__________________________________________________________ mario bieringer mario bieringer...
TRANSCRIPT
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 11 June 16 June 16thth, 2009, 2009
Neutron Powder Diffraction
Mario BieringerDepartment of Chemistry
University of Manitoba
presented at the
10th Canadian Neutron Summer School
June 15 – 18, 2009Chalk River, Ontario
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 22 June 16 June 16thth, 2009, 2009
Applications of Powder Diffraction
chemistry
physics
engineering
life sciences
biochemistry
materials science
geological sciences
archeology
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 33 June 16 June 16thth, 2009, 2009
Applications of Powder Diffractiondiffraction = elastic scattering momentum transfer at constant energy, i.e. incident = diffracted
Why do we care about diffraction experiments:
• identification of materials/phases
• determination of structural details, i.e. local environments within an extended structure
• evaluation of order and disorder in structures
• phase transitions (structural distortions or reconstruction)
• chemical reactions
• relate structure and properties
40 60 80 1000
100
200
300
400
500
600Si powder neutron diffraction patternC2 Chalk River = 1.329 Å
Inte
nsi
ty (
cou
nts
)
2 (0)
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 44 June 16 June 16thth, 2009, 2009
Routine Powder X-ray Diffraction:
• Powder X-ray diffractogram
matched with the PDF database
• links to crystallographic
data if available (i.e structure
details from ICSD)
• semi-quantitative analysis
D
S
A
M
Position [°2Theta]
20 30 40 50 60
Counts
0
2500
10000
group-1_1
Visible Ref. Code Chemical Formula
red 01-073-2141 La2 O3
blue 00-005-0378 Ba C O3
green 01-089-5898 Cu O
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 55 June 16 June 16thth, 2009, 2009
Routine Powder X-ray Diffraction:
Preferred Orientationof flat sample mounts:
D
S
A
M
a
c
b
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 66 June 16 June 16thth, 2009, 2009
2(0)
Inte
nsit
y (
a.u
.)
T (
0 C)
30.0
37.025
1000
In-situ Powder X-ray Diffraction:
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 77 June 16 June 16thth, 2009, 2009
What is a Powder?powder = polycrystalline solidlarge number of crystallites of m length scale
ideal powders (for diffraction) show random orientation of crystallites
orientational average of single crystals
• large number of preparative methods available.
• powders can be prepared in large quantities (g, kg, etc.)
• fast synthesis
• real world materials are often polycrystalline
• in reality powders are often multiphasic
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 88 June 16 June 16thth, 2009, 2009
Description of Crystallographic StructuresUnit Cell: Smallest repeating unit capable of describing the entire crystal by means of three non-parallel translation vectors.
paralleliped
The 7 Crystal Systems
System u.c. symmetry unit cell parameters
cubic m-3m a = b = c = = = 90˚
hexagonal 6/mmm a = b ≠ c = = 90˚ = 120˚
trigonal* 3/mmm a = b ≠ c = = 90˚ = 120˚
tetragonal 4/mmm a = b ≠ c = = = 90˚
orthorhombic mmm a ≠ b ≠ c = = = 90˚
monoclinic 2/m a ≠ b ≠ c = = 90˚ ≠ 90˚
triclinic -1 a ≠ b ≠ c ≠ ≠ ≠ 90˚
* also described as rhombohedral: a = b = c = = ≠ 90˚
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 99 June 16 June 16thth, 2009, 2009
Description of Crystallographic StructuresBravais Lattices:Centering conditions can be described with translation vectors:
Lattice Symbol translations lattice points
Primitive P +(0, 0, 0) 1
Body centered I +(½, ½, ½) 2
Base centered A +(0, ½, ½) 2
B +(½,0, ½) 2
C +(½, ½, 0) 2
Face centered F +(0, ½, ½), +(½, ½, 0), +(½,0, ½) 4
A total of 14 Bravais Lattices exist (see next page for illustration)
cubic: P, I, F orthorhombic: P, I, F, (A,B,C) hexagonal: P monoclinic: P, C trigonal: P triclinic: P tetragonal: P, I
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1010 June 16 June 16thth, 2009, 2009
figure taken from: www.chem.ox.ac.uk
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1111 June 16 June 16thth, 2009, 2009
Diffraction Peaks due to Periodicity:Due to the inherent crystal periodicity families of parallel virtual planes can be constructed. The scattering probe diffracts off those planes and generates a pattern that is characteristic of the spacing of the virtual planes and the composition of the unit cell. Virtual planes are identified by the Miller indices (h,k,l). The d-spacings, dhkl, (i.e. the perpendicular distance, between planes) can be determined with Braggs law:
= 2dhkl sin
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1212 June 16 June 16thth, 2009, 2009
(001)
Diffraction Peaks due to Periodicity:K2NiF4 structure: tetragonal phase
c
a
b
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1313 June 16 June 16thth, 2009, 2009
18 21 24 27 30 33 36
triclinic
tetragonal
monoclinic
orthorhombic
hexagonal
cubic
2 (0)
Powder Diffraction and Symmetry:Predict Bragg positions for primitive cells with V = 64 Å3 ( = 1.54 Å).
The higher the symmetry and
the smaller the cell volume the
smaller the number of diffraction
peaks.
peak multiplicities decrease from cubic to triclinic:
e.g. cubic d(100) = d(-100) = d(010) = d(0-10) = d(001) = d(00-1)
orthorhombic d(100) = d(-100) ≠ d(010) = d(0-10) ≠ d(001) = d(00-1)
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1414 June 16 June 16thth, 2009, 2009
Description of Crystallographic StructuresFractional coordinates:
Note: use the crystal system as the coordinate systemx = fraction along a axisy = fraction along b axisz = fraction along c axis
Symmetry Elements:
rotation axes: 1, 2, 3, 4, 6 foldinversion rotation axes: -1, -2, -3, -4, -6 foldmirror planes: mscrew axes (helices): 21, 31, 32, 41, 42, 43, 61, 62, 63, 64, 65
glide planes: a, b, c, n, d
Absent reflections due to translations!
230 Space Groups: (International Tables for Crystallography: Vol. A)
e.g. I41amd (number 141) tetragonal system, body centered 41 screw axis, a glide, mirror, d glide
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1515 June 16 June 16thth, 2009, 2009
Description of Crystallographic StructuresBaLaMnO4 (K2NiF4 structure type):
Space group I4/mmm (# 139)
Diffraction pattern:
No h+k+l = odd reflections
Body centered e (½,½,½) translation)
radii =Z
Ba(56) = 0,0,0.35
La(57)) = 0,0,0.35
Mn (25) = 0,0,0
O1(8) = 0,½,0
O2(8) = 0,0,1.4
0 0
2
0 1
1
0 0
4
0 1
31
1 0
1 1
2
0 0
60
1 5
1 1
4
0 2
00
2 2
1 2
11
1 6
0 1
70
2 4
0 0
81
2 3
0 10 20 30 40 50 60
BaLaMnO_4Lambda: 1.54178 Magnif: 1.0 FWHM: 0.200Space grp: I 4/m m m Direct cell: 4.0000 4.0000 13.6568 90.00 90.00 90.00
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1616 June 16 June 16thth, 2009, 2009
Diffraction Peak Intensities:
Structure Factor:
X-ray case:
Neutron case:
Powder Peak Intensities:
j
jjjjjhkl BlzkyhxifF 22)( /sinexp2exp
j
jjjjjhkl BlzkyhxibF 22)( /sinexp2exp
2
)()()()( hklhklhklhkl FPALpsI
2
)()( hklhkl FI
F(hkl) = structure factorfj = X-ray form factorb = neutron scatt. lengthh,k,l = Miller indicesxj, yj, zj = atomic coordinates of atom jBj = thermal parameter = diffraction angle = wavelength over entire unit cellI(hkl) = intensity
Correction factors:
s = scale factorL = Lorentz-polarization p = multiplicity A = absorption correction P = preferred orientation
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1717 June 16 June 16thth, 2009, 2009
0 10 20 30 40 50 60 70 80 90
-5
0
5
10
15
20
25
30
35
40
neutrons, b
X-rays, f sin/=0Å-1 sin/=0.5Å-1
scat
terin
g am
plitu
de (
10 -
13 c
m)
atomic number Z
Diffraction Peak Intensities:Scattering lengths X-ray form factor, f:
Temperature factor, Bj:
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1818 June 16 June 16thth, 2009, 2009
Description of Crystallographic StructuresBaLaMnO4 (K2NiF4 structure type):
b atom=x,y,z Z
5.07fm Ba=0,0,0.35 56e
8.24fm La=0,0,0.35 57e
-3.73fm Mn=0,0,0 25e
5.80fm O1=0,½,0 8e
5.80fm O2=0,0,1.4 8e
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 1919 June 16 June 16thth, 2009, 2009
Peak Widthscoherence length domain sizes crystallite sizes particle sizes
Scherrer equation:
= wavelength
B = integral breadth
= diffraction angle
The broader the peaks
the smaller the domains.
4.8 4.9 5.0 5.1 5.2 5.3 5.4 5.5 5.6-10
0
10
20
30
40
50
60
70
80
90
4.80 4.85 4.90 4.95 5.00 5.05 5.10 5.15 5.20
0
20
40
60
80
area = 5 a.u.
B
Inte
nsity
(a.
u.)
2 (0)
Inte
nsi
ty (
a.u
.)
2 (0)
cos9.0
BD
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2020 June 16 June 16thth, 2009, 2009
Diffraction from Randomly Oriented Crystals:
reciprocal lattice (diffraction pattern)
direct lattice (crystal structure)
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2121 June 16 June 16thth, 2009, 2009
Diffraction from Randomly Oriented Crystals:
1 single crystal
very large number of microcrystals
few crystals
Debye-Scherrer Camera
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2222 June 16 June 16thth, 2009, 2009
Single Crystal versus Powder Diffraction:
Single crystal diffraction:
• Use 3-dimensional reciprocal space: a*, b* and c* axes
• Use integrated intensities.
unambiguous peak assignment
Powder diffraction:
• Use a large assembly of microcrystals and record an average diffraction pattern in 1-dimension.
• Use profile points.
ambiguous peak assignment
Reminder: 1/d = 2 sin/
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2323 June 16 June 16thth, 2009, 2009
(110)
(101)(100)
(010) 1/dIn
tens
ity
Powder diffraction:
• Information gets buried in powder average.
• Try to extract peak intensities or fit the entire profile.
Rietveld Method
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2424 June 16 June 16thth, 2009, 2009
Powder X-ray vs. Powder Neutron Diffraction
0 10 20 30 40 50 60 70 80 90 100 110 120
Powder Neutron Diffraction ( = 1.54059A)
Powder X-ray Diffraction ( = 1.54059A)
2 (0)
simulations of Pr2Ta2O7Cl2 powder patterns
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2525 June 16 June 16thth, 2009, 2009
Simplified Powder Diffractogram
2 (˚) * crystal system
* unit cell dimensions
* space group
Intensity * atomic/ionic positions
* temperature factors
* order/disorder
FWHM * domain sizes
* habit
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2626 June 16 June 16thth, 2009, 2009
X-ray vs Neutron Powder Diffraction?
XRD NPD
phase I.D. YES NO
indexing YES YES
space group YES YES
structure refinement YES YES
light elements NO YES
neighbouring elements NO YES
structure solution YES YES
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2727 June 16 June 16thth, 2009, 2009
When to Use Neutrons:Ideally: always (most structure determinations and refinements benefit
from independent measurements (X-ray + neutron))
In particular:
• light and heavy elements present (e.g. oxides, fluoride, hydrides (deuterides) of heavy metals)
• neighbouring elements: e.g. Al & Si, Fe & Co, Yb & Lu, Ti & V, etc.
• multiple site occupancies: e.g. disordered structures
• interest in true bulk properties (i.e averaging over large samples)
• complex experimental set ups: chemical reactions, high temperatures, high pressures, low temperatures, magnetic fields, electrochemical cells, chemical/structural processes etc.
• magnetic samples
• etc.
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2828 June 16 June 16thth, 2009, 2009
Are Neutrons going to Answer Your Questions?•look up neutron scattering lengths and cross sections:
http://www.ncnr.nist.gov/resources/n-lengths/
Neutron News, Vol. 3, No. 3, 1992, pp. 29-37
Neutron scattering lengths and cross sections
Isotope conc Coh b Inc b Coh xs Inc xs Scatt xs Abs xs
O --- 5.803 --- 4.232 0.0008 4.232 0.00019
16O 99.762 5.803 0 4.232 0 4.232 0.0001
17O 0.038 5.78 0.18 4.2 0.004 4.2 0.236
18O 0.2 5.84 0 4.29 0 4.29 0.00016
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 2929 June 16 June 16thth, 2009, 2009
Are Neutrons going to Answer Your Questions?LaFeAs(O1−xFx) LiCoO2, LiNi1-xCoxO2, LiMn2O4
b(La=57) = 8.24 fm b(Li=3) = -1.90 fm
b(Fe=26) = 6.58 fm b(Co=27) = 2.49 fm
b(As=33) = 9.45 fm b(Ni=28) = 10.3 fm
b(O=8) = 5.803 fm b(Mn=25) = -3.73 fm
b(F=9) = 5.654 fm b(O=8) = 5.803 fm
BiFeO3, BaTiO3, LnMnO3 La0.9Ba0.1Ga0.8Mg0.2O2.8
b(Bi=83) = 8.532 fm b(La=57) = 8.24 fm
b(Fe 26) = 6.58 fm b(Ba=56) = 5.07 fm
b(O=8) = 5.803 fm b(Ga=31) = 7.288 fm
b(Mg=12) = 5.375 fm
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3030 June 16 June 16thth, 2009, 2009
Two Neutron Powder Diffraction Methods1. Continuous Wavelength (Reactor Sources):
• single (selectable) wavelength
• continuous neutron flux
• position sensitive detectors, record neutron rate as a function of diffraction angle
• Bragg’s law: = 2d sin
• d/d depends on: - monochromator - take-off angle, - monochromator mosaicity - and sample size
example: C2
M
sample
sample environment
detector wires
collimator
http://neutron.nrc-cnrc.gc.ca/c2gen.html
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3131 June 16 June 16thth, 2009, 2009
160-176 degbackscattering
detector
28 - 32 degdetector
87-93 deg detector
guide tube 100m beam Stop
sample
87-93deg detector
Two Neutron Powder Diffraction Methods2. Time of Flight Method (Spallation Sources):
example: HRPD (ISIS, U.K.)
2 choppers close to the target (6m and 9m)select neutron pulses
http://www.isis.rl.ac.uk/crystallography/HRPD/index.htm
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3232 June 16 June 16thth, 2009, 2009
Two Neutron Powder Diffraction Methods2. Time of Flight Method (Spallation Sources):
• white radiation (including epithermal fraction)
• pulsed neutron source (50 to 60 Hz)
• very high neutron flux during neutron burst
• multitude of time of flight detectors, record neutron rate vs. time
• Bragg’s law: de Broglie:
mn = neutron mass, vn = neutron velocity, t = flight time, L = flight distance, d = detector angle
• resolution: d/d depends on total flight path, L, and detector angle (d)
• use time focusing, large scattering volumes don’t degrade the resolution
th
Lm
vh
m n
n
n sin2d
dhklhkl dLt sin57.505 )()( )()( hklhkl dt
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3333 June 16 June 16thth, 2009, 2009
Data Comparison1. Continuous Wavelength (Chalk River – C2 (Pr2Ta2O7Cl2) ): :
10 20 30 40 50 60 70 80
0
2500
5000
7500
10000
12500
15000 Pr2Ta
2O
7Cl
2
Low Temperature Powder Neutron DiffractionC2 = 2.37A
Inte
nsi
ty (
a.u
.)
2 (0)
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3434 June 16 June 16thth, 2009, 2009
Data Comparison2. Time of Flight Method (IPNS – SEPD (Pr2Ta2O7Cl2) ):
13000 14000 15000 16000 170000
100
200
300
400
500IPNS - SEPD BANK #1 (144.850)
Inte
nsi
ty (
a.u
.)
TOF (s)
10000 11000 12000 130000
100
200
300
400
500
IPNS - SEPD BANK #2 (900)
Inte
nsi
ty (
a.u
.)
TOF (s)
5000 5500 6000 6500 7000100
150
200
250
300
350
400
450
IPNS - SEPD BANK #3 (440)
Inte
nsi
ty (
a.u
.)TOF (s)
0 5000 10000 15000 20000 25000 30000
0
50
100
150
200
250
300
350
400
IPNS - SEPD
BANK #3 (440)Inte
nsi
ty (
a.u
.)
TOF (s)0 5000 10000 15000 20000 25000 30000
0
100
200
300
400
500
600
IPNS - SEPD
BANK #2 (900)Inte
nsi
ty (
a.u
.)
TOF (s)5000 10000 15000 20000 25000 30000
0
200
400
600
800
1000
6 9 0 0 7 0 0 0 7 1 0 0 7 2 0 0 7 3 0 0 7 4 0 0 7 5 0 0 7 6 0 0 7 7 0 0 7 8 0 03 0 0
4 0 0
5 0 0
6 0 0
7 0 0
8 0 0
Inte
ns
ity
(a
.u.)
T O F (s )
IPNS - SEPD
BANK #1 (144.850)Inte
nsi
ty (
a.u
.)
TOF (s)
d-range: 0.33-4.0Å d-range: 0.45-5.4Å d-range: 0.85-10.2Å
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3535 June 16 June 16thth, 2009, 2009
Powder Data Analysis1)Record Powder Diffractogram (neutron and/or X-ray)
2)Identify the phase(s) (X-ray database)
3)Index phase (X-ray or neutron), i.e. find unit cell (i.e. crystal system)
4)Identify space group (X-ray or neutron)
5)If a structural model is available (isostructural compound known) proceed with Rietveld refinement
6)If no structural model is known proceed with ab-initio structure solution
7)Consider X-ray and neutron combined analysis
8)Consider different wavelengths
9)Consider different temperatures
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3636 June 16 June 16thth, 2009, 2009
Rietveld MethodProfile Fitting Method:
1. use a crystallographic model and compute the corresponding powder diffraction pattern
2. compare simullation with experimental diffraction data
3. minimize the difference between experimental and calculated diffraction pattern in a least squares refinement by varying a number of parameters:
minimize:
wi = 1/yi yi = observed intensity yci = calculated intensity
s = scale factor, L(hkl) = Lorentz, polarization and multipicity factors(2i-2(hkl)) = reflection profile function, P(hkl) = preferred orientation function, A = absorption factor, F(hkl) = structure factor, ybi = background intensity
j
ciiiy yywS 2
j
bihklciiihklhklci yAPFLsy )(2
)()( 22
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3737 June 16 June 16thth, 2009, 2009
Rietveld MethodRefinable Parameters:
GLOBAL PARAMETERS: FOR EACH PHASE
zero point atomic positions
instrumental profile thermal parameters
profile asymmetry site occupancies
background parameters scale factor
sample displacement lattice parameters
absorption preferred orientation
crystallite size
microstrain
magnetic vectors
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3838 June 16 June 16thth, 2009, 2009
Rietveld Method
14400 14500 14600 14700 14800 14900 15000 15100
0
300
600
Inte
nsi
ty (
a.u
.)
TOF (s)
observed calculated difference Bragg positions
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 3939 June 16 June 16thth, 2009, 2009
Rietveld MethodEvaluation of fitting quality (R-factors):
• R-pattern, Rp:
• R-weighted pattern, Rwp:
• R-Bragg factor, RB:
• R-expected, Re: Goodness of fit, S:
i
ciip y
yyR
2/1
2
2
ii
ciiiwp
yw
yywR
)'('
)()'(' )()(
obsI
calcIobsIR
i
hklhkl
B
2/1
2
iie yw
PNR
e
wp
R
RS
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4040 June 16 June 16thth, 2009, 2009
Rietveld Method
A large number of Rietveld programs are available:
To a large extent these programs have similar capabilities with individual strengths:
Rietveld Programs: GSAS
FullProf
Rietica
Rietan
BGMN
TOPAS
etc.
http://www.ccp14.ac.uk/
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4141 June 16 June 16thth, 2009, 2009
Rietveld Method
5000 10000 15000 20000 25000 30000
0
200
400
600
800
1000
5000 6000 7000 8000 9000 10000
0
200
400
600
800
Inte
nsity
(a.u
.)TOF (s)
Pr2Ta
2O
7Cl
2 (PTOC449)
Powder Neutron Diffraction
IPNS - SEPD BANK #1 (144.850)
Inte
nsi
ty (
a.u
.)
TOF (s)
observed calculated difference Bragg
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4242 June 16 June 16thth, 2009, 2009
Rietveld Method
Refinement of Pr2Ta2O7Cl2:
Parameters: Data:
varied: all atomic positions SEPD (IPNS)
anisotropic thermal parameters 3 scattering banks
unit cell parameters 11005 data points
background parameters 60 parameters varied
scale factor
peak shape parameters Results:
Rwp: 0.0448
Rp: 0.0280
Re: 0.0342
S: 1.17
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4343 June 16 June 16thth, 2009, 2009
Compare Single Crystal and Powder ResultsPr2Ta2O7Cl2: space group: I2/m
X-ray single X-tal 1 powder neutron (TOF) 2
atom x y z_________ x y z :
Pr 0.6925(1) 0 0.5270(1) 0.69114(24) 0 0.5273(4)
Ta 0.0343(0) 0 0.2361(1) 0.03451(13) 0 0.23741(24)
Cl 0.8219(3) ½ 0.3891(6) 0.82304(13) ½ 0.39002(25)
O1 0.0448(8) ½ 0.2060(18) 0.04401(18) ½ 0.21012(37)
O2 0.9190(8) 0 0.0679(16) 0.91882(16) 0 0.07140(34)
O3 0.8244(9) 0 0.7519(17) 0.82666(16) 0 0.75746(32)
O4 ½ ½ 0 ½ ½ 0
a = 14.109(1) Å a = 14.10763(22) Å
b = 3.9247(3) Å b = 3.92548(5) Å
c = 6.9051(6) Å c = 6.90610(10) Å
= 92.953(8)0 = 92.9626(14)0
1 U. Schaffrath and R. Gruhn Naturwissenschaften, 75 140 (1988) 2 P. Baudry and M. Bieringer (2003)
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4444 June 16 June 16thth, 2009, 2009
20 40 60 80 100
0
1000
2000
3000
4000 powder X-RAY diffraction pattern for Li
4MgReO
6
= 1.54059Å
Inte
nsity
(a.
u.)
2 (0)
20 40 60 80 100
0
10000
20000
30000
40000 powder NEUTRON diffraction pattern for Li
4MgReO
6
= 1.54059Å
Inte
nsity
(a.
u.)
2 (0)
N
nnnnnhkl lzkyhxifF
12exp)2(
N
nnnnnhkl lzkyhxibF
12exp
Powder X-ray vs. Neutron DiffractionLi4MgReO6:
an order-disorder study
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4545 June 16 June 16thth, 2009, 2009
neutronsb (10-12m)
X-raysZ
Li+ -1.90 3 (2)Mg2+ 5.37 12 (10)Re6+ 9.2 75 (69)O2- 5.803 8 (10)
Li4MgReO6:
Powder X-ray vs. Neutron Diffraction
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4646 June 16 June 16thth, 2009, 2009
High Temperature StudiesNeutron diffraction and IN-SITU reactions.
Preparation of microwave dielectric oxides of composition Ba3ZnTa2O9 (BZT).
3 BaCO3 + ZnO + Ta2O5 ---- Ba3ZnTa2O9 + 3 CO2
aa
a
a aa
aa
c
aa
a
aa
a
(b )(a ) (c )
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4747 June 16 June 16thth, 2009, 2009
High Temperature StudiesOnly a high flux neutron diffractometer will permit collection of diffraction patterns within one 1 minute.
GEM (ISIS, U.K.) TOF instrument with more than 6000 detectors and medium resolution (18 – 20 m flight path).
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4848 June 16 June 16thth, 2009, 2009
* =BZT
=ZnO
=Ta2O5
=BaCO3
T (0 C
)
d-spacing (Å)
* * * * *
Rhombohedral BaCO3and inter-mediate phases
BZT
Starting materials
High Temperature Studies3 BaCO3 + ZnO + Ta2O5 ---- Ba3ZnTa2O9 + CO2
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 4949 June 16 June 16thth, 2009, 2009
Low Temperature StudiesCrystal structure and magnetic long range order in Ba0.05Sr0.95LaMnO4
1 phase Rietveld refinement T=125K
phase 1: Ba0.05Sr0.95LaMnO4
crystal structure
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 5050 June 16 June 16thth, 2009, 2009
(Ba2+, Sr2+, La3+)
Mn3+
O2-
0 20 40 60 80 100 1203.780
3.782
3.784
3.786
3.788
3.790
13.15
13.16
13.17
13.18
c-ax
is (
A)
a-a
xis
(A)
T (K)
tetragonal:
I4/mmm
a = b ≠ c
Low Temperature StudiesCrystal structure refinement and unit cell evolution in Ba0.05Sr0.95LaMnO4
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Mario BieringerMario Bieringer__________________________________________________________________________
1010thth Canadian Neutron Summer School Canadian Neutron Summer School slide slide 5151 June 16 June 16thth, 2009, 2009
ResourcesR.A. Young,‘The Rietveld Method’, IUCr Monographs on Crystallography 5, Oxford University Press, New York (1993)
W.I.F. David, K. Shankland, L.B. McCusker, Ch. Baerlocher,‘Structure Determination from Powder Diffraction Data’, IUCr Monographs on Crystallography 13, Oxford University Press, New York (1993)
J. Baruchel, J.L. Hodeau, M.S. Lehmann, J.R. Regnard, C. Schlenker,‘Neutron and Synchrotron Radiation for Condensed Matter Studies’, Volume 1, 2 and 3, Springer Verlag, Berlin (1993)
G.E. Bacon, ‘Neutron Diffraction’, Claredon Press, Oxford, 3rd edition (1975)
Allen C. Larson, Robert von Dreele, ‘GSAS - General Structure Analysis System’
Juan Rodriguz-Carvajal, ‘An Introduction to the Program FULLPROF 2000’, Saclay, 2001 (ftp://ftp.cea.fr/pub/llb/divers/fullprof.2k/ )
Mark Ladd, Rex Palmer, ‘Structure Determination by X-Ray Crystallography’, Kluwer Academic, New York, 2003, 4th Edition
Vitalij K. Pecharsky, Peter Y. Zavalij, ‘Fundamentals of Powder Diffraction and Structural Characterization of Materials’, Springer, 2005
G.L. Squires, ‘Introduction to the theory of thermal neutron scattering’, Dover Publications, New York, 1978
Georg Will, ‘Powder Diffraction: The Rietveld Method and the Two-Stage Method’, Springer, Heidelberg, 2006
Abraham Clearfield, Joseph Reibenspies, Nattamai Bhuvanesh, ‘Principles and Applications of Powder Diffraction’ Wiley,2008
Rietveld program downloads, manuals and tutorials can be found at: http://www.ccp14.ac.uk
More: Structures: http://www.chem.ox.ac.uk/icl/heyes/structure_of_solids/lecture1/Lec1.html