https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc/Head https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc http://www.nanopub.org/nschema#hasAssertion https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc/assertion https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc http://www.nanopub.org/nschema#hasProvenance https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc/provenance https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc http://www.nanopub.org/nschema#hasPublicationInfo https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc/pubinfo https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://www.nanopub.org/nschema#Nanopublication https://w3id.org/np/RAhMORtQhs7CM10AbC3L4i4jd-a2T3eV__XdRrCtqPwrc/assertion https://w3id.org/delphi/resource/agent/delphisci-resolvability-assessor-gemini-4-argon-medium http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://www.w3.org/ns/prov#SoftwareAgent https://w3id.org/delphi/resource/agent/delphisci-resolvability-assessor-gemini-4-argon-medium http://www.w3.org/2000/01/rdf-schema#label delphisci dataset-resolvability assessor (Gemini 4 Argon) https://w3id.org/delphi/resource/agent/delphisci-resolvability-assessor-gemini-4-argon-medium http://www.w3.org/ns/prov#actedOnBehalfOf https://orcid.org/0009-0007-4948-9192 https://w3id.org/delphi/resource/agent/delphisci-resolvability-assessor-gemini-4-argon-medium https://w3id.org/delphi/ontology/usesModel https://w3id.org/delphi/resource/model/gemini-4-argon-medium https://w3id.org/delphi/resource/assessment/curie1880-01--gemini http://purl.org/dc/terms/description The Curies' claim links macroscopic pyroelectricity and piezoelectricity directly to crystal point-group symmetry. This can be tested immediately against the Materials Project's piezoelectric tensor database (thousands of structures) and symmetry tensor tables on the Bilbao Crystallographic Server: true pyroelectricity requires one of the 10 polar point groups, whereas piezoelectricity occurs across 20 non-centrosymmetric point groups (including 10 non-polar classes such as 32 in quartz and -43m in sphalerite that are piezoelectric but not pyroelectric). https://w3id.org/delphi/resource/assessment/curie1880-01--gemini http://purl.org/dc/terms/subject https://w3id.org/delphi/resource/concept/dataset-resolvability-0.2.0 https://w3id.org/delphi/resource/assessment/curie1880-01--gemini http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/delphi/ontology/LLMClaimAssessment https://w3id.org/delphi/resource/assessment/curie1880-01--gemini http://www.w3.org/2000/01/rdf-schema#comment Proposed test with existing data: Group crystalline materials by their 32 crystallographic point groups and test whether nonzero piezoelectric tensors (d_{ijk}) and pyroelectric vectors (p_i) occur exclusively in the 10 polar point groups ('hemihedral with inclined faces') or across the broader set of 20 non-centrosymmetric point groups. 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1880 terminology 'hémièdres à faces inclinées' grouped non-centrosymmetric crystals tested in Note I (which included quartz, point group 32, and sphalerite, point group -43m) before Voigt (1894) formalized the exact distinction between the 10 polar pyroelectric classes and the 20 piezoelectric classes https://w3id.org/delphi/resource/assessment/curie1880-01--gemini https://w3id.org/delphi/ontology/hasConfidence 0.95 https://w3id.org/delphi/resource/assessment/curie1880-01--gemini https://w3id.org/delphi/ontology/hasEvidence https://w3id.org/delphi/resource/evidence/curie1880-01--gemini--dataset-1 https://w3id.org/delphi/resource/assessment/curie1880-01--gemini https://w3id.org/delphi/ontology/hasEvidence https://w3id.org/delphi/resource/evidence/curie1880-01--gemini--dataset-2 https://w3id.org/delphi/resource/assessment/curie1880-01--gemini https://w3id.org/delphi/ontology/hasScore 0.94 https://w3id.org/delphi/resource/assessment/curie1880-01--gemini 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