• NEWSLETTER 전기공업
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• no.99-6 s.223
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• pp.29-33
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• 1999

• NEWSLETTER 전기공업
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• no.99-20 s.237
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• pp.31-36
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• 1999

• NEWSLETTER 전기공업
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• no.97-13 s.182
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• pp.30-35
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• 1997

• 전기산업
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• v.10 no.4
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• pp.105-111
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• 1999

• NEWSLETTER 전기공업
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• no.97-17 s.186
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• pp.30-32
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• 1997

• NEWSLETTER 전기공업
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• no.97-6 s.175
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• pp.41-43
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• 1997

• NEWSLETTER 전기공업
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• no.96-9 s.154
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• pp.40-43
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• 1996

• 방재와보험
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• s.123
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• pp.53-57
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• 2008

• 전기의세계
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• v.28 no.7
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• pp.9-13
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• 1979

이글은 다음과 같이 구성되어 있다. 1. 전선의 제조공정 2. 자동제어의 현황과 전망 3. 계장설비의 현황과 전망 4. 기타

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.6 no.3
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• pp.115-125
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• 2001

To examine the movement of the freshwater discharged artificially into the estuary during ebbing period in the Keum River dike we observed surface salinity variations in three stations along the estuary channel in May 1998 and July 1997 and surface temperature and salinity along the ferry-route between Kunsan and Changhang during eighteen days in July 1999. Based upon the typical features of observed salinity variation, we analyzed the excursion and decay processes of the discharged water. When freshwater is discharged, the low-salinity water forms strong salinity front over the entire estuary width, which basically moves forth and back by tidal modulation along the channel, producing the sudden change of surface salinity with the front passage. Salinity distribution along the channel, which is deduced from time variation of mean salinity over the estuary width, after one tidal period from gate operation suggests that diluted low-salinity water is trapped to the front and surface salinity increases gradually toward the upstream region. This frontal distribution of salinity is interpreted to be produced by the sudden gate operation supplying and stopping of freshwater within about two hours. Daily repeat of freshwater discharge produces separation (double front) or merge between decaying and new-generated fronts depending on dike-gate opening time, and the front decays with salinity increasing if the freshwater supply is stopped more than two days. In addition, the observed fluctuations and deviations in surface salinity variation is explained in terms of the differences of fronts intensity, their transition time and temporal salinity front running along the channel, which can be generated due to artificial gate-operation for the discharging time and water volume in the estuary dike.