globalchange  > 过去全球变化的重建
DOI: 10.1016/j.jhydrol.2019.03.076
WOS记录号: WOS:000474327800060
论文题名:
Evidence for conservative transport of dissolved organic carbon in major river basins in the Gulf of Maine Watershed
作者: Huntington, T. G.1; Roesler, C. S.; Aiken, G. R.
通讯作者: Huntington, T. G.
刊名: JOURNAL OF HYDROLOGY
ISSN: 0022-1694
EISSN: 1879-2707
出版年: 2019
卷: 573, 页码:755-767
语种: 英语
英文关键词: Dissolved organic carbon ; Carbon yield ; Fluvial carbon export ; Conservative transport ; Organic carbon uptake velocity ; Freshwater carbon dynamics
WOS关键词: MATTER CONCENTRATION ; TEMPERATE RIVER ; CLIMATE-CHANGE ; HUDSON RIVER ; NEW-YORK ; EXPORT ; TRENDS ; STREAM ; DOC ; FLUXES
WOS学科分类: Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
WOS研究方向: Engineering ; Geology ; Water Resources
英文摘要:

Transport and fate of dissolved organic carbon (DOC) in rivers arc important aspects of the carbon cycle and the critical linkage between terrestrial, aquatic, and marine systems. Recent studies have quantified fluvial export to the marine environment in many systems, but in-stream losses of DOC are poorly constrained. This study compares DOC yields (kg C/ha) between the area-weighted averages of several tributaries within larger watersheds with the DOC yields of the larger watersheds to gain insight on in-stream losses in larger river systems. Four large watersheds, 22 tributaries to those watersheds, and 5 additional main stem locations in Maine were studied during 1 April to 15 November in 2011 through 2013. There were no significant differences in the area weighted average DOC yield of the tributaries and the larger watersheds indicating little net in-stream loss in the main stems of the larger rivers. It is unlikely that inputs of DOC from un-gauged areas compensated for losses from gauged tributaries based on similarity in DOC yield longitudinally along the main stems of two of the rivers. In addition, wetland abundance, which is associated with higher DOC yield in this environment, did not consistently increase from tributaries to the larger watershed or longitudinally along the main stems. This geographic distribution of wetlands therefore also indicates that it is unlikely that inputs of DOC from un-gauged areas compensated for losses from gauged tributaries. These findings suggest that in-stream losses of DOC in these larger river systems are minimal and that the vast majority of DOC in major rivers in Maine is transported conservatively to the coastal ocean.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/139367
Appears in Collections:过去全球变化的重建

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作者单位: 1.US Geol Survey, Maine Off, New England Water Sci Ctr, Augusta, ME 04330 USA
2.Bowdoin Coll, Brunswick, ME 04011 USA
3.US Geol Survey, Natl Res Program, Boulder, CO USA

Recommended Citation:
Huntington, T. G.,Roesler, C. S.,Aiken, G. R.. Evidence for conservative transport of dissolved organic carbon in major river basins in the Gulf of Maine Watershed[J]. JOURNAL OF HYDROLOGY,2019-01-01,573:755-767
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