Interacting vs. non-interacting single domain behavior in natural and synthetic samples

Abstract The disparity in response to high alternating field (AF) demagnetization for samples containing fine magnetic carriers is apparently related to the degree of interactions between those carriers. The presence of interaction fields between single domain (SD) grains can be tested by plotting isothermal remanence (IRM) acquisition vs. saturation remanence (SIRM) demagnetization. For the case of non-interacting SD grains, the two curves will be symmetrical. For the interacting SD case, the acquisition curve will be steepest at higher fields, and the demagnetization curve steepest at lower fields, resulting in non-symmetry. The point of intersection of the two curves approximates the remanent coercive force ( H RC ) field for all cases. Minor hysteresis loops and anhysteretic remanence (ARM) acquisition curves are also strongly influenced by interaction fields. Because of the difficulty in dispersing strongly magnetic grains, fine grained synthetic samples made with highly magnetic materials will not display equivalent AF stability to natural samples with fine, dispersed grains.

[1]  D. Dunlop,et al.  An experimental evaluation of single domain theories , 1969 .

[2]  R. Hargraves,et al.  Source of stable remanent magnetism in Lambertville diabase , 1969 .

[3]  M. McElhinny,et al.  Single domain magnetite and high coercivities in a gabbroic intrusion , 1968 .

[4]  M. Fuller,et al.  Microanalysis of N.R.M. in a granodiorite intrusion , 1974 .

[5]  H. Johnson,et al.  Stability of Anhysteretic Remanent Magnetization in Fine and Coarse Magnetite and Maghemite Particles , 1975 .

[6]  Donald F. Eldridge,et al.  Quantitative Determination of the Interaction Fields in Aggregates of Single-Domain Particles , 1961 .

[7]  E. Wohlfarth Relations between Different Modes of Acquisition of the Remanent Magnetization of Ferromagnetic Particles , 1958 .

[8]  P. Davis,et al.  Interacting single-domain properties of magnetite intergrowths , 1976 .

[9]  E. E. Larson,et al.  Stability of Remanent Magnetization of Igneous Rocks , 1969 .

[10]  D. Dunlop Thermoremanent magnetization in submicroscopic magnetite , 1973 .

[11]  Joseph L. Kirschvink,et al.  Mineralization and magnetization of chiton teeth : Paleomagnetic, sedimentologic, and biologic implications of organic magnetite , 1979 .

[12]  W. Lowrie,et al.  On the alternating field demagnetization characteristics of multidomain thermoremanent magnetization in magnetite , 1971 .

[13]  Subir K. Banerjee,et al.  A new method for the determination of paleointensity from the A.R.M. properties of rocks , 1974 .

[14]  D. Dunlop,et al.  Indices of multidomain magnetic behavior in basic igneous rocks: Alternating-field demagnetization, hysteresis, and oxide petrology , 1973 .

[15]  D. Dunlop Magnetite: Behavior near the Single-Domain Threshold , 1972, Science.

[16]  L. Srnka,et al.  Magnetic field and shock effects and remanent magnetization in a hypervelocity impact experiment , 1979 .

[17]  W. F. Jaep Anhysteretic Magnetization of an Assembly of Single‐Domain Particles , 1969 .

[18]  N. Sugiura ARM, TRM and magnetic interactions: Concentration dependence , 1979 .

[19]  S. Cisowski The relationship between the magnetic properties of terrestrial igneous rocks and the composition and internal structure of their component Fe-oxide grains , 1980 .