Titlebook: Carbon and Nutrient Fluxes in Continental Margins; A Global Synthesis Kon-Kee Liu,Larry Atkinson,Liana Talaue-McManus Book 2010 Springer-Ve

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https://doi.org/10.1007/978-94-007-0723-8undwater discharge may be equally or even more important in terms of material transport across land/sea margins (Li et al. 1999; Kim et al. 2002; Burnett 2003; Kim et al. 2003a). In this chapter, we therefore define SGD to consist truly fresh groundwater, recirculated seawater, or a composite thereof.

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Isaac Elishakoff,Lova Andriamasytion rate. The burial of organic carbon is associated with fine-grained sediment, which covers about 22% of the area of the world’s shelf regions, while the burial of inorganic carbon takes place not only in fine-grained sediments but also in relict sediments, shell beds, and coral reefs on the shelf.

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Submarine Groundwater Discharge (SGD) and Associated Nutrient Fluxes to the Coastal Oceanundwater discharge may be equally or even more important in terms of material transport across land/sea margins (Li et al. 1999; Kim et al. 2002; Burnett 2003; Kim et al. 2003a). In this chapter, we therefore define SGD to consist truly fresh groundwater, recirculated seawater, or a composite thereof.

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Cross-Boundary Exchanges of Carbon and Nitrogen in Continental Margins1se surface waters, whether terrestrial or oceanic, generally reach an equilibrium with atmospheric CO. and other gases somewhat rapidly. By contrast, it takes several 100 years for the surface waters of the oceans to first sink to great depths in the polar regions, and then slowly move horizontally to fill in the deep basins of the world’s oceans.

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Sediment and Carbon Accumulation on Continental Shelves1tion rate. The burial of organic carbon is associated with fine-grained sediment, which covers about 22% of the area of the world’s shelf regions, while the burial of inorganic carbon takes place not only in fine-grained sediments but also in relict sediments, shell beds, and coral reefs on the shelf.

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Global Synthesis1astal or margin dimensions (e.g., distance from the shoreline to the 130m isobath; Wollast 1998; Mackenzie et al. 2004). However, many important transport processes that are directly associated with the margin often extend across these depth boundaries and the resulting budgets may not fully represent the role of margins in biogeochemical cycles.

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