• Magazine of the Korean Society of Agricultural Engineers
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• v.9 no.2
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• pp.1343-1356
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• 1967

• Magazine of the Korean Society of Agricultural Engineers
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• v.16 no.1
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• pp.3344-3358
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• 1974

• Magazine of the Korean Society of Agricultural Engineers
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• v.15 no.4
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• pp.3215-3225
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• 1973

• KCID journal
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• v.3 no.2
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• pp.114-122
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• 1996

• Magazine of the Korean Society of Agricultural Engineers
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• v.39 no.2
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• pp.19-25
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• 1997

Abstract [] The prediction of changes in the tidal regime due to the sea dike closure in the Saemankum area was performed using the nonlinear finite element model, TIDE. Based upon an overall comparison of calibrated model results with available field data, the TIDE model behaves well and is good representation of the hydrodynamic of the Saemankum tidal project area. It is shown that the TIDE model does an excellent job of computing the changes of tidal characteristics resulting in sea dike closure in an estuary area.

• Proceedings of the Korean Society of Agricultural Engineers Conference
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• 2002.10a
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• pp.81-84
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• 2002

The Sea dike tidal closure works has traditionally ended in the failure. Therefore, the success of the tidal closure in Hwaong in the sea near Inchon where has the greatest tidal gap in our country deserves to consider its meaning. While its process was going on, we had the difficulty like bad weather, unexpected ground settlement, flow velocity beyond the imagine, etc. Moreover, environment group's rush was so fierce that the works could have been delayed. This works showed that not only technical aspects but also social problems(environment group's rush and public discontents) were important factors in accomplishing the works. Finally, all of the difficulties were overcome and the tidal closure works were successful. So, This success is the best example in a kind of the another works in itself.

• Magazine of the Korean Society of Agricultural Engineers
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• v.37 no.E
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• pp.55-62
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• 1995

The topographic influences for the hydraulic characteristics in the estuary were studied by the hydraulic model test. The upstream boundary is set up at the Kumkang estuary dike and the downstream boundary at the Kunsan outer port. The geometrical model scales in horizontal and vertical are 1/300 and 1/100 respectively so that the distorted ratio is 3. If there is no or little river flow through the gate, the highest water levels are varied with $\pm$ 5cm compared with those before the project. If there is a flood flow through the gate, the highest water levels in front of the estuary dike are reduced 5~2Ocm depending on the frequency of flood compared with those before the project. This means that there is no important risk of excessive water level rise after the dredging.

• Journal of Ocean Engineering and Technology
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• v.14 no.3
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• pp.61-65
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• 2000

The estimation of soil stabilization is of great importance concerning the construction of structures on weak soil. A typical model of soil stabilization is considered as replacement, which is based on ground at failure due to direct loading on weak soil. The calculation of the line of predicting settlement was carried out using RPL and DIKE programs. The DIKE program is showing a tendency to excel totally about this embankment of the seadike. Hereafter, This program will be contributed widely to the construction of offshore structures on weak soil.

• KCID journal
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• v.13 no.2
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• pp.254-261
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• 2006

We applied electrical resistivity survey using modified pole-pole array and small-loop electromagnetic survey to delineate the zone of seawater inflow through a tide embankment. The tide embankment is generally affected by tidal variation and has low resistivity characteristic due to the high saturation of seawater. For this reason, the electrical resistivity survey using modified pole-pole array, which is relatively more effective to the conductive media, was carried out to detect the inflow zone of seawater and small-loop electromagnetic survey using multi-frequency with 300 to 20,010 Hz was conducted. As a result of both electrical resistivity survey using modified pole-pole array and small -loop electromagnetic survey, these survey methods are found to be quite effective for investigation of seawater inflow zone in the sea dike.

• Proceedings of the Korea Water Resources Association Conference
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• 2004.05b
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• pp.1413-1417
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• 2004

수제는 하천 흐름을 적극적으로 제어하여 수심을 유지하고, 소류력을 증가시키는 한편 수세를 줄여 토사의 침전을 유포하고자 하는 하천 시설물이다. 수제에 의한 역흐름장(diverse flow fields) 혹은 수제역 (spur-dike zone)의 형성은 다양한 수중생물의 서식환경을 조성하거나 홍수 시 어류의 피난처로 사용될 수 있기 때문에 최근 중시되고 있는 자연형 하천 공법에 수제가 도입되고 있다. 따라서 본 연구에서는 3차원 수치모형을 이용하여 수제주변 흐름을 수치모의 하여 Rajaratnam과 Nwachukwu (1983)의 수리실험 자료 및 Tingsanchali와 Maheswaran (1990)의 2차원 수치모의 결과와 비교하였다. 수치모의 결과 이차흐름과 역방향 흐름이 크게 나타나는 수제 안쪽 및 제방과 가까운 지점에서는 수치모의 자료와 실험자료가 잘 일치하지 않는 결과를 보였으면, 이러한 지점을 제외한 다른 지점에서는 실험자료와 유사한 결과를 나타내고 있음을 확인하였다. 단일 수제에 의한 재순환영역 (recirculation zone)은 수제길이의 약 10배 지점인 것으로 나타났으며, 이는 기존의 연구결과와 유사하였다. 또한 수제 뒤편에 형성되는 와의 중심이 수면에 가까운 지점일수록 뒤로 이동하는 것을 확인하였다. 이는 Tominaga 등 (2001)의 실험결과와 유사한 것으로서 수심에 비례하여 수제 뒷부분에 형성되는 와의 크기가 커지는 것을 파악하였다.