A clearer picture of how rivers and deltas develop

20 January 2011 by M&C

By adding information about the subsurface to an existing sedimentation and erosion model, researchers at TU Delft have obtained a clearer picture of how rivers and deltas develop over time. A better understanding of the interaction between the subsurface and flow processes in a river-delta system can play a key role in civil engineering (delta management), but also in geology (especially in the work of reservoir geologists). Nathanaël Geleynse et al. recently published on their work in this area in the journal Geophysical Research Letters. A related article has appeared in Earth and Planetary Science Letters.

Model

Many factors are involved in how a river behaves and the creation of a river delta. Firstly, of course, there is the river itself. What kind of material does it transport to the delta? Does this material consist of small particles (clay) or larger particles (sand)? But other important factors include the extent of the tidal differences at the coast and the height of the waves whipped up by the wind. In this study, researchers at TU Delft are working together with Deltares and making use of the institute''s computer models (Delft3D software). These models already take a large number of variables into account. Geleynse et al. have now supplemented them with information on the subsurface. It transpires that this variable also exerts a significant influence on how the river behaves and the closely related process of delta formation. 

Figure 1. Schematic model of a river-coast system (click onn picture for hires)

Room for the River

The extra dimension that Geleynse et al. have added to the model is important to delta management, among other things. If – as the Delta Commission recommends – we should be creating ''Room for the River'', it is important to know what a river will do with that space. Nathanaël Geleynse explains: ''Existing data do not enable us to give ready-made answers to specific management questions - nature is not so easily tamed - but they do offer plausible explanations for the patterns and shapes we see on the surface. The flow system carries the signature of the subsurface, something we were relatively unaware of until now. Our model provides ample scope for further development and for studying various scenarios in the current structure.''


Figure 2. Mapped results from the model for various types of sediment in the subsoil and for various types of water movement, for a given point in time. In all cases the initial situation (elevation) is as presented in Figure 1. The sedimentary composition of the subsurface along the horizontal white lines in the bottom three figures is shown in Figure 3 (click on picture for hires).

Geological information

River management is all about short-term and possible future scenarios. But the model developed by Geleynse et al. also offers greater insight into how a river/delta has developed over thousands of years. What might the subsurface have looked like and - a key factor for the oil industry - where might you expect to find oil reserves and what might their geometrical characteristics be? In combination with data from a limited number of core samples and other local measurements, the model can give a more detailed picture of the area in question than was possible until now.

The link between the creation of the delta and the structure of the delta subsurface is also of interest to engineers who wish to build there. Hundreds of millions of people across the globe live in deltas and these urban deltas are only expected to grow in the decades to come.


Figure 3. Results of the model for the sedimentary composition of the subsurface at the horizontal white lines in Figure 2. The initial situation (soil elevation) is indicated by the dotted black lines. The figure on the left represents a situation in which only sand is present in the subsoil at the beginning of the model simulation. The clay visible in this delta was therefore carried along by the upper-current river. The figure on the right shows a situation in which a great deal of clay is present in the initial subsoil, in addition to sand. The figure in the middle shows a situation in which there is more of a volumetric balance between sand and clay in the initial subsoil. The blue line indicates the calculated water surface. The figure presents the information as if the viewer is looking downstream.

Further details

''Controls on river delta formation; insights from numerical modelling'', Nathanaël Geleynse, Joep Storms, Dirk-Jan Walstra, Albert Jagers, Zheng Wang and Marcel Stive. Earth Planet. Sci. Lett., in press, http://dx.doi.org/10.1016/j.epsl.2010.12.013
 
''Modeling of a mixed-load fluvio-deltaic system'', N. Geleynse, J.E.A. Storms, M.J.F. Stive, H.R.A. Jagers, and D.J.R. Walstra, Geophys. Res. Lett., 37, L05402, http://dx.doi.org/10.1029/2009GL042000

Contact: Nathanaël Geleynse, Faculty of Civil Engineering and Geosciences, N.Geleynse@remove-this.tudelft.nl, +31 (0)15 2784419
TU Delft Science Information Officer Roy Meijer, r.e.t.meijer@remove-this.tudelft.nl, +31 (0)15 2781751

© 2014 TU Delft

Metamenu