terms are: c - the scale factor ~ counting time ~ amount of diffracting material j_hkl - multiplicity (this only applies to PXRD) ~ number of symmetry equivalent reflections Lp(2θ) - geometric factors - Lorentz, L - polarisation, p
70
the structure factor equation
summation is taken over all atoms, n within a single unit cell summation could be taken over all atoms in the crystal, but since all unit cells are the same: multiply F_hkl by the number of unit cells
71
the Interference Term
amount of constructive/destructive interference of X-ray wave depends on the scattering power of each atom, and its relative position (r_n) within the unit cell also depends on the diffracting planes hkl whose normal can be defined in terms of d* as d* = ha* + kb* + lc*
72
definition of structure factor F_hkl
the Fourier transform of the electron density ρ_xyz - x-rays 'see' electrons NOT atoms F_hkl is a vector quantity - can be thought of a wave expression with magnitude IF_hklI and a relative phase angle Φ
73
calculating Fhkl for CsCl
consider the hypothetical case where the atoms(/or ions) are stationary in space Debye-Waller factor exp(-Wn)=1 since the atomic displacements are zero (e^0=1)
74
100 planes
Cs atoms lie in the planes with the Cl atoms half-way between them - therefore destructive interference occurs
75
200 planes
both the Cs atoms and Cl atoms lie in the same planes - therefore constuctive interference occurs
76
calculating F_hkl for Fe metal
reflection intensities from planes such as 110, 220, 211, 220, etc. (even) of Fe will be strong reflection intensities from planes such as 100, 111, 210, 300, etc. (odd) of Fe have zero intensity such reflections are said to be missing/extinct or SYSTEMATICALLY ABSENT for the cases of non-zero intensities, they are usually referred to as a REFLECTION CONDITION
77
Debye-Waller factor exp(-W_n)
effect of atomic motion atoms vibrate - usually as harmonic oscillators - giving rise to a normal (Gaussian) distribution about a point - Fourier transform of this motion is a normal distribution simplest case is for isotropic vibration
78
Lorentz-polarisatiion term - effect on PXRD
structure factor has a marked effect on the RELATIVE intensity of peaks in a PXRD - e.g. CsCl: weak 100 but strong 110 Lorentz-polarisation term also has a big effect
79
ICDD (International Centre for Diffraction Data) PDF (Powder Diffraction File) database or JCPDS (Joint Committee on Powder Diffraction Standards) database
PDF database consists of a set of cards, one for each material with its powder diffraction pattern parameters contains: - file number for the database entry - chemical formula, chemical name, and mineral/common name (if one exists) - quality factor of the data entry: star indicates data of the highest quality and data is indexed with hkl values - experimental details on how the data was obtained (radiation used - Cu Kα1 and wavelength - 1.5405Å) - crystallographic information: crystal system, lattice parameters, no. formula units per unit cell, calculated density - physical properties: mp, optical refraction indices and colour - the PXRD data
80
the PXRD data of PDF
PXRD pattern represented as a set of d-spacings (from high to low values) relative peak intensities (I/I1) and hkl values for each observed peak (i.e. the fingerprint region) d spacings of the 3 most intense peaks in the powder pattern and their relative intensities are used to constuct HANAWALT search/match tables
81
Hanawalt
most intense peaks from each phase are the easiest to identify in a mixture of phases sorted into d-spacing ranges (e.g. 3.74-3.60 Å) faster for manual search-match lists d-spacings for 4th-8th strongest peaks in addition
82
qualitative PXRD analysis ~ search-match
for a match, d-spacing values should match within experimental error reasons for mis-match - wrong material made - measurement error - instrumental error - not comparing like with like (e.g. if measurement and databse entry refers to different temperatures OR comparing doped vs pure phase materials)
83
practical qualitative PXRD
material at lower temperatures is almost amorphous - peaks sharpen with increasing T narrower peaks indicate that crystallite size is getting bigger with higher T difficult to make definitive assignment with broad peaks using database - use the highest temperature dataset matching the strong peaks against a database entry can show the presence of a particular major componenet in a PXRD sample HOWEVER purity is demonstrated by accounting for ALL of the peaks in the measured PXRD pattern
84
quantitative PXRD analysis
concept of quantitative analysis by PXRD methods is based on the fact that scattering is proportional to the amount of material present
85
indexing PXRD data - simple cubic material
86
the diffraction technique
single crystal x-ray diffraciton (SXD) - IF(hkl)I^2 values provide detail of the material/compound/complex - atomic postions, average atomic motion, unit cell and crystal symmetry powder x-ray diffraction (PXRD) - used for qualitative and quantitative analysis - can determine: is this the right material? it is single phase? purity?
87
problem with PXRD data
88
the Rietveld Method
powder diffraction pattern yi(calc) can be calculated from: - peak positions (determined by unit cell and any instrument zero offsets) - peak intensities (determined by structure factor, scale factor, geometric factors etc)
89
applications of the Reitveld Method
analysis of PND data - mixed metal oxides (e.g. perovskites) used to fit all powder diffraction data - used for organic crystal structures - often done badly and data over interpreted
90
zeolite synthesis
used in petroleum industry - heterogeneous catalyst for hydrocarbon isomerisation reactions low density crystal structure is not normally favoured - synthetic methods need to exploit kinetic (and other) effects 1. hydrothermal methods 2. silica and alumina gels (F- to act as a mineraliser) 3. templating organic molecules (amine based e.g. diethylamine to make ZMS22) - removed after synthesis by calcination 4. [PO4] to replace [SiO4] to give ALPOs
91
Metal Organic Framework (MOF)
large, open pore network structures - created by (semi-) rigid organic linkers and metal cations syntheis is similar to that of zeolites - hydrothermal/solvothermal techniques used (crystals grow slowly from a hot solution) constructed from bridging organic ligands that remain intact throughout the synthesis and act as the templates - contrast with zeolites where amines are used and have to be removed later functionality built into MOF by an appropriate choice of ligand
92
typical ligands for MOFs
oxalic acid malonic acid isophthalic acid terephthalic acid trimesic acid
93
metal cation in MOFs
cation's coordination preference influences size and shape of pores - dictates how many ligands can bind to metal structures descibed in terms of primary building blocks (ligands) and secondary building blocks
94
scientific interest of MOFs
driven by materials for H2 storage/CO2 capture and storage large pore size - can store lots of gas pore size can change depending on whether absorbed gas is present or not
95
example of MOF: MOF-210
prepared from a solvothermal reaction of H3BTE, H2BPDC and zinc(II) nitrate hexahydrate - synthesis involved 2 topologically different organic linking groups (both carboxylic acids) has ultrahigh surface area
95
example of MOF: MOF-5
organic linker: 1,4-benzenedicarboxylate (BDC) framework formula: Zn4(O)(BDC)3 metal cluster: 4 tetrahedra of [ZnO4] corner shared by an O to give a tetrahedral arrangement of Zn around the central O prepared by diffusion of NEt3 into solution of Zn2+ nitrate and BDC in DMF/C6H5Cl + H2O2 cavity contains DMF and C6H5Cl solvents
96
diffraction vs spectroscopy
diffraction - the Fourier transform of the whole unit cell and its contents - d-spacings do not relate to bond lengths - crystal structure determination gives structure of the WHOLE molecule - not just the metal and atoms bound to in an organometallic complex spectroscopy (NMR, IR) - measures local information - can be tuned to specific parts of a molecule (i.e. energy of a metal carbonyl bond)