Three-dimensional oil spill transport and dispersion at sea by an event of blowout
The simulated droplet trajectories of the 3-D model at the Caribbean platform showed that droplets with a diameter of 50 µm formed a distinct subsurface plume, which was transported horizontally and could remain below the surface. This plume could have a very restricted area of impact because the di...
| Autores: | , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2014 |
| País: | Colombia |
| Institución: | Universidad Nacional de Colombia |
| Repositorio: | Repositorio UN |
| Idioma: | español |
| OAI Identifier: | oai:repositorio.unal.edu.co:unal/48920 |
| Acceso en línea: | https://repositorio.unal.edu.co/handle/unal/48920 http://bdigital.unal.edu.co/42377/ |
| Access Level: | acceso abierto |
| Palabra clave: | Blowout hydrodynamic spread oil spill |
| Sumario: | The simulated droplet trajectories of the 3-D model at the Caribbean platform showed that droplets with a diameter of 50 µm formed a distinct subsurface plume, which was transported horizontally and could remain below the surface. This plume could have a very restricted area of impact because the dispersion is only controlled by the ocean currents which, at 1000 m depth, have a low intensity and are quite turbulent. In this case, the formed plume stayed trapped at 1000 m depth, not posing a risk to the Caribbean Coast. In contrast, droplets with diameters of 250 µm, 1 and 10 mm rose rapidly to the surface, even with different velocities (6, 10, 20 ms-1).. |
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