변산.고사포 해수욕장 하부 조간대의 지형변동연구

권효근,최강원,장정렬,정지연,Kwon, Hyo-Keun,Choi, Kang-Won,Jang, Jeong-Ryeol,Jung, Ji-Yeon 한국관개배수위원회 2010 한국관개배수논문집 Vol.17 No.2

This study was carried out to survey for morphological change of lower tidal flat near Byunsan-Gosapo beach using single-beam echosounder and sound velocity profiler. Since October 2009 in the center of the region, the erosion occurred about 10~50cm, while either side of the study area is little change. Erosion occurred at the beach, each beach area in the southwest area rather than further accumulation occurred sandbank formed. Observed in the study area near the center of the erosion is the result of ongoing changes that were temporarily due to seasonal changes is not clear. However, the northwestward waves were expected to be a major source of erosion. Because of this, continue to observe the terrain and the local ocean circulation studies will be required.

하구언 수문작동으로 인한 금강 하구역의 물리적 환경변화: I. 평균해수면과 조석

권효근,이상호,Kwon, Hyo-Keun,Lee, Sang-Ho 한국해양학회 1999 바다 Vol.4 No.2

Analyzing the tide data taken at Kunsan inner and Outer ports, non-tidal and mean sea level and harmonic constants of major constituents are investigated to examine the effects of the dyke gate operation on the sea level change in Keum River estuary. Non-tidal and annual mean sea levels decrease at Kunsan Inner and Outer ports after the dyke gate operation, especially showing an abrupt drop of non-tidal sea level at Kunsan Inner port. This non-tidal sea level drop results in the mean sea level gradient change between the inner and outer port, which can be mainly explained in terms of the decrease of river discharge from the dyke. Amplitudes of the $M_2$ and $S_2$ tides at the Inner port increase after the dyke gate operation, showing an abrupt jump, and phases of both tides slightly decrease. Amplitude and phase of the $K_1$ and $O_1$ tides show slight changes after the dyke gate operation. This significant change of semi diurnal tide amplitude is believed as a result of superposition of incident tidal wave and reflected tidal wave from the dyke.

새만금 방조제 외해역의 저서생물 군집 변화

정지연,권효근,장정렬,최강원,Jung, Ji-Yeon,Kwon, Hyo-Keun,Jang, Jeong-Ryeol,Choi, Kang-Won 한국관개배수위원회 2010 한국관개배수논문집 Vol.17 No.2

This study was carried out to investigate the changing of benthic macrobenthos community in Saemangeum subtidal area. The distribution of macrobenthic community is important to assume the benthic environment in study area. Macrobenthic community was investigated three times in 2007 (March, June and September) in the Saemangeum subtidal area. The mean density of macrobenthos was $345{\sim}838ind./m^2$ and the most dominant taxa was benthic polychaete. Opportunistic species such as E.cordatum, T.fragilis, H.filiformis, and Tharyx sp. were shown high appearance rate in study area. The dominance of these opportunistic species suggest that the benthic environment of study area was unstable due to environmental disturbance. But, there are only few point that these species were recorded high densities, and also equilibrium species was dominant, too. It means disturbance and un stability of benthic environment in Seamangeum was not serious yet. so the dynamics and trends of these opportunistic species should be concerned.

하구언 수문 작동으로 인한 금강 하구역의 물리적 환경변화: III. 저염수의 조석동조

최현용,권효근,이상호,Choi, Hyun-Yong,Kwon, Hyo-Keun,Lee, Sang-Ho 한국해양학회 2001 바다 Vol.6 No.3

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.

하구언 수문작동으로 인한 금강 하구역의 물리적 환경변화: II. 염분구조와 하구유형

이상호,권효근,최현용,양재삼,최진용,Lee, Sang-Ho,Kwon, Hyo-Keun,Choi, Hyun-Yong,Yang, Jae-Sam,Choi, Jin-Yong 한국해양학회 1999 바다 Vol.4 No.4

CTD castings and current observations are taken in June, July and October, 1997 and May and July, 1998 to investigate the effect of the Keum River dyke on the structure of physical properties and the type of the Keum River estuary. Tide and tidal current relation shows that the ebbing is longer than the flooding by 1.5 hours with the early current reversing before high tide. In the rainy season (May to July), frequent large fresh water discharge during the ebbing from the dyke changes vertical salinity difference and time variation of salinity greatly near the head of the estuary, where salinity becomes lower than 2‰ in summer fresh water flooding. Halocline developed by the fresh water discharge makes two-layer structure, of which strength and depth increase in the low tide. The relationship between tide phase and surface salinity variation shows the phase lag of 2.5 hours near the head of the estuary but the standing wave relation down the estuary. This phase lag implies that a low salinity water diluted by the fresh water discharge for 2-3 hours in the ebb period moves with tidal excursion. In the dry season, vertical salinity difference reduces significantly. We calculate stratification and circulation parameters using the observed salinity structure, surface current and fresh water discharge. The Keum River estuary shows a partially mixed type, changing the stratification parameter from the rainy to the dry season. Mean flows of observed tidal current at lower and upper layer are landward and seaward, which are consistent with the circulation of a partially mixed estuary. Based upon the estuary type and circulation we suggest that the suspended materials will move toward the upstream due to low-layer mean flow and then the Keum River estuary will be a deposit environment.

해사채취에 따른 지형 및 생태복원의 추이분석

김재옥 ( Jae Ok Kim ),권효근 ( Hyo Keun Kwon ),홍대벽 ( Dae Byuk Hong ),최진용 ( Jin Yong Choi ) 한국물환경학회 ( 구 한국수질보전학회 ) 2008 공동 추계학술발표회 Vol.2008 No.-

새만금 4호 방조제 완성 전.후 HF 레이다로 관측된 표층 $M_2$ 조류의 변화

김창수,이상호,손영태,권효근,이광희,김영배,정우진,Kim Chang-Soo,Lee Sang-Ho,Son Young-Tae,Kwon Hyo-Keun,Lee Kwang-Hee,Kim Young-Bae,Jeong Ou-Jin 한국해양학회 2006 바다 Vol.11 No.2

2003년 6월에 고군산군도와 비응도를 완전히 연결한 새만금 4호 방조제의 완공이 연안역 표층 $M_2$조류분포에 미치는 영향을 알아보기 위하여 2002년과 2004년에 HF radar로 관측된 유동자료를 분석하였다. 분석에 사용된 자료와 유속계 계류에 의해 관측된 자료는 좋은 일치를 보였다. $M_2$조류는 관측구역 내에서 반시계방향의 회전성을 보였으며 방조제 완전 체절로 인하여 회전방향이 변경되지는 알았다. 2002년에는 방조제의 미체절 구간을 통해 서쪽으로 향하던 ebb jet가 관측되었지만, 2004년에는 이 흐름이 나타나지 않았다. 방조제 완전체절로 인하여 금강하구 입구부근에서 유속이 증가하였고, 고군산군도 및 방조제 부근에는 유속이 감소하였으며 최강 창조류의 방향이 동서방향에서 남북방향으로 변화되었고 최강 창조류 발생시각이 늦어졌다. 연도 주변해역에서도 최강 창조류 방향이 시계방향으로 변경되었으나 최강 창조류 발생시각은 오히려 빨라졌다. 이러한 $M_2$ 조류타원 특성의 변화는 방조제 체절의 영향이 연도와 말도를 잇는 지역까지 미치고 있음을 의미한다. HF radar-derived current data obtained in 2002 and 2004 are analyzed to examine the effects of the completion of the Saemangeum 4th tidal dyke in June 2003, connecting Gogunsan-Gundo and Bieung-Do, on the coastal surface $M_2$ current pattern. Comparison between the currents by HF radar and current meter mooring showed good agreements. Counterclockwise rotation of the $M_2$ current in the observed area did not change with the dyke construction. Strong westward ebb jet from the gap of the dyke was observed in 2002 but disappeared in 2004. The complete closing of the dyke gap caused the current speed increase around the mouth of the Kem River estuary, decrease around Gogunsan-Gundo and the dyke, the changes in the direction of maximum current to north-ward from eastward and the delay of the maximum flood current occurrence around Gogunsan-Gundo and the dyke. Around Yeon-Do, the maximum flood current directed more clockwise and occurred rather earlier. These changes of the $M_2$ current ellipse characteristics imply that the effects of the dyke construction reached the area connecting Mal-Do and Yeun-Do.

새만금 연안역에서 HF radar에 의해 관측된 조하주기 표층해류의 변화

김창수,이상호,손영태,권효근,이광희,최병주,Kim, Chang-Soo,Lee, Sang-Ho,Son, Young-Tae,Kwon, Hyo-Keun,Lee, Kwang-Hee,Choi, Byoung-Hy 한국해양학회 2008 바다 Vol.13 No.1

서해 중부에 위치한 새만금 연안역에서 HF radar를 이용하여 2002년 7월과 2004년 9월부터 11월 초까지 표층해류를 관측하였다. 관측 자료로부터 조하주기대(subtidal) 표층해류가 해안선 변화, 바람과 담수 방류량의 변화에 대하여 시 공간적으로 어떻게 변동하는지 조사하였다. 2002년 7월 관측 기간 동안 바람이 약 0.5 m/s로 불었으며, 일 평균 금강 담수 방류량이 $0.88{\times}10^7$ 톤이었다. 시간평균된 표층해류($\overline{U}$)는 금강하구입구에서 $7{\sim}10\;cm/s$의 크기로 북서쪽으로, 방조제 개방구간에서 13 cm/s 이상의 크기를 갖고 서쪽으로, 고군산군도 북측에서는 북서방향의 분포를 보였다. 이는 금강 담수와 새만금 방조제 개방구간에서 유출된 조석 잔차류에 의해 형성된 흐름이다. 또한 를 제거한 표층해류의 공간평균치(<$U-\overline{U}$>)의 방향변화가 바람방향변화와 상대적으로 높은 상관관계(r=0.98)를 보였다. 2004년 9월부터 11월에는 북북서풍이 2.5 m/s로 불었으며, 일평균 담수 방류량이 $11.9{\times}10^7$ 톤이었다. 표층해류($\overline{U}$)는 대부분의 연안에서 크기가 작았고, 새만금 방조제와 고군산군도가 이루는 해안선을 따라서 약 10 cm/s의 상대적으로 빠른 해류가 남서방향으로 흘렀다. 이는 강한 북서풍이 금강 담수를 새만금 방조제 쪽으로 이동시켜 형성된 흐름이다. 2004년도에는 방조제 개방구간에서 유출되는 조석 잔차류가 없어졌으며, 공간평균(<U>)된 표층해류의 방향변화가 바람방향변화와 0.69의 상관관계를 보였다. Subtidal surface currents are derived from HF radar measurements in the Saemangeum coastal ocean of the Yellow sea in July 2002 and from September to November 2004. The surface current field is analyzed to examine the effect of wind, river plume and coastline change on the spatial distribution and temporal variation of the surface currents. In July 2002, average wind speed was 0.5 m/s and freshwater discharge from the Keum River was $0.88{\times}10^7\;ton/day$. Temporal mean currents ($\overline{U}$) flow to the northwest with speed of $7{\sim}10\;cm/s$ near the Keum River estuary, to the west as fast as 13 cm/s near the opening gap of the Saemangeum $4^{th}$ dyke, and to the northwest off the Gogunsan-archipelago. This flow pattern is a result of the Keum River plume dispersal and tide-residual currents from the opening gap of the Saemangeum $4^{th}$ dyke. Time series of spatially-averaged current (<$U-\overline{U}$>) direction is highly (r=0.98) correlated with wind direction. From September to November 2004, the opening gap of the Saemangeum $4^{th}$ dyke was closed, northwesterly wind blew with speed of 2.5 m/s on average and the Keum River discharge was $1.19{\times}10^7\;ton/day$. Temporal mean current field ($\overline{U}$) has weak surface flow in most of the coastal ocean and relatively strong currents flow to the southwest with speed of 10 cm/s along the shape coastline of the Gogunsan-archipelago and the Saemangeum $4^{th}$ dyke. The strong flow is generated by the prevailing northwesterly wind which pushes the Keum River plume toward the Saemangeum $4^{th}$ dyke. The residual currents from the opening gap of the Saemangeum $4^{th}$ dyke disappeared and correlation coefficient between time series of spatially-averaged current (<U>) direction and the wind direction is 0.69.

빗물관리 ; 새만금 축산단지의 빗물 이용량 및 저장용량 추정

김남기 ( Nam Ki Kim ),정재운 ( Jae Woon Jung ),권효근 ( Hyo Keun Kwon ) 한국물환경학회 2010 한국물환경학회·대한상하수도학회 공동 춘계학술발표회 Vol.2010 No.-

빗물관리 ; 새만금 축산단지의 빗물 이용량 및 저장용량 추정

김남기 ( Nam Ki Kim ),정재운 ( Jae Woon Jung ),권효근 ( Hyo Keun Kwon ) 한국물환경학회 2010 공동 춘계학술발표회 Vol.2010 No.0