1887

Abstract

Summary

Compacting and expanding reservoirs cause respectively subsidence and heave at the surface which at present can be measured using different geodetic methods. Knowing the source of compaction and expansion is of large value to our subsurface operations as it aids in assessment of reservoir conformance and possible containment issues. However, measured subsidence cannot be related one-on-one to actual reservoir compaction: An inversion process is required. Due to the spatial convolution and filtering nature of the subsurface on the actual reservoir compaction or expansion problem, inversion is a complicated process.

This paper describes an iterative inversion workflow, taking full advantage of the speed of semi-analytical forward models while adhering to the actual complexity of the subsurface captured in a detailed finite element model. The iterative scheme allows for handling of the ill-posed nature of the problem. The workflow presented here shows the utility of integrating geodetic data sources to estimate reservoir volume changes. This technique has proven to add value when it comes to monitoring areal and temporal changes in the reservoir. It is relatively easy to implement as it does not require large amounts of input data and can be applied to any field where surface deformation data is available.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201800719
2018-06-11
2024-04-23
Loading full text...

Full text loading...

References

  1. Fokker, P.A., Wassing, B.B.T., van Leijen, F.J., Hanssen, R.F., Nieuwland, D.A.
    , 2016. Application of an ensemble smoother with multiple data assimilation to the Bergermeer gas field, using PS-In SAR. Geomech. Energy Enviro. 5, 16–28. doi:10.1016/j.gete.2015.11.003
    https://doi.org/10.1016/j.gete.2015.11.003 [Google Scholar]
  2. Geertsma, J., van Opstal, G.
    , 1973. A numerical technique for predicting subsidence above compacting reservoirs, based on the nucleus of strain concept. Verh. van het K. Ned. Geol. Mijnbouwkd. Genoot.28, 63–78.
    [Google Scholar]
  3. Kovtun, V.
    , 2013. Regularization based on Krylov subspace iteration. Charles University, Prague.
    [Google Scholar]
  4. Muntendam-Bos, A.G., Kroon, I.C., Fokker, P.A.
    , 2008. Time-dependent inversion of surface subsidence due to dynamic reservoir compaction. Math. Geosci.40, 159–177. doi:10.1007/s11004‑007‑9135‑3
    https://doi.org/10.1007/s11004-007-9135-3 [Google Scholar]
  5. Okada, Y.
    , 1992. Gravity and potential changes due to shear and tensile faults in a half-space. J. Geophys. Res.97, 7137. doi:10.1029/92JB00178
    https://doi.org/10.1029/92JB00178 [Google Scholar]
  6. Wahba, G.
    , 1979. How to Smooth Curves and Surfaces with Splines and Cross-Validation, in: 24th Conference on the Design of Experiments. pp. 167–192.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201800719
Loading
/content/papers/10.3997/2214-4609.201800719
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error