Publication Details

Category Text Publication
Reference Category Journals
DOI 10.1021/es903954u
Title (Primary) In-situ magnetic susceptibility measurements as a tool to follow ceomicrobiological transformation of Fe minerals
Author Porsch, K.; Dippon, U.; Lal Rijal, M.; Appel, E.; Kappler, A.
Source Titel Environmental Science & Technology
Year 2010
Department BIOENERGIE
Volume 44
Issue 10
Page From 3846
Page To 3852
Language englisch
Abstract Fe minerals sorb nutrients and pollutants and participate in microbial and abiotic redox reactions. Formation and transformation of Fe minerals is typically followed by mineral analysis at different time points. However, in lab studies the available sample amount is often limited and sampling may even influence the experimental conditions. We therefore evaluated the suitability of in situ magnetic susceptibility (MS) measurements, which do not require sampling, as an alternative tool to follow ferro(i)magnetic mineral (trans-)formation during ferrihydrite reduction by Shewanella oneidensis MR-1, and in soil microcosms. In our experiments with MR-1, a large initial increase in volume specific MS (κ) followed by a slight decrease correlated well with the initial formation of magnetite and further reduction of magnetite to siderite as also identified by μ-XRD. The presence of humic acids retarded magnetite formation, and even inhibited magnetite formation completely, depending on their concentration. In soil microcosms, an increase in κ accompanied by increasing concentrations of HCl-extractable Fe occurred only in microbially active set-ups, indicating a microbially induced change in soil Fe mineralogy. Based on our results, we conclude that MS measurements are suitable to follow microbial Fe mineral transformation in pure cultures as well as in complex soil samples.
Persistent UFZ Identifier https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=14768
Porsch, K., Dippon, U., Lal Rijal, M., Appel, E., Kappler, A. (2010):
In-situ magnetic susceptibility measurements as a tool to follow ceomicrobiological transformation of Fe minerals
Environ. Sci. Technol. 44 (10), 3846 - 3852 10.1021/es903954u