{"state_type":"pith_open_graph_state","state_version":"1.0","pith_number":"pith:2023:WSQPSZUFLGXY3XR5ZVYCLBASJP","merge_version":"pith-open-graph-merge-v1","event_count":2,"valid_event_count":2,"invalid_event_count":0,"equivocation_count":0,"current":{"canonical_record":{"metadata":{"abstract_canon_sha256":"48400870b19d19eefb206c44eb4bda17e51de65ff341635b9ff98a11d2a49ffa","cross_cats_sorted":[],"license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"physics.geo-ph","submitted_at":"2023-01-24T08:02:21Z","title_canon_sha256":"37132a488269945eca6463318c3508d946e64434e1e36c5e7b16add497cd36ed"},"schema_version":"1.0","source":{"id":"2301.09853","kind":"arxiv","version":1}},"source_aliases":[{"alias_kind":"arxiv","alias_value":"2301.09853","created_at":"2026-07-05T05:35:35Z"},{"alias_kind":"arxiv_version","alias_value":"2301.09853v1","created_at":"2026-07-05T05:35:35Z"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.2301.09853","created_at":"2026-07-05T05:35:35Z"},{"alias_kind":"pith_short_12","alias_value":"WSQPSZUFLGXY","created_at":"2026-07-05T05:35:35Z"},{"alias_kind":"pith_short_16","alias_value":"WSQPSZUFLGXY3XR5","created_at":"2026-07-05T05:35:35Z"},{"alias_kind":"pith_short_8","alias_value":"WSQPSZUF","created_at":"2026-07-05T05:35:35Z"}],"graph_snapshots":[{"event_id":"sha256:3103897e0235fbbf81ffb21c2a1454fa9a9bb5c825af2de440bdf5766cc47f26","target":"graph","created_at":"2026-07-05T05:35:35Z","signer":{"key_id":"pith-v1-2026-05","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54","signer_id":"pith.science","signer_type":"pith_registry"},"payload":{"graph_snapshot":{"author_claims":{"count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57","strong_count":0},"builder_version":"pith-number-builder-2026-05-17-v1","claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"formal_canon":{"evidence_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"integrity":{"available":true,"clean":true,"detectors_run":[],"endpoint":"/pith/2301.09853/integrity.json","findings":[],"snapshot_sha256":"c28c3603d3b5d939e8dc4c7e95fa8dfce3d595e45f758748cecf8e644a296938","summary":{"advisory":0,"by_detector":{},"critical":0,"informational":0}},"paper":{"abstract_excerpt":"The partial differential equations describing immiscible, but soluble, carbon dioxide (CO2) displacement of brine are developed including local mass-transfer effects. Scaling relationships for characteristic time among laboratory and representative storage formation conditions are found upon assumption that free-phase CO2 transport during injection is dominated by convection. The implication is that an hour in the FluidFlower (large-scale visual model) scales to hundreds of years of elapsed time in the storage formation. The scaling criteria permit extrapolation of the effects of changes in pa","authors_text":"Anthony R. Kovscek, Jan Martin Nordbotten, Martin A. Ferno","cross_cats":[],"headline":"","license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"physics.geo-ph","submitted_at":"2023-01-24T08:02:21Z","title":"Scaling up FluidFlower results for carbon dioxide storage in geological media"},"references":{"count":0,"internal_anchors":0,"resolved_work":0,"sample":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"2301.09853","kind":"arxiv","version":1},"verdict":{"created_at":null,"id":null,"model_set":{},"one_line_summary":"","pipeline_version":null,"pith_extraction_headline":"","strongest_claim":"","weakest_assumption":""}},"verdict_id":null}}],"author_attestations":[],"timestamp_anchors":[],"storage_attestations":[],"citation_signatures":[],"replication_records":[],"corrections":[],"mirror_hints":[],"record_created":{"event_id":"sha256:e60d778feab7189699fcd194f19f96eab12969ca3b7bfaa7804c4c2a313748cd","target":"record","created_at":"2026-07-05T05:35:35Z","signer":{"key_id":"pith-v1-2026-05","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54","signer_id":"pith.science","signer_type":"pith_registry"},"payload":{"attestation_state":"computed","canonical_record":{"metadata":{"abstract_canon_sha256":"48400870b19d19eefb206c44eb4bda17e51de65ff341635b9ff98a11d2a49ffa","cross_cats_sorted":[],"license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"physics.geo-ph","submitted_at":"2023-01-24T08:02:21Z","title_canon_sha256":"37132a488269945eca6463318c3508d946e64434e1e36c5e7b16add497cd36ed"},"schema_version":"1.0","source":{"id":"2301.09853","kind":"arxiv","version":1}},"canonical_sha256":"b4a0f9668559af8dde3dcd702584124bffdeaaa8cd4d8019d450a00445252fa4","receipt":{"algorithm":"ed25519","builder_version":"pith-number-builder-2026-05-17-v1","canonical_sha256":"b4a0f9668559af8dde3dcd702584124bffdeaaa8cd4d8019d450a00445252fa4","first_computed_at":"2026-07-05T05:35:35.016075Z","key_id":"pith-v1-2026-05","kind":"pith_receipt","last_reissued_at":"2026-07-05T05:35:35.016075Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54","receipt_version":"0.3","signature_b64":"0fRv4MKHmkPfh9+4ig8I10gR/n8/Mq0RBxwf11Ah4FvTERauChhtnFTY3NiLnhrlzEOC7nalXCj65jf4Qx+GDw==","signature_status":"signed_v1","signed_at":"2026-07-05T05:35:35.016599Z","signed_message":"canonical_sha256_bytes"},"source_id":"2301.09853","source_kind":"arxiv","source_version":1}}},"equivocations":[],"invalid_events":[],"applied_event_ids":["sha256:e60d778feab7189699fcd194f19f96eab12969ca3b7bfaa7804c4c2a313748cd","sha256:3103897e0235fbbf81ffb21c2a1454fa9a9bb5c825af2de440bdf5766cc47f26"],"state_sha256":"0c9ca90a8fa7320d16c1e8e544dcfcdd0aea8ac73b6f2226f8c1965526579fb8"}