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Numerical Simulation of Pore Fluid Movements in the Upper Rotliegend of the North German Depression

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Computerized Basin Analysis

Part of the book series: Computer Applications in the Earth Sciences ((CAES))

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Abstract

The paper presents a method and some results for the numerical simulation of pore fluid movements, which are connected strongly with migration of hydrocarbons. The mathematical model consists of a two-dimensional initial/boundary value problem with a partial differential equation for the pore pressure in a sedimentary layer. From the given input data (initial condition, hydrodynamic boundary conditions, material parameters) the pore pressure and the Darcy velocity of pore fluids may be computed as functions of space and time. A case study is given from the Upper Rotliegend sediments in a part of the North-German Depression bordered by a system of faults. It is assumed that the overlying Zechstein salt layers hindered the escape of pore fluids, and so an abnormally high pore pressure is produced in the considered sediments. The simulation describes the temporal change of pore pressure and horizontal water flow after some tectonic movements which allowed the fluids to escape along the faults.

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© 1993 Springer Science+Business Media New York

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Springer, J., Schwab, G. (1993). Numerical Simulation of Pore Fluid Movements in the Upper Rotliegend of the North German Depression. In: Harff, J., Merriam, D.F. (eds) Computerized Basin Analysis. Computer Applications in the Earth Sciences. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-2826-5_3

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  • DOI: https://doi.org/10.1007/978-1-4615-2826-5_3

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4613-6222-7

  • Online ISBN: 978-1-4615-2826-5

  • eBook Packages: Springer Book Archive

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