3-7 September 2018
Audimax | Kiel University
Europe/Berlin timezone

Dynamics of ammonium in the Pearl River Estuary under summer hypoxic conditions

Not scheduled
15m
Audimax | Kiel University

Audimax | Kiel University

Christian-Albrechts-Platz 2 | 24118 Kiel | GERMANY
Poster 08 Coastal Systems: From Understanding to Management

Speaker

Ms Jing Liu (State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, China)

Description

We examine ammonium dynamics in the Pearl River Estuary (PRE), a highly eutrophic system where extensive hypoxia is emerging in its lower estuary in the summer time. A total of 312 water samples for ammonium were collected from the PRE in July 2017 when an extensive area in the lower PRE was under hypoxic conditions. Ammonium was measured on board by using the indophenol blue colorimetric method at uM level concentrations or by using a more sensitive fluorescence method with preconcentration was at nM concentration levels. Ammonium concentration ranged from 37 uM in the upper estuary down to 100nM~2 uM in the lower estuary, and to 35 nM~300 nM in the offshore area. Our data showed that ammonium was overall non-conservative during the estuarine mixing showing rapid removal in the upper estuary due probably to nitrification but significant additions in the lower estuary around Shenzhen, Hong Kong and Macau due likely to the sewage discharge. Such ammonium additions were also obvious in the subsurface and bottom waters where we found consistently high concentrations of total suspend matter suggesting that degradation of organic particles is a major source of ammonium therein. We adopted a multiple end-members model to further characterize the ammonium dynamics in different regimes of the lower estuary. Ammonium was slightly removed in the surface layer (0.8±0.3 umol/kg) where nitrate was much more profoundly removed (28±5 umol/kg), indicating that nitrate was the major nitrogen species fueled the phytoplankton bloom. Ammonium was slightly added in the hypoxic bottom water (<0.5 umol/kg) where nitrate was much more significantly regenerated (15±5 umol/kg). This inferred that nitrification contributed to the oxygen consumption in the hypoxic zone. However, the ratio between oxygen consumption vs inorganic nitrogen production amounted to 25±5.1, which was much higher than the Redfield stoichiometry, indicating nitrogen losses relative to the oxygen consumption, the exact reason of which remains however unknown. We contend that ammonia dynamics in the hypoxic zone is much more complex than what was previously thought.

Position PhD Candidate
Affiliation State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, China
Email Address LiuJing@stu.xmu.edu.cn
Are you a SFB 754 / Future Ocean member? No

Primary author

Ms Jing Liu (State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, China)

Co-authors

Ms Khanittha Uthaipan (State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, China) Mr Lifang Wang Prof. Minhan Dai Mr Tao Huang Mr Yangyang Zhao

Presentation Materials

There are no materials yet.