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| Content Provider | Springer Nature Link |
|---|---|
| Author | Patchineelam, S. M. de Figueiredo, A. G. |
| Copyright Year | 2000 |
| Abstract | Seventy-five surface and subsurface sediment samples collected on the Amazon continental shelf were analyzed by X-ray diffraction (XRD) in the grain-size fractions smaller than 2 μm. The groups of clay minerals thus identified were smectite, kaolinite, illite, and mixed-layer illite/smectite. Calculation of relative abundance shows a predominance of smectite (37%) in the whole area, followed by kaolinite (27%), illite (23%), and a small percentage of mixed-layer illite/smectite (12%). The distal, northwest region of the continental shelf is characterized by a high abundance of smectite (41%), high salinity values, and high sediment accumulation rates (10 cm year−1), whereas the proximal region is characterized by a comparatively low abundance of smectite (30%), low salinity values, and low sediment accumulation rates (<1 cm year−1). This trend of increasing abundance northwestwards documents a preferential settling of smectite in the distal and more saline regions of this estuarine system. |
| Starting Page | 37 |
| Ending Page | 42 |
| Page Count | 6 |
| File Format | |
| ISSN | 02760460 |
| Journal | Geo-Marine Letters |
| Volume Number | 20 |
| Issue Number | 1 |
| e-ISSN | 14321157 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2000-07-05 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Content Type | Text |
| Resource Type | Article |
| Subject | Environmental Science Geotechnical Engineering and Engineering Geology Oceanography |
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