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Abstract
Application
of Compositional Basin Modeling to GOR and API Prediction in the
North Sea
10.
Application
of Compositional Basin Modeling to GOR and API Prediction in the North Sea
J. Wendebourg,1 S.J. Dppenbecker2
1Institut Franais du P
trole, Rueil-Malmaison, France
2BP, Houston TX, U.S.A.
ACKNOWLEDGMENTS
We thank our colleagues M. Vandenbroucke and J.-L. Rudkiewicz of IFP and A. Pepper T. Dodd and J. Bunney of BP for their valuable discussions. We also thank S. Wolf of IFP and W. Choueiri of Beicip for implementation of the first versions of compositional Temispack. We thank B. Horsfield and P. Kaufman for their constructive reviews and BP for permission to publish the data.
ABSTRACT
The
application
of basin modeling is commonly aimed at constraining prospect risk of source rock effectiveness and charge presence. The simulation of compositional
petroleum
generation and multiphase fluid migration of miscible and compressible fluids adds the ability to predict
petroleum
value, i.e., fluid phase and properties, in undrilled traps. This functionality was implemented in Institut Franais du P
trole's (IFP) 2-D Temispack program and applied successfully in a case study that was aimed at reconstructing gas-oil ratio (GOR) and liquid
petroleum
density at surface conditions (API) for two North Sea fields, the low-GOR Ninian oil field and the high-GOR Huldra condensate field.
In both fields, the Upper Jurassic Kimmeridge and Heather Formations do overlay the middle Jurassic Brent reservoir/carrier beds and contain source rock intervals with kerogen of Type II (IFP classification) or of class B (BP classification). The modeling study links the low-GOR Ninian oil to the
petroleum
composition migrating from the half graben west of the field where secondary cracking is not significant. The
petroleum
fluid at Huldra, a condensate, is derived from a local deep kitchen to the east where all source rocks are mature and secondary cracking is providing the high gas fraction of the trapped
petroleum
. In both fields, the GOR is closely linked to the cracking reactions of heavy components (nitrogen, sulfur, oxygen organic compounds [NSO], C14+ aromatics) and late gas generation from kerogen cracking. The molecular weight of the C14+ components determines the API. Most importantly, the pressure-volume-temperature (PVT) behavior of the fluids during migration indicates that a single-phase
petroleum
flow is by far the dominating process. A significant three-phase migration may occur only at depths less than about 3 km.
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