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Transport-reaction models for porous media flow




Generally                                                                                                                                              
Transport-reaction in terms of convection-diffusion-reaction type of models appear in many different applications like modeling of water-rock systems, biological systems involving cell-motion phenomena, various aspects of chemical engineering, material science, and even problems within financial engineering. The subtle interplay between motion and change in terms of reactions gives rise to an astounding richness of natural phenomena, and often manifests itself in the emergence of intricate spatial or temporal patterns.
Some nice examples of processes which involve a combination of flow and chemical reactions are illustrated in the figures below from the book "Chemistry in Motion" by Prof B.A. Grzybowski.

http://books.google.co.uk/books?id=tgxV2Vco8xIC&dq=Grzybowski+chemistry+in+motion

These figures show different examples of diffusion-reaction processes for animate as well as inanimate systems and how the combined effect of flow and chemical reactions may give rise to characteristic patterns.



Water-rock chemistry  
                                                                                                                                        
The flow of aqueous reacting solutes through soil or porous rock involves a complex system of geochemical, hydrological, and biochemical processes and is of fundamental importance in many different contexts.


"Chalk weakening effects"                                                                                                             
Compaction of chalk reservoirs is experienced at the Ekofisk field in the North Sea, and is not only a result of an increase in effective stresses linked to pore pressure depletion during oil recovery. There is, however, an additional impact of the seawater injection when water replaces oil in chalks; it causes enhanced compaction of the rock, which further has shown to induce additional seabed subsidence. This phenomenon is often referred to as the water weakening effect on chalks. Examples of issues that we deal with in this context are:


We also seek to use mathematical methods to analyse the models (in addition to numerical calculations) and extract more qualitative insight into the behaviour predicted by the model. In particular, we are interested in issues like


Another issue that naturally comes into play as a part of this activity is to explore different discretization techniques in order to find the most efficient ways to solve the systems of PDEs in question.

An important motivation for the modeling activity is that it can provide visualizations of possible scenarios relevant for the lab experiments that in turn open up for new ideas about design of further experiments.

We are also interested in exploring different coupling mechansims between the stress-strain behavior and the water-rock chemical interaction.































"Optimized water chemistry for enhanced oil recovery"
It has been observed through numerous lab experiments that the oil recovery depends on the brine composition both for chalk and sandstone core plugs.
See the figure above for a visualization of this phenomenon. In view of these experimental observations a main purpose is to deal with the following questions:


The objective of this research activity is to bring forth mathematical models that can allow for systematic and quantitative studies of the relation between brine
composition and produced oil as observed in a lab scale setting. In particular, we suggest models by combining two different modeling components:


In particular, a model has been formulated that takes the form of a system of convection-diffusion-reaction equations that are inherently nonlinear and strongly coupled.
It should also be noted that generally speaking transport-reaction phenomena typically are inherently nonlinear, and the participating chemicals may evolve into final structures
via nontrivial and sometimes counter-intuitive ways. Consequently, much work remains to be done to carefully evaluate different aspects of the proposed models like:


Based on the development of models for lab scale experiments we will in a next phase put together models relevant for reservoir scale considerations by using the lab scale models as building blocks.


The modeling activity is relevant for the study of:
















































Relevant publications:  

[1]  L.Yu, S. Evje, I. Fjelde, H. Kleppe, T. Kaarstad, S.M. Skjaeveland,
Modelling of wettability alteration processes in carbonate oil reservoirs, Networks and Heterogeneous Media Vol 3 (1), 2008.

[2]  L.Yu, S. Evje, I. Fjelde, H. Kleppe, T. Kaarstad, S.M. Skjaeveland,
Spontaneous Imbibition of Seawater into Preferentially Oil-Wet Chalk Cores - Experiments and Simulations, Journal Pet. Sci. Eng., accepted in 2008.

[3]  S. Evje, A. Hiorth, M. Madland, and R. Korsnes,
A mathematical model relevant for weakening of chalk reservoirs due to chemical reactions, Networks and Heterogeneous Media Vol 4 (4), 2009.

[4]  S. Evje, A. Hiorth
A mathematical model for dynamic wettability alteration controlled by water-rock chemistry, Networks and Heterogeneous Media, to appear, 2010.



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A striking feature reflected by the experimental data for spontaneous imbibition found in the literature is that the steady state level of oil recovery, for a  fixed temperature, depends directly on the brine composition. Oil recovery curves for imbibition tests on chalk cores performed at 130 C at various SO4 concentrations in the imbibing fluids. SW represents seawater whereas SW-0S represents seawater without SO4, SW-2S represents seawater with 2 times seawater concentration of SO4, and so on. Figure has been reproduced from the work [Zhang and Austad, Wettability and Oil recovery from Carbonates: Effects of Temperature and Potential Determining Ions, Colloids and Surfaces A: Physicochem. Eng. Aspects 279, 179--187, 2006].

Results produced by the mathematical model suggested in [Evje and Hiorth, "A Mathematical Model for Dynamic Wettability Alteration Controlled by Water-Rock Chemistry", Networks and Heterogeneous Media] showing how oil recovery is sensitive for the brine composition of the imbibing fluid. See the publication for more details. 

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