REVIEW 3 major objections 4 minor 62 references
Kolmogorov-Arnold networks, with spline-based learnable activations, can replace costly Gibbs-energy-minimization solvers for geochemical equilibria, cutting errors versus multilayer perceptrons by 62% and evaluation time by up to 93%.
Reviewed by Pith at T0; open to challenge. T0 means a machine referee read the full paper against a public rubric. the ladder, T0–T4 →
T0 review · deepseek-v4-flash
2026-08-04 05:45 UTC pith:55HACMNP
load-bearing objection A credible, well-documented first KAN application to radionuclide coprecipitation surrogates, but the headline KAN-over-MLP claim rests on a single benchmark and single training runs. the 3 major comments →
A Kolmogorov-Arnold Surrogate Model for Chemical Equilibria: Application to Solid Solutions
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
The paper's central claim is that for the chemical systems and input ranges studied, Kolmogorov-Arnold networks are strictly better surrogates than multilayer perceptrons: lower absolute and relative errors at equal or smaller parameter counts, no degradation as thermodynamic complexity increases to non-ideal ternary solid solutions, and evaluation times roughly an order of magnitude faster than the reference Gibbs-energy-minimization solver. The KAN replaces each fixed neuron activation with a learnable B-spline, letting the network fit sharp composition-dependent solubility behavior with fewer parameters. The study is, per the authors, the first surrogate model for radionuclide coprecipita
What carries the argument
The Kolmogorov-Arnold network is the load-bearing object: its learnable univariate B-spline activation functions sit on every connection, and the composition of these one-dimensional functions plus addition is what approximates the equilibrium state mapping. The paper also relies on a regular solid-solution model with binary interaction parameters to generate training data of increasing thermodynamic complexity, and on low-discrepancy Sobol sampling to cover the input space.
Load-bearing premise
That the Gibbs-energy-minimization solver with its thermodynamic database gives the correct equilibrium, and that accuracy measured on one-time Sobol-sampled equilibrium states carries over to the time-stepped reactive transport settings where the surrogate would be deployed.
What would settle it
Generate equilibria with the reference solver at compositions and temperatures outside the sampled ranges, especially near solid-solution miscibility or phase-boundary transitions, and check whether KAN errors stay below the 10% threshold; alternatively, couple the KAN to a reactive transport code and track total mass balance over hundreds of time steps. If either test shows errors above 10% or systematic mass drift, the central claim that KANs can replace the solver fails.
If this is right
- On the tested input ranges, the KAN surrogate can replace the Gibbs-energy-minimization solver for one-shot equilibrium predictions, keeping median relative errors near 0.1%.
- The 87–93% per-evaluation speedup translates, in principle, to reactive transport simulations that currently spend most of their runtime on chemistry.
- KANs achieve this with fewer trainable parameters than MLPs, lowering memory requirements for storing the model inside large simulation codes.
- Treating temperature as an input variable opens the door to temperature-scanning safety assessments that were previously too expensive.
- The longer KAN training time, on the order of minutes, is a one-time cost amortized over billions of subsequent evaluations.
Where Pith is reading between the lines
- The reported speedups are per-equilibrium-call, not end-to-end reactive transport speedups; time-dependent coupling, mass-conservation drift, and error accumulation remain unmeasured, so the practical simulation speedup could be smaller.
- Because the network is trained entirely on solver-generated points, its accuracy is bounded by the thermodynamic database; a systematically wrong reference model would make the surrogate confidently wrong.
- Error statistics over Sobol samples may not hold near phase boundaries or outside the sampled ranges; extrapolation testing would tell whether the surrogate can be trusted for exploratory safety assessments.
- The spline activations could be inspected to recover interpretable composition-to-solubility relationships, offering a route from black-box prediction to thermodynamic insight.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper proposes Kolmogorov-Arnold networks (KANs) as surrogate models for geochemical equilibrium calculations. It first benchmarks KANs against a published multilayer perceptron (MLP) on a CaO-SiO2-H2O cement hydration dataset, reporting 62% and 59% reductions in absolute and relative error, respectively. It then builds GEM-Selektor datasets for three radium sulfate cases of increasing thermodynamic complexity: a mechanical mixture, a binary (Ba,Ra)SO4 solid solution, and a ternary (Sr,Ba,Ra)SO4 solid solution. For these cases, the paper reports median relative errors near 1e-3, no test predictions exceeding a 10% error threshold for the binary and ternary solid-solution cases, and 87-93% reductions in evaluation time relative to GEM-Selektor. The datasets, GEM-Selektor input files, and generation scripts are made publicly available.
Significance. If the reported results are robust, the paper would provide useful evidence that KANs are viable surrogates for expensive Gibbs-energy-minimization solvers over bounded input ranges, and it would be the first surrogate-model study of radionuclide co-precipitation in sulfate solid solutions. The open-data policy and the use of a well-established thermodynamic database are strengths, as is the systematic progression from mechanical mixtures to binary and ternary solid solutions. The central quantitative claim, however, is the KAN-over-MLP improvement on the cement benchmark, and that claim rests on a comparison whose fairness and statistical reliability are not yet established. The work is a solid application-oriented contribution if the comparison is placed on equal footing and uncertainty quantification is added.
major comments (3)
- [Section 4.1, Tables 2-3] The headline 62%/59% improvements compare two KAN configurations against an MLP taken verbatim from Prasianakis et al. with no Optuna re-tuning on the current train/validation/test split. Sections 3.1 and 3.2 state that both MLPs and KANs use Optuna for hyperparameter selection, but in Section 4.1 only the KANs appear to be selected or tuned for this dataset; the MLP is fixed as the 'reference model.' This asymmetry is load-bearing because the central claim is architectural superiority. Please retune the MLP on the same split with a comparable search budget, or clearly justify why the literature MLP is the correct baseline, and report the resulting error distributions.
- [Section 4.2, dataset split] The text says datasets of size 2^m are 'split in half to obtain the training and validation sets. From the latter, 5000 points are subtracted for testing.' If the test points are a subset of the validation set used for early stopping or learning-rate scheduling, the test errors are optimistically biased. Please clarify whether the test set was held out before training and never used for model selection; if not, redesign the split so that training, validation, and test subsets are disjoint.
- [Figures 4-7, Tables 2-5] All reported errors, medians, high-error counts, and run-time improvements come from single training runs with no seed-level statistics. Given the noise in neural-network training, a single favorable seed cannot be distinguished from genuine architecture-level advantage, especially for the claim that 'no predictions exceed the 10% error threshold' in Sections 4.3-4.4. Please repeat training for at least 5-10 seeds, report median/interquartile ranges or worst-case error, and state whether the no-threshold-exceedance claim holds across all seeds.
minor comments (4)
- [Equation (6)] The nested composition formula for the MLP has malformed superscripts and parentheses (e.g., 'f n+1' and misplaced b terms). Please rewrite it with consistent indexing for readability.
- [Tables 2-3] The variable 'AmorfSi' appears to be a typo; please use a consistent naming convention. Also, define the units for the RMSE columns or note that they are in the scaled/log-transformed space.
- [Figure 4-7] The box plots lack axis labels and legend definitions. Please add explicit labels (e.g., 'Output variable' on the x-axis, 'Relative error' on the y-axis) and explain what the red counts represent in captions.
- [Section 4.5 and 5] The discussion appropriately acknowledges that only one-time equilibria were studied and that mass conservation remains an issue for time-dependent reactive transport. Please make the scope limitation more explicit in the abstract or introduction so that the strong wording in the Conclusion does not overstate readiness for RTM deployment.
Circularity Check
No circular derivation: KAN/MLP accuracy claims are empirical supervised fits against external solver outputs; thermodynamic parameters are imported literature inputs, not fitted or derived here.
full rationale
The paper makes no claimed derivation from first principles; its central results are supervised-learning accuracies and runtime measurements. Thermodynamic inputs (Margules parameters, PSI-Nagra database, GEM-Selektor mixing models) are imported from prior external literature (e.g., Vinograd et al. 2018) and are not fitted or derived in this work. The GEM-Selektor-generated datasets serve as training labels, and evaluating on held-out solver points is standard supervised approximation testing, not a circular 'prediction' in the derivational sense. The KAN-versus-MLP comparison is an empirical benchmark: Section 4.2 states both models are trained on identical datasets, and the cement benchmark uses a pre-published reference MLP from Prasianakis et al. Possible asymmetric hyperparameter tuning is a benchmark-fairness and correctness concern, not circularity, because the comparison does not reduce to an identity, fitted parameter, or self-citation. The self-citations to prior geochemical studies provide thermodynamic context and parameter values rather than load-bearing uniqueness arguments or ansatz smuggling. Section 4.5 explicitly acknowledges the scope limitation to one-time equilibrium predictions and the risk of mass-conservation error accumulation in reactive transport, which is an external-validity caveat, not a circular step. Thus no specific reduction to inputs by construction can be exhibited.
Axiom & Free-Parameter Ledger
free parameters (4)
- KAN architecture hyperparameters, cement KAN1 =
4 hidden layers, 28 neurons/layer, spline order 7, 10 grid points
- KAN architecture hyperparameters, cement KAN2 =
5 hidden layers, 40 neurons/layer, spline order 8, 12 grid points, ~1.5e5 parameters
- KAN architecture hyperparameters, radium cases =
Mechanical mixing: Optuna-selected up to 4 layers/24 neurons/order 8/15 grid points; binary: 3 layers/24 neurons/order 8
- Training hyperparameters (batch size, learning rate, scheduler, epochs) =
Batch size 192, initial learning rate 0.01, reduce-on-plateau scheduler, 100-200 epochs
axioms (5)
- domain assumption GEM-Selektor/TSolMod Gibbs-energy minimization is the correct ground truth for chemical equilibria.
- domain assumption The PSI-Nagra 12/07 thermodynamic database and SUPCRT98/92 equations of state are accurate for the studied species.
- domain assumption The regular solution model with Margules parameters w_RaBa = 2470, w_SrRa = 1750, w_SrBa = 750 J/mol from [47] describes binary and ternary sulfate solid-solution mixing.
- standard math The Kolmogorov-Arnold representation theorem holds for the target functions and the specific spline parameterization is sufficiently expressive.
- domain assumption The cement benchmark dataset published by Prasianakis et al. [23] is valid, and the Sobol-sampled input ranges in Table 1 are representative of repository-relevant conditions.
read the original abstract
The computational cost of geochemical solvers is a challenging matter. For reactive transport simulations, where chemical calculations are performed up to billions of times, it is crucial to reduce the total computational time. Existing publications have explored various machine-learning approaches to determine the most effective data-driven surrogate model. In particular, multilayer perceptrons are widely employed due to their ability to recognize nonlinear relationships. In this work, we focus on the recent Kolmogorov-Arnold networks, where learnable spline-based functions replace classical fixed activation functions. This architecture has achieved higher accuracy with fewer trainable parameters and has become increasingly popular for solving partial differential equations. First, we train a surrogate model based on an existing cement system benchmark. Then, we move to an application case for the geological disposal of nuclear waste, i.e., the determination of radionuclide-bearing solids solubilities. To the best of our knowledge, this work is the first to investigate co-precipitation with radionuclide incorporation using data-driven surrogate models, considering increasing levels of thermodynamic complexity from simple mechanical mixtures to non-ideal solid solutions of binary (Ba,Ra)SO$_4$ and ternary (Sr,Ba,Ra)SO$_4$ systems. On the cement benchmark, we demonstrate that the Kolmogorov-Arnold architecture outperforms multilayer perceptrons in both absolute and relative error metrics, reducing them by 62% and 59%, respectively. On the binary and ternary radium solid solution models, Kolmogorov-Arnold networks maintain median prediction errors near $1\times10^{-3}$. This is the first step toward employing surrogate models to speed up reactive transport simulations and optimize the safety assessment of deep geological waste repositories.
Figures
Reference graph
Works this paper leans on
-
[1]
C. Steefel, D. Depaolo, P. Lichtner, Reactive transport modeling: An essential tool and a new research approach for the Earth sciences, Earth and Planetary Science Letters 240 (3-4) (2005) 539–558. doi:10.1016/j.epsl. 2005.09.017
doi:10.1016/j.epsl 2005
-
[2]
C. I. Steefel, Reactive Transport at the Crossroads, Reviews in Mineralogy and Geochemistry 85 (1) (2019) 1–26. doi:10.2138/rmg.2019.85.1
-
[3]
Q. Kang, P. C. Lichtner, H. S. Viswanathan, A. I. Abdel-Fattah, Pore Scale Modeling of Reactive Transport Involved in Geologic CO2 Sequestration, Transport in Porous Media 82 (1) (2010) 197–213. doi:10.1007/ s11242-009-9443-9
2010
-
[4]
D. Liu, R. Agarwal, Y . Li, S. Yang, Reactive transport modeling of mineral carbonation in unaltered and altered basalts during CO2 sequestration, International Journal of Greenhouse Gas Control 85 (2019) 109–120. doi:10.1016/j.ijggc.2019.04.006
-
[5]
A. Yapparova, G. D. Miron, D. A. Kulik, G. Kosakowski, T. Driesner, An advanced reactive transport simulation scheme for hydrothermal systems modelling, Geothermics 78 (2019) 138–153. doi:10.1016/j.geothermics. 2018.12.003
-
[6]
S. Erol, T. Akın, A. Ba¸ ser, Ö. Saraço˘glu, S. Akın, Fluid-CO2 injection impact in a geothermal reservoir: Evaluation with 3-D reactive transport modeling, Geothermics 98 (2022) 102271. doi:10.1016/j.geothermics.2021. 102271
-
[7]
A. Visser, H. P. Broers, R. Heerdink, M. F. P. Bierkens, Trends in pollutant concentrations in relation to time of recharge and reactive transport at the groundwater body scale, Journal of Hydrology 369 (3) (2009) 427–439. doi:10.1016/j.jhydrol.2009.02.008
-
[8]
B. Leterme, P. Blanc, D. Jacques, A reactive transport model for mercury fate in soil—application to different anthropogenic pollution sources, Environmental Science and Pollution Research 21 (21) (2014) 12279–12293. doi:10.1007/s11356-014-3135-x
-
[9]
J. M. Paz-García, B. Johannesson, L. M. Ottosen, A. N. Alshawabkeh, A. B. Ribeiro, J. M. Rodríguez-Maroto, Modeling of electrokinetic desalination of bricks, Electrochimica Acta 86 (2012) 213–222. doi:10.1016/j. electacta.2012.05.132
doi:10.1016/j 2012
-
[10]
L. Montenegro, J. Samper, A. Mon, L. De Windt, A.-C. Samper, E. García, A non-isothermal reactive transport model of the long-term geochemical evolution at the disposal cell scale in a hlw repository in granite, Applied Clay Science 242 (2023) 107018.doi:https://doi.org/10.1016/j.clay.2023.107018
arXiv 2023
-
[11]
F. Claret, N. I. Prasianakis, A. Baksay, D. Lukin, G. Pepin, E. Ahusborde, B. Amaziane, G. Bátor, D. Becker, A. Bednár, M. Béreš, S. Bérešová, Z. Böthi, V . Brendler, K. Brenner, J. B ˇrezina, F. Chave, S. V . Churakov, M. Hokr, D. Horák, D. Jacques, F. Jankovský, C. Kazymyrenko, T. Koudelka, T. Kovács, T. Krej ˇcí, J. Kruis, E. Laloy, J. Landa, T. Ligurs...
arXiv 2024
-
[12]
J. Samper, C. López-Vázquez, B. Pisani, A. Mon, A. C. Samper-Pilar, F. J. Samper-Pilar, Global sensitivity analysis of reactive transport modelling for the geochemical evolution of a high-level radioactive waste repository, Applied Geochemistry 180 (2025) 106286.doi:10.1016/j.apgeochem.2025.106286
arXiv 2025
-
[13]
Kolditz, D
O. Kolditz, D. Jacques, F. Claret, J. Bertrand, S. V . Churakov, C. Debayle, D. Diaconu, K. Fuzik, D. Garcia, N. Graebling, B. Grambow, E. Holt, A. Idiart, P. Leira, V . Montoya, E. Niederleithinger, M. Olin, W. Pfingsten, N. I. Prasianakis, K. Rink, J. Samper, I. Szöke, R. Szöke, L. Theodon, J. Wendling, Digitalisation for nuclear waste management: predi...
2023
-
[14]
A. M. M. Leal, D. A. Kulik, W. R. Smith, M. O. Saar, An overview of computational methods for chemical equilibrium and kinetic calculations for geochemical and reactive transport modeling, Pure and Applied Chemistry 89 (5) (2017) 597–643.doi:10.1515/pac-2016-1107
-
[15]
A. M. M. Leal, S. Kyas, D. A. Kulik, M. O. Saar, Accelerating Reactive Transport Modeling: On-Demand Machine Learning Algorithm for Chemical Equilibrium Calculations, Transport in Porous Media 133 (2) (2020) 161–204.doi:10.1007/s11242-020-01412-1. 13 L. Boledi et al. Preprint submitted to ArXiv
-
[16]
M. De Lucia, M. Kühn, A. Lindemann, M. Lübke, B. Schnor, POET (v0.1): speedup of many-core parallel reactive transport simulations with fast DHT lookups, Geoscientific Model Development 14 (12) (2021) 7391– 7409, publisher: Copernicus GmbH.doi:10.5194/gmd-14-7391-2021
-
[17]
M. Lübke, M. De Lucia, S. Petri, B. Schnor, A Fast MPI-Based Distributed Hash-Table as Surrogate Model for HPC Applications, in: M. H. Lees, W. Cai, S. A. Cheong, Y . Su, D. Abramson, J. J. Dongarra, P. M. A. Sloot (Eds.), Computational Science – ICCS 2025, Springer Nature Switzerland, Cham, 2025, pp. 233–240. doi:10.1007/978-3-031-97635-3_28
-
[18]
S. Kyas, D. V olpatto, M. O. Saar, A. M. M. Leal, Accelerated reactive transport simulations in heterogeneous porous media using Reaktoro and Firedrake, Computational Geosciences 26 (2) (2022) 295–327. doi:10.1007/ s10596-021-10126-2
2022
-
[19]
E. Laloy, D. Jacques, Emulation of CPU-demanding reactive transport models: a comparison of Gaussian processes, polynomial chaos expansion, and deep neural networks, Computational Geosciences 23 (5) (2019) 1193–1215.doi:10.1007/s10596-019-09875-y
-
[20]
E. Laloy, D. Jacques, Speeding Up Reactive Transport Simulations in Cement Systems by Surrogate Geochemical Modeling: Deep Neural Networks and k-Nearest Neighbors, Transport in Porous Media 143 (2) (2022) 433–462. doi:10.1007/s11242-022-01779-3
-
[21]
E. Demirer, E. Coene, A. Iraola, A. Nardi, E. Abarca, A. Idiart, G. de Paola, N. Rodríguez-Morillas, Improving the Performance of Reactive Transport Simulations Using Artificial Neural Networks, Transport in Porous Media 149 (1) (2023) 271–297.doi:10.1007/s11242-022-01856-7
-
[22]
V . L. S. Silva, G. Regnier, P. Salinas, C. E. Heaney, M. D. Jackson, C. C. Pain, Rapid modelling of reactive transport in porous media using machine learning: limitations and solutions, arXiv:2405.14548 [cs] (2025). doi:10.48550/arXiv.2405.14548
work page internal anchor Pith review Pith/arXiv arXiv doi:10.48550/arxiv.2405.14548 2025
-
[23]
N. I. Prasianakis, E. Laloy, D. Jacques, J. C. L. Meeussen, G. D. Miron, D. A. Kulik, A. Idiart, E. Demirer, E. Coene, B. Cochepin, M. Leconte, M. E. Savino, J. Samper-Pilar, M. De Lucia, S. V . Churakov, O. Kolditz, C. Yang, J. Samper, F. Claret, Geochemistry and machine learning: methods and benchmarking, Environmental Earth Sciences 84 (5) (2025) 121.d...
-
[24]
Z. Liu, Y . Wang, S. Vaidya, F. Ruehle, J. Halverson, M. Soljaˇci´c, T. Y . Hou, M. Tegmark, KAN: Kolmogorov- Arnold Networks, arXiv:2404.19756 [cs] (2025).doi:10.48550/arXiv.2404.19756
-
[25]
C. Guo, L. Sun, S. Li, Z. Yuan, C. Wang, Physics-informed Kolmogorov–Arnold network with Chebyshev polynomials for fluid mechanics, Physics of Fluids 37 (9) (2025) 095120.doi:10.1063/5.0284999
-
[26]
K. Xu, L. Chen, S. Wang, Kolmogorov-Arnold Networks for Time Series: Bridging Predictive Power and Interpretability, arXiv:2406.02496 [cs] (2024).doi:10.48550/arXiv.2406.02496
-
[27]
L. Li, Y . Zhang, G. Wang, K. Xia, Kolmogorov–Arnold graph neural networks for molecular property prediction, Nature Machine Intelligence 7 (8) (2025) 1346–1354, publisher: Nature Publishing Group. doi:10.1038/ s42256-025-01087-7
2025
-
[28]
A. D. Bodner, A. S. Tepsich, J. N. Spolski, S. Pourteau, Convolutional Kolmogorov-Arnold Networks, arXiv:2406.13155 [cs] (2025).doi:10.48550/arXiv.2406.13155
-
[29]
M. Kiamari, M. Kiamari, B. Krishnamachari, GKAN: Graph Kolmogorov-Arnold Networks, arXiv:2406.06470 [cs] (2024).doi:10.48550/arXiv.2406.06470
-
[30]
K. Shukla, J. D. Toscano, Z. Wang, Z. Zou, G. E. Karniadakis, A comprehensive and FAIR comparison between MLP and KAN representations for differential equations and operator networks, Computer Methods in Applied Mechanics and Engineering 431 (2024) 117290.doi:10.1016/j.cma.2024.117290
arXiv 2024
-
[31]
Y . Hou, T. Ji, D. Zhang, A. Stefanidis, Kolmogorov-Arnold Networks: A Critical Assessment of Claims, Performance, and Practical Viability, arXiv:2407.11075 [cs] (2025).doi:10.48550/arXiv.2407.11075
-
[32]
J. D. Toscano, V . Oommen, A. J. Varghese, Z. Zou, N. Ahmadi Daryakenari, C. Wu, G. E. Karniadakis, From PINNs to PIKANs: recent advances in physics-informed machine learning, Machine Learning for Computational Science and Engineering 1 (1) (2025) 15.doi:10.1007/s44379-025-00015-1
-
[33]
B. Jacob, A. A. Howard, P. Stinis, SPIKANs: separable physics-informed Kolmogorov–Arnold networks, Machine Learning: Science and Technology 6 (3) (2025) 035060, publisher: IOP Publishing. doi:10.1088/2632-2153/ ae05af
-
[34]
T. Wagner, D. A. Kulik, F. F. Hingerl, S. V . Dmytrieva, GEM-SELEKTOR GEOCHEMICAL MODELING PACKAGE: TSolMod LIBRARY AND DATA INTERFACE FOR MULTICOMPONENT PHASE MODELS, The Canadian Mineralogist 50 (5) (2012) 1173–1195.doi:10.3749/canmin.50.5.1173. 14 L. Boledi et al. Preprint submitted to ArXiv
-
[35]
D. A. Kulik, T. Wagner, S. V . Dmytrieva, G. Kosakowski, F. F. Hingerl, K. V . Chudnenko, U. R. Berner, GEM- Selektor geochemical modeling package: revised algorithm and GEMS3K numerical kernel for coupled simulation codes, Computational Geosciences 17 (1) (2013) 1–24.doi:10.1007/s10596-012-9310-6
-
[36]
T. Zhang, K. Gregory, R. W. Hammack, R. D. Vidic, Co-precipitation of Radium with Barium and Strontium Sulfate and Its Impact on the Fate of Radium during Treatment of Produced Water from Unconventional Gas Extraction, Environmental Science & Technology 48 (8) (2014) 4596–4603.doi:10.1021/es405168b
-
[37]
Programme for research, development and demonstration of methods for the management and disposal of nuclear waste, Tech
SKB, RD&D Programme 2022. Programme for research, development and demonstration of methods for the management and disposal of nuclear waste, Tech. Rep. TR-22-11, Svensk Kärnbränslehantering AB (2022)
2022
-
[38]
F. Brandt, E. Curti, M. Klinkenberg, K. Rozov, D. Bosbach, Replacement of barite by a (Ba,Ra)SO4 solid solution at close-to-equilibrium conditions: A combined experimental and theoretical study, Geochimica et Cosmochimica Acta 155 (2015) 1 – 15.doi:10.1016/j.gca.2015.01.016
-
[39]
F. Brandt, M. Klinkenberg, J. Poonoosamy, J. Weber, D. Bosbach, The Effect of Ionic Strength and Sraq upon the Uptake of Ra during the Recrystallization of Barite, Minerals 8 (11) (2018).doi:10.3390/min8110502
-
[40]
F. Brandt, M. Klinkenberg, J. Poonoosamy, D. Bosbach, Recrystallization and Uptake of 226Ra into Ba-Rich (Ba,Sr)SO4 Solid Solutions, Minerals 10 (9) (2020) 1 – 28.doi:10.3390/min10090812
-
[41]
M. Klinkenberg, F. Brandt, U. Breuer, D. Bosbach, Uptake of Ra during the Recrystallization of Barite: A Microscopic and Time of Flight-Secondary Ion Mass Spectrometry Study, Environmental Science and Technology 48 (12) (2014) 6620 – 6627.doi:10.1021/es405502e
-
[42]
M. Klinkenberg, J. Weber, J. Barthel, V . Vinograd, J. Poonoosamy, M. Kruth, D. Bosbach, F. Brandt, The solid solution–aqueous solution system (Sr,Ba,Ra)SO4 + H2O: A combined experimental and theoretical study of phase equilibria at Sr-rich compositions, Chemical Geology 497 (2018) 1 – 17. doi:10.1016/j.chemgeo.2018.08. 009
-
[43]
J. Poonoosamy, A. Kaspor, C. Schreinemachers, D. Bosbach, O. Cheong, P. M. Kowalski, A. Obaied, A radio- chemical lab-on-a-chip paired with computer vision to unlock the crystallization kinetics of (Ba,Ra)SO4, Scientific Reports 14 (2024) 9502.doi:10.1038/s41598-024-59888-6
-
[44]
J. Weber, J. Barthel, M. Klinkenberg, D. Bosbach, M. Kruth, F. Brandt, Retention of226Ra by barite: The role of internal porosity, Chemical Geology 466 (2017) 722 – 732.doi:10.1016/j.chemgeo.2017.07.021
-
[45]
V . Vinograd, F. Brandt, K. Rozov, M. Klinkenberg, K. Refson, B. Winkler, D. Bosbach, Solid-aqueous equilibrium in the BaSO4 RaSO4 H2O system: First-principles calculations and a thermodynamic assessment, Geochimica et Cosmochimica Acta 122 (2013) 398 – 417.doi:10.1016/j.gca.2013.08.028
-
[46]
V . Vinograd, D. Kulik, F. Brandt, M. Klinkenberg, J. Weber, B. Winkler, D. Bosbach, Thermodynamics of the solid solution - Aqueous solution system (Ba,Sr,Ra)SO4 + H2O: II. Radium retention in barite-type minerals at elevated temperatures, Applied Geochemistry 93 (2018) 190 – 208.doi:10.1016/j.apgeochem.2017.10.019
-
[47]
V . Vinograd, D. Kulik, F. Brandt, M. Klinkenberg, J. Weber, B. Winkler, D. Bosbach, Thermodynamics of the solid solution - Aqueous solution system (Ba,Sr,Ra)SO 4 + H2O: I. The effect of strontium content on radium uptake by barite, Applied Geochemistry 89 (2018) 59 – 74.doi:10.1016/j.apgeochem.2017.11.009
-
[48]
Hummel, U
W. Hummel, U. Berner, E. Curti, F. J. Pearson, T. Thoenen, Nagra/PSI Chemical Thermodynamic Data Base 01/01, Universal-Publishers, 2002
2002
-
[49]
Thoenen, W
T. Thoenen, W. Hummel, U. Berner, E. Curti, The PSI/Nagra Chemical Thermodynamic Database 12/07 (2014)
2014
-
[50]
H. Helgeson, D. Kirkham, G. Flowers, Theoretical prediction of the thermodynamic behavior of aqueous electrolytes by high pressures and temperatures; IV, Calculation of activity coefficients, osmotic coefficients, and apparent molal and standard and relative partial molal properties to 600 degrees C and 5kb, American Journal of Science 281 (10) (1981) 124...
-
[51]
J. W. Johnson, E. H. Oelkers, H. C. Helgeson, SUPCRT92: A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1 to 5000 bar and 0 to 1000°C, Computers and Geosciences 18 (7) (1992) 899 – 947.doi:10.1016/0098-3004(92)90029-Q
-
[52]
Y . Wang, P. Alt-Epping, G. Deissmann, Y . Yang, J. Hu, D. Bosbach, J. Poonoosamy, Contrasting coprecipitation and recrystallization mechanisms for Ra immobilization via (Ba,Ra)SO 4 solid solution formation in fractured crystalline rocks: Insights from 3D reactive transport modeling, Geochimica et Cosmochimica Acta (2026). doi:10.1016/j.gca.2026.01.045
-
[53]
I. M. Sobol’, On the distribution of points in a cube and the approximate evaluation of integrals, USSR Computa- tional Mathematics and Mathematical Physics 7 (4) (1967) 86–112.doi:10.1016/0041-5553(67)90144-9. 15 L. Boledi et al. Preprint submitted to ArXiv
-
[54]
Williams, S
B. Williams, S. Cremaschi, Novel Tool for Selecting Surrogate Modeling Techniques for Surface Approxi- mation, in: Computer Aided Chemical Engineering, V ol. 50, Elsevier, 2021, pp. 451–456. doi:10.1016/ B978-0-323-88506-5.50071-1
2021
-
[55]
C. G. Hounmenou, K. E. Gneyou, R. L. Glele Kakaï, A Formalism of the General Mathematical Expression of Multilayer Perceptron Neural Networks (2021).doi:10.20944/preprints202105.0412.v1
arXiv 2021
-
[56]
K. Y . Chan, B. Abu-Salih, R. Qaddoura, A. M. Al-Zoubi, V . Palade, D.-S. Pham, J. D. Ser, K. Muhammad, Deep neural networks in the cloud: Review, applications, challenges and research directions, Neurocomputing 545 (2023) 126327.doi:10.1016/j.neucom.2023.126327
arXiv 2023
-
[57]
Falcon, The PyTorch Lightning team, PyTorch Lightning (2019).doi:10.5281/zenodo.3828935
W. Falcon, The PyTorch Lightning team, PyTorch Lightning (2019).doi:10.5281/zenodo.3828935. URLhttps://github.com/Lightning-AI/lightning
-
[58]
T. Akiba, S. Sano, T. Yanase, T. Ohta, M. Koyama, Optuna: A Next-generation Hyperparameter Optimization Framework, in: Proceedings of the 25th ACM SIGKDD International Conference on Knowledge Discovery & Data Mining, KDD ’19, Association for Computing Machinery, New York, NY , USA, 2019, pp. 2623–2631. doi:10.1145/3292500.3330701
arXiv 2019
-
[59]
H. Prautzsch, W. Boehm, M. Paluszny, Bézier and B-Spline Techniques, Mathematics and Visualization, Springer, Berlin, Heidelberg, 2002.doi:10.1007/978-3-662-04919-8
-
[60]
Blealtan, A
C. Blealtan, A. Dash, efficient-kan (2024). URLhttps://github.com/Blealtan/efficient-kan
2024
-
[61]
Prasianakis, E
N. Prasianakis, E. Laloy, D. Jacques, J. Meeussen, C. Tournassat, G. Miron, D. Kulik, A. Idiart, E. Demirer, E. Coene, B. Cochepin, M. Leconte, M. Savino, J. Samper II, M. De Lucia, S. Churakov, O. Kolditz, C. Yang, J. Samper, F. Claret, Geochemistry and Machine Learning: Methods and Benchmarking (2025). doi:10.5281/ zenodo.14904784
2025
-
[62]
H. Peng, A. Rajyaguru, E. Curti, D. Grolimund, S. V . Churakov, N. I. Prasianakis, Machine Learning-Enhanced Modeling of Calcium Carbonate Nucleation in Porous Media Under Counter-Diffusion Conditions, Water Re- sources Research 61 (11) (2025) e2025WR040484.doi:10.1029/2025WR040484. 16
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