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Biogeosciences An interactive open-access journal of the European Geosciences Union

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Biogeosciences, 8, 597-620, 2011
http://www.biogeosciences.net/8/597/2011/
doi:10.5194/bg-8-597-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
 
07 Mar 2011
Global spatial distribution of natural riverine silica inputs to the coastal zone
H. H. Dürr1,2,3, M. Meybeck2, J. Hartmann4,6, G. G. Laruelle5, and V. Roubeix3,7 1Department of Physical Geography, Faculty of Geosciences, Utrecht University, The Netherlands
2UMR 7619 Sisyphe, Université Pierre et Marie Curie (Paris VI), Paris, France
3ESA (Ecologie des Systèmes Aquatiques), Université Libre de Bruxelles, Belgium
4Institute for Applied Geosciences, Darmstadt University of Technology, Germany
5Department of Earth Sciences – Geochemistry, Faculty of Geosciences, Utrecht University, The Netherlands
6Institute for Biogeochemistry & Marine Chemistry, KlimaCampus, Universität Hamburg, Germany
7Cemagref Bordeaux, Gazinet-Cestas, France
Abstract. Silica, SiO2, in dissolved (DSi) and particulate (PSi) form, is both a major product of continental weathering as well as an essential nutrient in terrestrial and aquatic systems. Here we present estimates of the spatial distribution of riverine silica fluxes under natural conditions, i.e. without human influence, to ~140 segments of the global coastal zone. Focussing on the construction of the DSi budget, natural DSi concentration is multiplied with discharge of rivers for each segment for documented basins and segments. Segments with no documentation available are estimated using clustered information based mainly on considerations of local lithology, climate, and lake retention. We approximate fluxes of particulate silica in various forms (PSi) from fluxes of suspended matter, calculated from existing models. Results have been established for silica fluxes, concentrations and yields for drainage basins of the different continents, oceans basins as well as coastal segment basins. For the continental surfaces actually draining into the oceans (exorheic regions, representing 114.7 million (M) km2), 371 M t y−1 of DSi and 8835 M t y−1 of PSi are transported, corresponding to a mean concentration of 9.5 mg l−1 and 226 mg l−1, and to a mean yield of 3.3 t km−2 y−1 and 77 t km−2 y−1, respectively. DSi yields exceeding 6.6 t km−2 y−1, i.e. >2× the global average, represent 17.4% of the global continental ice-free exorheic area but correspond to 56.0% of DSi fluxes. Pacific catchments hold most of the hyper-active areas (>5× global average), suggesting a close connection between tectonic activity and DSi fluxes resulting from silicate weathering. The macro-filters of regional and marginal seas intercept 33% and 46% of the total dissolved and particulate silica fluxes. The mass of DSi received from rivers per unit square area of various oceans ranges over more than one order of magnitude. When expressed per unit volume and when individual regional seas are considered this figure ranges over two to three orders of magnitude, an illustration of the heterogeneity of the land to sea connection.

Citation: Dürr, H. H., Meybeck, M., Hartmann, J., Laruelle, G. G., and Roubeix, V.: Global spatial distribution of natural riverine silica inputs to the coastal zone, Biogeosciences, 8, 597-620, doi:10.5194/bg-8-597-2011, 2011.
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