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NTIS 바로가기대한토목학회논문집 = Journal of the Korean Society of Civil Engineers, v.34 no.6, 2014년, pp.1779 - 1786
김태준 (연세대학교 대학원 토목환경공학과) , 최병웅 (연세대학교 토목환경공학과) , 최성욱 (연세대학교 공과대학 토목환경공학과)
Artificial Intelligence-based techniques have been applied to problems where mathematical relations can not be presented due to complicatedness of the physical process. A representative example in hydraulics is the local scour around bridge piers. This study presents a GEP model for predicting the l...
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핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
교각주위의 국부세굴은 어떠한 운동인가? | 교각주위에서 유수가 가속되어 교각주위에 세굴공이 형성되어 하상이 변화되고 이는 다시 유수에 영향을 주게 된다. 교각주위의 국부세굴은 하강류와 말발굽 형태의 渦 및 후류를 동반하는 복잡한 난류 운동이다. Fig. | |
국부세굴이란 무엇인가? | 국부세굴이란 수중에 설치된 구조물에 의해 흐름의 원활한 소통을 방해 받아 국부적으로 가속되어 하상이 침식되는 현상이다. 이런 유수의 가속에 의해 교각주위에 세굴공이 형성되며, 이는 흐름에 영향을 미치게 된다. | |
하강류와 말발굽 형태의 渦 및 후류를 동반하는 복잡한 3차원 난류 운동을 보이는 교각주위의 세굴은 어떻게 형성되는가? | 국부세굴이란 수중에 설치된 구조물에 의해 흐름의 원활한 소통을 방해 받아 국부적으로 가속되어 하상이 침식되는 현상이다. 이런 유수의 가속에 의해 교각주위에 세굴공이 형성되며, 이는 흐름에 영향을 미치게 된다. 이런 과정을 통해 발생되는 교각주위의 세굴은 하강류와 말발굽 형태의 渦 및 후류를 동반하는 복잡한 3차원 난류 운동을 보인다. |
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