Sea surface pCO in an urbanized coastal system (Jiaozhou Bay, China) during summer.
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ID: 16170
2019
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Abstract
Various biogeochemical processes complicate carbon dioxide (CO) behaviour in coastal oceans. Through eight summer surveys, detailed variations in CO mechanisms in the urbanized Jiaozhou Bay, China, were analysed. During the rainless period, respiration and dissolved inorganic carbon input from treated wastewater made the northeastern region a strong CO source, while the western region with cleaner seawater was a weak source because calcium carbonate (CaCO) precipitation exceeded primary production. Rainfall events with different intensities and locations caused significantly different effects. When rainfall occurred over the sea, enhanced primary production caused a CO sink; when rainfall induced little terrestrial pollutant input, CaCO precipitation exceeded net primary production, leading to a CO source. When heavy rain caused bulk runoff, the northeastern region was a strong CO source because rivers flowing through downtown regions inputted considerable organic matter, while in the western region, runoff through suburbs and wetlands led to a strong sink.
| Reference Key |
liu2019seamarine
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|---|---|
| Authors | Liu, Xiang-Yu;Yang, Xu-Feng;Li, Yun-Xiao;Zhang, Long-Jun; |
| Journal | Marine pollution bulletin |
| Year | 2019 |
| DOI |
S0025-326X(19)30577-6
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| URL | |
| Keywords | Keywords not found |
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