4.7 Article

A multi-stable isotopic constraint on water column oxygen sinks in the Pearl River Estuary, South China

期刊

MARINE ENVIRONMENTAL RESEARCH
卷 178, 期 -, 页码 -

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.marenvres.2022.105643

关键词

Oxygen depletion; Stable isotopes; Organic matter degradation; Nitrification; The Pearl river estuary

资金

  1. Guangzhou Science, Technology and Innovation Commission [201904010431]
  2. Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (Guangzhou) [GML2019ZD0308]
  3. National Science Foundation of China [42073074]
  4. Youth Innovation Promotion Association of CAS [2019346]

向作者/读者索取更多资源

This study uses a multi-stable isotope approach to quantitatively analyze oxygen consumption processes in the Pearl River Estuary. The results show that organic carbon degradation through oxygen respiration is the dominant oxygen-consuming process in the upper reach and inner estuary, while nitrification also plays a significant role in the upper reach.
Bottom water oxygen depletion is a central concern in estuaries and coastal oceans worldwide. However, a mechanistic understanding and quantitative diagnosis of different oxygen-consuming processes are less clear. In this study, a multi-stable isotope approach is developed to delineate the role of oxygen respiration and nitrification contributing to total oxygen consumption in the Pearl River Estuary (PRE), a large eutrophic estuary in south China. The approach highly couples with analysis of the carbon isotope composition of dissolved inorganic carbon (delta C-13-DIC) and with stable nitrogen isotope analysis in ammonium (delta N-15-NH4+) and nitrate (delta N-15-NOi). In all seasons, relatively low DO concentrations were observed in the upper reach and, to some extent, in the outer estuary during summer, while high concentrations of DO were found in the transition zone between the inner and outer estuary. On the basis of isotopic differentiation, our data reveal that much more depleted delta C-13-DIC is coincident with DIC additions and low oxygen in the upper reach and inner estuary during most seasons. This is most likely a consequence of organic carbon (OC) degradation via aerobic respiration. Based on the carbon isotopic mass balance of DIC and the stoichiometry ratio of -delta DO/&delta DIC, we found that the OC degradation dominates the total oxygen consumption in the upper reach, as well as in the inner estuary during summer (48.3%-93.5%). In addition, nitrification is another key process in contributing to total oxygen loss in the upper reach, as supported by the well-coupled variations of delta N-15 of NH4+ and NO3 and apparent oxygen utilization (AOU). Using the formerly determined N isotopic fractionation and observed delta N-15 variation, we estimated that nitrification could account for 35.3%-44.1% and 28.5%-31.6% of the total oxygen consumption in the upper reach during winter and summer, respectively, while its contribution to total oxygen loss is minor in the inner and outer estuary. Overall, this study demonstrates the potential of the multi-stable isotopic approach to assess oxygen sink partitioning in large human-perturbed estuaries.

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