Abstract
Six sediment cores collected from the Northwestern Arabian/Persian Gulf have been radiometrically dated by 210Pb. Three cores were collected from stations within the Kuwait Bay, and three others were collected from stations outside the bay. Two models have been used for 210Pb dating of sediment cores, i.e. Constant Flux: Constant Sedimentation (CF:CS) Model and the Constant Rate of Supply (CRS) Model. The average rates were found to vary significantly between 0.16 and 1.00 cm y-1 for stations outside and within the bay respectively. The variability of the sedimentation rate was essentially physiographic characteristics and variable hydrodynamic condition. In this study, 137Cs fallout radiotracer was also used to construct a realistic chronology. It was observed that the 137Cs in the entire vertical profile has been continuously contributed by fluvial and atmospheric deposition.
| Original language | English |
|---|---|
| Pages (from-to) | 247-255 |
| Number of pages | 9 |
| Journal | Journal of Radioanalytical and Nuclear Chemistry |
| Volume | 301 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jul 2014 |
Keywords
- Kuwait Bay
- Recent sediment deposition
Funding Agency
- Kuwait Foundation for the Advancement of Sciences