By Bianchi T., Allison M., Cai W.-J. (eds.)
This quantity presents a state of the art precis of biogeochemical dynamics at significant river-coastal interfaces for complex scholars and researchers. River platforms play an enormous function (via the carbon cycle) within the traditional self-regulation of Earth's floor stipulations via serving as a big sink for anthropogenic CO2. nearly ninety percentage of worldwide carbon burial happens in ocean margins, with nearly all of this considered buried in huge delta-front estuaries (LDEs). This publication presents info on how people have altered carbon biking, sediment dynamics, CO2 budgets, wetland dynamics, and foodstuff and hint aspect biking on the land-margin interface. some of the globally vital LDEs are mentioned throughout a number of latitudes, elevation and weather within the drainage basin, coastal oceanographic environment, and nature and measure of human alteration. it really is this breadth of exam that offers the reader with a finished figuring out of the overarching controls on significant river biogeochemistry
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Additional resources for Biogeochemical Dynamics at Major River-Coastal Interfaces: Linkages with Global Change
Lin. 2004. Sediment dynamics in a submarine canyon: a case of river–sea interaction. Mar. Geol. 207: 55–81. , Z. Xue, K. J. S. C. Li, and S. Gao. 2009. Fate of sediments delivered to the sea by Asian large rivers: long-distance transport and formation of remote alongshore clinothems. Sediment. Rec. 7: 4–9. Lohnis, F. 1926. Nitrogen availability of green manure. Soil Sci. 22: 253–290. L. Probst. 1998. River sediment discharge to the oceans: present-day controls and global budget. Am. J. Sci. 298: 265–295.
Zepp, and Y. Wang. 2004. Photooxidation and its effects on the carboxyl content of dissolved organic matter in two coastal rivers in the southeastern United States. Environ. Sci. Technol. 38: 4113–4119. Section II Water and sediment dynamics from source to sink 2 Water and sediment dynamics through the wetlands and coastal water bodies of large river deltaic plains M. A. Allison, A. Kolker, and E. Meselhe 1. Introduction The biogeochemical dynamics of major and trace elements, including nutrients and pollutants, and organic matter, at the coastal-ocean interface of major rivers is controlled in the first order by the physics of water and sediment transport.
S. Blackbird, J. Ingels, A. A. Wolff. 2011. Organic geochemistry of submarine canyons – The Portuguese Margin. Deep-Sea Res. Part II Top. Stud. Oceanogr. 58: 2477–2488. L. Lin. 2004. Sediment dynamics in a submarine canyon: a case of river–sea interaction. Mar. Geol. 207: 55–81. , Z. Xue, K. J. S. C. Li, and S. Gao. 2009. Fate of sediments delivered to the sea by Asian large rivers: long-distance transport and formation of remote alongshore clinothems. Sediment. Rec. 7: 4–9. Lohnis, F. 1926. Nitrogen availability of green manure.
Biogeochemical Dynamics at Major River-Coastal Interfaces: Linkages with Global Change by Bianchi T., Allison M., Cai W.-J. (eds.)