Electron microscopy and 57Fe Mössbauer spectra of 10 nm particles, intermediate in composition between Fe3O4and γ-Fe2O3, produced by bacteria
Clicks: 188
ID: 114494
1996
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Star Article
30.0
/100
188 views
30 readers
AI Quality Assessment
Not analyzed
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
An analysis was made of magnetic 10 nm particles produced by bacteria under anaerobic conditions in an aqueous liquid. By means of transmission electron microscopy, applying electron diffraction, the particles were found to consist of Fe3O4 (magnetite) or γ-Fe2O3 (maghemite). Low temperature 57Fe Mössbauer spectra showed the particles to consist probably of an intermediate solid solution between both compounds.
| Reference Key |
m.1996georlelectron
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | Hanzlik, M.;Petersen, N.;Keller, R.;Schmidbauer, E.;Hanzlik, M.;Petersen, N.;Keller, R.;Schmidbauer, E.; |
| Journal | georl |
| Year | 1996 |
| DOI |
doi:10.1029/96GL00249
|
| URL | |
| Keywords |
|
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.