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

By Bianchi T., Allison M., Cai W.-J. (eds.)

This quantity presents a cutting-edge precis of biogeochemical dynamics at significant river-coastal interfaces for complex scholars and researchers. River structures play a tremendous position (via the carbon cycle) within the average self-regulation of Earth's floor stipulations by way of serving as a massive sink for anthropogenic CO2. nearly ninety percentage of world carbon burial happens in ocean margins, with the vast majority of this regarded as buried in huge delta-front estuaries (LDEs). This ebook offers details on how people have altered carbon biking, sediment dynamics, CO2 budgets, wetland dynamics, and meals and hint aspect biking on the land-margin interface. a number of the globally very important LDEs are mentioned throughout a variety of latitudes, elevation and weather within the drainage basin, coastal oceanographic atmosphere, and nature and measure of human alteration. it's this breadth of exam that offers the reader with a finished knowing of the overarching controls on significant river biogeochemistry

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By Bianchi T., Allison M., Cai W.-J. (eds.)

This quantity presents a cutting-edge precis of biogeochemical dynamics at significant river-coastal interfaces for complex scholars and researchers. River structures play a tremendous position (via the carbon cycle) within the average self-regulation of Earth's floor stipulations by way of serving as a massive sink for anthropogenic CO2. nearly ninety percentage of world carbon burial happens in ocean margins, with the vast majority of this regarded as buried in huge delta-front estuaries (LDEs). This ebook offers details on how people have altered carbon biking, sediment dynamics, CO2 budgets, wetland dynamics, and meals and hint aspect biking on the land-margin interface. a number of the globally very important LDEs are mentioned throughout a variety of latitudes, elevation and weather within the drainage basin, coastal oceanographic atmosphere, and nature and measure of human alteration. it's this breadth of exam that offers the reader with a finished knowing of the overarching controls on significant river biogeochemistry

Show description

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Rates of C, N, P and Si recycling and denitrification at the US Mid-Atlantic continental slope depocenter. Deep-Sea Res. I. 47: 1405–1428. P. A. E. T. R. M. Walz. 2001. The annual cycle of iron and the biological response in central California coastal waters. Geophys. Res. Lett. 28: 1247–1250. , X. Zhou, and K. Mopper. 1990. Formation of carbonyl compounds from UV-induced photodegradation of humic substances in natural waters: fate of riverine carbon in the sea. Limnol. Oceanogr. 35: 1503–1515.

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. , P. L. Probst. 1996. River discharges of carbon to the world’s oceans: Determining local inputs of alkalinity and of dissolved and particulate organic carbon.

And Smith 2004). This process is most evident in sediment-load dominated systems such as the Mississippi, where wave, tide, and current redistribution are less important in controlling where the bulk of riverine sediment accumulates; at least six individual and overlapping, distributary lobe phases have formed in the Mississippi system over the last ß7,500 years (Frazier 1967; Penland et al. 1988). The subaerial deltaic plain, and intervening open water bodies and their fringing wetlands, are the focus of the present chapter.

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