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Critically evaluated Curie temperatures are available in every standard magnetic database (MAGNDATA on the Bilbao Crystallographic Server, Landolt-Börnstein/SpringerMaterials, NIST), allowing an immediate comparison that confirms the phenomenon and ordering while quantifying the 15–50 °C offset from 1895 thermometry and sample purity." } ], "http://purl.org/dc/terms/subject": [ { "@id": "https://w3id.org/delphi/resource/concept/dataset-resolvability-0.2.0" } ], "@type": [ "https://w3id.org/delphi/ontology/LLMClaimAssessment" ], "http://www.w3.org/2000/01/rdf-schema#comment": [ { "@value": "Proposed test with existing data: Compare Curie's reported magnetic transformation temperatures (745 °C for iron, 530 °C for magnetite, 340 °C for nickel) against modern standard reference determinations of the ferromagnetic/ferrimagnetic Curie temperature T_C (defined by the inflection point of steepest descent in M(T) or vanishing spontaneous magnetization M_s → 0). Confirm if modern values (Fe ≈ 770 °C / 1043 K, Fe3O4 ≈ 580 °C / 853 K, Ni ≈ 354–358 °C / 627–631 K) match the ordering and approximate magnitudes within 19th-century thermocouple calibration and sample-purity tolerances (~15–50 °C)." } ], "http://www.w3.org/2000/01/rdf-schema#label": [ { "@value": "Gemini 4 Argon on curie1895-06: resolvable-now, resolvability 0.96" } ], "http://www.w3.org/ns/prov#wasAttributedTo": [ { "@id": "https://w3id.org/delphi/resource/agent/delphisci-resolvability-assessor-gemini-4-argon-medium" } ], "https://w3id.org/delphi/ontology/assessmentType": [ { "@value": "dataset-resolvability/0.2.0" } ], "https://w3id.org/delphi/ontology/evidenceAgainst": [ { "@value": "1895 thermoelectric pyrometry and trace impurities (e.g., carbon in iron, Ti/cation vacancies in natural magnetite) shifted Curie's numbers slightly below modern high-purity standards (745 vs 770 °C for Fe; 530 vs 580 °C for Fe3O4; 340 vs 358 °C for Ni)" } ], 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