4.2 Article

A simplified approach to address turbulence modulation in turbidity currents as a response to slope breaks and loss of lateral confinement

Journal

ENVIRONMENTAL FLUID MECHANICS
Volume 14, Issue 2, Pages 371-385

Publisher

SPRINGER
DOI: 10.1007/s10652-013-9302-7

Keywords

Turbidity currents; Turbulence modulation; Sediment transport; Direct numerical simulation

Funding

  1. CONICET
  2. CNEA
  3. ANPCyT [PICT-2010-2459]
  4. Shell International Exploration and Production
  5. National Center for Supercomputing Applications (NCSA) at the University of Illinois at Urbana-Champaign (UIUC)
  6. U.S. National Science Foundation
  7. National Science Foundation [OCE-1131016, OISE-0968313]
  8. Division Of Ocean Sciences
  9. Directorate For Geosciences [1131016, 1130217] Funding Source: National Science Foundation
  10. Office Of Internatl Science &Engineering
  11. Office Of The Director [968313] Funding Source: National Science Foundation

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Turbidity currents traversing canyon-fan systems flow over bed slopes that decrease in the downstream direction. This slope decrease eventually causes turbidity currents to decelerate and enter a net-depositional mode. When the slope decrease is relatively rapid in the downstream direction, the turbidity current undergoes a concomitantly rapid and substantial transition. Similar conditions are found when turbidity currents debouch to fan systems with loss of lateral confinement. In this work a simplified approach to perform direct numerical simulation of continuous turbidity currents undergoing slope breaks and loss of lateral confinement is presented and applied to study turbulence modulation in the flow. The presence of settling sediment particles breaks the top-bottom symmetry of the flow, with a tendency to self-stratify. This self-stratification damps turbulence, particularly near the bottom wall, affecting substantially the flow's ability to transport sediment in suspension. This work reports results on two different situations: turbidity currents driven by fine and coarser sediment flowing through a decreasing slope. In the case of fine sediment, after the reduction in the slope of the channel, the flow remains turbulent with only a modest influence on turbulence statistics. In the case of coarse sediments, after the change in slope, turbulence is totally suppressed.

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