Repeated heating and cooling cycles appear frequently in thermomagnetic experiments used to infer the palaeomagnetic field intensity. According to the fundamental assumptions used to interpret these measurements, a remanence acquired at some temperature T is not influenced by subsequent heating and cooling cycles at lower temperatures. This presumption is tested for natural and synthetic multidomain particle ensembles in the case of the so-called tail of pTRM* (partial thermoremanent magnetization). This case is of special interest, since hitherto no theoretical explanation for the tail of pTRM* has been available. The experimental results for all samples show that repeating the acquisition process for the tail of pTRM* leads to an asymptotic saturation. This phenomenon can be explained in terms of a statistical theory of multidomain thermoremanence based on concepts of non-equilibrium thermodynamics. The presented experiments support the hypothesis that domain state stabilization by iterated thermal magnetization processes in multidomain particle ensembles is a statistical process. Iterative saturation of the tail of pTRM* can be interpreted using a combination of exponential saturation functions related to the subspectrum of the involved transition matrix. Its explanation does not require chemical alteration or irreversible after-effects. © 2004 RAS.
CITATION STYLE
Fabian, K., & Shcherbakov, V. P. (2004). Domain state stabilization by iterated thermal magnetization processes. Geophysical Journal International, 159(2), 486–494. https://doi.org/10.1111/j.1365-246X.2004.02394.x
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