A hybrid numerical model system of LCO2 and CO2 enriched seawater dynamics in the ocean induced by moving-ship releasing
| Autor: | Makoto Akai, Yongchen Song, T. Ohsumi, Masahiro Nishio, Baixin Chen |
|---|---|
| Rok vydání: | 2004 |
| Předmět: |
Mechanical Engineering
Dynamics (mechanics) Ocean current Scalar (physics) Mineralogy Model system Building and Construction Pollution Industrial and Manufacturing Engineering Plume chemistry.chemical_compound General Energy chemistry Carbon dioxide Mass flow rate Environmental science Seawater Electrical and Electronic Engineering Civil and Structural Engineering |
| Zdroj: | Energy. 29:1487-1497 |
| ISSN: | 0360-5442 |
| DOI: | 10.1016/j.energy.2004.03.082 |
| Popis: | A numerical modeling system has been developed, based on an engineering background, of the direct disposal of liquid carbon dioxide into the ocean by a moving-ship, to predict the physico–chemical dynamics of liquid carbon dioxide droplets and carbon dioxide enriched seawater in the ocean. This is a hybrid simulation model system consisting of a three-dimensional small-scale near-field model and a two-dimensional horizontal turbulent dispersion model. The dynamics near to release sites include double-plume creation, interaction, evolution, and coupling with ocean currents; these are described by using two-fluid large-eddy simulation technology. The further development of carbon dioxide enriched seawater, as a passive-inert scalar, in relatively larger spatial and time scales (28×28 km and up to 100 h) is then simulated by a horizontal turbulent dispersion model. For the case of liquid carbon dioxide release at a depth of 2000 m with mass flow rate of 100 kg/s and initial droplet diameter of 8.0 mm, and with ship speed of 3.0 m/s, the model predicts a vertically separated carbon dioxide enriched seawater plume, 330 m in height and 40 m in width at time about 1 h after release with a minimum pH of 6.20 corresponding to carbon dioxide concentration of 0.18 kg/m3, in the surrounding area. This carbon dioxide enriched seawater plume diffused turbulently in the horizontal surface to an area of 9.8×10.5 km2 after 100 h. |
| Databáze: | OpenAIRE |
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