{"record_type":"pith_number_record","schema_url":"https://pith.science/schemas/pith-number/v1.json","pith_number":"pith:2011:DOKEI6IIOMAFUJ6DR5O54JLT7V","short_pith_number":"pith:DOKEI6II","schema_version":"1.0","canonical_sha256":"1b9444790873005a27c38f5dde2573fd4c881a8bcbf0ce762164e662dced5352","source":{"kind":"arxiv","id":"1110.3956","version":1},"attestation_state":"computed","paper":{"title":"Quantum critical point and spin fluctuations in the lower-mantle ferropericlase","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":["physics.chem-ph","physics.geo-ph"],"primary_cat":"cond-mat.str-el","authors_text":"A. A. Mironovich, A. G. Gavriliuk, I. S. Lyubutin, J. F. Lin, P. Chow, P. G. Naumov, S. G. Ovchinnikov, S. Sinogeikin, V.V. Struzhkin, Y. Xiao","submitted_at":"2011-10-18T12:37:57Z","abstract_excerpt":"Ferropericlase, (Mg,Fe)O is one of the most abundant minerals of the Earth's lower mantle. The high-spin (HS) to low-spin (LS) transition in the Fe2+ ions can dramatically alter the physical and chemical properties of (Mg,Fe)O in the deep mantle, thereby changing our understanding of the Earth's deep interior. To establish a fundamental understanding of the ground electronic state of iron, the electronic and magnetic states of Fe2+ in (Mg0.75,Fe0.25)O have been investigated by transmission (TMS) and synchrotron (NFS) M\\\"ossbauer spectroscopy at high pressures and low temperatures (down to 5 K)"},"verification_status":{"content_addressed":true,"pith_receipt":true,"author_attested":false,"weak_author_claims":0,"strong_author_claims":0,"externally_anchored":false,"storage_verified":false,"citation_signatures":0,"replication_records":0,"graph_snapshot":true,"references_resolved":false,"formal_links_present":false},"canonical_record":{"source":{"id":"1110.3956","kind":"arxiv","version":1},"metadata":{"license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","primary_cat":"cond-mat.str-el","submitted_at":"2011-10-18T12:37:57Z","cross_cats_sorted":["physics.chem-ph","physics.geo-ph"],"title_canon_sha256":"95cd50986b65ba61f7d767162a555ad8c136999294b98ded0366f9bcd8411b29","abstract_canon_sha256":"75e530fba17289871fd4b489472443a9068eb79da99297247fdba96e92964d57"},"schema_version":"1.0"},"receipt":{"kind":"pith_receipt","key_id":"pith-v1-2026-05","algorithm":"ed25519","signed_at":"2026-05-18T04:10:47.618326Z","signature_b64":"pkCx9N5BGPmhQHyBHMefqVoKf0VahyibLcupYttg1ZDiKCW4snMxhNVQ52AEW4vCMXNMLaNerOlWNjG9TC8aBg==","signed_message":"canonical_sha256_bytes","builder_version":"pith-number-builder-2026-05-17-v1","receipt_version":"0.3","canonical_sha256":"1b9444790873005a27c38f5dde2573fd4c881a8bcbf0ce762164e662dced5352","last_reissued_at":"2026-05-18T04:10:47.617926Z","signature_status":"signed_v1","first_computed_at":"2026-05-18T04:10:47.617926Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54"},"graph_snapshot":{"paper":{"title":"Quantum critical point and spin fluctuations in the lower-mantle ferropericlase","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":["physics.chem-ph","physics.geo-ph"],"primary_cat":"cond-mat.str-el","authors_text":"A. A. Mironovich, A. G. Gavriliuk, I. S. Lyubutin, J. F. Lin, P. Chow, P. G. Naumov, S. G. Ovchinnikov, S. Sinogeikin, V.V. Struzhkin, Y. Xiao","submitted_at":"2011-10-18T12:37:57Z","abstract_excerpt":"Ferropericlase, (Mg,Fe)O is one of the most abundant minerals of the Earth's lower mantle. The high-spin (HS) to low-spin (LS) transition in the Fe2+ ions can dramatically alter the physical and chemical properties of (Mg,Fe)O in the deep mantle, thereby changing our understanding of the Earth's deep interior. To establish a fundamental understanding of the ground electronic state of iron, the electronic and magnetic states of Fe2+ in (Mg0.75,Fe0.25)O have been investigated by transmission (TMS) and synchrotron (NFS) M\\\"ossbauer spectroscopy at high pressures and low temperatures (down to 5 K)"},"claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"1110.3956","kind":"arxiv","version":1},"verdict":{"id":null,"model_set":{},"created_at":null,"strongest_claim":"","one_line_summary":"","pipeline_version":null,"weakest_assumption":"","pith_extraction_headline":""},"references":{"count":0,"sample":[],"resolved_work":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57","internal_anchors":0},"formal_canon":{"evidence_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"author_claims":{"count":0,"strong_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"builder_version":"pith-number-builder-2026-05-17-v1"},"aliases":[{"alias_kind":"arxiv","alias_value":"1110.3956","created_at":"2026-05-18T04:10:47.617983+00:00"},{"alias_kind":"arxiv_version","alias_value":"1110.3956v1","created_at":"2026-05-18T04:10:47.617983+00:00"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.1110.3956","created_at":"2026-05-18T04:10:47.617983+00:00"},{"alias_kind":"pith_short_12","alias_value":"DOKEI6IIOMAF","created_at":"2026-05-18T12:26:26.731475+00:00"},{"alias_kind":"pith_short_16","alias_value":"DOKEI6IIOMAFUJ6D","created_at":"2026-05-18T12:26:26.731475+00:00"},{"alias_kind":"pith_short_8","alias_value":"DOKEI6II","created_at":"2026-05-18T12:26:26.731475+00:00"}],"events":[],"event_summary":{},"paper_claims":[],"inbound_citations":{"count":0,"internal_anchor_count":0,"sample":[]},"formal_canon":{"evidence_count":0,"sample":[],"anchors":[]},"links":{"html":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V","json":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V.json","graph_json":"https://pith.science/api/pith-number/DOKEI6IIOMAFUJ6DR5O54JLT7V/graph.json","events_json":"https://pith.science/api/pith-number/DOKEI6IIOMAFUJ6DR5O54JLT7V/events.json","paper":"https://pith.science/paper/DOKEI6II"},"agent_actions":{"view_html":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V","download_json":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V.json","view_paper":"https://pith.science/paper/DOKEI6II","resolve_alias":"https://pith.science/api/pith-number/resolve?arxiv=1110.3956&json=true","fetch_graph":"https://pith.science/api/pith-number/DOKEI6IIOMAFUJ6DR5O54JLT7V/graph.json","fetch_events":"https://pith.science/api/pith-number/DOKEI6IIOMAFUJ6DR5O54JLT7V/events.json","actions":{"anchor_timestamp":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V/action/timestamp_anchor","attest_storage":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V/action/storage_attestation","attest_author":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V/action/author_attestation","sign_citation":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V/action/citation_signature","submit_replication":"https://pith.science/pith/DOKEI6IIOMAFUJ6DR5O54JLT7V/action/replication_record"}},"created_at":"2026-05-18T04:10:47.617983+00:00","updated_at":"2026-05-18T04:10:47.617983+00:00"}