Geochemistry of Suspended Matter from Waters of the Amazon Basin
- 12 Downloads
The geochemical study of the suspended matter in the waters of the Amazon River and its tributaries revealed that the chemical composition of this material ranges widely; however, generally, it is similar to the average composition of the suspended matter in the rivers and clayey sedimentary rocks around the world. Against this background, an essential regional Hg enrichment due to the anthropogenic factor is distinguished. The suspensions from the so-called clear waters from the tributaries of the Amazon River—Xingu and Trombetas—demonstrate the local enrichment in Pb, Sn, Zn, and organic carbon indicating the ore mineralization of the drainage basin, and points to the presence of metal-organic complexes.
Unable to display preview. Download preview PDF.
- 1.A. P. Lisitsyn, Sedimentation in the Oceans (Nauka, Moscow, 1974) [in Russian].Google Scholar
- 2.A. S. Monin and V. V. Gordeev, Amazonia (Nauka, Moscow, 1988) [in Russian].Google Scholar
- 3.G. N. Baturin, Oceanic Ores (Nauka, Moscow, 1993) [in Russian].Google Scholar
- 10.V. V. Gordeev, Okeanologiya 29 (4), 713–717 (1984).Google Scholar
- 11.V. Gordeev, A. A. Miklishansky, V. E. Migdisov, and V. E. Artemyev, Mitt. Geol.-Palaeontol. Inst. Univ. Hamburg, No. 58, 225–243 (1985).Google Scholar
- 12.V. V. Gordeev and V. N. Oreshkin, Geokhimiya, No. 2, 244–256 (1990).Google Scholar
- 14.V. S. Savenko, Chemical Composition of Suspended Sediments in the World Rivers (GEOS, Moscow, 2006) [in Russian].Google Scholar
- 15.N. A. Grigor’ev, Geochem. Int. 41 (7), 711–718 (2003).Google Scholar