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Microbial participation in iodine volatilization from soils
Seigo Amachi1, Mizuyo Kasahara, Satoshi Hanada
1Department of Bioresources Chemistry, Chiba University, 648 Matsudo, Matsudo-shi, Chiba 271-8510, Japan.
Environmental Science & Technology
|September 12, 2003
Summary
Soil bacteria methylate and volatilize iodine as methyl iodide (CH3I). This microbial process is widespread in soils and crucial for understanding iodine
Area of Science:
- Environmental Microbiology
- Biogeochemistry
- Soil Science
Background:
- Microorganisms play a significant role in the transformation and cycling of elements within soil ecosystems.
- Iodine's biogeochemical cycle is not fully understood, particularly the mechanisms of its volatilization from terrestrial environments.
Purpose of the Study:
- To investigate the role of soil microorganisms in the volatilization of iodine from soils.
- To identify the specific microbial species and pathways involved in iodine methylation and emission.
Main Methods:
- Incubation of soils with iodide ions and analysis of volatile organic iodine species using gas chromatography.
- Use of radioactive iodine tracers (125I) to quantify iodine emission.
- Isolation and characterization of iodine-volatilizing bacterial strains and phylogenetic analysis based on 16S ribosomal DNA sequences.
Main Results:
- Iodine was primarily emitted as methyl iodide (CH3I), with emission enhanced by glucose and yeast extract.
- Microbial activity was essential, as autoclaving inhibited iodine emission, while antibiotics targeting bacteria (streptomycin, tetracycline) strongly reduced it.
- Fourteen out of forty isolated bacterial strains demonstrated significant iodine volatilization capabilities.
- Phylogenetic analysis revealed that these iodine-volatilizing bacteria are widely distributed across the bacterial domain.
Conclusions:
- Soil bacteria are key agents in methylating and volatilizing iodine as CH3I.
- Iodine-volatilizing bacteria are ubiquitous in soil environments.
- Understanding these microbial pathways is vital for the biogeochemical cycling of iodine and managing radioactive iodine (129I) in the environment.