Cited by 26Calcium Carbonate Crystallization and InhibitionAdvanced Chemical Physics StudiesCO2 Sequestration and Geologic Interactions

Computational Insights into Mg2+ Dehydration in the Presence of Carbonate

Open access
Aufort, Julie, Raiteri, Paolo, Gale, Julian D.·2022·ACS Earth and Space Chemistry

Abstract

Water exchange around a free magnesium ion and magnesium paired with carbonate in aqueous solution was studied using free energy methods. Both a rigid-ion and a polarizable force field based on the AMOEBA model were examined. The parameters were adjusted to accurately reproduce the hydration structures of magnesium and carbonate in aqueous solution. The magnesium carbonate ion pairing free energies calculated with both force fields were found to be in excellent agreement with experimental data. Metadynamics simulations of the water exchange conducted with both models revealed that the formation of a contact magnesium carbonate ion pair significantly decreases the energy barrier for water exchange relative to the free magnesium ion in solution. This finding suggests that the presence of carbonate could accelerate the water exchange around magnesium and constitutes a first step toward a better understanding of the atomic-scale mechanisms involved in the nucleation of magnesium-bearing carbonate minerals.

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Crossref · 10.1021/acsearthspacechem.1c00389

Cites

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Claims the paper makes

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  • Findingown data

    No water exchange was observed during the entire molecular dynamics simulation.

    “No water exchange was observed during the whole MD simulation”
    Quote in the paperSubstantial claim
  • Findingcitation

    The former rigid-ion parameters produce a bimodal first peak in the C-Ow RDF, indicating a wider distribution of C-Ow distances in the first hydration shell.

    “the RDF between carbon of carbonate and oxygen of water obtained with the former rigid-ion parameters 20 displays a bimodal first peak, indicating a wider distribution of C-O w distances in the first hydration shell.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [20] source

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  • Findingcitation

    The AMOEBA Mg-O radial distribution function has its first maximum at 2.08 Å, within the experimental range of 2.00-2.15 Å for Mg2+.

    “The position of the first peak of the magnesium-oxygen pair distribution function for the AMOEBA model, 2.08 Å, falls within the 2.00-2.15Å range of experimental values reported for Mg 2+ in the literature.52”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [52] source

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  • Findingown data

    AIMD calculations show that water oxygen density in the first hydration shell of carbonate is distributed in three narrow toroids located on top of the carbonate oxygen atoms and centered around the three C-Oc directions.

    “The AIMD calculations reveal that the water oxygen density in the first hydration shell of carbonate is distributed in three narrow toroids located on top of the carbonate oxygen atoms and centered around the three C-O c directions.”
    Quote in the paperSubstantial claim
  • Findingown data

    The new rigid-ion model has a significantly worse hydration free energy than the older force field.

    “the new rigid-ion model appears to have a significantly worse hydration free energy that the older force field (Table 3).”
    Quote in the paperSubstantial claim
  • May combine two claims. 43
  • Classified as probably not a substantial claim. 19
  • The quote only partly states this claim. 1
  • May combine two claims.

    Findingown data

    Formation of a contact MgCO3 ion pair either lowers the water-exchange energy barrier relative to free Mg2+ and/or substantially destabilizes the Mg-water contact state.

    “Metadynamics simulations of the water exchange conducted with both models revealed that the formation of a contact magnesium carbonate ion pair either decreased the energy barrier for water exchange relative to the free magnesium ion in solution and/or significantly destabilized the magnesium-water contact state.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    The AMOEBA model overestimates the self-diffusion coefficient of Mg2+ by 13% compared with experiment, while the new and former rigid-ion force fields overestimate it by about 30% and 21%, respectively.

    “The AMOEBA model was found to overestimate the self-diffusion coefficient by 13% compared to the experimental value but still gave better agreement than the new and former rigid-ion force fields for which the overestimation was about 30% and 21%, respectively.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingreasoning

    The current and former rigid-ion force fields predict shorter Mg-O distances in the first solvation shell, 1.94 Å for this work and 1.99 Å for Raiteri et al.

    “both the current and former non-polarizable rigid-ion force fields predict slightly shorter Mg-O distances in the first solvation shell, with r M g-O = 1.94 Å (this work) and r M g-O = 1.99 Å. 20”
    Quote in the paperNot a substantial claim0 of 1 sources checked
    • cites [20] source

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  • May combine two claims.

    Findingown data

    The AMOEBA and new rigid-ion force fields reproduce the toroidal water oxygen density around carbonate, whereas the former rigid-ion parameters concentrate water oxygen density predominantly along each C-Oc direction.

    “While the AMOEBA and new rigid-ion force fields are both able to reproduce this specific structure, this is not the case of the former rigid-ion parameters 20 which seem to concentrate the water oxygen density predominantly along each C-O c direction instead.”
    Quote in the paperSubstantial claim0 of 1 sources checked
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  • May combine two claims.

    Findingreasoning

    The former rigid-ion force field showed a significant free energy barrier of about 27 kJ/mol, lower than the current models, consistent with its less exergonic Mg2+ hydration free energy.

    “this model also showed a significant free energy barrier (≈27”
    • Also stated in: § Mg 2+ -CO 2 - 3 ion pairing free energy · plain
      “though it is lower than for the current models, which is consistent with the less exergonic Mg 2+ hydration free energy of that force field (Table 2).”
    Quote in the paperNot a substantial claim0 of 1 sources checked
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  • May combine two claims.

    Findingreasoning

    The barrier for Mg-CO3 ion pair formation is about 39 kJ/mol for AMOEBA and about 51 kJ/mol for the new rigid-ion force field.

    “leading to a high energy barrier of ≈39 kJ/mol and ≈ 51 kJ/mol for the AMOEBA and the new rigid-ion force fields, respectively.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    The reverse bidentate-to-monodentate process appears almost barrierless in one dimension (3.8 kJ/mol) but has a 17.5 kJ/mol barrier in the 2D free energy surface.

    “While the reverse process appears almost barrierless in one-dimension (3.8 kJ/mol), there is in fact a higher 17.5 kJ/mol barrier to return to the monodentate configuration.”
    Quote in the paperSubstantial claim
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    Findingown data

    Three free energy minima were obtained: a bidentate state, a five-fold coordinated monodentate state, and a six-fold coordinated monodentate state, listed in order of increasing stability.

    “Three free energy minima were obtained, corresponding to the bidentate state, a monodentate state in which Mg is only five-fold coordinated, and the expected monodentate state with a six-fold coordinated cation, in order of increasing stability.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingreasoning

    The AMOEBA force field simulation did not show a minimum for the five-fold Mg2+ monodentate state and predicted a free energy barrier halfway between 20 and 40 kJ/mol.

    “It is thus not surprising that the simulation carried out with the AMOEBA force field, which did not show a minimum for the five-fold Mg 2+ monodentate state (i.e.CNw=4, CNcarb=1), predicted a free energy barrier falling halfway between 20 and 40 kJ/mol.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    The transition from monodentate to bidentate involved overcoming two consecutive barriers of about 20 kJ/mol each: first a water molecule left the Mg2+ hydration shell, and then carbonate bound in a bidentate configuration.

    “The transition from the monodentate to the bidentate state involved overcoming two consecutive ≈20 kJ/mol barriers for one water molecule to leave the Mg 2+ hydration shell first, and finally for the carbonate to bind in a bidentate configuration.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    Results with the new rigid-ion parameterization are more ambiguous, and the minimum free energy path suggests a one-step process with concerted movement of carbonate entering the magnesium inner shell while a water molecule leaves.

    “Results obtained with the new parameterization of the rigid-ion force field are more ambiguous and the minimum free energy path seems to suggest a one step process with a concerted movement of the carbonate entering the magnesium inner shell while a water molecule simultaneously leaves.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    With both the AMOEBA and new rigid-ion force fields, the solvent-shared ion pair state at dMg-C ≈ 4.5 Å is the most stable state, more stable than the contact ion pair by 15 and 9 kJ/mol, respectively.

    “the reverse was obtained here with both the polarizable AMOEBA and new rigid-ion force fields, which find the SSHIP state at d M g-C ≈ 4.5 Å to be the most stable state by 15 and 9 kJ/mol, respectively.”
    Quote in the paperSubstantial claim
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    Findingown data

    From the intermediate state, an additional 11.5 kJ/mol is needed to form the monodentate ion pair, giving an overall free energy barrier of about 39 kJ/mol from SSHIP to CIP.

    “From this intermediate state a further 11.5 kJ/mol is then needed to form the monodentate ion pair, which leads to an overall free energy barrier of ≈39 kJ/mol to be overcome to go from the SSHIP to the CIP.”
    Quote in the paperSubstantial claim
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    Findingown data

    Reaching the five-fold coordinated Mg2+ configuration from the SSHIP state requires overcoming a barrier of 33.6 kJ/mol, and the state has stability of order 2kBT with a 5.5 kJ/mol barrier to return to SSHIP.

    “Reaching this five-fold coordinated Mg 2+ configuration from the SSHIP state is an activated process that requires a high energy barrier (33.6 kJ/mol) to be overcome and its stability is of the order of 2k B T with only a 5.5 kJ/mol barrier to return to the SSHIP minimum.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    The monodentate state was more stable than the bidentate configuration by about 15 kJ/mol, in good agreement with the AMOEBA results.

    “The monodentate state was found to be more stable than the bidentate configuration by about 15 kJ/mol which is in good agreement with the AMOEBA results.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    The Raiteri et al. rigid-ion force field overestimated the Mg-CO3 association free energy by more than 10 kJ/mol, largely because the contact ion pair state was excessively stable.

    “this force field overestimated the Mg-CO 3 association free energy by more than 10 kJ/mol (Table 4), which was largely due to the excessive stability of the contact ion pair state.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [20] source

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  • May combine two claims.

    Findingreasoning

    The ion-pairing formation free energy is -15 kJ/mol for AMOEBA and -19 kJ/mol for the new rigid-ion model, compared with -30.4 kJ/mol for the old rigid-ion force field and -17.2 kJ/mol experimentally.

    “significantly decrease the strength of the ion pairing formation free energy (-15 kJ/mol and -19 kJ/mol for AMOEBA and the new rigid-ion model, respectively) compared to the old rigid-ion force field (-30.4 kJ/mol) which brings the current values much closer to the experimental value (-17.2 kJ/mol)”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites De Visscher et al., 67

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  • May combine two claims.

    Findingown data

    The relative stabilities of the monodentate and bidentate states remain the same, with the monodentate ion pair more stable by about 12 kJ/mol.

    “In both cases, the relative stabilities of the two states remain the same, with the monodentate ion pair more stable by about ≈12 kJ/mol.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingown data

    The new rigid-ion model predicts a free energy difference between monodentate and bidentate states of about 33 kJ/mol, more than double the ab initio (~15 kJ/mol) and AMOEBA (~12 kJ/mol) values.

    “Here, poorer agreement is obtained with the new rigid-ion model, which predicts the free energy difference between monodentate and bidentate states, ≈33 kJ/mol, to be more than double the ab initio (≈15 kJ/mol) and AMOEBA (≈12 kJ/mol) values.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Findingcitation

    The old rigid-ion force field did not display such an intermediate minimum, and its minimum energy path suggests that ion pair formation occurs with carbonate moving closer first and then pushing away a water molecule.

    “This is at variance with the prediction from the old rigid-ion force field, which did not display such minimum in the 2D FES, and whose minimum energy path seems to suggest that the formation of the ion pair would occur with the carbonate group moving closer to Mg 2+ first and then pushing away one water molecule from the coordination shell.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [20] source

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  • May combine two claims.

    Findingcitation

    In the case of Mg2+, two collective variables are required to describe the water exchange mechanism, in agreement with a previous study by Schwierz.

    “We have demonstrated how in the case of Mg 2+ two collective variables are required to describe the water exchange mechanism, which is in agreement with a previous study by Schwierz 3 that suggests that this process requires the concerted motion of all the water molecules in the ion's hydration shell.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [3] source

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  • May combine two claims.

    Findingcitation

    The magnesium carbonate ion pairing free energies are now in excellent agreement with experimental data, which is a significant improvement over former rigid-ion models.

    “Importantly, the magnesium carbonate ion pairing free energies are now in excellent agreement with experimental data, which is a significant improvement over former rigid-ion models.20”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [20] source

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  • Classified as probably not a substantial claim.

    Findingcitation

    The prediction that water exchange is more labile around the Mg-CO3 complex is at variance with the computational results from Yang et al. and Hamm et al., who did not observe any significant increase in the water exchange rate when Mg2+ formed a complex with either HS- or aspartate.

    “Our prediction that water exchange is more labile around the Mg-CO 3 complex is at variance with the computational results from Yang et al. 27 and Hamm et al., 28 who did not observe any significant increase in the water exchange rate when Mg 2+ formed a complex with either HS -or aspartate.”
    Quote in the paperSubstantial claim0 of 2 sources checked
    • cites [27] source

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  • Classified as probably not a substantial claim. May combine two claims.

    Premisecitation

    Schwierz found that water exchange around Mg2+ requires concerted motion of two water molecules and collective rearrangement of all first-shell water molecules, implying a time scale of about 40 ms.

    “Schwierz 3 found, using transition path sampling, that a concerted motion of two water molecules and a collective rearrangement of all the water molecules in the first solvation shell of Mg 2+ was required for water exchange to occur, leading to a much longer time scale than previously estimated, of ≈40 ms.”
    Quote in the paperSubstantial claim0 of 1 sources checked
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  • Classified as probably not a substantial claim.

    Premisecitation

    Martinek et al. showed that a full ionic charge force field can overestimate the stability of the contact ion pair between divalent cations and negatively charged residues.

    “Martinek et al. 23 showed that the use of a full ionic charge force field could lead to an overestimation of the stability of the contact ion pair between divalent cations and negatively charged residues.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [23] source

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  • Classified as probably not a substantial claim.

    Premisecitation

    Water exchange between the first and second solvation shells of Mg2+ is the most fundamental step governing processes that occur in aqueous environments.

    “water exchange between the first and second solvation shells of magnesium is the most fundamental step governing all stages of these processes occurring in aqueous environments.3”
    Quote in the paperSubstantial claim0 of 1 sources checked
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    Premisecitation

    De Oliveira et al. reported Mg-acetate binding energies but did not investigate how complexation affects the water-exchange rate.

    “De Oliveira et al. 29 used a scaled-charge force field to probe the interaction between divalent cations and carboxylate groups, and reported Mg-acetate binding energies but did not investigate the effect of complexation on the water exchange rate.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [29] source

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  • May combine two claims.

    Interpretationreasoning

    The lack of polarization in the SPC/Fw water model underestimates the water dipole moment next to Mg2+ and causes shorter water-cation distances in order to reproduce the experimental hydration free energy.

    “This is due to the lack of polarization in the SPC/Fw water model that leads to the underestimation of the water dipole moment adjacent to magnesium and cause the water-cation distances to be shorter in order to reproduce the experimental hydration free energy.”
    Quote in the paperSubstantial claim
  • Probably not a substantial claim: may not pass S3 (load-bearing).

    Premisecitation

    Yang et al. found that HS- had little effect on lowering the water-exchange energy barrier around Mg2+.

    “Yang et al. 27 conducted ab initio Reaction Path Ensemble (RPE) simulations to explore the possibility that HS -, a product of bacterial sulphate reduction, might promote Mg 2+ dehydration in aqueous solution, but found that it had little effect on lowering the water exchange energy barrier.”
    Quote in the paperNot a substantial claim0 of 1 sources checked
    • cites [27] source

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  • May combine two claims.

    Premisecitation

    An accurate description of the Mg-carbonate ion pair in solution and quantitative data on the energy barrier for Mg2+ dehydration in the presence of carbonate are still lacking.

    “An accurate description of the Mg-carbonate ion pair in solution and quantitative data on the energy barrier for the dehydration of Mg 2+ in the presence of carbonate remain lacking”
    Quote in the paperSubstantial claim0 of 3 sources checked
    • cites [27] source

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  • Probably not a substantial claim: may not pass S3 (load-bearing).

    Premisecitation

    The authors previously introduced AMOEBA parameters for Ca-carbonate in solution that improved Ca-carbonate ion binding free energies relative to earlier non-polarizable models.

    “We have recently introduced a new set of parameters based on the AMOEBA model for the interaction of calcium in solution with carbonate 26 that have improved the Ca-carbonate ion binding free energies compared to previous non-polarizable models.”
    Quote in the paperNot a substantial claim0 of 1 sources checked
    • cites [26] source

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  • Classified as probably not a substantial claim. May combine two claims.

    Premisecitation

    Hamm et al. found that aspartate did not affect the magnesium solvation sphere and did not appear to lower the energetic cost of dehydration, although they used the non-polarizable CHARMM22 force field.

    “Hamm et al. 28 found, using umbrella sampling, that the solvation sphere of magnesium was unaffected by the presence of aspartate, which did not seem to lower the energetic cost for dehydration, though they used the non-polarizable CHARMM22 force field for proteins.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [28] source

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  • May combine two claims.

    Premisecitation

    Mg2+ strongly polarizes its environment, a feature that fixed-charge rigid-ion force fields do not treat explicitly.

    “a second difficulty lies with the magnesium ion's tendency to strongly polarize its environment, 22 a feature that fixed charge rigid-ion force fields fail to consider explicitly.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [22] source

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  • May combine two claims.

    Study design and conductcitation

    The new rigid-ion force field was developed by targeting the experimental hydration free energy of the aqueous ions and using ab initio carbonate-water radial distribution functions to guide refitting of CO3-water interactions.

    “Analogously to the AMOEBA potential, we targeted the experimental hydration free energy of the aqueous ions reported by Marcus, 38 and we used the ab initio carbonate water radial distribution functions 26 to guide the refitting of the CO 3 -water interactions.”
    Quote in the paperSubstantial claim0 of 2 sources checked
    • cites [38] source

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    • cites [26] source

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  • May combine two claims. The quote only partly states this claim.

    Study design and conductown data

    The rigid-ion metadynamics simulations used 30 independent walkers and a bias factor of 20; repeating them with a bias factor of 30 produced no significant difference.

    “Because of the lower computational cost, this allowed for the simulations to be run with 30 independent walkers”
    • Also stated in: § Simulations with the rigid-ion force field · plain
      “for these simulations we used a bias factor of 20 to ensure that a correct description of the transition state was achieved.”
    • Also stated in: § Simulations with the rigid-ion force field · plain
      “we also repeated the simulations with a bias factor of 30, and no significant difference was observed.”
    Quote in the paperNot a substantial claim
  • Classified as probably not a substantial claim. May combine two claims.

    Study design and conductown data

    The AMOEBA metadynamics simulations used 16 independent walkers, a bias factor of 15, and at least 300 ns aggregate time to ensure well-converged sampling.

    “All the AMOEBA metadynamics simulations were run using 16 independent walkers with a bias factor of 15 for an aggregate simulation time of at least 300 ns to ensure well-converged sampling.”
    Quote in the paperSubstantial claim
  • Probably not a substantial claim: may not pass S3 (load-bearing).

    Premisecitation

    The AMOEBA model explicitly includes polarizability through static and self-consistent induced dipoles.

    “polarizability can be explicitly considered via a model such as AMOEBA that includes both static and self-consistent induced dipoles.25”
    Quote in the paperNot a substantial claim0 of 1 sources checked
    • cites [25] source

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  • May combine two claims.

    Interpretationown data

    The absence of water exchange suggests a water residence time greater than 50 ns and a high energy barrier for water exchange at Mg2+.

    “suggesting a water residence time greater than 50 ns and a high energy barrier for water exchange at Mg 2+ , in agreement with previous experimental 19 and theoretical 20,63 results.”
    Quote in the paperSubstantial claim0 of 3 sources checked
    • cites [19]

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    • cites [20] source

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    • cites [63] source

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  • Probably not a substantial claim: may not pass S3 (load-bearing), S4 (based).

    Study design and conductnone given

    Limiting as much as possible the size of the space explored during the AIMD and using two walkers should slightly reduce the bias due to the choice of the starting configuration.

    “Importantly, we have limited as much as possible the size of the space to be explored during the AIMD and have used two walkers, which should slightly reduce the bias due to the choice of the starting configuration.”
    Quote in the paperNot a substantial claim
  • May combine two claims.

    Study design and conductown data

    The well-tempered method does not flatten the free energy surface but reduces barrier heights by the magnitude of the chosen bias factor.

    “In fact the well-tempered method does not flatten out the free energy surface, but it reduces the barrier heights by the magnitude of the bias factor chosen, e.g a bias factor of 20 would reduce a free energy barrier of 60 kJ/mol to 3 kJ/mol, which can be easily overcome by thermal fluctuations (Figures S13 and S14 in the SI).”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Study design and conductreasoning

    A bias factor that is too small does not allow an accurate estimate of the free energy barrier, while a value that is too large wastes computational resources by making the simulation very slow to converge.

    “Hence, a bias factor that is too small does not allow for an accurate estimate of the free energy barrier, while using a value that is too large would waste computational resources by making the simulation very slow to converge.”
    Quote in the paperNot a substantial claim
  • May combine two claims.

    Study design and conductreasoning

    Starting each walker from different positions predetermines how the space will be explored; if the walkers cannot cross the free energy barriers, this limits the accuracy of barrier estimates and biases the relative stability of the free energy minima.

    “In fact, by starting each walker from different positions within the region of interest, we effectively predetermine how the space will be explored and if the walkers are not able to cross the free energy barriers, this not only limits our accuracy as to the estimate of the free energy barriers but it also biases the relative stability of the free energy minima.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Interpretationown data

    Because of the computational cost of the polarizable AMOEBA force field, such an extensive set of validation calculations could not be performed, but given the agreement between the results shown here, a similar degree of accuracy is expected.

    “Due to the computational cost of the polarizable AMOEBA force field we could not perform such an extensive set of validation calculations but given the agreement between the results shown here we would expect a similar degree of accuracy.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Study design and conductown data

    The free energies reported here have an accuracy comparable to kBT, with the caveat that the free energy barriers are a lower bound to the exact barrier on the real reaction coordinate.

    “Overall, we believe that the free energies reported here have an accuracy comparable to k B T , with the caveat that the free energy barriers are a lower bound to the exact barrier on the real reaction coordinate.”
    Quote in the paperSubstantial claim
  • Classified as probably not a substantial claim.

    Study design and conductreasoning

    Without knowing a priori the largest free energy barrier in the system, the appropriateness of the chosen bias factor can only be assessed in post-processing by monitoring the multiple walkers and ensuring that all free energy barriers are regularly crossed, particularly toward the end of the simulations.

    “Without knowing a priori what the largest free energy barrier in the system actually is, we can only assess whether the chosen bias factor is appropriate for the simulation in post-processing by monitoring the behaviour of the multiple walkers and making sure that all the free energy barriers are regularly crossed, particularly toward the end of the simulations.”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Interpretationown data

    The minimum free energy path on the 2D FES suggests that bidentate CIP formation first involves a decrease in the water coordination number while the Mg-C distance remains unchanged, followed by shortening of the Mg-C distance, in agreement with ab initio results.

    “the minimum free energy path on the 2D FES would suggest that, similarly to the SSHIP-to-monodentate transition, the formation of the bidentate CIP first involves a decrease of the water coordination number by Mg while the Mg-C distance remains unchanged, and then a shortening of the Mg-C distance, i.e. bidentate binding, in agreement”
    Quote in the paperSubstantial claim
  • May combine two claims.

    Study design and conductreasoning

    The coordination number CV introduces a bias potential on the coordination shell that is orthogonal to the distance CV and allows a more accurate description of the water exchange barrier.

    “Although the coordination number does not impose any symmetry on the structure of the hydration shell, it introduces a bias potential on the coordination shell that is orthogonal to the distance collective variable and allows for a more accurate description of the water exchange barrier.”
    Quote in the paperSubstantial claim
  • Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.

    Study design and conductnone given

    Any statistical error in the AIMD calculations is expected to be much larger than for the rigid-ion simulations, and strategies were employed to minimize the influence of this factor.

    “Although any statistical error is expected to be much larger than for the rigidion simulations, we have employed strategies to try minimize the influence of this factor.”
    Quote in the paperNot a substantial claim
  • Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.

    Study design and conductreasoning

    Non-reproducible free energy surfaces indicate either that an important slow collective variable has been missed or that the well-tempered parameters were not appropriate for the system.

    “Non-reproducible free energy surfaces are a clear indication that either an important (slow) collective variable has been missed or that the well-tempered parameters were not appropriate for the system at hand.”
    Quote in the paperNot a substantial claim
  • Classified as probably not a substantial claim.

    Premisecitation

    Water exchange around the Mg ion involves the concerted movement of all water molecules in the Mg2+ solvation shell to produce a symmetric transition state.

    “This choice of CVs was inspired by the work of Schwierz 3 where the water exchange around the Mg ion was found to involve the concerted movement of all the water molecules in the Mg 2+ solvation shell to produce a symmetric transition state.”
    Quote in the paperSubstantial claim0 of 1 sources checked
    • cites [3] source

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  • Probably not a substantial claim: may not pass S3 (load-bearing), S4 (based).

    Premisenone given

    The accurate calculation of water exchange rates around aqueous ions is not a trivial task, even after determining the free energy barrier, because transition state theory may not provide a reliable estimate without correction for recrossing events.

    “The accurate calculation of water exchange rates around aqueous ions is not a trivial task, even having determined the free energy barrier, since transition state theory may not provide a reliable estimate without correction for recrossing events.”
    Quote in the paperNot a substantial claim
  • May combine two claims.

    Interpretationreasoning

    Although the polarizable AMOEBA force field appears superior to the rigid-ion one, the latter would still provide a qualitatively accurate description of the thermodynamics of the aqueous Mg-CO3 system.

    “Although the polarizable AMOEBA force field appears to be superior to the rigid-ion one, the latter would still provide a qualitatively accurate description of the thermodynamics of the aqueous Mg-CO 3 system.”
    Quote in the paperSubstantial claim
  • Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.

    Premisecitation

    Lincoln suggested that each metal ion-ligand complex behaves differently; for example, he reported that CrO4^2- increases the water lability of the aqueous Ca2+ ion but has little effect on the water exchange around Mg2+.

    “However, Lincoln 69 suggested that each metal ion-ligand complex behaves differently; for example he reported that CrO 2 - 4 increases the water lability of the aqueous Ca 2+ ion but has little effect on the water exchange around Mg 2+ , therefore more experimental work on the magnesium carbonate system is required to corroborate our results.”
    Quote in the paperNot a substantial claim0 of 1 sources checked
    • cites [69] source

      Not checked in the free run.

  • Classified as probably not a substantial claim.

    Interpretationreasoning

    Due to its lower computational cost, the rigid-ion force field could be more readily used to explore Mg/CaCO3 nucleation and growth processes where long simulations with large systems are needed.

    “Due to its lower computational cost, this rigid-ion force field could therefore be more readily used to explore Mg/CaCO 3 nucleation and growth processes where long simulations with large systems need to be used.”
    Quote in the paperSubstantial claim
  • Probably not a substantial claim: may not pass S2 (checkable), S3 (load-bearing), S4 (based).

    Interpretationnone given

    The presence of ion pairs could also play a significant role in a wide range of geochemical phenomena such as ion adsorption, nucleation and biomineralization, and could have significant implications in biochemistry.

    “The presence of ion pairs could also play a significant role in a wide range of geochemical phenomena such as ion adsorption, nucleation and biomineralization, and this result could have significant implications in biochemistry where the transport of Mg 2+ ions across cell membranes and their catalytic activity help regulate many physiological processes in living organisms.”
    Quote in the paperNot a substantial claim
  • Probably not a substantial claim: may not pass S3 (load-bearing).

    Premisecitation

    Similar behaviour has been reported for other metal ion-ligand complexes.

    “Similar behaviour has been reported for other metal ion-ligand complexes, 69,70 but to the best of our knowledge no experimental values are available for water exchange around the Mg-CO 3 complex.”
    Quote in the paperNot a substantial claim0 of 2 sources checked
    • cites [69] source

      Not checked in the free run.

    • cites [70] source

      Not checked in the free run.

56 of 56
  • The paper relies on this without support.

    The total free energy of the system does not depend on which water molecule coordinates the Mg2+ ion.

    “Despite the fact that the system's total free energy is independent of which water molecule coordinates the Mg 2+ ion”
  • The paper relies on this without support.

    No experimental values are available for water exchange around the Mg-CO3 complex.

    “but to the best of our knowledge no experimental values are available for water exchange around the Mg-CO 3 complex”
  • The paper relies on this without support.

    Water exchange around aqueous Mg2+ is the rate-limiting step for the nucleation of magnesium-bearing minerals.

    “which is generally regarded as the rate-limiting step for the nucleation of magnesium-bearing minerals”
3 of 3

Self-check

Percentages, sums and reported differences re-computed from the paper’s own numbers.

Each contradiction between two passages listed here was confirmed by an independent check.

  • Ion-pairing source is assigned the wrong reference number

    Minor

    The text attributes the experimental ion-pairing value to De Visscher et al. as reference 67, but the bibliography lists De Visscher et al. as reference 68.

1 of 1

Cites

Flagged first, then by citations

Research works printed but not linked: 2

  1. Kaczmarek, S. E.; Gregg, J. M.; Bish, D. L.; Machel, H. G.; Fouke, B. W. Characterization and Modeling of Carbonates-Mountjoy Symposium 1; SEPM (Society for Sedimentary Geology), 2017; pp 7–20.
  2. Mills R., 1989, Self-Diffusion in Electrolyte Solutions

Authors
Aufort, J., Raiteri, P., & Gale, J. D.
Affiliations
  • Centre National de la Recherche Scientifique (FR)
  • Curtin University (AU)
Corresponding author
Raiteri, Paolo
Venue
ACS Earth and Space Chemistry
Published
2022-02-16
Volume
6
Issue
3
Pages
733-745
ISSN
2472-3452 (ISSN-L)
OpenAlex
W4212848184
Cited by
26
References
70
Citations by year
2026: 6 · 2025: 4 · 2024: 6 · 2023: 9 · 2022: 1
FWCI
1.25
Type
journal article
Language
en
Open access
Locations
  • ACS Earth and Space Chemistry (publishedVersion)
  • eSpace (Curtin University) (submittedVersion)
  • HAL (submittedVersion)
Funders
Australian Research Council (FL180100087)
Topics
  • Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
  • Physical Sciences › Physics and Astronomy › Atomic and Molecular Physics, and Optics › Advanced Chemical Physics Studies
  • Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
Keywords
magnesium carbonate, water exchange, ion pairing, free energy, polarizable force field, amoebae, metadynamics, aqueous solutions

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Claims read by deepseek-v4.1-flash under definition version 3 (extract-v3) on 2026-10-05.

Classified by jev-1.13-20260917 (gold-guideline-v0.2) on 2026-10-05.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

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