• Title/Summary/Keyword: Sukmo channel

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Seasonal Variation in Species Composition of the Larval Fish in the Han River Estuary, Korea (한강 하구역 자치어 종조성의 계절 변동)

  • Kim, Ji Hye;Kim, Byung Gi;Han, Kyung Nam
    • Korean Journal of Ichthyology
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    • v.26 no.2
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    • pp.125-132
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    • 2014
  • Seasonal variation and abundance of fish larvae in Han River estuary were determined by analysis of seasonal samples collected from three channels in the Han River estuary from May 2007 to August 2008. During the study, a total of 3,642 fish larvae were collected belonging to 13 taxa. Coilia spp. was the most abundant (48.8%). The highest number of taxa (11 taxa) was collected in the Jangbong channel and abundance was high in the Sukmo channel (2,428 ind./$1,000m^3$). Brackish-water species were prevailed in the Yumhwa channel and the Sukmo channel, while coastal species were abundant in the Jangbong channel. Canonical correspondence analysis revealed that the environmental factors such as water temperature and salinity had a strong relationship with the abundance of major larvae species.

Sedimentology of Inclined Heterolithic Stratification in Sukmo Channel, Kyonggi Bay, Korea - Application to Oil Sand Exploration (경기만 석모수도 수로제방 조간대층에 발달하는 경사이질암상층리의 퇴적학적 연구 - 오일샌드 탐사 적용가능성)

  • Choi, Kyung-Sik;Dalrymple, R.W.;Chun, Seung-Soo;Kim, Sung-Pil;Park, Se-Jin
    • The Korean Journal of Petroleum Geology
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    • v.11 no.1 s.12
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    • pp.18-26
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    • 2005
  • An occurrence of inclined heterolithic stratification (IHS) is described from a tidal point bar in a 40-m-deep distributary of the macrotidai, Han River delta, Korea. The channel bank demonstrates a convex-upward profile with intermittent presence or wave-formed scarps and terraces near the low-water level. The vertical succession of IHS is approximately 25 m thick and dips into the channel with angles reaching up to $14^{\circ}C$. The IHS overlies 15 m of trough cross-bedded sand deposited in the channel bottom. Even though the channel as a whole is ebb dominated, the preserved cross bedding is predominantly flood directed because the mutually evasive nature of the ebb and flood currents causes the point bar surface to be flood dominated. The IHS itself consists of inter-stratified fine sand, sandy silt, and silt with an fining-upward textural trend. Seasonal discharge variations of the Han River are not obvious in the deposits, because tile large size, distal location, and energetic tidal environment of the studied channel reduces the impart of river-stage fluctuations.

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