4.6 Article

Limited capacity of suspended particulate matter in the Yangtze River Estuary and Hangzhou Bay to carry phosphorus into coastal seas

Journal

ESTUARINE COASTAL AND SHELF SCIENCE
Volume 258, Issue -, Pages -

Publisher

ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ecss.2021.107417

Keywords

Yangtze river estuary; Suspended particulate matter; Dissolved inorganic phosphorous; Exchangeable inorganic phosphorus; Incubation; Particulate phosphorous; Salinity gradients

Funding

  1. National Natural Science Foundation of China [NSFC 41673078]

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The Yangtze River carries high loads of suspended particulate matter and phosphorus into the estuary, but primary production in coastal seas is limited by phosphorus. The release of exchangeable inorganic phosphorus (Ex-iP) from suspended particulate matter is affected by salinity, with high salinity increasing the efficiency of release. However, the contribution of Ex-iP from suspended particulate matter declines rapidly with decreasing concentrations, impacting the capacity to carry bioavailable phosphorus to coastal seas.
The Yangtze River carries high fluxes of suspended particulate matter (SPM) and associated particulate phosphorus into the Yangtze River Estuary (YRE), but primary production in coastal seas is phosphorus-limited. Understanding the kinetics of exchangeable inorganic phosphorus (Ex-iP) released from SPM in response to different salinities and SPM concentrations is the key to demonstrating their capacity to carry bioavailable phosphorus into coastal seas. We conducted field investigations and set up a series of incubation experiments with SPM collected from marine and freshwater settings under controlled conditions, with biotic activities inhibited. Our incubation experiments showed that initial rise in salinity substantially increases the efficiency and rates of Ex-iP release, leading to an early release of majority of Ex-iP from riverine SPM when encountering saline waters, but high salinity may result in desorption. Concentrations of released DIP are linearly related to SPM concentrations, but concentrations of DIP in micromoles per gram of SPM are negatively logarithmically related to SPM concentrations, which help prevent SPM from full release of Ex-iP at the river mouth. Release of Ex-iP is insufficient to buffer DIP in the YRE. The contribution of Ex-iP from SPM decline rapidly with the attenuation of SPM concentration, and becomes negligible offshore. Extremely high loads of SPM in Hangzhou Bay allows it to retain some capacity to carry Ex-iP offshore. High concentrations of SPM in a turbid estuary are more important in reducing the removal of DIP by phytoplankton uptake through restriction of light penetration, as the SPM possesses a very limited capacity to carry Ex-iP to coastal seas. However, such high concentrations might be a key contributor to the regeneration of remineralization of organic phosphorus in an estuary.

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