{
  "annotation_id": "690c4295-b777-41bd-a87f-38d42d4e4287",
  "date_created": "2026-03-02T18:00:46.909000Z",
  "date_modified": "2026-03-02T18:00:46.909000Z",
  "file_hash": "e2c9ae886d049eded605da94dcda096c017b9184783fbf65573705647b374064",
  "private": false,
  "record": {
    "abstract": "A prototypical problem in the study of wetting phenomena is that of a solid\nplunging into or being withdrawn from a liquid bath. In the latter, de-wetting\ncase, a critical speed exists above which a stationary contact line is no\nlonger sustainable and a liquid film is being deposited on the solid.\nDemonstrating this behavior to be a hydrodynamic instability close to the\ncontact line, we provide the first theoretical explanation of a classical\nprediction due to Derjaguin and Levi: instability occurs when the outer, static\nmeniscus approaches the shape corresponding to a perfectly wetting fluid.",
    "arxiv_id": "physics/0312140",
    "authors": [
      "Jens Eggers"
    ],
    "categories": [
      "physics.flu-dyn"
    ],
    "doi": "10.1103/PhysRevLett.93.094502",
    "title": "Hydrodynamic theory of de-wetting",
    "url": "https://arxiv.org/abs/physics/0312140"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "c5add1dd-1a99-4926-8957-c1ed13fe8ec8",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}