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Related Concept Videos

Complexometric Titration: Ligands00:43

Complexometric Titration: Ligands

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Different monodentate and polydentate ligands are used as complexing agents in complexometric titration reactions. The formation of complexes by mono- and bidentate ligands involves two or more intermediate steps, limiting their use as complexing agents. In comparison, polydentate ligands can form complexes with metal ions in a single-step process, facilitating sharper end points. This means polydentate ligands, such as amino carboxylic acid derivatives, are most commonly employed in...
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In gravimetry, the precipitant is chosen carefully to obtain a pure solid that can be easily filtered. Common inorganic precipitants can be used to determine several cations and anions. In some cases, the formation of the same precipitate can be used to determine the cation and the anion. For example, the reaction of barium and chromate ions to give barium chromate is used to determine both barium and chromate. However, precipitates such as hydroxides, oxalates, and metal ammonium phosphates...
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Metal ions can be separated from one another by complexation with organic ligands–the chelating agent– to form uncharged chelates. Here, the chelating agent must contain hydrophobic groups and behave as a weak acid, losing a proton to bind with the metal. Since most organic ligands used in this process are insoluble or undergo oxidation in the aqueous phase, the chelating agent is initially added to the organic phase and extracted into the aqueous phase. The metal-ligand complex is...
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Machine learning surrogates for surface complexation model of uranium sorption to oxides.

Chunhui Li1, Elijah O Adeniyi2, Piotr Zarzycki3

  • 1Energy Geosciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, USA. chunhuili@lbl.gov.

Scientific Reports
|March 20, 2024
PubMed
Summary

Machine learning models accurately predict uranium sorption to minerals, overcoming computational issues in safety assessments for geological nuclear waste storage. This accelerates understanding of radionuclide mobility and repository safety.

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Area of Science:

  • Geochemistry and Environmental Science
  • Nuclear Waste Management
  • Computational Modeling

Background:

  • Geological disposal of spent nuclear fuel necessitates understanding radionuclide mobility, particularly uranium, which is highly mobile in its oxidized state (U(VI)).
  • Uranium sorption to surrounding mineral surfaces is a key process limiting its migration, but traditional surface complexation models (SCMs) face numerical convergence challenges.
  • Accurate modeling of uranium mobility is crucial for the safety assessment of nuclear waste repositories.

Purpose of the Study:

  • To develop and evaluate machine learning (ML) surrogates for complex surface complexation models (SCMs) of uranium sorption.
  • To address the computational cost and convergence issues associated with traditional SCM solvers.
  • To provide ultrafast AI/ML tools for enhancing nuclear waste migration models.

Main Methods:

  • Explored two ML surrogates: Random Forest Regressor and Deep Neural Networks (DNNs).
  • Trained and validated ML models using predictions from the 2-pK Triple Layer Model for uranium retention by oxide surfaces.
  • Integrated the developed ML surrogate model into a larger-scale contaminant migration model.

Main Results:

  • Both ML surrogates accurately reproduced SCM predictions for uranium sorption.
  • Deep Neural Networks (DNNs) demonstrated particular efficacy, achieving high accuracy at a significantly reduced computational cost.
  • The ML surrogates successfully avoided the convergence problems inherent in numerical SCM solvers.

Conclusions:

  • AI/ML surrogates offer a computationally efficient and reliable alternative to traditional SCMs for modeling uranium sorption.
  • These ultrafast ML surrogates can be readily integrated into larger contaminant migration models for improved repository safety assessments.
  • The study presents a novel ML-based approach to enhance the understanding and prediction of radionuclide migration in geological repositories.