• Title/Summary/Keyword: Ice Scour-Seabed Interaction Models

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A Comparative Study of Ice Scour-Seabed Interaction Models (빙쇄굴-해저지반 상호작용 모델 비교연구)

  • 최경식;이종호
    • Journal of Ocean Engineering and Technology
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    • v.16 no.1
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    • pp.27-35
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    • 2002
  • The interaction of grounded ice ridges with underlying seabed is one of the major considerations in the design of Arctic pipeline system. Previously several ice scour models were developed by researchers to describe the ice scour-seabed interaction mechanism. In view of possible improvements, a comparative study of those ice scour models is performed and their limitation in modeling is discussed. Simple laboratory tests are carried out and then the shape pattern of deposited soil around the ice model is newly defined. Unlike the rectangular idealization of an ice block, in this modified ice scour model, trapezoidal cross sections are assumed to represent the typical shape of an ice ridge based on the field observation data. With the horizontal and vertical motion of ice model, the ice scour depth and soil reacting forces on seabed are calculated with varying the keel angle of an ice ridge.

A Parametric Study on Ice Scouring Mechanism for Determination of Pipeline Burial Depths

  • Park, Kyung-Sik;Lee, Jong-Ho
    • Journal of Ship and Ocean Technology
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    • v.8 no.2
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    • pp.29-40
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    • 2004
  • Interaction of grounded ice ridges with underlying seabed is one of the major considerations in the design of Arctic pipeline system. Previously several ice scour models were developed by researchers to describe the ice scour-seabed interaction mechanism. In this paper, a parametric study on ice scouring mechanism is performed and the limitation of ice scour-seabed interaction models is discussed. Simple laboratory tests are carried out and then the shape pattern of deposited soil around the ice is redefined. New ice scour model assumes trapezoidal cross section based on the field observation data. Ice scour depth and soil resistance forces on seabed are calculated with varying the keel angle of a model ice ridge.