Using time- and temperature-dependent Preisach models to investigate the limitations of modelling isothermal remanent magnetization acquisition curves with cumulative log Gaussian functions

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Understanding fine magnetic particle systems through use of first‐order reversal curve diagrams (2014, background): “The reliability of IRM unmixing can be affected strongly by undetected magnetostatic interactions [Heslop et al., 2002, 2004].”
Characterization of Individual Rock Magnetic Components by Analysis of Remanence Curves, 1. Unmixing Natural Sediments (2004, methodology): “Heslop et al. (2004) came to the same conclusion by modelling acquisition curves of isothermal remanent magnetization (IRM) with a temperature dependant Preisach-Neel model.”
MAX UnMix: A web application for unmixing magnetic coercivity distributions (2016, background): “Skew-right distributions ( >S 1) are less well understood on a physical basis and may indicate mixed mineralogy within a single skew-right component (Heslop et al., 2004).”