磁铁矿
材料科学
千分尺
位错
剩磁
矫顽力
粒度
矿物学
磁滞
结晶学
复合材料
冶金
磁场
凝聚态物理
磁化
地质学
化学
光学
物理
量子力学
作者
Franz Heider,David J. Dunlop,Naoji Sugiura
出处
期刊:Science
[American Association for the Advancement of Science]
日期:1987-06-05
卷期号:236 (4806): 1287-1290
被引量:181
标识
DOI:10.1126/science.236.4806.1287
摘要
The discrepancy between the magnetic hysteresis properties of magnetite crystals that are precipitated from solution (<0.3 micrometer) and of crushed sifted grains (>0.3 micrometer) is not an inherent property of magnetite but is caused by the highly stressed state of crushed material and by adhering finer fragments. The size trends of magnetic properties exhibited by submicrometer-size precipitated grains continue in the size range from 1 micrometer to 1 millimeter in a set of hydrothermally recrystallized magnetite crystals. Coercive forces of these narrowly sized crystals follow a power law over a wide size range (0.1 micrometer to 1 millimeter) as predicted by theory. Dislocation etch pits show similar dislocation densities for hydrothermally grown (3 x 10(10) meter (-2)) and natural (1 x 10(10) meter(-2)) magnetite crystals. Hysteresis parameters of hydrothermally grown crystals are similar to those of natural crystals but are about one-fifth of those for crushed grains.
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