{
  "annotation_id": "293791ec-da7d-4edb-afa4-a80e877cf97f",
  "date_created": "2026-03-02T18:01:00.640000Z",
  "date_modified": "2026-03-02T18:01:00.640000Z",
  "file_hash": "9b5c7a85749e53db089dd3edd545ba8f96bb1d0aa4dd41e485f5ed43259a6620",
  "private": false,
  "record": {
    "abstract": "In preparation to the experimental results which will be available in the\nfuture, we study geo-neutrino production for different models of mantle\nconvection and composition. By using global mass balance for the Bulk Silicate\nEarth, the predicted flux contribution from distant sources in the crust and in\nthe mantle is fixed within a total uncertainty of +-15%. We also discuss\nregional effects, provided by subducting slabs or plumes near the detector. In\nfour years a five-kton detector operating at a site relatively far from nuclear\npower plants can achieve measurements of the geo-neutrino signal accurate to\nwithin +-5%. It will provide a crucial test of the Bulk Silicate Earth and a\ndirect estimate of the radiogenic contribution to terrestrial heat.",
    "arxiv_id": "physics/0508019",
    "authors": [
      "Gianni Fiorentini",
      "Marcello Lissia",
      "Fabio Mantovani",
      "Riccardo Vannucci"
    ],
    "categories": [
      "physics.geo-ph",
      "nucl-th"
    ],
    "doi": "10.1016/j.epsl.2005.06.061",
    "journal_ref": "Earth Planet.Sci.Lett.238:235-247,2005",
    "title": "Geo-neutrinos: a new probe of Earth\u0027s interior",
    "url": "https://arxiv.org/abs/physics/0508019"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "aaff628f-b527-4ed8-9f05-703237361ce3",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}