Critical superparamagnetic/single-domain grain sizes in interacting magnetite particles: implications for magnetosome crystals.
Magnetotactic bacteria contain chains of magnetically interacting crystals (magnetosome crystals), which they use for navigation (magnetotaxis). To improve magnetotaxis efficiency, the magnetosome crystals (usually magnetite or greigite in composition) should be magnetically stable single-domain (SSD) particles. Smaller single-domain particles become magnetically unstable owing to thermal fluctuations and are termed superparamagnetic (SP). Previous calculations for the SSD/SP threshold size or blocking volume did not include the contribution of magnetic interactions. In this study, the blocking volume has been calculated as a function of grain elongation and separation for chains of identical magnetite grains. The inclusion of magnetic interactions was found to decrease the blocking volume, thereby increasing the range of SSD behaviour. Combining the results with previously published calculations for the SSD to multidomain threshold size in chains of magnetite reveals that interactions significantly increase the SSD range. We argue that chains of interacting magnetosome crystals found in magnetotactic bacteria have used this effect to improve magnetotaxis.
Muxworthy
Adrian R
AR
Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK. adrian.muxworthy@imperial.ac.uk
Williams
Wyn
W
D000465:Algorithms; D001419:Bacteria / Q000737:chemistry / Q000648:ultrastructure*; D003460:Crystallization; D004574:Electromagnetic Fields; D052203:Ferrosoferric Oxide / Q000737:chemistry*; D005580:Fossils; D006358:Hot Temperature; D008280:Magnetics; D008903:Minerals / Q000737:chemistry*; D008954:Models, Biological; D015233:Models, Statistical; D010087:Oxides / Q000032:analysis
D008903:Minerals; D010087:Oxides; D052203:Ferrosoferric Oxide