首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Abundance, distribution, and fluxes of dissolved organic carbon (DOC) in four small sub-tropical rivers of the Tampa Bay Estuary (Florida, USA)
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Abundance, distribution, and fluxes of dissolved organic carbon (DOC) in four small sub-tropical rivers of the Tampa Bay Estuary (Florida, USA)

机译:坦帕湾河口(美国佛罗里达州)的四条亚热带小河中溶解有机碳(DOC)的丰度,分布和通量

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The delivery of organic carbon (C) from rivers to the coastal ocean via estuaries is recognized as an important component of the global C budget however, smaller river systems are often overlooked and modern flux estimates are not very different from historical estimates. Here, the seasonal (wet vs. dry) concentration and fluxes of dissolved organic C (DOC) were measured in five small sub-tropical rivers that drain into the Tampa Bay (FL, USA) estuary. DOC distributions were highly variable among riverine, mesohaline, and marine end-member samples in all river catchments and no significant differences were observed among or between DOC concentrations with respect to river catchment, season, or year of sampling. In general, DOC mixed non-conservatively during the wet seasons, and conservatively during the dry seasons, with the estuarine reaches of each river serving as a sink of DOC. Fluxes were strongly tied to discharge irrespective of season, and the estuaries removed 15-65% of DOC prior to export to coastal Bay and Gulf of Mexico waters. DOC concentrations were similar to others reported for low-elevation sub-tropical rivers, and a combination of elevation, residence time, and climate appear to control the abundance and variability of DOC in sub-tropical vs. tropical river systems. The characterization of DOC in small, sub-tropical rivers, which share characteristics with both their temperate and tropical counterparts, is critical for quantitatively constraining the importance of these systems in local-to-regional scale ocean C budgets. In addition to geomorphic properties, the role of past, present, and future land cover and other environmental change in small coastal rivers also exerts control on the quantity and flux of DOC in these systems. (C) 2015 Elsevier Ltd. All rights reserved.
机译:经由河口从河流向沿海海洋的有机碳(C)输送被认为是全球C预算的重要组成部分,但是,较小的河流系统经常被忽视,现代通量估算值与历史估算值相差无几。在这里,在流入坦帕湾(美国佛罗里达州)河口的五条小型亚热带河流中,测量了季节性(湿与干)浓度和溶解有机碳(DOC)通量。在所有河流集水区的河流,中盐和海洋末段样品中,DOC的分布变化很大,在河流集水区,季节或年份方面,DOC浓度之间或之间没有发现显着差异。通常,DOC在雨季非保守地混合,而在旱季则保守地混合,每条河的河口段都是DOC的汇。无论季节如何,通量都与排放紧密相关,在出口到沿海海湾和墨西哥湾水域之前,河口去除了DOC的15-65%。低海拔的亚热带河流的DOC浓度与其他报告的相似,并且海拔,停留时间和气候的组合似乎控制了亚热带与热带河流系统中DOC的丰度和变异性。与温带和热带河流都有共同特征的亚热带小河中DOC的特征,对于从数量上限制这些系统在地方到区域规模的海洋碳预算中的重要性至关重要。除了地貌特征外,沿海小河流中过去,现在和将来的土地覆盖以及其他环境变化的作用还控制着这些系统中DOC的数量和通量。 (C)2015 Elsevier Ltd.保留所有权利。

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