| Автор | Dunlop, David J. |
| Автор | Argyle, Kenneth S. |
| Автор | Bailey, Monika E. |
| Дата выпуска | 1990 |
| dc.description | We describe three useful techniques for investigating magnetic microstructure and granulometry, high‐temperature alternating‐field (AF) demagnetization, thermal fluctuation analysis (TFA), and determination of the demagnetizing factor N, and give examples of their use. For synthetic magnetite samples, thennoremanent magnetization and anhysteretic rémanent magnetization are shown to differ in their AF demagnetization spectra at all temperatures up to the blocking range. Moreover, various coercivity fractions of either spectrum evolve differently with temperature than does the bulk coercive force. TFA of high‐temperature coercive force data for dispersed magnetite crystals with mean sizes of 215, 390 and 540 run indicate that ≈200 nm regions are thermally activated in each case. These regions may be responsible for pseudo‐single‐domain behaviour. A crude estimate of N for multidomain grains at any temperature is the ratio between bulk coercive force and saturation remanence. The 215–540 nm magnetites appear to contain two or three domains between −100°C and 400°C; new domains may nucleate at higher temperatures. |
| Формат | application.pdf |
| Копирайт | Copyright 1990 by the American Geophysical Union. |
| Тема | Application of Optical and Magnetic Techniques in Rock Magnetism |
| Тема | Geomagnetism and Paleomagnetism |
| Тема | Geomagnetism and Paleomagnetism: Instruments and techniques |
| Тема | Geomagnetism and Paleomagnetism: Rock and mineral magnetism |
| Тема | Geomagnetism and Paleomagnetism: Biomagnetism |
| Тема | Geomagnetism and Paleomagnetism: Paleomagnetism applied to tectonics |
| Название | High‐temperature techniques for measuring microcoercivity, crystallite size, and domain state |
| Тип | article |
| DOI | 10.1029/GL017i006p00767 |
| Electronic ISSN | 1944-8007 |
| Print ISSN | 0094-8276 |
| Журнал | Geophysical Research Letters |
| Том | 17 |
| Первая страница | 767 |
| Последняя страница | 770 |
| Аффилиация | Dunlop, David J.; Geophysics Laboratory, Department of Physics, University of Toronto |
| Аффилиация | Argyle, Kenneth S.; Geophysics Laboratory, Department of Physics, University of Toronto |
| Аффилиация | Bailey, Monika E.; Geophysics Laboratory, Department of Physics, University of Toronto |
| Выпуск | 6 |
| Библиографическая ссылка | Argyle, K. S.D. J.Dunlop, Low‐temperature and high‐temperature hysteresis of small multidomain in magnetites (215‐540 nm), J. Geophys. Res., 95, 1990 |
| Библиографическая ссылка | Dunlop, D. J., Thermal fluctuation analysis: a new technique in rock magnetism, J. Geophys. Res., 81, 3511–3517, 1976 |
| Библиографическая ссылка | Dunlop, D. J., On the demagnetizing energy and demagnetizing factor of a multidomain ferromagnetic cube, Geophys. Res. Lett., 10, 79–82, 1983 |
| Библиографическая ссылка | Dunlop, D. J., A method of determining demagnetizing factor from multidomain hysteresis, J. Geophys. Res., 89, 553–558, 1984 |
| Библиографическая ссылка | Dunlop, D. J., Temperature dependence of hysteresis in 0.04‐0.22 μm magnetites and implications for domain structure, Phys. Earth Planet. Inter., 46, 100–119, 1987 |
| Библиографическая ссылка | Dunlop, D. J.M‐M.Bina, The coercive force spectrum of magnetite at high temperatures: evidence for thermal activation below the blocking temperature, Geophys. J. Roy. Astron. Soc., 51, 121–147, 1977 |
| Библиографическая ссылка | Dunlop, D. J.Ö.ÖzdemirR. J.Enkin, Multidomain and single‐domain relations between susceptibility and coercive force, Phys. Earth Planet. Inter., 49, 181–191, 1987 |
| Библиографическая ссылка | Halgedahl, S. L., Domain pattern observations in rock magnetism: progress and problems, Phys. Earth Planet. Inter., 46, 127–163, 1987 |
| Библиографическая ссылка | Heider, F.S. L.HalgedahlD. J.Dunlop, Temperature dependence of magnetic domains in magnetite crystals, Geophys. Res. Lett., 15, 499–502, 1988 |
| Библиографическая ссылка | Hodych, J. P., Determination of self‐demagnetizing factor N for multidomain magnetite grains in rock, Phys. Earth Planet. Inter., 41, 283–291, 1986 |
| Библиографическая ссылка | Levi, S.R. T.Merrill, Properties of single‐domain pseudo‐single‐domain and multidomain magnetite, J. Geophys. Res., 83, 309–323, 1978 |
| Библиографическая ссылка | Néel, L., Théorie du traînage magnétique des ferromagnétiques en grains fins avec applications aux terres cuites, Ann. Geophys., 5, 99–136, 1949 |
| Библиографическая ссылка | Néel, L., Some theoretical aspects of rock magnetism, Adv. Phys., 4, 191–243, 1955 |
| Библиографическая ссылка | Smith, G. M.R. T.Merrill, The determination of the internal field in magnetic grains, J. Geophys. Res., 87, 9419–9423, 1982 |
| Библиографическая ссылка | Spratt, G.W.D.P. R.BissellR. W.Chantrell, Static and dynamic switching field distribution for magnetic tape systems, IEEE Trans. Magnetics, MAG22, 659–661, 1986 |
| Библиографическая ссылка | Stacey, F. D.S. K.BanerjeeThe Physical Principles of Rock Magnetism, Elsevier, New York, 1974 |
| Библиографическая ссылка | Sugiura, N., On the origin of PSD moment in magnetite, Geophys. J., 92, 479–485, 1988 |
| Библиографическая ссылка | Xu, S.R. T.Merrill, The demagnetizing factors in multidomain grains, J. Geophys. Res., 92, 10657–10665, 1987 |