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- W766766897 abstract "금강하구둑 축조 전 <TEX>${cdot}$</TEX> 후의 조석변화를 알기위하여 금강하구의 조류조화상수 및 비조화상수를 분석하였다. 그 결과, 하구둑 축조 후에 조화상수 및 비조화상수가 증가하였다. 또한 연도별 해도자료를 이용하여 구간별 수심변화를 분석하였다. 그 결과 남 <TEX>${cdot}$</TEX> 북측도류제 사이의 수로에서는 세굴이 발생하였다. 그리고 군산외항에서 하구둑까지의 수로에서는 퇴적이 발생하였다. 조석변화는 건설과 준설, 금강하구둑의 수문닫힘의 영향으로 판단된다 그리고 수심변화는 금강하구둑 건설과 남측도류제, 군장 국가공단 조성사업, 새만금 4호 방조제 건설의 영향에 의하여 야기된 것으로 판단된다. We analyzed the harmonic and non-harmonic constant of Geum River estuary to know tidal change of the before and after construction at Geum River estuary dike. As a result of analysis, the harmonic and non-harmonic constant after estuary dike building increased. Also, depth change analyzed at each section by using each year chart data. As a result, scour was occurred in the channel between south and north side guide bank. And accretion was occurred at channel from Kunsan outer port to estuary dike. Tidal change was judged as the effect of construction and dredge, watergate closing at Geum River estuary dike. And water depth change is a cause by effection of Geum River estuary dike construction and, south-north side guide bank, Kunjang country industrial complex furtherance business, seamangeum 4th sea bankment construction." @default.
- W766766897 created "2016-06-24" @default.
- W766766897 date "2006-02-01" @default.
- W766766897 modified "2023-09-24" @default.
- W766766897 title "A Study on the Topography Change of the Before and After Construction at Geum River Estuary Dike" @default.
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- W766766897 doi "https://doi.org/10.3741/jkwra.2006.39.2.179" @default.
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