Abstract
Interaction of freshly precipitated silica gel with aqueous solutions was studied at laboratory batch experiments under ambient and near neutral pH-conditions. The overall process showed excellent reversibility: gel growth could be considered as an opposite process to dissolution and a linear rate law could be applied to experimental data. Depending on the used rate law form, the resulting rate constants were sensitive to errors in parameters/variables such as gel surface area, equilibrium constants, Si-fluxes, and reaction quotients. The application of an Integrated Exponential Model appeared to be the best approach for dissolution data evaluation. It yielded the rate constants k dissol ∼ (4.50 ± 0.68) × 10−12 and k growth ∼ (2.58 ± 0.39) × 10−9 mol m−2 s−1 for zero ionic strength. In contrast, a Differential Model gave best results for growth data modeling. It yielded the rate constants k dissol ∼ (1.14 ± 0.44) × 10−11 and k growth ∼ (6.08 ± 2.37) × 10−9 mol m−2 s−1 for higher ionic strength (I ∼ 0.04 to 0.11 mol L−1). The found silica gel solubility at zero ionic strength was somewhat lower than the generally accepted value. Based on the \({}^{298}K_{\rm SS}^{(I=0)} = 10^{-2.754\pm 0.017}\) and \(^{298}K_{\rm DBP}^{(I=0)} = 10^{-2.728\pm 0.003},\) standard Gibbs free energy of silica gel formation was calculated as \(\Updelta{G}_{\rm f}^0(298\,{\rm K}) \sim -\hbox{850,463} \pm 98\hbox{ J mol}^{-1}\) and −850,318 ± 20 J mol−1, respectively. Activation energies for silica gel dissolution and growth were determined as \(E_{\rm A}^{\rm dissol} \sim 62.0\pm 3.2\,\hbox{kJ mol}^{-1}\) and \(E_{\rm A}^{\rm growth} \sim 48.8\pm 4.4\,\hbox{ kJ mol}^{-1},\) respectively. An universal value for growth of any silica polymorph, \(E_{\rm A}^{\rm growth} \sim 37.4 \pm 9.4\,\hbox{kJ mol}^{-1},\) is not consistent with the value for silica gel growth, which questions the hypothesis about one unique activated complex controlling the silica polymorph growth.
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Abbreviations
- A :
-
Pre-exponential factor of the Arrhenius equation
- {A}:
-
Total surface area (m2)
- {A i }:
-
Surface area of single gel particle (m2)
- a Si :
-
Activity of silicic acid
- \({a}_{\rm Si}^{\rm eq} \) :
-
Equilibrium silicic acid activity
- a gel :
-
Silica gel activity
- \({a}_{\rm gel}^{\rm eq} \) :
-
Equilibrium silica gel activity
- AT:
-
Affinity term
- a w :
-
Water activity
- d i :
-
Gel particle diameter (m)
- \(\Updelta G_{\rm r}\) :
-
Gibbs free energy of an overall reaction
- \(\Updelta G_{\rm {gel}{-}{w}}\) :
-
Gibbs free energy of the silica gel–water reaction (J mol−1)
- \(\Updelta G_{\rm f}^{0}\) :
-
Standard Gibbs free energy of formation (J mol−1)
- \(\Updelta x/x\) :
-
Relative error in x-variable
- E A :
-
Activation energy
- I :
-
Ionic strength (mol L−1)
- j :
-
Overall Si-flux from silica into solution (mol s−1)
- j norm :
-
Overall Si-flux from silica into solution normalized to unitary surface area (mol m−2 s−1)
- j d :
-
Partial Si-flux linked to silica dissolution (mol s−1)
- j g :
-
Partial Si-flux linked to silica growth (mol s−1)
- k (pH,T) :
-
A rate constant, pH and temperature-dependent
- k d :
-
Dissolution rate constant (mol m−2 s−1)
- k g :
-
Growth rate constant (mol m−2 s−1)
- K PHREEQC :
-
Equilibrium constant taken from PHREEQC database
- K DBP :
-
Equilibrium constant based on detailed balancing principle
- K SS :
-
Equilibrium constant based on steady-state concentrations
- N :
-
Gel particle number
- n :
-
Rate law empirical constant
- m :
-
Rate law empirical constant
- M Si :
-
Total Si-content in solution (mol)
- \(M_{\rm Si}^{0}\) :
-
Initial Si-content in solution (mol)
- p :
-
Parameter of regression power function
- q :
-
Parameter of regression power function
- Q (gel–w) :
-
Ion activity quotient of silica gel–water reaction
- r :
-
Parameter of regression power function
- R :
-
Gas constant (J mol−1 K−1)
- ρgel :
-
Silica gel density (g cm−3)
- SI gel :
-
Saturation index with respect to silica gel
- \(c_{{\rm H}_4{\rm SiO}_4}\) :
-
Silicic acid concentration (mol L−1)
- \(c_{{\rm H}_4{\rm SiO}_4}^{0}\) :
-
Initial silicic acid concentration (mol L−1)
- t :
-
Time (s)
- T :
-
Temperature (K)
- V :
-
Volume of solution (L)
- W gel :
-
Total weight of silica gel sample (g)
- W i :
-
Weight of single gel particle (g)
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Acknowledgments
The authors wish to thank Dr. Ondra Sracek for critical reading of the manuscript. Anonymous referee is thanked for inspiring comments. The work was supported by the MSM0021622412 grants of Ministry of Education, Youth and Sports of Czech Republic.
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Appendices
Appendix A
Appendix B: Error Propagation
In general, a propagation of errors in a F(x i ) function with uncorrelated variables is given by
where \(\Updelta{ x}_{i}\) is an absolute error of x i -variable (see, e.g., Papoulis 1991).
2.1 Saturation Index Error
The uncertainty in saturation index was derived from the expression
A rewriting gives
Developing of A3 according to Eq. A1 with respect to Q a K gives
After dividing by the squared Eq. A3, it becomes
and, after substituting for the multiplicative terms,
where Λ = 1/(ln10 SI). The significance of the multiplicative term Λ is enormous close to equilibrium where \(\lim\limits_{{Q}\rightarrow {K}} [1/\log ({Q/K})]=\infty.\)
Based on the relation \(\Updelta{G}_{\rm {gel}{-}{w}} = 2.3{RTSI}_{\rm {gel}{-}{w}}\), the relative error in \(\Updelta G_{\rm {gel}{-}{w}}\) is the same as in SI.
2.2 Affinity Term Error
The error in affinity term was derived from the equation
Based on the evaluation of Eq. A7 according to A1 with respect to Q and K, it is
Dividing by A 2 yields
and, after substituting for multiplicative terms,
The share of Q and K errors depends on the Φ multiplicative term. The Q errors are insignificant when Q approaches zero. Their role increases if Φ2 > 1, i.e., if Q > K eq/2. An extreme multiplication effect of the Φ2 term is close to equilibrium, as indicated by \(\lim \limits_{Q\rightarrow K} \, \Upphi =\infty. \) If \(Q \gg K_{\rm eq},\) the multiplicative effect diminishes, as K eq may be omitted in comparison with Q.
2.3 Normalized Flux Error
The error propagation was derived from the expression
Evaluating Eq. A11 according to A1 with respect to j and {A} variables yields
After dividing by the squared Eq. A11 and rewriting, we obtain
2.4 DIFFEREL Modeling Error
An uncertainty in the DIFFEREL modeling was derived from Eq. 12. Assuming the term \(a_{\rm gel} a_{\rm w}^{2} \cong 1\) and rewriting, it yields
The rearrangement of Eq. A14 according to Eq. A1 with respect to j norm and Q variables gives
After dividing by the squared Eq. A14 and rewriting, the equation becomes
or, after substituting for the multiplicative term,
Because k g is linked to k d by the simple relation of k g = k d/K eq, the uncertainty in k g is the same as in the k d.
As it can be seen, the share of Q errors depends on the Φ2 multiplicative term. The Q errors themselves are insignificant if Q approaches zero. Their role increases if Φ2 > 1, i.e., if Q > K eq/2. An extreme multiplication effect of the Φ2 term is close to equilibrium, as indicated by \(\lim\limits_{Q\rightarrow K} \, \Upphi =\infty.\) When \(Q\gg K_{\rm eq},\) the multiplicative effect diminishes, as K eq may be omitted in comparison with Q.
2.5 INTEGEXPEL Modeling Error
Error linked to the INTEGEXPEL modeling was derived from Eq. 16. It was rewritten as
An rearrangement according to Eq. A1 with respect to the {A} and Q variables yields
After dividing by the squared Eq. A18, it simplifies to
and, after substituting the multiplicative terms, to
Close to equilibrium, the term is of fatal relevance as \(\lim\limits_{Q\rightarrow {K}} \Upphi^{2}\Upomega^{2}=\infty \) shows. The term value is enormous also at the start of experiment as indicated by \(\lim\limits_{{Q}\rightarrow {Q}^{0}} \Upphi^{2}\Upomega^{2}=\infty.\) Because k g is linked to k d by the simple relation of k g = k d/K eq, the uncertainty in k g is the same as in k d.
2.6 INTEGLOGEL Modeling Error
Error linked to the INTEGLOGEL modeling was derived from Eq. 16. It can be rewritten as
Assuming {A}, K eq, and Q as variables, we can write
Dividing by the squared Eq. A22 and a rewriting yield
and, after substituting for the error multiplicative terms, it gives
The analysis of a share of K eq and Q error shows that the both Γ2Ψ2Ω2 and Φ2Ω2 multiplicative terms effect is at maximum close to equilibrium, as indicated by \(\lim\limits_{Q\rightarrow K} \Upgamma \Uppsi \Upomega =\infty \) and \(\lim \limits_{Q\rightarrow K} \Upphi \Upomega =\infty.\)
2.7 The AFFINEL Modeling
Error propagation linked to the AFFINEL modeling was derived from Eqs. 12 and A14. In contrast to the DIFFEREL case, the equation was evaluated with respect to j norm, Q, and K. The rearrangement of Eq. A14 according to Eq. A1 gives
Dividing by the squared Eq. A14 and a rewriting yield
and, after substituting for the multiplicative terms, it gives
The analysis of K eq and Q error shares shows that the maximum effect of the Φ multiplicative term is close to equilibrium, as indicated by \(\lim \limits_{Q\rightarrow K} \Upphi =\infty.\)
2.8 The Equilibrium Constant Based on Detailed Balancing Principle
The uncertainty in the \(K_{\rm eq}^{\rm DBP}\) was calculated from the equation \({K}_{\rm eq}^{\rm \rm DBP}\, =\, {k}_{\rm d}/{k}_{\rm g}.\) Because k d and k g values are correlated, we must use a modified form of the function A1,
where C is correlation coefficient (Papoulis 1991).
Developing the equation \({K}_{\rm eq}^{\rm DBP}\, =\, {k}_{\rm d}/{k}_{\rm g} \) according to Eq. A29 with respect to k d and k g gives
After dividing by \( \left({{K}_{\rm eq}^{\rm DBP}} \right)^{2}\, =\, ({k}_{\rm d})^{2}/({k}_{\rm g})^{2}\) and rewriting, Eq. A30 yields
When C ∼ 1, the Eq. A31 simplifies to
In the case that \(\Updelta {k}_{\rm d}/{k}_{\rm d} \approx \Updelta {k}_{\rm g}/{k}_{\rm g},\) the uncertainty stemming from error propagation approaches zero.
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Faimon, J., Blecha, M. Interaction of Freshly Precipitated Silica Gel with Aqueous Silicic Acid Solutions under Ambient and Near Neutral pH-conditions: A Detailed Analysis of Linear Rate Law. Aquat Geochem 14, 1–40 (2008). https://doi.org/10.1007/s10498-007-9024-x
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DOI: https://doi.org/10.1007/s10498-007-9024-x