Preliminary results of using ESR to examine biofilms
This preliminary work shows ESR (Electron Spin Resonance) can be used to detect biofilms, particularly from Fe-metabolising bacteria. A film was detected by ESR as early as 1 day, hence possibly more sensitively than by fluorescent methods. Films can probably be detected as early as one hour. Spectr...
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Pontificia Universidad Católica de Valparaíso
2004
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oai:scielo:S0717-345820040003000112005-05-31Preliminary results of using ESR to examine biofilmsWhitehead,Neil EvanTani,AtushiKazue,TazakiMotoji,Ikeya This preliminary work shows ESR (Electron Spin Resonance) can be used to detect biofilms, particularly from Fe-metabolising bacteria. A film was detected by ESR as early as 1 day, hence possibly more sensitively than by fluorescent methods. Films can probably be detected as early as one hour. Spectra contain a very broad peak at g=2.13, probably due to ferrihydrite. Results of field experiments from streams and ponds in New Zealand and Japan, particularly the Minoh River, showed a general increase of ferrihydrite with time. Loss by exfoliation was later than 20 days. The rate of accumulation was faster in a nutrient-rich stagnant pond. Hematite (g=4.3) was often observed, magnetite (g=9) once, and usually small amounts of a common bacterial decay product. The latter was detected for at least 18 months film storage. ESR is a particularly good tool for observing the growth of oxic biofilms containing Fe-metabolising bacteria, and should be just as sensitive for observing Mn-metabolising bacteria in reducing conditions.info:eu-repo/semantics/openAccessPontificia Universidad Católica de ValparaísoElectronic Journal of Biotechnology v.7 n.3 20042004-12-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-34582004000300011en |
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Scielo Chile |
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English |
description |
This preliminary work shows ESR (Electron Spin Resonance) can be used to detect biofilms, particularly from Fe-metabolising bacteria. A film was detected by ESR as early as 1 day, hence possibly more sensitively than by fluorescent methods. Films can probably be detected as early as one hour. Spectra contain a very broad peak at g=2.13, probably due to ferrihydrite. Results of field experiments from streams and ponds in New Zealand and Japan, particularly the Minoh River, showed a general increase of ferrihydrite with time. Loss by exfoliation was later than 20 days. The rate of accumulation was faster in a nutrient-rich stagnant pond. Hematite (g=4.3) was often observed, magnetite (g=9) once, and usually small amounts of a common bacterial decay product. The latter was detected for at least 18 months film storage. ESR is a particularly good tool for observing the growth of oxic biofilms containing Fe-metabolising bacteria, and should be just as sensitive for observing Mn-metabolising bacteria in reducing conditions. |
author |
Whitehead,Neil Evan Tani,Atushi Kazue,Tazaki Motoji,Ikeya |
spellingShingle |
Whitehead,Neil Evan Tani,Atushi Kazue,Tazaki Motoji,Ikeya Preliminary results of using ESR to examine biofilms |
author_facet |
Whitehead,Neil Evan Tani,Atushi Kazue,Tazaki Motoji,Ikeya |
author_sort |
Whitehead,Neil Evan |
title |
Preliminary results of using ESR to examine biofilms |
title_short |
Preliminary results of using ESR to examine biofilms |
title_full |
Preliminary results of using ESR to examine biofilms |
title_fullStr |
Preliminary results of using ESR to examine biofilms |
title_full_unstemmed |
Preliminary results of using ESR to examine biofilms |
title_sort |
preliminary results of using esr to examine biofilms |
publisher |
Pontificia Universidad Católica de Valparaíso |
publishDate |
2004 |
url |
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-34582004000300011 |
work_keys_str_mv |
AT whiteheadneilevan preliminaryresultsofusingesrtoexaminebiofilms AT taniatushi preliminaryresultsofusingesrtoexaminebiofilms AT kazuetazaki preliminaryresultsofusingesrtoexaminebiofilms AT motojiikeya preliminaryresultsofusingesrtoexaminebiofilms |
_version_ |
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