{
  "annotation_id": "3424596c-e88c-4600-96f0-0ebeddb9ef55",
  "date_created": "2026-03-02T18:00:49.900000Z",
  "date_modified": "2026-03-02T18:00:49.900000Z",
  "file_hash": "43e7cf1f06d5c8bbd9415d3a691c9524f780947a503aaebec5d26f01210aad05",
  "private": false,
  "record": {
    "abstract": "Surface-tension-related phenomena have fascinated researchers for a long\ntime, and the mathematical description pioneered by Young and Laplace opened\nthe door to their systematic study. The time scale on which\nsurface-tension-driven motion takes place is usually quite short, making\nexperimental investigation quite demanding. Accordingly, most theoretical and\nexperimental work has focused on static phenomena, and in particular the\nmeasurement of surface tension, by physicists like E\\\"otv\\\"os, Lenard, and\nBohr. Here we will review some of the work that has eventually lead to a closer\nscrutiny of time-dependent flows, highly non-linear in nature. Often this\nmotion is self-similar in nature, such that it can in fact be mapped onto a\npseudo-stationary problem, amenable to mathematical analysis.",
    "arxiv_id": "physics/0403056",
    "authors": [
      "Jens Eggers"
    ],
    "categories": [
      "physics.flu-dyn"
    ],
    "title": "A brief history of drop formation",
    "url": "https://arxiv.org/abs/physics/0403056"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "1475a816-31a8-4eca-8e3f-d875a89f52a4",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}