• 제목/요약/키워드: slackwater deposits

검색결과 2건 처리시간 0.019초

Slackwater 퇴적물을 이용한 고범람 연구 (Palaeoflood Study by using the Slackwater Deposits)

  • 김송현;다나카 유키야
    • 한국지형학회지
    • /
    • 제18권4호
    • /
    • pp.163-175
    • /
    • 2011
  • Slackwater 퇴적물은 범람이 발생되는 동안 유속이 감소되는 지역에 축적되는 미립의 범람 퇴적물이다. 이는 고범람 수문학에서 가장 흔하게 사용되는 고단계(palaeostage) 지시자로서, 과거 범람의 크기와 빈도를 추정하기 위해 국제적으로 수많은 연구에서 이용되었다. 또한 slackwater 퇴적물을 통한 고범람 기록은 범람-가능성 추정치를 개선시키고, 과거 환경 및 수문을 복원하는데 기여하였다. 그러나 이러한 범람 퇴적물을 이용한 국내 연구는 거의 찾아볼 수 없다. 따라서 본 연구는 slackwater 퇴적물을 이용한 고범람 연구에 대한 선행 연구 결과를 정리하고, slackwater 퇴적물의 특성 및 연구 방법론과 국내에서의 연구 가능성에 대해 알아보고자 한다.

Architectural Elements of the Fluvial Deposits of Meander Bends in Midstream of the Yeongsan River, Korea

  • Chung, Gong-Soo;Lee, Jin-Young;Yang, Dong-Yoon;Kim, Ju-Yong
    • 한국지구과학회지
    • /
    • 제26권8호
    • /
    • pp.809-820
    • /
    • 2005
  • The fluvial sequence developed along the channel margin of meander bends in the midstream of the Yeongsan River consists of channel deposits at the bottom and overbank deposits at the top, and shows a fining-upward trend. The fluvial deposits consist of 7 sedimentary facies, and facies association forms 7 architectural elements. The channel deposits formed as channel bar or point bar. The channel bar deposits consisted of architectural element of gravel bedform were formed by channel lag deposits within the channel; whereas, the channel bar deposits consisted of architectural elements of downcurrent-dipping inclined strata sets, cross-stratified and horizontally stratified sets, and horizontally stratified sets were formed by downstream migration of sand wave or downstream transport of sand by traction current in the upper flow regime conditions within the channel. The point bar deposits consist of architectural elements of down current-dipping inclined strata sets, horizontally stratified sets, cross-stratified and horizontally stratified sets, and laterally inclined and horizontally stratified sets. These architectural elements are thought to have been formed by the combined effects of the migration of sand dunes and the formation of horizontal lamination in the upper flow regime plane bed conditions. The overbank deposits consist of the architectural elements of overbank fine and sand sheet and lens. The overbank fines were formed by settling of mud from slackwater during flooding over floodplain whereas the sand sheet and lens were formed by traction of sands introduced episodically fiom channel to the overbank during flooding.