• The Korean Journal of Petroleum Geology
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• v.10 no.1_2 s.11
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• pp.10-17
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• 2004

The Doowoo-ri tidal flat in the southwestern Korean coast is a typical open-coast tidal flat which has no barriers in the offshore such as barrier island and sand bars. The difference of induced wave energy with seasons is affected directly on the distribution of surface sediment and the formation of sedimentary structures because the sedimentation by wind wave is relatively much important element in this open-coast tidal flat. This open-coast tidal flat can be classified into tidal beach, intertidal flat and lower mudflat according to the pattern of geomorphology and sediment type. The intertidal flat can be again divided into 3 types: sand flat, mixed flat and mud flat based on the primary sedimentary structure and sand/mud ratio. Doowoori tidal flat shows a seasonal change in the surface sedimentary facies based on sediment composition and primary sedimentary structure. The change is closely related to the direction and magnitude of monsoon wind and also to storm frequency. In winter and spring, when northwesterly wind is most dominant and strong and also storms are common, sand-flat facies is largely distributed on the intertidal flat, whereas mud-flat facies is most dominant during summer when weak southeasterly wind is common. In the fall season, mixed-flat facies is dominant on the flat. The Doowoori intertidal flat is covered by mud sediment which is ca. 20 cm in thickness in summer season. In winter season, surface sediment is changed from mud to sand because the summer mud is mostly eroded by strong wave action. Can-core peels in the intertidal flat show that parallel laminated mud or sand/mud and climbing ripple cross-laminated sandy silt are dominant on the upper intertidal flat $(0-1.3 {\cal}km)$ during summer season. On the other hand, on lower intertidal flat $(1.7-2.3 {\cal}km)$, dominant sedimentary facies is homogeneous mud. In winter, it is changed into parallel laminated and ripple cross-laminated sand facies.

• Journal of the Korean association of regional geographers
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• v.12 no.3
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• pp.339-351
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• 2006

The purpose of this study is to investigate and analyze the relationships between tidal cycles, surface landforms, and sediments of tidal flats and their resident life. The study areas are Uengdo Ri in the Garolim Bay with wide the mud flat, Doou Ri in the Youngwang tidal flat which is developed sand flat and salt field, and Gomso Bay which is developed aquaculture industry. For resident around tidal flats, sea working takes precedence over farming, and main earnings gets from tidal flats. Resident life around the tidal flats is deeply related to tidal cycles, and low water level of spring tide becomes, they are most active and get more earnings than usual day, so it seems to be periodic markets. It is usually developed shellfish aquafarms in the mud flat, the stow net fishery in the sand flat, and salt fields in the mixed flat near the coast. Also a tidal flat has specialization of economic activity, and is divided into salt field and fish-farming in the supratidal zone, shellfish aquafarm in the intertidal zone, and oyster and porphyra culture in the subtidal zone.

• The Korean Journal of Malacology
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• v.12 no.2
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• pp.123-131
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• 1996

진해만 바위해안 조간대에 서식하는 뿔소라과 2종, 대수리(Thais clavigera)와 뿔두드럭고둥(T. luteostoma), 에서 수컷의 성징이 암컷에게서 발현되는 임포섹스 현상을 조사하였다. 임포섹스는 전 조사정점에서 100% 나타나고 있었으므로 본 조사에서 수컷의 성징을 보이지 않은 암컷은 발견할 수 없었다. 임포섹스의 강도를 나타내는 상대 성기 길이 지수(relative penislength index: RPL)는 34.7%에서 81.1%의 범위에 있었다. 특히 마산만 안쪽의 조사정점에서는 암컷의 구성비가 크게 감소하고 어린 개체를 거의 발견할 수 없는 등 개체군이 임포섹스의 영향을 받고 있음을 알 수 있었다. 두 종의 체내에 함유된 트리부틸주석(TBT)과 트리페닐주석(TPT)의 농도를 분석한 결과 각각 0.18-1.45 $\mu\textrm{g}$/g, 0.42-6.30 $\mu\textrm{g}$/g의 범위에 있었으며, 임포섹스의 정도는 트리부틸주석과 트리페닐주석의 체내 농도와 밀접한 관계를 보였다. s 대수리와 뿔두드럭고등의 임포섹스는 우리 나라에서 유기주석 화합물의 오염을 나타내는 좋은 지표로 사용될 수 있으며, TBT의 사용 규제이후 그 효과를 감시하기 위한 용도로도 유용하게 사용될 수 있다.