| Literature DB >> 17784416 |
Abstract
Maximum values for the single-domain threshold d(0) and superpara-magnetic threshold d(8) in pure magnetite are found to be 570+/-50 and 350+/-50 angstroms, respectively. Particles larger than do but smaller than about 0.25 micron have size-dependent saturation remanences and coercive forces like those of multidomain particles, but intense and stable thermoremanent magnetization like that of single-domain particles. The presence of magnetite grains in this size range could account for the essentially single-domain character of stable natural remanence in many volcanic and intrusive rocks.Entities:
Year: 1972 PMID: 17784416 DOI: 10.1126/science.176.4030.41
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728