Mineral-Specific Element Sorption onto Geological Repository Rocks

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Environmental Mineralogy and Biogeochemistry".

Deadline for manuscript submissions: closed (22 May 2022) | Viewed by 2246

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Guest Editor
A.N. Frumkin Institute of Physical Chemistry and Electrochemistry, Russian Academy of Sciences, 119991 Moscow, Russia
Interests: nuclear waste; severe nuclear accidents; radiation defects; diamond

Special Issue Information

Dear Colleagues,

Long-term disposal of high-level nuclear waste is an important problem of the modern nuclear industry. Although many potentially promising technological solutions for recycling actinides and other useful nuclides have been proposed, most of them are still far from a mature state. In any case, even most advanced reprocessing technologies will leave behind an important amount of radioactive material, which is difficult to reuse from an economical point of view, and thus should be safely disposed of. The creation of deep geological repositories for high level nuclear waste is currently being considered in many countries, but numerous scientific and engineering issues remain unsolved.

This Special Issue aims to collect high quality papers focusing on studies of radionuclides on various types of rocks and backfill materials. Both experimental and modeling studies are invited.

Prof. Dr. Andrey A. Shiryaev
Guest Editor

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Keywords

  • nuclear waste
  • radioecology
  • sorption
  • deep geological repository

Published Papers (1 paper)

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Research

37 pages, 8501 KiB  
Article
Uranium Retardation Capacity of Lithologies from the Negev Desert, Israel—Rock Characterization and Sorption Experiments
by Martin A. Dangelmayr, Gilles Y. Bussod, Paul W. Reimus, Giday WoldeGabriel, Ran Calvo, Rose J. Harris, Philip H. Stauffer, Hakim Boukhalfa, Ofra Klein-BenDavid, Noa Balaban and Ravid Rosenzweig
Minerals 2022, 12(6), 728; https://0-doi-org.brum.beds.ac.uk/10.3390/min12060728 - 06 Jun 2022
Cited by 3 | Viewed by 1909
Abstract
A series of batch experiments were performed to assess the uranium sorption capacity of four mineralogically distinct lithologies from the Negev Desert, Israel, to evaluate the suitability of a potential site for subsurface radioactive waste disposal. The rock specimens consisted of an organic-rich [...] Read more.
A series of batch experiments were performed to assess the uranium sorption capacity of four mineralogically distinct lithologies from the Negev Desert, Israel, to evaluate the suitability of a potential site for subsurface radioactive waste disposal. The rock specimens consisted of an organic-rich phosphorite, a bituminous marl, a chalk, and a sandstone. The sorption data for each lithology were fitted using a general composite surface complexation model (GC SCM) implemented in PHREEQC. Sorption data were also fitted by a non-mechanistic Langmuir sorption isotherm, which can be used as an alternative to the GC SCM to provide a more computationally efficient method for uranium sorption. This is because all the rocks tested have high pH/alkalinity/calcium buffering capacities that restrict groundwater chemistry variations, so that the use of a GC SCM is not advantageous. The mineralogy of the rocks points to several dominant sorption phases for uranyl (UO22+), including apatite, organic carbon, clays, and iron-bearing phases. The surface complexation parameters based on literature values for the minerals identified overestimate the uranium sorption capacities, so that for our application, an empirical approach that makes direct use of the experimental data to estimate mineral-specific sorption parameters appears to be more practical for predicting uranium sorption. Full article
(This article belongs to the Special Issue Mineral-Specific Element Sorption onto Geological Repository Rocks)
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