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Investigation of the role of alkali cation in early stage of oligomerization in silicate fluids: a molecular dynamics
study
Amaury Coste, Olivier Diat, Arnaud Poulesquen, Jean-François Dufrêche, Magali Duvail
To cite this version:
Amaury Coste, Olivier Diat, Arnaud Poulesquen, Jean-François Dufrêche, Magali Duvail. Investiga-tion of the role of alkali caInvestiga-tion in early stage of oligomerizaInvestiga-tion in silicate fluids: a molecular dynamics study. 7th EuCheMS Chemistry Congress, Aug 2018, Liverpool, United Kingdom. �hal-02142629�
220 240 260 280 300
Number of Si inside the aggregate
0 50 100 150 200 count MD profile Gaussian fit Lorentzian fit µ=257 σ = 8.2 5 6 7 8 9 10 11 12 13 10-3 10-2 10-1 10-0 Insolubility Domain SiO2 (amorph) Monomeric solution
H4SiO4 H3SiO4- H2SiO42-
Olig ome ric so lutio n mo l kg -1 Si pH
Investigation of the role of alkali cation in early stage of
oligomerization in silicate fluids: a molecular dynamics
study
amaury.coste @cea.fr
Context
This work was made possible thanks to the financial support of the ANR DYNAMISTE (ANR-15-CE07-0013-01) and high performance computing facilities of TGCC/CCRT and the computing center of CEA Marcoule.
Amaury Coste
a, Olivier Diat
a, Arnaud Poulesquen
b, Jean-François Dufrêche
aand Magali Duvail
aa Institute for Separation Chemistry in Marcoule (ICSM), UMR 5257 CEA – Université Montpellier - CNRS - ENSCM, BP 17171, F-30207 Bagnols-sur-Cèze
b CEA, Nuclear Energy Division, Research DE2D (SEAD, LCBC) BP 17171, F-30207 Bagnols-sur-Cèze
§
Solutions of activation (= alkali media) of alumino-silicate are environmentally friendly and considered as green chemistry (used for ground stabilization, painting….)
§
The formulation is complex since the parameters are various and numerous
Conclusions and Outlooks
§
Understanding the ion-ion interactions for the oligomerization process where the nature and concentration of alkali drives the final properties of the gel [1]
§
Molecular dynamics is a useful tool to fill the gap between theoretical and experimental studies
§
Molecular dynamics allows the calculation of the structural and dynamical properties of the solutes in solution
§
Effect of water, alkali and hydroxide are explicitly taking into account
[1] L. Provis et al., Ind. Eng. Chem. Res. 2005, 44, 8899
[2] C. T. Knight and S. D. Kinrade, Silicon in Agriculture, Elsevier,
2001, vol. 8, chap. 4
[3] D.A. Case et al., Computat. Chem., 2005, 26, 1668 [4] A. Coste et al., J. Chem. Phys., submitted (2018)
Ground stabilization on building site (Wöllner GmbH&Co.KG)
§ Structure of the solution depends on the oligomer composition and nature:
- Spontaneous aggregation of dimers in solution: aggregates composed of silicates and Na+
- Dimers Si2O3(OH)42- interact strongly with Na+
- Monomers SiO(OH)3-: small aggregates, and destabilize the aggregation (entropic effect)
§ Similar behaviours of Na+: “buffer media” with the hydroxide anions
§ MD simulations of “real” solutions:
- Different [Si]/[Na+] ratios with respect to NMR experiments
- Influence of the alkali nature on the aggregation
n Si(OH)4 + n OH- = SiO(OH) 3- SiO2(OH)22- Si2O2(OH)5 Si2O3(OH)42- Si3O5(OH)53- Si4O8(OH)44- etc…
Method
§ Molecular dynamics simulations using explicit
polarization with AMBER14 [3]
Classical Molecular Dynamics (MD)
SiO(OH)3- Si 2O2(OH)5- Si2O3(OH)4 2-anionic fragment neutral fragment § Development of a polarizable silicate force
field for describing all the silicate oligomers by assembling neutral and anionic fragment (10 types of atom)
§ MD simulations focused on 3 species:
§ Calculation of I(q) from radial distribution functions
§ Theoretical I(q) directly comparable to experimental one
§ Efficient method for describing alkali media [4] è study
of silicate oligomers in such media 1 10
q (Å-1) 0 1×104 2×104 3×104 4×104 5×104 6×104 7×104 I(q) + offset MD Experiments 9.66 mol L-1 5.0 mol L-1 3.0 mol L-1 1.0 mol L-1 0.5 mol L-1 pure water
X ray scattering intensity from MD simulation
I(q) =
X
↵
X
f
↵(q)f (q)
p
N
↵N S
↵(q)
S
↵(q) =
↵+ p⇢
↵⇢ FT
3D(g
↵(r)
1)
Concentrated aqueous solutions of NaOH 0.01 0.1 1 10 Q / Å-1 0 1 2 3 4 5 6 7 I(Q)/I 0 SiO(OH)3 -Si2O2(OH)5 -Si2O3(OH)4 2-mixture of dimers mixture of all
box size cut-off
SAXS WAXS SiO(OH)3- Si2O2(OH)5- Si2O3(OH)4 2-mixture of dimers mixture of dimers and monomers
Silicate in NaOH concentrated media
§ Same structure for Q > 1 Å-1
§ Rise for Q < 0.4 Å-1
(aggregation)
§ Presence of monomers
decreases the I(Q) at small angles
Mixtures of oligomers
300 Na+ 75 Si2O2(OH)5- 75 Si2O3(OH)42- 75 OH- 300 Na+ 37 Si2O2(OH)5- 37 Si2O3(OH)42- 152 SiO(OH)3- 37 OH- Mixture of dimers and monomersScattering intensities from MD
300 Na+ 150 Si2O2(OH)5- 150 OH- 300 Na+ 150 Si2O3(OH)42- 300 Na+ 300 SiO(OH)3- 65 Å
Pure oligomer solutions
[Si]/[Na+] = 1§ Monomers: “homogeneous” media
§ Dimers: spontaneous aggregation
0 4 8 12 16 20 24 28 32 60 50 40 30 20 10 2 40 10 1 time (ns) N umb er o f Si in si de the ag gre ga te
Evolution of the silicate oligomers without considering the main aggregate Percentage 0 5 10 15 20 25 30 35 40 60 50 40 30 20 10 2 40 10 1 time (ns) N umb er o f Si in si de the ag gre ga te Percentage § [Na+]free constant
§ Provide a “buffer media”
Mixture of dimers 0 5 10 15 20 25 30 35 40 time / ns 0 20 40 60 80 100 Percentage 0 10 20 30 40 50 time / ns 0 20 40 60 80 100 Percentage
Si inside the main aggregate Na+ free 0 10 20 30 40 50 time / ns 0 20 40 60 80 100 Percentage
Si inside the main aggregate Na+ free
Stability diagram for soluble silicates at 298 K [2]