The distinguishing feature of streamline simulation is that fluids are transported over a time step (t to t+Δt) along streamlines rather than from cell-to-cell as in conventional Eulerian grid methods. Components are assumed to move with the total velocity field (streamlines) until the velocity field is updated to account for its dynamic behavior in time. The geometry of the streamlines and the velocity of phases and components traveling along streamlines are calculated from the spatial distribution of the static petrophysical properties (permeability, porosity, relative permeability regions, etc.) and the volumes produced/injected at the wells. The ability of streamlines to visualize flow is powerful, even to the untrained eye. The most striking advantage of SL simulation compared to other approaches is the information provided by the streamlines themselves. There are two particularly useful sources of data:
To find out more please see When And Why To Use Streamlines. Streamlines have been in the literature for a long time. For one of the earliest papers on the subject see Morris Muskat's and Ralph Wyckoff's 1933 paper: A Theoretical Analysis of Water-flooding Networks, which is freely downloadable from the SPE website. |
What makes streamlines so attractive? Streamlines are an attractive alternative to more traditional simulation approaches under the right set of assumptions. Here a set of publications giving an overview of the methodology.
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