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Magnetic bacteria exhibit a directed movement called magnetotaxis, driven by structures called magnetosomes. These magnetosomes consist of chains of magnetic particles made of either magnetite (Fe₃O₄) or greigite (Fe₃S₄) and are organized in a linear conformation by a protein scaffold within invaginations of the cell membrane. The bacteria align along the north–south magnetic field lines, much like a compass needle. They are typically microaerophilic or anaerobic...
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Updated: Aug 6, 2025

Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films
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Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films

Published on: November 9, 2015

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Evolving radon diffusion through earthen barriers at uranium waste disposal sites.

Mark Fuhrmann1, Todd G Caldwell2, William J Likos3

  • 1Office of Nuclear Regulatory Research, U.S. Nuclear Regulatory Commission, Rockville, MD, 20852, USA.

Journal of Environmental Radioactivity
|March 22, 2023
PubMed
Summary
This summary is machine-generated.

Compacted clay radon barriers show effective radon diffusion coefficients (DRn) influenced by preferential pathways, not just water saturation. These findings assess long-term cover performance at uranium waste disposal sites.

Keywords:
DiffusionMoisture saturationPreferential pathwaysRadon-222Uranium waste

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Area of Science:

  • Geotechnical Engineering
  • Environmental Science
  • Radiological Protection

Background:

  • Compacted clay barriers are crucial for isolating radioactive waste.
  • Assessing long-term performance of engineered barriers is vital for environmental safety.
  • Radon-222 (Rn) gas migration is a key concern in uranium waste disposal.

Purpose of the Study:

  • To evaluate the performance of compacted clay radon barriers after 20 years.
  • To determine effective radon diffusion coefficients (DRn) in situ.
  • To investigate the influence of water saturation on DRn and identify factors affecting barrier performance.

Main Methods:

  • Field measurements of Rn-222 fluxes from clay barrier surfaces.
  • Calculation of effective DRn using field data.
  • Analysis of soil core samples to determine water saturation (SW).

Main Results:

  • Effective DRn values ranged from 6.0 × 10-9 to 7.4 × 10-7 m2/s, averaging 1.42 × 10-7 m2/s.
  • Water saturation had less control over DRn than predicted by steady-state models, especially at higher moisture levels.
  • Preferential pathways (cracks, root channels, burrows) significantly influenced DRn, requiring model modifications to account for fast and slow diffusion pathways.

Conclusions:

  • Engineered earthen barriers exhibit complex DRn behavior influenced by structural heterogeneities.
  • Modified diffusion models incorporating preferential pathways provide a better representation of field data.
  • Understanding these pathways is critical for accurate long-term performance predictions of radon barriers.