Lodestone: Natures only permanent magnet - What it is and how it gets charged

Citation
P. Wasilewski et G. Kletetschka, Lodestone: Natures only permanent magnet - What it is and how it gets charged, GEOPHYS R L, 26(15), 1999, pp. 2275-2278
Citations number
31
Categorie Soggetti
Earth Sciences
Journal title
GEOPHYSICAL RESEARCH LETTERS
ISSN journal
00948276 → ACNP
Volume
26
Issue
15
Year of publication
1999
Pages
2275 - 2278
Database
ISI
SICI code
0094-8276(19990801)26:15<2275:LNOPM->2.0.ZU;2-Z
Abstract
Magnetite and Titanomagnetite exhibit magnetic properties which are attribu table to the micro-structures developed during oxidation and exsolution: Al l magnetite iron ores which are lodestones contain maghemite. These lodesto nes have He between 10 and 30 mT, SIRM between 8 and 18 Am(2)kg(1), and R-1 between 0.10 and 0.26. Magnetite, titanomagnetite and metals have REM valu es (ratio of NRM to SWM) < 0.05. Samples (called fulgarites) obtained from the Smithsonian Institution have REM values ranging from 0.45 to 0.92. The REM value serves as a witness parameter to the magnetic fields associated w ith the lightning bolt. If a high REM value (say >> 0.1) can be verified as not to be due to contamination by man and does not contain MD hematite the n the rock has LRM (lightning remanent magnetization). The magnetic field a ssociated with lightning can be revealed from an isothermal remanent acquis ition (RA) curve.