Articles | Volume 372
Proc. IAHS, 372, 367–373, 2015
https://doi.org/10.5194/piahs-372-367-2015
Proc. IAHS, 372, 367–373, 2015
https://doi.org/10.5194/piahs-372-367-2015

  12 Nov 2015

12 Nov 2015

Compaction and subsidence of the Groningen gas field in the Netherlands

K. van Thienen-Visser et al.

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Inversion of double-difference measurements from optical levelling for the Groningen gas field
P. A. Fokker and K. Van Thienen-Visser
Proc. IAHS, 372, 375–378, https://doi.org/10.5194/piahs-372-375-2015,https://doi.org/10.5194/piahs-372-375-2015, 2015
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Cited articles

den Haan, E.: A compression model for non-brittle soft clays and peat, Geotechnique, 46, 1–16, 1996.
de Waal, J.: On the rate type compaction behaviour of sandstone reservoir rock, PhD thesis, Delft University of Technology, Delft, the Netherlands, available at: http://repository.tudelft.nl/view/ir/uuid:b805782b-2eb4-4f72-98f4-f727c4ea9df0 (last access: 19 October 2015), 1986.
de Waal, J., van Thienen-Visser, K., and Pruiksma, J. P.: Rate type isotach compaction of consolidates sandstone, 49th US Rock mechanics/Geomechanics symposium (ARMA), San Franscisco, USA, 28 June–1 July, American Rock Mechanics Association (ARMA), 15-436, 2015.
Mijnlieff, H. F. and Geluk, M.: Paleotopography-governed sediment distribution: a new predictive model for the Permian Upper Rotliegend in the Dutch sector of the Southern Permian Basin, SEPM Special Publication: The Permian Rotliegend of the Netherlands 01/2011, 98, 47–160, https://doi.org/10.2110/pec.11.98.0147 2011.
Mossop, A.: An explanation for anomalous time dependent subsidence, 46th US Rock Mechanics/Geomechanics Symposium, Chicago, Illinois, USA, 24–27 June 2012, 12-518, 2012.
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Short summary
The Groningen gas field in the Netherlands is Europe’s largest gas field. It has been produced since 1963 and production is expected to continue until 2080. Subsidence occurring due to the pressure depletion is measured annually. In this study different compaction models are tested using the subsidence measurements. The pattern of over- and underestimation of the subsidence can be explained by variations in reservoir parameters.