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Thermomagnetic data analysis

These notebooks support the analysis of thermomagnetic data.

A note on methods and their applicability

Curie temperature estimates are method-dependent, and the appropriate methods differ between data types. Estimates from different methods applied to the same curve differ systematically — by several degrees to several tens of degrees (Lattard et al., 2006) — so the estimation method (and any smoothing or fitting windows) is part of the result and should be reported with it.

For strong-field magnetization Mₛ(T) curves, the Landau-theory analysis of Fabian et al. (2013) places the Curie temperature at the inflection point of the in-field curve (the minimum of dM/dT), a position that is effectively independent of the applied field. The classical maximum-curvature (second-derivative maximum) and “two-tangent” (Grommé et al., 1969) estimates coincide with each other and lie systematically above the inflection-point T꜀, typically by 10–15 °C. RockmagPy provides all of these — inflection, max_curvature, two_tangent, and a Landau equation-of-state fit (landau) with formal uncertainty — so that estimates can be compared and the bias structure made explicit.

For low-field susceptibility χ-T curves, the two-tangent construction is not physically justified, and RockmagPy flags it when it is requested on susceptibility data. Fabian et al. (2013) explain this well:

“The importance of the difference between determining Tc from Mₛ(T) and χ-T is pointed out by Petrovský and Kapicka (2006), where methods to determine Tc from measurements of the initial susceptibility are analyzed. They conclude that the two-tangent method is not suitable for χ-T and can considerably overestimate Tc. The physical origin of χ-T close to Tc is more challenging than that of Mₛ(T), because a number of low-field effects are important for χ-T, but become negligible in the higher fields used to infer Mₛ(T). The variation of m depends not only on the variation of Mₛ(H,T) with field H, it also contains a contribution from a rotation of the ordered moment with respect to an easy magnetization axis, and contributions from thermally activated switching of small independent – but already magnetically ordered – regions (e.g., SP particles). In large bulk material, domain-wall movement contributes to χ-T even slightly below Tc. In nanoparticles, the inhomogeneity of Mₛ due to the different exchange coupling of inner and surface atoms is of additional importance.”

And from Petrovský and Kapicka (2006):

“...susceptibility for T > Tc and T < Tc increases to infinity, and we have to use analytical formulas developed for susceptibility behavior above the Curie point. Here, due to the geometry of the susceptibility curve, the two-tangent method will always yield temperature above the inflection point, which is higher than the temperature at which the substance starts to obey the paramagnetic Curie-Weiss law. The resulting error in Tc (or TN1) can be on the order of several degrees to several tens of degrees. Therefore, in the case of temperature dependence of magnetic susceptibility, application of the two-tangent method is not justified.”

Furthermore:

“In the case of synthetic magnetite and hematite, with sharp Hopkinson peak, the difference between transition temperatures determined using the two-tangent method and Curie-Weiss paramagnetic law is in the order of some few degrees. In the case of samples with wide susceptibility maximum and gradual decrease, reflecting e.g., wide distribution of grain sizes, or in the case of substituted hematite, application of the two-tangent method to susceptibility curves overestimates the transition temperature by several tens of degrees.”

For χ-T data, the derivative-based estimates on the descending step and the inverse-susceptibility (Curie-Weiss) extrapolation advocated by Petrovský and Kapicka (2006) are the appropriate quantitative approaches — with the caveats that the Hopkinson peak marks blocking rather than the Curie temperature, and that the Curie-Weiss extrapolation yields the paramagnetic Curie temperature θT꜀. The Curie temperature estimation notebook demonstrates each of these methods and their caveats on measured data.

References
  1. Lattard, D., Engelmann, R., Kontny, A., & Sauerzapf, U. (2006). Curie temperatures of synthetic titanomagnetites in the Fe-Ti-O system: Effects of composition, crystal chemistry, and thermomagnetic methods. Journal of Geophysical Research: Solid Earth, 111, B12S28. 10.1029/2006JB004591
  2. Fabian, K., Shcherbakov, V. P., & McEnroe, S. A. (2013). Measuring the Curie temperature. Geochemistry, Geophysics, Geosystems, 14(4), 947–961. 10.1029/2012GC004440
  3. Grommé, C. S., Wright, T. L., & Peck, D. L. (1969). Magnetic properties and oxidation of iron-titanium oxide minerals in Alae and Makaopuhi Lava Lakes, Hawaii. Journal of Geophysical Research, 74(22), 5277–5294. 10.1029/JB074i022p05277
  4. Petrovský, E., & Kapička, A. (2006). On determination of the Curie point from thermomagnetic curves. Journal of Geophysical Research: Solid Earth, 111, B12S27. 10.1029/2006JB004507