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Contributions from Jaco H. Baas

1993 Ph.D. Utrecht University; 1988 B.Sc. Utrecht University

The research interests of Jaco H. Baas have straddled the boundary between sedimentary geology and  physical geography since graduating from Utrecht University (Netherlands). He had research positions in Kiel (Germany), Rouen (France), Bergen (Norway) and Leeds (England) before moving to Bangor (Wales), where he is now a University Reader in fine particle dynamics. Jaco’s research combines mathematical modelling, laboratory simulations and fieldwork to better understand sedimentary processes in river, shallow-marine and deep-marine environments.  He adopts a comparative approach by studying these processes in modern environments and in the laboratory to better interpret the depositional products of these processes in the geological record. Jaco’s research has been funded by national governments and industry, encompassing different aspects of fine-grained, clay-rich sediment. Clays are ‘sticky’, cohesive, and therefore behave differently in terms of erosion, transport and deposition from sand and gravel-sized particles. Jaco manages the Hydrodynamics Laboratory and the Laser Particle Sizer laboratory in the School of Ocean Sciences, Bangor University. He also runs two B.Sc. degree courses at Bangor: Physical Geography & Oceanography. Jaco has published 75 scientific papers in peer-reviewed journals.

Current research

Jaco’s current research involves collaborations with colleagues in the United Kingdom, Ireland, Germany, Poland, U.S.A. and Brazil. Examples of current research projects are:

  • Silt and very fine sand as main drivers of sediment deposition in submarine fans.  
  • Effect of ‘sticky’ biological polymers on the transport of sand and clay by underwater landslides.
  • Validating a new model for particle suspension using laboratory flume experiments.
  • An integrated process-based model of flutes and tool marks in deep-water environments.
  • Dynamics of reef-derived sediment gravity flows.
  • Experimental fluid dynamics of transient turbulent clay flows.

Email: j.baas@bangor.ac.uk

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dip and strike compass
Measuring dip and strike
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Classification of sandstones
Calcite cemented subarkose, Proterozoic Altyn Fm. southern Alberta
Sandstones in thin section
poles to bedding great circles
Stereographic projection – poles to planes
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Fluid flow: Froude and Reynolds numbers
Stokes Law for particle settling in a schematic context of other fluid flow functions
Fluid flow: Stokes Law and particle settling
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Classification of sedimentary basins
Model are representational descriptions are written in different languages - diagrammatic, descriptive, mathematical, and conceptual. They commonly contain variables and dimensionless quantities that permit quantitative analysis of the physical systems the models represent.
Geological models
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