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A Modeling Study on Hypoxia Formation in the Bottom Water of the Youngsan River Estuary, Korea한국 영산강 하구역 저층 저산소층 형성에 관한 모델링 연구

Other Titles
한국 영산강 하구역 저층 저산소층 형성에 관한 모델링 연구
Authors
조창우송용식김충기김태인한종수우승범
Issue Date
2-1월-2014
Publisher
Coastal Education & Research Foundation
Keywords
Estuary dam; Estuarine circulation; hydrodynamic modeling; hypoxia; water quality
Citation
JOURNAL OF COASTAL RESEARCH, v.0, no.0, pp 000 - 000
Pages
1
Journal Title
JOURNAL OF COASTAL RESEARCH
Volume
0
Number
0
Start Page
000
End Page
000
URI
https://www.kriso.re.kr/sciwatch/handle/2021.sw.kriso/7912
DOI
10.2112/JCOASTRES-D-13-00099.1
ISSN
0749-0208
1551-5036
Abstract
Hypoxia negatively affects marine environment and organisms and is an important indicator of estuarine water quality. We conducted a field survey and a three-dimensional particle transport modeling study to investigate summer hypoxia formation in the bottom water of the Youngsan River estuary (YRE). The field survey showed that dissolved oxygen (DO) decreased upstream and toward the bottom. The lowest DO, at 4.4 mg L1, occurred in the bottom water in front of the estuary dam. We found persistent two-layer estuarine circulation driven by freshwater discharge, which is the main mechanism for delivering offshore water mass upstream. Applying the total oxygen consumption rate (0.50 mg L1 d1) observed in the estuary, the offshore water mass entering the estuary loses as much as 4.4 mg L1 of oxygen during the average travel time (8.8 days) from the mouth of the estuary to the dam. These findings indicate that bottom hypoxia can be formed in front of the estuary dam in summer if offshore water mass with relatively low DO (,8.4 mg L1) enters the estuary. For the sound management of water quality in the YRE, therefore, we recommend improving the quality of the offshore water entering the YRE and also decreasing oxygen demand by reducing nutrient loading from the YRE dam.ion in the bottom water of the Youngsan River estuary (YRE). The field survey showed that dissolved oxygen (DO) decreased upstream and toward the bottom. The lowest DO, at 4.4 mg L1, occurred in the bottom water in front of the estuary dam. We found persistent two-layer estuarine circulation driven by freshwater discharge, which is the main mechanism for delivering offshore water mass upstream. Applying the total oxygen consumption rate (0.50 mg L1 d1) observed in the estuary, the offshore water mass entering the estuary loses as much as 4.4 mg L1 of oxygen during the average travel time (8.8 days) from the mouth of the estuary to the dam. These findings indicate that bottom hypoxia can be formed in front of the estuary dam in summer if offshore water mass with relatively low DO (,8.4 mg L1) enters the estuary. For the sound management of water quality in the YRE, therefore, we recommend improving the quality of the offshore water entering the YRE and also decreasing oxygen demand by reducing nutrient loading from the YRE dam.
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