• 해양환경안전학회지
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• 제29권2호
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• pp.98-105
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• 2023

세계 5대 갯벌해역으로 유명한 한국 서해 경기만의 기후변화 영향을 파악하고, 기후변화 영향을 최소화하기 위한 적응방안 연구하였다. 경기만의 기후변화 영향으로 2100년에 수온은 1.2 ℃ 증가하고, 염분이 1.1 PSU 감소하며, 해수면은 35.2 cm 상승하는 것으로 예측되었다. 또한 해수면 상승의 효과로 150.5 km²의 해안지역이 침수될 것으로 예상되었다. 기후변화로 인한 경기만 생태환경 영향을 최소화하기 위한 적응대책으로는 1) 경기만 자체 자연환경의 적응능력 유지를 위한 지원, 2) 생물 서식지 확보를 위한 인간 활동 조정 등 두가지 방안이 제시되었다.

• 자원환경지질
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• 제11권3호
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• pp.109-114
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• 1978

Seismic and side scan sonar traverses in the inner part of Gyeonggi bay was completed during 1976 and 1977 to depict the distribution and thickness of holocene sediments. Special attention was given to the locations of sand and gravel resources. The area of sand sediments is about $50km^2$ mostly distributed in outer part of inner bay. Maximum thickness of sand sediments is 40m with the averge of 10-15m. Tidal current prevailing in the bay seems to be the most important agent modifying the distributions and thickness of sediments in the Gyeonggi bay.

• 환경영향평가
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• 제16권6호
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• pp.421-432
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• 2007

To investigate temporal and spatial variations of hydrodynamics and environmental conditions in Gyeonggi Bay, including Han River estuary, numerical experiments were performed using 3-dimensional fine grid numerical ocean model. The model successfully reproduced the physical phenomena already known in Gyeonggi Bay where tide and fresh water discharge are dominant forcings. The calculated harmonic constants of tide and tidal current agreed well with those of observations at nine tide stations and two tidal current stations. Tidal asymmetries along the Yeomha Waterway, mainly caused by non-linear effect, were well reproduced and agreed well with observations. Time series of salinity at four stations(A, B, C and D) and horizontal distributions of monthly averaged salinity show that Gyodong and Seokmo Waterways play an important role in fresh water discharge into the Gyeonggi Bay rather than Yeomha Waterway.

• Ocean and Polar Research
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• 제29권3호
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• pp.205-216
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• 2007

The purpose of this study was to investigate effects of large scale marine sand mining on the marine ecological community. For the study, four stations along the coast were selected and monitored in 1998 and 2001 at mining areas and non-mining areas about the Gyeonggi Bay. The result revealed that in 1998, 9 species of fishes, 16 species of crustaceans, and 6 species of mollusks were collected where as in 2001, 11 species of fishes, 5 species of crustaceans, and 2 species of mollusks were collected, uncovering the fact that fishes have diversified while crustaceans and mollusks have reduced on a grand scale. Also, there were two key characteristics regarding the changes of biological communities in mining and nonmining areas. The first was the dwindling of crustaceans inhabiting the sand area. This outcome may be accounted for by the facts that physical removal of seabed sediments and re-sediment due to expansion of floating particles cause direct influence on the ocean floor ecosystem and have continuous effect on the communities of crustaceans which feed on them. Secondly, the newly arrived species and their population during spring and summer seasons have increased in the non-mining areas and have decreased in the mining area. It can be concluded that highly nomadic fish species migrate toward areas with less disturbance or destruction of ecosystem from marine sand mining, and consequently, the communities of fishes change in the sea area. Setting aside the characteristics of the investigated sea areas where the arriving conditions of species vary by seasons, the clear differences of population of organisms in those areas are due to environmental alterations owing to the marine sand mining ; if those large-scale marine sand mining activities continue in the Gyeonggi Bay, their effects on biological communities in the areas will only grow.

• 한국주거학회:학술대회논문집
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• 한국주거학회 2008년 추계학술발표대회 논문집
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• pp.375-378
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• 2008

The purpose of this study was analyzing characteristics of $85m^2$-sizes housing units with 3-bay and 4-bay and the residents' satisfaction with them. The subjects for analyzing $85m^2$-sizes housing units with 3-bay and 4-bay in the new town, yongin, in Gyeonggi-do. The study result was show that the residents satisfaction who have experienced the 3-bay housing unit than 4-bay housing unit.

• 한국군사과학기술학회지
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• 제12권1호
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• pp.29-36
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• 2009

Realtime tide and storm-surge computations for the Yellow Sea were conducted using the Parallel Finite Element Model. For these computations a high resolution grid system was constructed with a minimum node interval of loom in Gyeonggi Bay. In the modeling, eight main tidal constituents were analyzed and their results agreed well with the observed data. The realtime tide computation with the eight main tidal constituents and the storm-surge simulation for Typhoon Sarah(1959) were also conducted using parallel computing system of MPI-based LINUX clusters. The result showed a good performance in simulating Typhoon Sarah and reducing the computation time.

• 한국지구과학회지
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• 제33권1호
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• pp.1-10
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• 2012

서해 경기만 조석사주에서 획득한 고해상도 탄성파 탐사자료와 해상시추코어 분석에 의하면 연구지역의 제 4기 후기에 형성된 퇴적층은 총 4개의 퇴적단위(상부층부터 Unit I에서 Unit IV)로 구성된다. 퇴적단위 I은 조간대 및 조수로-충진 퇴적체로서, 홀로세 고해수면 시기동안 퇴적된 것으로 해석된다. 퇴적단위 II는 천해 퇴적상이 나타나는 외해역과 하천과 연계된 하성 퇴적상이 나타나는 조간대에서 조석사주 근접부로 나누어진다. 퇴적단위 III은 조석작용에 의한 조간대 퇴적환경 및 상부의 풍화된 퇴적층으로 각각 구분되며, 퇴적층은 산소동위원소 시기5동안 퇴적된 것으로 판단된다. 퇴적단위 IV는 조석사주 퇴적층의 최하부층으로 중생대 기반암 또는 산소동위원소 시기 5 이전에 퇴적된 층으로 해석된다.

• 환경생물
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• 제20권1호
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• pp.25-34
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• 2002

경기만 염습지의 식물상을 1999년 8월부터 2001년 10월까지 조사하였다. 본 조사는 경기만에 위치한 14개 내륙연안과 도서지역의 38개 지역에서 자연염습지, 사구, 폐염전 및 해안제방을 구분하여 수행되었다. 이 지역에서 조사된 염생식물은 17과 32속 46종이었는데, 이중 자연염습지에만 자라는 식물은 지채 (Triglochin mariti-mum L.), 천일사초 (Carex scabrifolia Steud.), 퉁퉁마디(Salicornia herbacea L.), 방석나물 (Suaeda australis (R. Br.) Moq.), 해홍나물 (S. martima Dum.), 칠면초 (S. japonica Makino), 기수초(S. malacosperma Hara) 등 7종이었으며, 사구에만 자라는 식물은 갯방풍(Glehnia littoralis Fr. Schm.), 갯사상자 (Cnidium japonicum Miq.), 모래지치 (Messerschmidia sibirica L.), 갯씀바귀(Ixeris repens A. Gray), 호모초(Corispermum stauntonii Miq.), 순비기나무 (Vitex rotundifolia L. fil.), 갯쇠보리(Ischaemum anthephoroides Miq.), 통보리사초 (Carex kobomugi Ohwi) 등 8종이었다. 각 조사지 역별 염생식물은 교동도 21종, 석모도 17종, 강화도 남쪽해안과 동검도 28종, 장봉도 16종, 신,시도 16종, 대무의도 23종, 덕적도 23종, 이작도 10종, 영흥도 29종, 소래 25종, 대부도 15종, 쌍송리 6종, 호곡리 16종, 매향리 10종 등으로 조사되었다.

• 환경생물
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• 제32권2호
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• pp.118-128
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• 2014

경기만에서 분리된 Skeletonema marinoi-dohrnii complex의 생장률을 구하기 위하여 영양염이 제한되지 않는 조건 하에서 무균 회분배양으로 넓은 범위의 광조건($5{\sim}500{\mu}mol\;m^{-2}s^{-1}$)과 수온($2{\sim}35^{\circ}C$)에 걸쳐 실험하였다. 실험 결과로부터 온도와 광이 각각 $26.1^{\circ}C$, $197{\mu}mol\;m^{-2}s^{-1}$인 최적조건에서 이 종의 최대 ${\mu}_{max}$는 $2.48d^{-1}$을 보였다. 또한 실제 해역에서 Skeletonema 종들의 온도에 따른 자원경쟁을 고려할 때 $5{\sim}15^{\circ}C$에서 S. marinoi-dohrnii complex의 상대적으로 높은 생장률 ($0.79{\sim}1.61d^{-1}$)은 늦겨울에서 봄철에 대증식을 일으킬 수 있음을 시사한다. 이 결과는 해양생태계 모델의 정확성과 실재성을 개선하는데 기초자료로 활용될 수 있다.

• Ocean and Polar Research
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• 제35권1호
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• pp.51-61
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• 2013

Two surveys were conducted in January 2006 and September 2007 with multibeam echosounder to investigate the dune shape, migration rate, and bedload transport rate using dune-tracking method on an offshore sand ridge at southern Gyeonggi Bay. The migration rates of dunes range from 1.8 $myr^{-1}$) to 56.0 $myr^{-1}$), at the upper northwestern side of sand ridge towards the southwest direction and from the center of the sand ridge towards the northeast direction respectively. Large (i.e. length 10-100 m) dunes show faster migration (0.3-23.4 $myr^{-1}$) ) than very large (i.e. length > 100 m) dunes because larger dunes have required a larger volume of sediments to be displaced. The decreases in dimensions and migration rates of dunes from the center of sand ridge to the lower part of southeastern side on the sand ridge can be ascribed to the decrease of sandy sediments availability, tidal currents with depth, and the coarsening of surface sediments from the crest of the sand ridge to the trough. Bedload transport rates on the basis of migration rates and dune dimensions decrease from 74.5 $m^2yr^{-1}$) at C transect to 35.6 $m^2yr^{-1}$) at R-02 transect.