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283 Cards in this Set

  • Front
  • Back
crystals are solids
but solids are not necessarily crystalline
crystals
have symmetry (kepler) and long range order
Lattice points
point which have identical environments, connected to form unit cells
unit cell
small shape, which can be repeated regularly over infinte area
tetrangonal
a=b, not equal to c, all angles 90
orthohormbic
a not equal to b not equal to c, all angles 90
hexagonal
a=b, not equal to c, alfa and beta = 90, gamma = 120
difference between Rhombohedral and Monoclinic
Rhombohedrual has a=b (min) and Monoclinic has not cell parameter equalities
crystal system is defined
in terms of symetry, not by crystal shape
triclinic
nothing equal to each other
orthogonal
when all angles = 90
non-orthogonal
when one of the angles are not 90
mirror line
reflect across line, an object can be bisected by mirror line
n fold rotation
360/n
Combinations that make 10 plane point groups
1,2,3,4,6,m,mm,3m,4m,6m
Cubic essential symetry
4 3 fold axes, along body diagonals
Tetrangonal essential symetry
1 4 fold axis, parallel to c, in center of ab
Orthorhomic essential symetry
3 mirrors or 3 2 fold axes, perpendicular to each other
Hexagonal essential symetry
1 6 fold axis, down c
Trigonal essential symetry
1 3 fold axis, down the long diagonal
Monoclinic essential symetry
1 n fold axis, along the "unique" axis
Triclinic essential symetry
none
3 types of centering/structuring or lattices
body centered, face centered, primitive. also side centering, but not very common
coordination number
(example) how many Na are in contact with Cl (6)
distance between adjacent lattice planes
d spacing
to tranlate fractional into miller index
take reciporocals, multiply to get integers
In reverse, a plane with miller index (hkl) has intercepts at:
a/h, b/k, c/l
planes parallel to faces:
intercepts: infinity 1 infinity, infinity, 1/2, infinity
(010), (020)
note that (100) not equal to (001)
when not cubic, in tetragonal, c not equal to a or b
optical diffraction grating
1 dimensional analogue of X-ray diffraction, coherent incident light impinges upon an evenly spaced grating: the parallel lines in the grating act as secondary light sources
optical diffraction grating
coherent indicent light goes through slits and you get diffracted light
planes in crystals are
considered to be reflecting planes
Braggs Law
2dsin (theta) = n (lambda)
in packing two dimentions: two packing arrangements
hexagonal and square
in three dimentions, three packing arrangments are common
heagonal close packing (hcp)
body centered cubic (bcc)
face centered cub or cubic close packing (fcc)
Hexagonal close packing
ABABAB
Cubic Close Packing/fcc
ABCABC
Tetrahedral intersital sites
CN 4
Octrahedral intersitial sites
CN 6
two types of tetrahedral sites
T+ means hole is above 3 molecules
T- means hole is under 3 molecules
packing fraction
space occupied by atoms/available space
Diamond and Zinc Blend, both important in semiconductor industry
Carbon at face centered and tetrahedral positions in diamonds, S in face centered, tetrahedral positions is Zn
Antifluorite, Na2O
oygen atoms in all fcc positions, sodium atoms in all tetrahedral sites
Flourite CaF2, ZrO2
Ca atoms in all fcc positions, F atoms in all tetrahedral sites
In both flourite and antiflorite
there is 4 fcc atoms and 8 filled tetrahedral sites in a unit cell
With ccp anion array
Rock Salt NaCl
Zinc Blend ZnS
Antiflourite Na2O
O occupied
T+ or T- occupied
T+ and T- occupied
With hcp anion array
Nickle Arsenide NiAs
Wurtzite ZnS
O occupied
T+ or T- occupied
With ccp cation array
Flourite ZrO2
T+ and T- occupied
Peroskite ABX3
can be polorizable
Laue model takes in
account the 3-d nature of the crystal lattice
X rays are
electromagnetic radiation
X ray photon energy
E=hv
X ray wavelength vary from
.01-10 Anstroms
X ray diffraction
X ray source, Sample, Detector
First assumption
X rays elastically scattered by electrons
Second assumption
spherical discrete atoms
interaction is weak
so need many electrons
Laue Method, fixed crystal
Uses: alignment of single cystal, infomration on unit cell, imformation on imperfections, defects in crystal
4 circle diffractometer
Uses: unit cell derermination, crystal structure detirmination
Powder diffraction
assume a random orientation of large number of small crystalines so that Braggs condition is always satified,
"Fingerprinting"
matches whole patterns with information from a database, ICDD Powder diffraction File, there is also a Inorganic Crystal Structure database
Why is is listed as D spacing and not 2 theta
D spacing is constant, different sample of same material
Uses of Fingerprinting
identify substance or mixture (could following a reaction), distinquish between different structures (even if chemically similar), distinquish between different polymorphs
Problems of Fingerprinting
some rubbish information, not sensitive
If we use X ray powder diffraction, a crystalline material will lead to
very sharp diffraction peaks, whereas an amorphous material will give several broad bands
If the crystals are small,
the diffraction lines broaden
B is the line broading, measured in radians
from the peak width at half maximum (BM) reffered to a standard (BS)
peaks are
connected to unit cell dimentions
Rietveld method
refinement technique, not structural detirmination, used when there is a similarity to an existing structure, basis behind qualntitaive X ray diffraction
Systematic Absences P
P: no restrictions, all allowed
Systematic Absenses I
h+k+l = 2n
Systematic Absenses F
h,k,l, all odd or all even
even though mocules have similar structure
behavior is different
ionic radii
hard to measure, estimated, composmise between attractive and repulsive
random dipoles
paraelectric
aligned dipole
ferroelectric
Solids
single crystal, glass, polymer, inorganic, compsite material
Macro
overall structure
micro
grains, defects
Nano
crystal structure, atomic level, focus of XRD
surface v bulk
at surface, structure is not perfect, bulk is better
properties like mechanical, magnetic, chemical
not investigated by XRD
Different kinds of diffraction
single crystal, powder, X ray, Neutron, Electron
For XRD, we must have
constructive interferance, exactly in phase
Laue Equations
basic idea is still constructive interference and interger wavelength
why not use microscope
can't focus x rays, costly, electron miscroscope are only 2 d
Electrons stopped at target
converted into X rays
Incident electrons displace inner shell electrongs
each target has a characteristic wavelength
Scattering will depend on
Z and angle
Laue Method
white source is weak, very slow, each spot represents a crystal plane
4 circle method
primary method to find crystal structure
(222)
all intersect at 1/2 1/2 1/2
when miller indices increase
plane numbers increase, d spacing decrease
X ray diffraction by crstal is anologous to
light difraction through a gradting. Braggs law is essential in describing x ray diffraction
Detector
as x ray detector scans through a range of theta values, peak intensities are noted, allowing calculation of d for different spacings
For CCP and FCC
they have same coordination numbers
tetrahedral sites
8 tetrahedral sites in a fcc structure, 1/4, 1/4, 1/4
in cubic unit cell
octrahedral bond length is a/2
tetrahedral is 1/4 a square root 3
In FCC and HCP
For primitaive
.74
.524
E=hv
for phontons
c=lamda v
another equation
lamda = hc/E
another equation
each element
has characteristic wavelenth
K beta
is transition from 3p-1s or from M-K
K alpha
transition from L-k or 2p - 1s
To find energy between levels
use E=hv and V=c/lamda
the whole pattern is what matters
not just one peak
Powder diffraction
main use is fingerprinting
2 theta
depends on lamda used
ICSD
Inorganic crystal structure database, free to acadmeics, can specify elements, will list artiles, draw pictures, can be exported into ATOMS
Advantages to Powder Diffraction
quick and easy, non destruvie for forensics
Problems with Powder diffraction
need reliable standards, some entries not good, not very sensivitve, not good for organics
Prefered orientation
if crystals are platey or needle shaped, orentiation wil not be random, matchen then relies on a peak possition rather than intersites
Peak Broadening
don't get perfect lines in reality, radiation not perfectly monochromatic, heisenburg uncertainy, focussing geometry
Schere Equation
t=.9lamda/Bcostheta, B is line boundary by reference to a standard, measure in radians
B=
Bm^2-Bs^2
convert from degrees to radians
multiply by pi/180
start with larges d spacing
7 and 15 cannot be obtained
due to symmetry, certain reflections cancel each other out. Destructive interfearance
systematic absenses
Bravais Lattice
P-no restrictions
I h+k+l=2n allowed
R (face centered) hkl, all odd or all even
face centered is sparcer of reflections
so first reflection not necessarily 110
sum of scattering
is sum of all waveds diffracted from crystal
centrosymetric
if you have an atom at x y z, you also have one at -x, -y, -z
2pi (hx+ky+lz)
phase difference/geometric structure factor
Intensity proportional to FF*
F* is complex conjugate
Scattering factor depends on
Z, but electron density is the important factor
structure factor is
fourier transform of electron density, can switch back and forth using a computer program
direct method
make a sensible guess, then test and repeat as needed
Patterson Method-
uses peaks corresponding to vectors between atoms
Heavy atom method
heavy atoms dominate, easy to locate, Patterson to find others
neutron and electron diffraction
matterwave-particles rather than EM
De Broglie,
everything has wavelenth
neutrons scatter by
interaction with nucleus, interaction with spin of unpaired electrons
2 types of scattering
elastic-diffraction
inelastic-spectrometer, we concentrate on elastic scatering
isotypes detirmined easly,
wide range of d spacing, more hkl
some atoms good neutron absorber
such as CD, Gd, LI6
Some atoms
near zero scattering, can be cases where you don't want scattering
source
need reactor and accelerator, expensive to set up, not routine but more common
ISIS
being developed even further, HPRD, on the highest resolution instraments in world, HPRD2 will be the next one, currently being built
ILL in Genenoble France
Not a synchroton
IPNS Argonne Chicago
one of best in US, 20 worldwide
At many sources, neturons are produced by fission, then selected by wavelength
losses many neutrons
Alternative, H- produced at source, plused at 50 hz
electrons stripted, protons 3*10^13 for pluse, proton beam hits target, each proton-25 neturons
electrongs move, creating a dipole
inducing opposite dipole in adjacent atom, dipole dipole puls together
Ti almost always octrahedral
SI almost alwasy tetrahedtral
Ionic radii increase
with CN
Ionic radii increse
going down a group (more electron shellss added)
Anions bigger than
cations
Neutrons possess of magnetic
dipole moment
4 types of magneticm
para, ferro, anti ferro, ferri
Paramagneticm
distorted
Ferromagneticim
aligned
Antiferomagnet
opposed in ordered way, net mag zero
Ferrimagnetion
inequally opposed, net mag not zero
Why solids
most elements solid at room temperature, atoms in fixed position
classical x rays
interact with electrons in atom, caustng them to oscillate with x ray beam
Compton Scattering
results in loss of energy, classically, no frequency shift
acceleration in a circle
by magnet, large spectural range, focused and intense x rays produced
booster and synchoront
ring of electromagnets, high count rates, wavlength variable, sharp peaks, incident beam is usally monochormatic and parallel
synchroton diffraction uses
high resolution, x ray power diffraction, resonate x ray power diffraction, sample environment, surface xrd, small cystals
photoelectron ejected with energy equal to that of the incoming photons-minus binding energy
what the heck does that mean?
symetry element
symmetry axis
many inorganic structures may be described as
space filling polyhedra, or tetrahedrah or octahedrah
CN 3-D
12, both types
cations are smaller
and hense fill the intersitial sites
set volume in terms of A and R,
and solve for R
CsCl
CN=8
NaCl, NiAs
CN=6
wurtzite
ZnS sphalerite
CN = 4
Ion radii for given element increase with CN
Ion radii for given element decrease with increasing oxidation state/positive charge
Ion radii for given element increase with increasing CN and with decreasing oxidation state
yep
Solids are
Powder
Single crystal
Glass/amorphous
Polymer
Inorganic/Organic
Composite material
what scale are we interested in?
What scale are we interested in?
Bulk/Macro – overall structure
Micro (microstructure) – grains, defects
Nano – crystal structure
Diffraction
to find atom level structures
Laue, Bragg and Bragg
responsible for advances in XRD
closer the slits
further diffraction lines
With X-rays, the interaction with matter is very weak – most pass straight through
Therefore we need many (100-1000s) of waves
Laue's Equation
These work well and describe the interactions
Basic idea is still the constructive interference which occurs at an integer no. of wavelengths
However, not routinely used
If we draw the Bragg construction in the same way as the optical grating, we can clearly see that the diffracted angle is 2. The plane of “reflection” bisects this angle.
Thus we measure 2 in the experiment – next section…
X-rays - electromagnetic waves
So X-ray photon has E = hv
X-ray wavelengths vary from .01 - 10Å; those used in crystallography have frequencies 2 - 6 x 1018 Hz
use Kev
so you get Anstroms out
2 things happen with X ray emission
Electrons stopped by target; kinetic energy converted to X-rays
Incident electrons displace inner shell electrons, intershell electron transitions from outer shell to inner shell vacancy
x ray spectrum
mixture of line and not
2p (L) - 1s (K), known as the Kalpha line
3p (M) - 1s (K), known as the Kbeta line
sample can be
solid or powder
X ray assumptions
First assumption: X-rays elastically scattered by electrons.
Second assumption: Spherical, discrete atoms
More electrons means more scattering ( Z)
Scattering per electron adds together, so helium scatters twice as strongly as H
We define an atomic (X-ray) scattering factor, fj, which depends on:
the number of electrons in the atom (Z)
the angle of scattering
f varies as a function of angle , usually quoted as a function of (sin )/
The more diffuse the electron cloud, the more rapid the reduction in the scattering function with scattering angle.
theta = 0, f is equal to the total number of electrons in the atom, so
ftheta=0 = Z, but ions have the same number of electrons,But as  increases, Cl- has smaller f as it has a more diffuse electron cloud
Changes d-spacing and atoms within the planes
So we need to either (a) rotate the crystal or (b) have lots of crystals at different orientations simultaneously
you must
Laue method: Each spot corresponds to a different crystal plane
USES:
alignment of single crystal
info on unit cell
info on imperfections, defects in crystal
4-circle Method
Crystal can be oriented so that intensities for any (hkl) value can be measured
area detector
area detector which removes one circle.
uses of XRD
Unit cell determination
Crystal structure determination (primary method)
Powder Diffraction
By “powder”, we mean polycrystalline, so equally we can use a piece of metal, bone, etc.
We assume that the crystals are randomly oriented so that there are always some crystals oriented to satisfy the Bragg condition for any set of planes
Debye-Scherrer Camera
no longer used
Single crystal is a primary technique for structure determination
Powder diffraction relies on a random orientation of (small) crystallites
XRD
fingerprinting
ICDD
(International Centre for Diffraction Data)
Remember: we rely on a random orientation of crystallites.
When crystals are platey or needle-shaped (acicular) they will pack in a non-random fashion, preferentially exposing some planes to the incident radiation.
Intensity mismatch –
due to using single crystal
Even if two structures are the same (and they are chemically similar) differences can be observed:
Peak positions (unit cell changes) and relative intensities (atoms)
In an X-ray diffraction pattern, peak width depends on
the instrument
radiation not pure monochromatic
Heisenberg uncertainty principle
focussing geometry

the sample…
- a crystalline substance gives rise to sharp lines, whereas a truly amorphous material gives a broad “hump”.
If crystal size < 0.2 m, then peak broadening occurs
At <50nm, becomes significant.
At slightly higher  than the Bragg angle, each plane gives a “lag” in the diffracted beam.
For many planes, these end up cancelling out and thus the net diffraction is zero.

In small crystals, there are relatively fewer planes, so there is a “remanent” diffraction
Particle size determinaton
An estimate, rather than an absolute value - also will be dominated by smallest particles.
Good for indication of trends.
A useful complement to other measurements such as surface area, electron microscopy etc.
Amorphous / micro-crystalline?
It can be difficult to distinguish between an amorphous material and a crystalline sample with very small particle size.
BUT the idea of such a small size “crystal” being crystalline doesn’t make sense!
5nm = 50Å = e.g. 10 unit cells
Is this sufficient for long range order??
if you heat a sample up
you can change unit cell parameters
Structure refinement –
the Rietveld method
Here there was a similarity between the powder pattern of this phase and an existing one – also chemical composition similar.
Caveat Indexer
Other symmetry elements can cause additional systematic absences in, e.g. (h00), (hk0) reflections.
Thus even for cubic symmetry indexing is not a trivial task
Have to beware of preferred orientation (see previous)
Often a major task requiring trial and error computer packages
Much easier with single crystal data – but still needs computer power!
This is obviously wavelength dependent
Hence in principle using a smaller wavelength will access higher hkl values
Indexing a powder pattern means correctly assigning the Miller index (hkl) to the peak in the pattern.
If we know the unit cell parameters, then it is easy to do this, even by hand.
Due to symmetry, certain reflections cancel each other out.
These are non-random – hence “systematic absences”
For each Bravais lattice, there are thus rules for allowed reflections:
So a plot of (h2 +k2 + l2) against sin  has slope 2a/
yep
It’s a fundamental equation in crystallography.
structure factor equation
Structure factor equation
Builds on concepts we have encountered already:
Miller index
fj  Z
Unit cells
Positions of atoms (x,y,z)
Symmetry
(Wave equations)
What makes a diffraction pattern?
Positions of peaks/spots
entirely due to size and shape of unit cell a,b,c, ,, which gives d ( 2)
Intensities of peaks
following section: why all different?
Sample, instrumental factors
Intensities depend on…
scattering power of atoms ( Z)
position of atoms (x,y,z)
vibrations of atoms - “temperature” factor B
Polarisation factor (function of sin /) (see previous)
Lorentz factor (geometry)
absorption
extinction
preferred orientation (powders)
multiplicities (i.e. 100=010=001 etc)
Scattering
From before: “the scattering from the plane will reflect which atoms are in the plane”. The scattering is the sum of all waves diffracted from the crystal.
Atomic scattering factor
Again, from before:
The atomic scattering factor, fj, depends on:
the number of electrons in the atom (Z)
the angle of scattering
f varies as a function of angle , usually quoted as a function of (sin )/
f=0 = Z
Summing the waves
The overall scattering intensity depends on
Atom types (as above) - “electron density”
Their position relative to one another.
This is the sum of the (cos) waves, where:
- fj is the atomic scattering factor for atom j
- hkl are the Miller indices
- xj, yj, zj are the atomic (fractional) coordinates
The expression 2(hx+ky+lz) = 
phase difference
Thus we get:
I  fj2
as the cos (or exp) terms cancel out.
So something quite complex becomes simple, but….
measure intensity which is proportional to FF*
Thus, the odd reflections are systematically absent
Generally true for all body centred structures
The phase problem
We can calculate the diffraction pattern (i.e. all Fhkl) from the structure using the structure factor equation
Each Fhkl depends on (hkl) (x,y,z) and fj
fj depends primarily on Z, the number of electrons (or electron density) of atom j
The structure factor is thus related to the electron density, so if we can measure the structure factor, we can tell where the atoms are.
We measure intensity I = F.F*
so we know amplitude of F.….but phases lost.
Several methods to help – complex but briefly
Direct methods
(Nobel Prize 1985 - Hauptmann and Karle)
Statistical trial and error method. Fhkl’s are interdependent so by “guessing” a few we can extrapolate
Patterson Methods
Uses an adapted electron density map where peaks correspond to vectors between atoms - peak height  Z1Z2
Heavy Atom Methods
High Z atoms will dominate the electron density - “easy” to locate
Use Patterson vectors to find other atoms.
Limitations of X-ray Structure determination
gives average structure
light atoms are difficult to detect (f  Z) e.g. Li, H
difficult to distinguish atoms of similar Z (e.g. Al, Si)
need to grow single crystals ~ 0.5mm
time for data collection and analysis (?)

new instruments mean smaller crystals, shorter collection times! So in fact – data can pile up….
De Broglie
Extended the idea of wave-particle duality
1923 – particles can be wavelike
Idea that everything has a wavelength!
E = mc2 = (mc)c but momentum, p=mv
and for a photon v=c
E = pc = p f  but E=hf (Planck/Einstein)
hf = p f 
Neutron scattering
Neutron can be scattered by atoms by:
interaction with nucleus
interaction with spin of unpaired electrons - magnetic interaction, magnetic scattering. This happens because the neutron has a magnetic moment. (later)
More Neutron Scattering
Also the interaction can be:
elastic (diffractometer) structural studies
inelastic (spectrometer)
loss of energy on scattering gives information on phonon dispersion (effect of vibrations in lattice) and stretching of bonds
Scattering from neutrons
X-rays: fj  Z - can be calculated
Neutrons: small dependence of fj on Z but major part Z independent. fj must be determined experimentally
Good points to neutron scattering
Can detect light atoms
Can often distinguish between adjacent atoms
Can distinguish between isotopes
Can accurately find atoms in presence of very high Z atoms
Covers a wide range of d-spacings - more hkl - BUT

excellent complimentary to XRD
bad points to neutron scattering
Some atoms/isotopes good neutron absorbers (e.g. Cd, Gd (Gadolinium), 6Li (so use 7Li)
V has very low, ~0 scattering (but..)
need neutron source
VERY expensive (~£10,000 per DAY!)
Clifford Schull
for the development of the neutron diffraction technique
Bertram Brockhouse
"for the development of neutron spectroscopy
IPNS, Argonne, Chicago IL
Intense Pulsed Neutron Source
Other neutron sources are also available…
Los Alamos Neutron Science Center (New Mexico, US)
Lucas Heights (Sydney Australia)
Oak Ridge (Tennessee, USA)
KENS (Tsukuba, Japan)
Chalk River (Ontario, Canada)
Risø (Roskilde, Denmark)
The experiment
At many sources (e.g. ILL at Grenoble) neutrons are produced by fission in a nuclear reactor and then selected by wavelength - but with neutrons there are no “characteristic” wavelengths:
..so by selecting a wavelength we lose neutrons and lose intensity
Alternative
UK neutron source at Rutherford Appleton Laboratory uses “time of flight” neutron diffraction
Electrons stripped
 protons (~3 x 1013)
H- produced at source (pulsed)
Time-of-flight neutron diffraction
We are measuring d, so two variables,  and 
In lab X-ray powder diffraction,  is constant,  variable
In time-of-flight (t.o.f),  is constant,  variable
This takes advantage of the full “white” spectrum
Errors
The biggest error in the experiment is where the neutrons originate
This gives an error in the flight path, L
typical value ~5cm
Hence as L increases, error in d is reduced - resolution of the instrument is improved
e.g. instrument at 10m compared to instrument at 100m
100m = HRPD, currently highest resolution in the world
Magnetic Diffraction
Neutrons possess a magnetic dipole moment
Heavy equipment
Furnaces, cryostats, pressure cells, magnets, humidity chambers, etc.
Electron Diffraction
Similar principle – matter waves, but me = 9.109 x 10-31 kg
Also applied “accelerating potential” V such that:
G. P. Thomson
Experiments performed at Marischal College in the late 1920's
(also Lester Werner and Clinton Davisson at Bell labs in New York)
Picture of electron diffraction taken by Thomson
Bragg’s Law redux
Since l is very small, q is also very small, so we can rewrite Bragg’s law as:

l = 2d q
As previously, we can derive:
d ~ L/D
Uses (of what)
Can be used to look at individual crystallites: must be thin (why?)
Useful to help determine unit cell parameters; need many orientations (see animation here)
Shape of spots: streaking can give information on crystal size and shape
Can identify packing defects (see later)
Added extra: EDX for elemental analysis:
Electrons knock out inner shell electrons
Characteristic X-rays emitted as outer shell electron drops down to fill gap
Both neutron and electron diffraction are very useful complementary techniques to X-ray diffraction
Neutron diffraction has a number of advantages over X-ray diffraction – but cost is a major disadvantage!
Both fission and spallation sources are used
Magnetic diffraction is possible due to the dipole present with neutrons
Electrons can be focussed, allowing high resolution imaging as well as diffraction
Information on defects (see later) and unit cells
Classical vs quantum
In the classical treatment, X-rays interact with electrons in an atom, causing them to oscillate with the X-ray beam.
The electron then acts as a source of an electric field with the same frequency
 Electrons scatter X-rays with no frequency shift
Compton Scattering
Some radiation is also scattered, resulting in a loss of energy [and hence, E=h, shorter frequency and, c=  , longer wavelength].
The change in frequency/wavelength depends on the angle of scattering.
This effect is known as Compton scattering
It is a quantum effect - remember classically there should be no frequency shift.
Moseley’s Law
Moseley corrected anomalies:

Also identified a gap at Z=43 (Tc)
Absorption
X-ray photons absorbed when E is slightly greater than that required to cause a transition
- i.e. wavelength slightly shorter than K

So, as well as characteristic emission spectra, elements have characteristic absorption wavelengths
Uses of absorption
We want to choose an element which absorbs K [and high energy/low  white radiation] but transmits K
e.g. Ni K absorption edge = 1.45 Å
As a general rule use an element whose Z is one or two less than that of the emitting atom
Monochromator
Choose a crystal (quartz, germanium etc.) with a strong reflection from one set of lattice planes, then orient the crystal at the Bragg angle for K1
Synchrotron X-rays
When charged particles are accelerated in an external magnetic field (according to Lorentz force), they will emit radiation (and lose energy)
Synchrotron X-rays
Acceleration in a circle…

Electrons are kept in a narrow path by magnets
Emit e.m. radiation ahead
Large spectral range
Very focussed and intense X-rays produced (GeV)

(also applications in particle, medical physics amongst other things)
SchematicSynchrotron X-rays
electron gun (2) linear accelerator
(3) booster synchrotron (4) storage ring
(5) beamlines (6) experiment stations.
Inside the synchrotron
Electrons emitted from cathode ~1100° C.
Accelerated by high-voltage alternating electric fields in linac. Accelerates the electrons to 450 MeV - relativistic

Electrons injected into booster synchrotron (a ring of electromagnets); accelerated to 7 GeV
7 GeV electrons injected into the 1 km storage ring
Circle of > 1,000 electromagnets etc.
Synchrotron vs lab data
Much higher count rates  signal to noise better
Wavelengths are variable.
Incident beam is usually monochromatic and parallel.
Very sharp peaks (smaller instrumental contribution) – FWHM can be 10 times narrower – better resolution
Synchrotron Diffraction - Uses
High resolution X-ray powder diffraction
“Resonant” X-ray powder diffraction (can select wavelength)
Analysis of strain (see later)
Sample environment (as with neutrons)
Surface XRD
Diffraction on very small single crystals (0.0001 mm3)
Back to absorption
Photoelectron ejected with energy equal to that of the incoming photon minus the binding energy.
Characteristic of element.
The ejected photoelectron then interacts with the surrounding atoms
Absorption energies
Energies of K edges  Z2
Elements with Z>18 have either a K or L edge between 3 and 35 keV
Interference effects
The ejected photoelectron then interacts with the surrounding atoms
This gives information on the local environment round a particular element within the crystal structure
XAS
X-ray Absorption spectroscopy complements diffraction

Diffraction gives you information on average 3d structure of crystalline solids

XAS gives you localised environment in solids (including glasses), liquids, gases.
Info on bonds, coordination, valence
XANES/EXAFS
X-ray Absorption – near edge structure
Extended X-ray Absorption – Fine Structure
Summary
The interaction of X-rays with matter produces a small wavelength shift (Compton scattering)
The wavelength of X-rays varies as a function of atomic number - Moseley’s law
Filters can be used to eliminate K radiation; monochromators are used to select K1 radiation.
Synchrotrons can produce high intensity beams of X-rays suitable for structural studies
Absorption can be exploited to give localised information on elements within a crystal structure.
Close Packing
Each atom excludes others from the space it occupies
Attraction?
Electrons are moving so that, at some instant, distribution is uneven
Positively (electron-deficient) and negatively (electron-rich) charged regions  electrical dipole
Dipole induces an opposing dipole in neighbouring atom  attraction
Attractive force is known as:
van der Waals interaction
London interaction
induced dipole-induced dipole interaction
yep
The total potential energy for two atoms a distance, r, apart can be written, sum of forces U[] equation
This is called the Lennard-Jones (12,6) potential function
First term is repulsive, second term is attractive.
We want to find a minimum - so differentiate w.r.t. r
2^1/6=r
This is the van der Waals radius, the distance between the atoms that minimises their energy
subsitute van dervals r into equation
U min = - crazy E
Ionic radius
Previously we looked at trends in ionic radius of atoms
The “absolute” value is important, but relative values also give useful information
Can give information on likely coordination (see following sections) and also viability of a structure (e.g. “Goldschmidt tolerance factor” for perovskites
Radius ratio rules
Rationalisation for octahedral coordination: R= radius of large ion, r=radius of small ion
Radius ratio rules
Rationalisation for 8-fold coordination
Unit cell edge a = 2R
Atoms touch along diagonal (if small ion fits perfectly into space) so a3 = 2(R+r)
Divide: 3 = (R+r)/R
Multiply out 3R = R+r
R(3 -1) = r
r/R = 3 -1 = 0.732
Other ways of classifying structures
1) Structure Field Maps
e.g. for AxByOz compounds, plot radius of A against radius of B and note trends of structure as rA and rB change.

2) Mooser-Pearson plots
Focuses on the covalent character of bonds. Plot of difference in electronegativity versus average principal quantum number of atoms involved.
at higher temperature
paramagetim
high penetration and flux of neturons
so used heavy instruments
if ration < square root of two+
then CN is less than 6
pressure
can reduce bond length