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- W156600131 abstract "Publisher SummaryThe objective of this chapter is to examine and synthesize the published literature with respect to the sources and production of terrestrially derived Dissolved Organic Carbon (DOC), its relationship with Dissolved Organic Nitrogen (DON), and the mechanistic controls on their export from terrestrial ecosystems to surface waters. Allochthonous dissolved organic matter is a source of organic carbon, nitrogen, phosphorus, and sulfur to aquatic systems that is derived from the surrounding terrestrial ecosystem. Dissolved Organic Matter (DOM) is produced as precipitation moves through the atmosphere, washes through vegetation, infiltrates the soil organic horizon, and percolates downward through mineral soil horizons. Organic forms of carbon, nitrogen, sulfur, and phosphorus contribute to bulk DOM. The contribution of mineral soil solution DOM to allochthonous inputs will depend on: (1) watershed slope, (2) depth of water table, (3) antecedent soil moisture, and (4) barriers to organic soil solution infiltration of the mineral soil. Delivery of terrestrially derived DOC and DON to the surface waters depends on the balance between production and loss from solution, and the opportunity for hydrological transport. Large fluxes of atlochthonous DOM to surface waters occur when there is a barrier precluding water infiltration of the soil column. Saturated soils— such as wetlands and peatlands also tend to produce runoff with higher DOC concentrations." @default.
- W156600131 created "2016-06-24" @default.
- W156600131 creator A5044126812 @default.
- W156600131 creator A5050845910 @default.
- W156600131 creator A5078193448 @default.
- W156600131 date "2003-01-01" @default.
- W156600131 modified "2023-10-14" @default.
- W156600131 title "Sources, Production, and Regulation of Allochthonous Dissolved Organic Matter Inputs to Surface Waters" @default.
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