PUKYONG

냉배수 유입에 따른 진해만의 수질 변동 예측

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Alternative Title
Prediction of Water Quality Change in Jinhae Bay due to Cold Water Discharge
Abstract
In order to evaluate the effect of cold water discharge from Tongyeong LNG station on changes of water quality and primary production of Jingae Bay, tidal current model(Princeton Ocean Model) considering the cold water discharge was simulated during a year(2018.01.01. ∼ 2019.01.01.). Base on the model results, PEA(stratification strength parameter), space-specific growth rates of phytoplankton and macroalgae(Saccharina japonica) in Jinhae Bay were estimated. And DO concentration in Jinhae Bay with various volume of cold discharge was predicted using Gaussian Process Regression method.
In case of discharge volume of 10 m3 sec-1, the changes in environment of the Jinhae Bay due to cold discharge were very insignificant. The effects of cold discharge were most pronounced in May(except stratification strength(Aug) and primary production(Nov)), the results of discharge volume of 1000 m3 sec-1 in May are as follows: Water temperature in near-by discharge outlet was decreased up to ca. –5.35℃ and -4.05℃ respectively in the surface and bottom layers. The PEA in near-by Geoje-Gaduk open boundary increased up to ca. 23 J m-3, it has increased by more than 5 J m-3 in area of ca. 104 km2 of Jinhae Bay in Aug. While the water temperature decrease by cold discharge reduced primary production(PP) of phytoplankton in the center of bay to ca. 15% in Nov, it promoted net growth rate of macroalgae in Haengam Bay up to ca. 7% in May. The DO concentration in the center of bay was predicted to increase ca. 1.01 mg L-1 due to water temperature decrease.
From the above results, we confirmed that the environmental changes in Jinhae Bay by cold discharge from Tongyeong LNG production base are very insignificant. As a results of discharge volume of 1000 m3 sec-1, it is expected that special purposes utilize of cold discharge (water temperature reduction, red tide prevention, macroalgae growth, and DO increase) will be possible in small-areas considering actual discharge volume.
Author(s)
박성식
Issued Date
2021
Awarded Date
2021. 2
Type
Dissertation
Keyword
냉배수 진해만 Potential Energy Anomaly 조류 성장 속도
Publisher
부경대학교
URI
https://repository.pknu.ac.kr:8443/handle/2021.oak/2261
http://pknu.dcollection.net/common/orgView/200000374445
Alternative Author(s)
Seongsik Park
Affiliation
부경대학교 대학원
Department
대학원 해양공학과
Advisor
김경회
Table Of Contents
1. 서론 1
1.1. 연구 배경 1
1.2. 연구 목적 및 내용 3
2. 재료 및 방법 5
2.1. 기초/검증자료 수집 5
2.2. 3차원 유동 모델 8
2.2.1. Princeton Ocean Model 개요 8
2.2.1.1. 지배방정식 8
2.2.1.2. 연직경계조건 13
2.2.1.3. 연직적분방정식 15
2.2.2. 계산 조건 17
2.2.2.1. 격자 구성 17
2.2.2.2. 유동 모델 조건 18
2.2.2.3. 냉배수 조건 27
2.3. 성층강도 27
2.4. 식물플랑크톤 및 해조류 성장 속도 28
2.5. Gaussian Process Regression 31
3. 결과 및 고찰 35
3.1. 유동 모델 검증 35
3.1.1. 조석 및 조류 검증 35
3.1.2. 수온 및 염분 검증 43
3.2. 유동 모델 결과 50
3.2.1. 수온 50
3.2.2. 염분 72
3.2.3. 유동 94
3.3. 성층강도 100
3.4. 식물플랑크톤 및 해조류 성장 속도 109
3.5. 용존산소농도 118
4. 요약 및 결론 126
5. 참고문헌 130
Degree
Master
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대학원 > 해양공학과
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