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Forward prediction of aeolian systems using fuzzy logic, constrained by data from recent and ancient analogues

Published online by Cambridge University Press:  01 April 2016

Caroline Hern*
Affiliation:
Department of Petroleum Engineering, Heriot-Watt University, Edinburgh, UK
Ulf Nordlund
Affiliation:
Dept. Earth Sci., Historical Geology & Palaeontology, Uppsala University, Sweden
Kees van der Zwan
Affiliation:
SIEP-RTS, EPT-HM, Volmerlaan 8, Rijswijk, the Netherlands
Kenny Ladipo
Affiliation:
NAM, Assen, the Netherlands.
*
1Corresponding author; e-mail: [email protected]
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Abstract

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Aeolian sands are the main reservoir rock in some of the largest gas fields, such as the Shell-Exxon Groningen Field, operated by NAM. Although aeolian reservoirs have been studied for many years, there is still room for improvement in the predictive modeling of such reservoirs. A pilot project with this objective was initiated by SIEP B.V. in 1997, together with Heriot-Watt University in Edinburgh, UK and with Uppsala University, Sweden, to evaluate the factors influencing aeolian systems, and to formulate a forward model using ‘fuzzy logic’.

The project was initiated to develop a fuzzy system for generic modeling of aeolian architectures. The key aims were to be able to predict the type, amount and distribution of major facies in generic aeolian systems and specifically to model regional-scale architecture in the sub-surface. Fuzzy rules and sets, which defined the behaviour of aeolian systems, were constructed and used to modify the pre-existing fuzzy modeling software which had been designed for shallow and deep marine systems. The modeling procedure used input data appropriate to the Rotliegend climate, and was validated by comparing the resulting models, in terms of thickness and spatial distribution of facies types, to well data from the Upper Rotliegend interval of the Lauwerszee Trough area, NE Netherlands (Figures 1 & 2).

Type
Conference papers
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2001

References

Allen, J.R.L., 1994. Palaeowind: Geological Criteria for Direction and Strength. In: Allen, J.R.L., Hoskins, B.J., Sellwood, B.W., Spicer, R.A. & Valdes, R.J. (eds.): Palaeoclimates and their Modeling - With Special Reference to the Mesozoic Era: 2734.CrossRefGoogle Scholar
Arens, S.M., 1996. Rates of Aeolian Transport on a Beach in a Temperate Humid Climate. Geomorphology 17: 318.Google Scholar
Bagnold, R.A., 1941. The Physics of Blown Sand and Desert Dunes, Methuen, London. 265pp.Google Scholar
Blakey, R.C. et al., 1988. Synthesis of Late Palaeozoic and Mesozoic Eolian Deposits of the Western Interior of the United States. Sedimentary Geology 56: 3125.CrossRefGoogle Scholar
Breed, C.S., Fryberger, S.G., Andrews, S., McCauley, C. Lennartz, F., Gebei, D. & Horstman, K., 1979. Regional studies of sand seas, using LANDSAT (ERTS) imagery. In: McKee, E.D. (ed.): A Study of Global Sand Seas. Professional Paper U.S. Geological Survey 1052: 305397.Google Scholar
Cooke, R.U., Warren, A. & Goudie, A.S., 1993. Desert Geomorphology. UCL Press, London: 526.CrossRefGoogle Scholar
De Jongh, R., 1996. STRATAGEM., a 2D stratigraphie forward modeling package. Krefeld 1996 (abstract)Google Scholar
Dawson, P.J. and Marwitz, J.D., 1982. Wave Structures and Turbulent Features of the Winter Airflow in Southern Wyoming. Geol. Soc. Am. Sp. Paper 192: 5563.Google Scholar
Fischer, A.G. and Bottjer, D.J., 1991. Orbital Forcing and Sedimentary Sequences. Journal of Sedimentary Petrology 61/7: 10631069.Google Scholar
Fonseca, C. 1999. STRATAGEM - Can 2D modeling of a 3D world still be state-of-the-art? Tronheim August 1999 (abstract)Google Scholar
Fryberger, S.G. & Ahlbrandt, T.S., 1979. Mechanism for the Formation of Aeolian Sand Seas. Zeitschrift für Geomorphologie NF 23: 440460.Google Scholar
Glennie, K.W. Pugh, J.M. & Goodall, T.M., 1994. Late Quaternary Arabian Desert Models of Permian Rotliegend Reservoirs. Exploration Bulletin 274: 119.Google Scholar
Haq, B.U., Hardenbol, J. and Vail, P.R., 1988. Mesozoic and Cenozoic Chronostratigraphy and Cycles of Sea-Level Change. In: Sea-Level Changes - An Integrated Approach, SEPM Sp. Pubi. 42. ISBN 0-918985-74-9.CrossRefGoogle Scholar
Imbrie, J. and Imbrie, K., 1979. Ice Ages: Solving the Mystery: Short Hills, N.J. Harvard University Press: 224pp.Google Scholar
Kocurek, G. & Havholm, K.G., 1993. Eolian Sequence Stratigraphy - A Conceptual Framework. AAPG Memoir 58: 393409.Google Scholar
Kutzbach, J.E. & Ziegler, A.M., 1994. Simulation of Late Permian Climate and Biomes with an Atmosphere-Ocean Model: Comparisons with Observations. In: Allen, J.R.L., Hoskins, B.J., Sell-wood, B.W., Spicer, R.A. & Valdes, P.J. (eds.): Palaeoclimates and their Modeling - With Special Reference to the Mesozoic Era: 119132.CrossRefGoogle Scholar
Ladipo, K.O., 1997. Cyclostratigraphy of the Upper Rotliegend Slochteren Formation, NE Netherlands: A Genetic Unit Subdivision and Correlation of Fluvio-Aeolian Facies. In: Barren Sequences Special Issue, SIEP 977021.Google Scholar
Lancaster, N., 1983. Controls on Dune Morphology in the Namib Sand Sea. In: Ahlbrandt, T.S. & Brookfield, M.E. (eds.): Eolian Sediments and Processes. Elsevier: 261289.Google Scholar
Loope, D.B., 1995. Episodic deposition and preservation of eolian sands: A late Palaeozoic example from Southeastern Utah. Geology 13:7376.2.0.CO;2>CrossRefGoogle Scholar
Mainguet, M., 1978. The Influence of Trade Winds, Local Air Masses, and Topographic Obstacles on the Aeolian Movement of Sand Particles and the Origin and Distribution of Dunes and Ergs in the Sahara and Australia. Geoforum 9: 1728.Google Scholar
Marsh, N.D. & Ditlevsen, , 1997. Observation of Atmospheric and Climate Dynamics from a High Resolution Ice Core Record of a Passive Tracer over the Last Glaciation. Journal of Geophysical Research 102 (DIO): 1121911224.CrossRefGoogle Scholar
Nickling, W.G., 1988. The Initiation of Particle Movement by Wind. Sedimentology 35: 499511.Google Scholar
Nordlund, U., 1996. Formalizing geological knowledge with an example of modeling stratigraphy, using Fuzzy logic. J.Sedimentary Res. 66: 689698.Google Scholar
Perlmutter, M.A. & Matthews, M.D., 1989. Global Cyclostratigraphy - A Model. In: Cross, T.A. (ed.): Quantitative Dynamic Stratigraphy. Prentice Hall: 233260.Google Scholar
Sarnthein, M., 1978. Sand Deserts during Glacial Maximum and Climatic Optimum. Nature 272: 4346.Google Scholar
Sarnthein, M., Tetzlaff, G., Koopman, B., Wolter, K. & Pflaumann, U., 1981. Glacial and Interglacial Wind Regimes over the Eastern Subtropical Atlantic and Northwest Africa. Nature 293: 193196.Google Scholar
Thomas, D.S.G. & Shaw, P.A., 1991. ‘Relict’ Desert Dune Systems: Interpretations and Problems. Journal of Arid Environments 20: 114.CrossRefGoogle Scholar
Wiggs, G.F.S., Thomas, D.S.G. & Bullard, J.E., 1995. Dune Mobility and Vegetation Cover in the Southwest Kalahari Desert. Earth Surface Processes and Landforms 20: 515529.CrossRefGoogle Scholar
Williams, S.H. & Lee, J.A., 1995. Aeolian Saltation Transport Rate: an Example of the Effect of Sediment Supply. Journal of Arid Environments 30: 153160.CrossRefGoogle Scholar
Wilson, I.G., 1971. Aeolian Bedforms - Their Development and Origins. Sedimentology 19: 173210.Google Scholar
Wilson, I.G., 1973. Ergs. Sedimentary Geology 10: 77106.CrossRefGoogle Scholar
Zadeh, L.A., 1965. ‘Fuzzy Sets’, Information and Control 8: 338353.Google Scholar