refs, eqs and text

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Marco De Lucia 2023-08-26 13:55:06 +02:00
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@ -27,10 +27,9 @@ mpirun -np 4 ./poet --interp barite_interp_eval.R barite_results
* Chemical system
The benchmark depicts a porous system where pure water is initially at
equilibrium with *celestite* (strontium sulfate; brute formula:
SrSO_4).
The benchmark depicts an isotherm porous system at *25 °C* where pure
water is initially at equilibrium with *celestite* (strontium sulfate;
brute formula: SrSO_4).
A solution containing only dissolved Ba^{2+} and Cl^- diffuses into
the system causing celestite dissolution. The increased concentration
of dissolved sulfate SO_{4}^{2-} induces precipitation of *barite*
@ -50,28 +49,41 @@ saturation ratio, i.e., the ratio of the ion activity product of the
reacting species and the solubility constant.
For barite, the reaction rate is computed as sum of two mechanisms,
/acid/ and /neutral/:
r_{/acid/} and r_{/neutral/}:
rate_{barite} = S_{m} (acid + neutral) * (1 - SR_{barite})
rate_{barite} = S_{barite} (r_{/acid/} + r_{/neutral/}) * (1 - SR_{barite})
where
where:
acid = 10^{-6.9} \exp(\frac {-30800 \cdot T'} R) * act(H^{+})^{0.22}
r_{/acid/} = 10^{-6.9} e^{-30800 / R} \cdot act(H^{+})^{0.22}
and
r_{/neutral/} = 10^{-7.9} e^{-30800 / R}
neutral = 10^{-7.9} \exp( \frac {-30800 * T'} R)
R (8.314462 J K^{-1} mol^{-1}) is the gas constant.
R is the gas constant (8.314462 J / K / mol) and T' (K^{-1}) accounts
for temperature dependence of the kinetic coefficients which are
experimentally determined at 25 °C or 298.15 K
For celestite the kinetic law considers only the acidic term and
reads:
T' = (1 / K) - (1 / 298.15)
rate_{celestite} = S_{celestite} 10^{-5.66} e^{-23800 / R} \cdot
act(H^{+})^{0.109} \cdot (1 - SR_{celestite})
The kinetic rate law as implemented in the =db_barite.dat= file
The kinetic rate laws as implemented in the =db_barite.dat= file
accepts one parameter which represents reactive surface area in m^{2}.
For this benchmarks the surface areas are set to
For the benchmarks the surface areas are set to
- S_{barite}: 50 m^{2}
- S_{celestite}: 10 m^{2}
- S_{celestite}: 10 m^{2}
** Initial conditions
The parametrization
* References
- Tranter, Wetzel, De Lucia and Kühn (2021): Reactive transport model
of kinetically controlled celestite to barite replacement, Adv.
Geosci., 1, 19 ,https://doi.org/10.5194/adgeo-1-1-2021