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