抜粋
A model is developed to simulate the temporal and spatial distributions of suspended sediment in the surf zone. The model is solved numerically in a time domain and in a two-dimensional vertical plane. At each time step of computation, the upper moving boundary (water surface) and the velocity field are determined through the solution of a hydrodynamic model which is based on the Reynolds equations of motion. The sediment concentration field is then determined by solving the convection-diffusion equation of the sediment mass. The comparisons with laboratory data of various experimental conditions show reasonable agreements for the simulated wave field and the concentration field in the surf zone.
| 元の言語 | English |
|---|---|
| 記事番号 | 97JC00790 |
| ページ（範囲） | 23169-23186 |
| ページ数 | 18 |
| ジャーナル | Journal of Geophysical Research C: Oceans |
| 巻 | 102 |
| 発行部数 | C10 |
| DOI | |
| 出版物ステータス | Published - 1997 1 1 |
| 外部発表 | Yes |
ASJC Scopus subject areas
- Geophysics
- Forestry
- Oceanography
- Aquatic Science
- Ecology
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth-Surface Processes
- Atmospheric Science
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science
- Palaeontology
フィンガープリント A convection-diffusion model for suspended sediment in the surf zone' の研究トピックを掘り下げます。これらはともに一意のフィンガープリントを構成します。
これを引用
Duy, N. T., & Shibayama, T. (1997). A convection-diffusion model for suspended sediment in the surf zone. Journal of Geophysical Research C: Oceans, 102(C10), 23169-23186. [97JC00790]. https://doi.org/10.1029/97JC00790