Please use this identifier to cite or link to this item:
http://hdl.handle.net/10397/111195
| DC Field | Value | Language |
|---|---|---|
| dc.contributor | Department of Civil and Environmental Engineering | - |
| dc.creator | De Leo, A | - |
| dc.creator | Stocchino, A | - |
| dc.date.accessioned | 2025-02-17T01:37:55Z | - |
| dc.date.available | 2025-02-17T01:37:55Z | - |
| dc.identifier.issn | 1070-6631 | - |
| dc.identifier.uri | http://hdl.handle.net/10397/111195 | - |
| dc.language.iso | en | en_US |
| dc.publisher | AIP Publishing LLC | en_US |
| dc.rights | © 2022 Author(s). Published under an exclusive license by AIP Publishing. | en_US |
| dc.rights | This article may be downloaded for personal use only. Any other use requires prior permission of the author and AIP Publishing. This article appeared in De Leo, A., & Stocchino, A. (2022). Dispersion of heavy particles under sea waves. Physics of Fluids, 34(1) and may be found at https://doi.org/10.1063/5.0074760. | en_US |
| dc.title | Dispersion of heavy particles under sea waves | en_US |
| dc.type | Journal/Magazine Article | en_US |
| dc.identifier.spage | 013305-1 | - |
| dc.identifier.epage | 013305-14 | - |
| dc.identifier.volume | 34 | - |
| dc.identifier.issue | 1 | - |
| dc.identifier.doi | 10.1063/5.0074760 | - |
| dcterms.abstract | We report the results of a series of numerical simulations performed with the aim to describe the dispersion of heavy particles transported by sea waves. Recent studies investigated the interplay between the wave Stokes drift and the inertial character of negatively buoyant particles that, ultimately, yields an augmented settling velocity. Our interest is to investigate the possible occurrence of a Brownian regime that would allow for the definition of a diffusion coefficient. The velocity and acceleration auto-correlation functions and the corresponding integral time scales show that already at a very low Stokes number the particles behave very differently from the fluid. The main consequence is that an asymptotic diffusive regime is rarely observed, except as a transient regime or when the background random noise is comparable with the wave field velocities. | - |
| dcterms.accessRights | open access | en_US |
| dcterms.bibliographicCitation | Physics of fluids, Jan. 2022, v. 34, no. 1, 013305, p. 013305-1 - 013305-14 | - |
| dcterms.isPartOf | Physics of fluids | - |
| dcterms.issued | 2022-01 | - |
| dc.identifier.scopus | 2-s2.0-85123016913 | - |
| dc.identifier.eissn | 1089-7666 | - |
| dc.identifier.artn | 013305 | - |
| dc.description.validate | 202502 bcch | - |
| dc.description.oa | Version of Record | en_US |
| dc.identifier.FolderNumber | OA_Others | en_US |
| dc.description.fundingSource | Others | en_US |
| dc.description.fundingText | Interreg Program Italia-Francia Marittimo | en_US |
| dc.description.pubStatus | Published | en_US |
| dc.description.oaCategory | VoR allowed | en_US |
| Appears in Collections: | Journal/Magazine Article | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| 013305_1_online.pdf | 5.22 MB | Adobe PDF | View/Open |
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