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Iron traps terrestrially derived dissolved organic matter at redox interfaces
Reactive iron and organic carbon are intimately associated in soils and sediments. However, to date, the organic compounds involved are uncharacterized on the molecular level. At redox interfaces in peatlands, where the biogeochemical cycles of iron and dissolved organic matter (DOM) are coupled, th...
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| Main Authors: | , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2013
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3690857/ https://ncbi.nlm.nih.gov/pubmed/23733946 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1221487110 |
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