Detection of noninteracting single domain particles using first‐order reversal curve diagrams

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Understanding fine magnetic particle systems through use of first‐order reversal curve diagrams (2014, methodology): “For example, the magnetic signal in some samples can be so weak that stacking of multiple measurements [Egli et al., 2010; Heslop and Roberts, 2012a] is required to enable adequate identification of signals of interest (where noise is reduced as the square root of the number ofmeasurements if noise ”
Searching for single domain magnetite in the “pseudo‐single‐domain” sedimentary haystack: Implications of biogenic magnetite preservation for sediment magnetism and relative paleointensity determinations (2012, background): “Again, high-resolution FORC diagrams contain a sharp central ridge, which is consistent with the presence of intact magnetofossil chains [Egli et al., 2010].”