지원사업
학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
커뮤니티
연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
논문 기본 정보
- 자료유형
- 학위논문
- 저자정보
- 지도교수
- 김경섭
- 발행연도
- 2014
- 저작권
- 한경대학교 논문은 저작권에 의해 보호받습니다.
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이 논문의 연구 히스토리 (2)
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The purpose of this study is to simulate the construction of tidal plantation in Asan bay by the validity of the tidal level, tidal current and temperature and quality of water.
In this study, EFDC model was used which is applicable in
various areas such as stream, lake and estuary. To increase the reliability of the analyzed result, the water quality data of 2011 and 2012 were used to revise and verify the data. As a result, the simulated value of flow and water quality expressed similarly.
The parameter values were used for comparative analysis of the before/after tidal plantation to the inland sea and open sea. As a result, before/after open sea showed similar trend as the before construction, and there was no obvious distinction due to seawater encroachment and exchange. In the case of inland sea, there was subtle distinction due to a construction of the tidal barrage. And also due to the difference of the tidal range compared to effluent water of Asan lake and Sap-gyo lake there is large number of seawater movement that the difference is small.
In this study, EFDC model was used which is applicable in
various areas such as stream, lake and estuary. To increase the reliability of the analyzed result, the water quality data of 2011 and 2012 were used to revise and verify the data. As a result, the simulated value of flow and water quality expressed similarly.
The parameter values were used for comparative analysis of the before/after tidal plantation to the inland sea and open sea. As a result, before/after open sea showed similar trend as the before construction, and there was no obvious distinction due to seawater encroachment and exchange. In the case of inland sea, there was subtle distinction due to a construction of the tidal barrage. And also due to the difference of the tidal range compared to effluent water of Asan lake and Sap-gyo lake there is large number of seawater movement that the difference is small.
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