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High Resolution Simulations of Turbidity Currents and River Outflows

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High Resolution Simulations of Turbidity Currents and River Outflows. Eckart Meiburg UC Santa Barbara. Coastal margin processes. Turbidity current. Underwater sediment flow down the continental slope Can transport many km 3 of sediment Can flow O(1,000)km or more - PowerPoint PPT Presentation
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High Resolution Simulations of Turbidity Currents and River Outflows Eckart Meiburg UC Santa Barbara
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Page 1: High Resolution Simulations of Turbidity Currents  and River Outflows

High Resolution Simulations ofTurbidity Currents and River Outflows

Eckart Meiburg

UC Santa Barbara

Page 2: High Resolution Simulations of Turbidity Currents  and River Outflows

Coastal margin processes

Page 3: High Resolution Simulations of Turbidity Currents  and River Outflows

Turbidity current

Turbidity current.http://www.clas.ufl.edu/

• Underwater sediment flow down the continental slope• Can transport many km3 of sediment• Can flow O(1,000)km or more• Often triggered by storms or earthquakes• Repeated turbidity currents in the same region can lead to the formation of hydrocarbon reservoirs• Properties of turbidite: - particle layer thickness - particle size distribution - pore size distribution

Page 4: High Resolution Simulations of Turbidity Currents  and River Outflows

Results: 3D turbidity current – Temporal evolution

Necker, Härtel, Kleiser and Meiburg (2002a,b)

DNS simulation (Fourier, spectral element, 7x107 grid points)

• turbidity current develops lobe-and-cleft instability of the front

• current is fully turbulent

• erosion, resuspension not accounted for

Page 5: High Resolution Simulations of Turbidity Currents  and River Outflows

Interaction of gravity currents with submarine topography:

Filling of a minibasin (w. M. Nasr, B. Hall)

Page 6: High Resolution Simulations of Turbidity Currents  and River Outflows

Turbidity current/sediment bed interaction (w. M. Nasr)

‘Flow stripping’ in channel turns: lateral overflows

Page 7: High Resolution Simulations of Turbidity Currents  and River Outflows

Long term strategy:

• carry out simulation of polydisperse turbidity current

• obtain spatial grain size distribution of the deposit

• convert grain size distribution into permeability and

porosity distribution

• feed permeability/porosity distribution into reservoir simulator

• carry out simulations of porous media displacement processes

Couple turbidity current solver to reservoir simulator

Page 8: High Resolution Simulations of Turbidity Currents  and River Outflows

Channelization by turbidity currents: A Navier-Stokes based linear instability mechanism (with B. Hall, B. Kneller)

• Hydrodynamic instability?

Field data show regularly spaced channels along the ocean floor

Page 9: High Resolution Simulations of Turbidity Currents  and River Outflows

Sediment wave formation by turbidity currents (w. B. Hall, L. Lesshafft, B. Kneller)

Large scale wave forms at the ocean floor

• sediment waves are prime targets for oil reservoir formation• formed by turbidity currents and bottom flows; mechanism?• traditional assumption: lee waves, but no rigorous stability analysis available

Page 10: High Resolution Simulations of Turbidity Currents  and River Outflows

Sedimentation from river outflows (w. Peter Burns)

• Leaking mode


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