Title: W' M' Kriven, J'L Bell and P' Sarin
1The Complex Structure of Geopolymers
W. M. Kriven, J.L Bell and P. Sarin University of
Illinois at Urbana-Champaign Department of
Materials Science and Engineering
Funded by the US AFOSR through 2 STTRs and one
Nanoinitiative contract
2Geopolymers (Polysialates)
- Are a type of chemically-bonded ceramics
(alkali bonded ceramics or inorganic polymers) - Inorganic polymeric ceramics formed from both
aluminum and silicon sources containing AlO4- and
SiO4 tetrahedral units, under highly alkaline
conditions (NaOH, KOH, CsOH) at ambient
temperatures - They are a rigid, hydrated, alumino-silicate gel
containing group I, charge-balancing cations - They result in an amorphous, cross-linked,
impervious, acid-resistant, 3-D structure
3Introduction Geopolymer Structure
- Formula Mn-(SiO2)z-AlO2-n,wH2O
-
- where M is a typically Na or K cation, n is
the degree of polycondensation and z is 1, 2, or
3 - The poly(sialates) were said to form chain or
ring polymers with Si4 and Al3 in IV-fold
coordination -
Davidovits, J., Journal of Thermal Analysis,
1991. 37 p. 1633-1656.
4Introduction Geopolymer Structure
- Are generally X-ray amorphous
- Al is integrated into a network of (IV) AlO4- and
SiO4, such that the negative charge on AlO4- is
balanced by the alkali cation.
Davidovits, J., Geopolymer 88 Conference, San
Quentin, France, 1988. 1p. 25-48 Barbosa, V.F.F.
and K.J.D. MacKenzie, Materials Research
Bulletin, 2003. 38(2) p. 319-331. Barbosa,
V.F.F., K.J.D. MacKenzie, and C. Thaumaturgo,.
International Journal of Inorganic Materials,
2000. 2(4)p. 309-317.
5How to Make a Geopolymer
Example
Molar oxide ratio SiO2 / Al2O3 4.0 K2O /
SiO2 0.25 H2O / K2O 10-12
Step 1
Step 2
Step 3
Step 4
alkali silicate solution
metakaolin clay
mix
cast and seal
store at RT or in an oven at low T
Davidovits, J. Journal of Thermal Analysis 1991,
37, 1633.
6GEOPOLYMER COVERSION TO CERAMIC POLLUCITE
Ex-situ X-ray diffraction patterns of Cs-GP and
SynMK
7Intrinsic Microstructure and Properties as a
Function of Composition Experimental Procedure
Table I. Compositions of Interest
- Other Processing Parameters
- M2OH2O 11 (M Na K)
- Cure temperature 50oC
- Cure time varied
- Mixing time 10 min.
8Intrinsic Microstructure and Properties as a
Function of Composition SEM of MIP samples
1000 psi autoclave polished surfaces 1000x
magnification p average pore size
0 K, 100 Na p 73.1nm
30 K, 70 Na p 33.5nm
- K2ONa2O SEM micrographs of 41 SiO2Al2O3, cured
80oC for 24 h
Effect of Alkali Choice on Geopolymer
Properties, W. M., Kriven and J., Bell, Cer.
Eng. and Sci. Proc. vol. 25 3-4 (2004).
60 K, 40 Na p 25.8
80 K, 20 Na p 19.7nm
100 K, 0 Na p 11.3nm
9Intrinsic Microstructure and Properties as a
Function of Composition SEM Micrographs as a
Function of Composition
100K
100 Na
50K- 50Na
41 SiO2Al2O3
31 SiO2Al2O3
21 SiO2Al2O3
10Intrinsic Microstructure and Properties as a
Function of Composition - SEM
Unreacted metakaolin sheet
Region of intrinsic GP
Microstructure and Microchemistry of
Fully-Reacted Geopolymers and Geopolymer Matrix
Composites, W. M., Kriven, J., Bell, and M.,
Gordon, Ceramic Transactions vol. 153, 227-250
(2003).
11Intrinsic Microstructure and Properties as a
Function of Composition - SEM
Individual precipitates of GP
Microstructure and Microchemistry of
Fully-Reacted Geopolymers and Geopolymer Matrix
Composites, W. M., Kriven, J., Bell, and M.,
Gordon, Ceramic Transactions vol. 153, 227-250
(2003).
12TEM BF at RT
13TEM of crushed Na-geopolymer
14High angle, annular dark field TEM (HAADF)
15High angle, annular dark field TEM (HAADF)
16Nanoporosity
Differential distribution of surface against pore
radius
17Nanoporosity in kaolin-based GP
Summary of Properties
- Average logarithmic pore radius 0.4362 nm
- Average pore radius 3.3711 nm
- Porosity over weight 0.3165 cm3/g
- Porosity over volume 0.4106 cm3/cm3
- Meso- and macro-pore surface over weight
190.5778 m2/g - Meso- and macro-pore surface over volume
247.2794 m2/cm3 - Total pore surface over weight 274.6912 m2/g
- Total pore surface over volume 356.4186 m2/cm3
- Density of solid phase 2.0481 g/cm3
Nanoporosity in synthetic-based GP 0.8 nm
18INTRODUCTION TWO USEFUL CERAMIC PHASES
Leucite KAlSi2O6
Pollucite CsAlSi2O6
Bollin, P.J., Glass Formation in the System
Cs2O-Al2O3-SiO2, J. Am. Cerm. Soc. 55, 483
(1972)
Schairer J.F., and N.L. Bowen, The system
K2OAl2O3 SiO2, Am. J. Sci., 253, 681 (1955)
19INTRODUCTION USEFUL CERAMIC PHASES
- Pollucite (CsAlSi2O6)
- Very refractory (Tm 1940oC)
- Exceptional creep resistance comparable to YAG
- Low thermal expansion (0.45 from 25 1000oC) or
(1.2 3.3 x 10-6 oK-1) - Relatively low density (3.3 g/cm3)
- High thermal shock resistance
- Tolerates a high degree of ionic substitution
which can be used to further lower thermal
expansion or even make it negative - May be useful for ceramic matrix composites and
thermal barrier coatings
- Leucite (KAlSi2O6)
- Refractory (Tm 1693oC)
- High thermal expansion (15.1 31 x 10-6 oK-1)
- Tolerates a high degree of ionic substitution
- High fracture toughness
- Useful as a cermet due to high thermal expansion
- Used widely in dentistry
- Potential as a thermal barrier coating or ceramic
matrix composite - Leucite crystals enhance the toughness of glass
ceramics
20GEOPOLYMER COVERSION TO CERAMIC POLLUCITE
Ex-situ X-ray diffraction patterns of
Cs-geopolymer after heating at a set temperature
for 1 hour.
21Pair Distribution Function (PDF) Work
- Novel materials are often disordered/complex on a
local level - PDF method allow us to sit on an atom and look
at our neighborhood - PDF procedure
- Collect total scattering data (X-ray or neutron)
for material - Subtract background and apply appropriate
corrections to raw data - This gives us the structure function, S(Q)
- Apply Fourier transform to get the PDF, G(r)
22Experimental Setup Argonne National Lab
- Advanced Photon Source beamline 11IDB
- ? 0.1372 Å (90.3 keV), (Q 30 Å-1, 2? 39o)
- 2.84mm OD Polyimide (Kapton) tubes as sample
holder - Transmission geometry
- GE amorphous Si Angio flat plate detector
23Scattering in PDF
- Elastic scattering no exchange of energy
between the scattering particle and the system it
is scattering off of - Inelastic scattering the is an exchange of
energy - Coherent waves interfere and resulting
intensity is given by the square of the sum of
the wave amplitudes - Incoherent no definite phase relationship
between the wave as they do no interfere and the
resulting intensity is the sum of the individual
waves themselves - ALL scattering can be classified as listed above
24Scattering in PDF
25Scattering in PDF
- PDF uses total elastic scattering making it
necessary to subtract out inelastic contributions
and other sources of error - Non X-ray specific corrections
- Flat plate geometrical correction
- Detector deadtime and flux normalization
- Background (air, container)
- Random errors
- X-ray Specific corrections
- Compton scattering
- Thomson scattering process polarization of
X-ray beam - Self scattering and multiple scattering
- Laue diffuse scattering
26?- Alumina (Corundum) Procedure
Subtract dark current and sum raw detector data
Use PDFgetX2 software to get structure fun.
Correct for background Compton, flat
plate, weighting function
FIT2D
Take Fourier transform to get PDF
Apply corrections and calibrations and
convert from 2D image to 1D via FIT2D software
27Pair Distribution Function (PDF) Work
Alpha Alumina after heating to 1300 oC for X.X h
Amorphous Alumina Prepared via PVA method
28?- Alumina (Corundum) Modeling Partials
MODEL Kirfel, A., Eichhorn, K. Accurate
Structure Analysis with Synchrotron Radiation
The Electron Density in Al2O3 and Cu2O, Acta
Cryst. A46 (1990) 271-284
29?- Alumina (Corundum) Modeling Best Fit
R-value82.62
MODEL Kirfel, A., Eichhorn, K. Accurate
Structure Analysis with Synchrotron Radiation
The Electron Density in Al2O3 and Cu2O, Acta
Cryst. A46 (1990) 271-284
30?- Alumina (Corundum) Modeling Best Fit
R-value16.75
31?- Alumina (Corundum) Modeling Best Fit
R-value16.75
32Cs based geopolymer conversion to Pollucite
33Cs based geopolymer conversion to Pollucite
34K based geopolymer conversion to Leucite
35Na based geopolymer Ordering in Na-GP
36K based geopolymer Ordering in K-GP
37Cs based geopolymer Ordering in Cs-GP
38Geopolymer PDF as function of Alkali Choice
39Geopolymer PDF as function of water for K-GP
40(No Transcript)
41Geopolymers (Polysialates)
- Are a type of chemically-bonded ceramics
(alkali bonded ceramics or inorganic polymers) - Inorganic polymeric ceramics formed from both
aluminum and silicon sources containing AlO4- and
SiO4 tetrahedral units, under highly alkaline
conditions (NaOH, KOH, CsOH) at ambient
temperatures - They are a rigid, hydrated, alumino-silicate gel
containing group I, charge-balancing cations - They result in an amorphous, cross-linked,
impervious, acid-resistant, 3-D structure
42Geopolymers (Polysialates)
- A great deal of complementary information on
the structure at the local atomic level can be
obtained from - conventional Bragg diffraction techniques
- Rietveld analysis
- (reciprocal space)
- Pair distribution function (PDF) analysis
- (real space