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Download Biogeochemical Dynamics at Major River-Coastal Interfaces: by Bianchi T., Allison M., Cai W.-J. (eds.) PDF

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 complicated scholars and researchers. River platforms play a big position (via the carbon cycle) within the usual self-regulation of Earth's floor stipulations by way of serving as an incredible sink for anthropogenic CO2. nearly ninety percentage of world carbon burial happens in ocean margins, with nearly all of this considered buried in huge delta-front estuaries (LDEs). This publication presents details on how people have altered carbon biking, sediment dynamics, CO2 budgets, wetland dynamics, and food and hint point biking on the land-margin interface. the various globally very important LDEs are mentioned throughout a variety of latitudes, elevation and weather within the drainage basin, coastal oceanographic surroundings, and nature and measure of human alteration. it truly is this breadth of exam that offers the reader with a finished knowing of the overarching controls on significant river biogeochemistry

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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.

3). Periodically, all or part of an active channel belt is abandoned because of a river switching, or avulsion. Avulsion is a process that is controlled by both intrabasinal processes, such as lobe switching and river meandering, and external forcing, such as tectonics, eustasy, and climate change (Beerbower 1964; Allen 1978; Holbrook and Schumm 1999; Stouthamer and Berendsen 2007). The exact conditions for avulsions remain uncertain (Reitz et al. 2010), but Slingerland and Smith (1998) suggested that the occurrence of an avulsion depends on (1) the nature of sediment transport partitioning at the bifurcation, and (2) the ability of channels to change their capacities controlled by stream power and bank cohesion.

Sources of sedimentary organic matter in the Mississippi River and adjacent Gulf of Mexico as revealed by lipid biomarker and d13 CTOC analyses. Org. Geochem. 39: 422–439. B. H. Kenyon, and J. Evans. 2000. Continental margin sedimentation, with special reference to the northeast Atlantic margin. Sedimentology 47: 239–256. I. Gordon. 1970. Carbon-13: carbon-12 ratios in dissolved and particulate organic matter in the sea. Deep-Sea Res. 17: 17–27. 18 An introduction to the biogeochemistry of river-coastal systems Wollast, R.

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