https://w3id.org/np/RAdAs_Chkd9XBmJNFRITlwJpOyNsfKJm-n67_Eouhayhg
.trig | .trig.txt | .jelly | .jelly.txt | .jsonld | .jsonld.txt | .nq | .nq.txt | .xml | .xml.txt
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dc:description "Curie's claim that ferromagnets heated well above their transformation point (specifically magnetite from 850 to 1370 °C) obey an asymptotic inverse-temperature susceptibility law of paramagnetic magnitude is directly testable using Curie's own 1895 data and modern high-temperature susceptibility tables in Landolt-Börnstein/SpringerMaterials. Furthermore, modern data distinguish the asymptotic linear 1/χ(T) Curie-Weiss regime from Néel ferrimagnetic curvature closer to T_C.";
dc:subject <https://w3id.org/delphi/resource/concept/dataset-resolvability-0.2.0>;
<http://www.w3.org/2000/01/rdf-schema#comment> "Proposed test with existing data: For magnetite (Fe3O4) in the high-temperature paramagnetic regime (850 to 1370 °C, i.e., 1123 to 1643 K, well above T_C ≈ 853 K) and other ferromagnets far above T_C, plot inverse susceptibility 1/χ against T. Evaluate whether χ(T) approaches the asymptotic Curie-Weiss / inverse-temperature scaling χ = C/(T - θ) (with ∂(1/χ)/∂T → constant and log-log slope approaching -1 at T >> T_C) and has magnitude comparable to standard paramagnetic salts.";
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<https://w3id.org/delphi/ontology/evidenceAgainst> "Because magnetite is a two-sublattice ferrimagnet, its exact inverse susceptibility above T_C follows Néel's hyperbolic law 1/χ = (T - θ_a)/C - σ/(T - θ'), which only asymptotically approaches a straight line at temperatures well above T_C";
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dc:description "Contains high-temperature paramagnetic susceptibility data 1/χ(T) above T_C for Fe3O4 and ferromagnetic metals.";
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