The Magnus Field: extending field life through good reservoir management and enhanced oil recovery

Author:

MACGREGOR A. G.1,TRUSSELL P.1,LAUVER S.1,BEDROCK M.1,BRYCE J.1,MOULDS T.1

Affiliation:

1. BP Exploration Operating Company Ltd, Farburn Industrial Estate, Dyce, Aberdeen AB21 7PB, UK (e-mail:macgreag@bp.com)

Abstract

The Magnus Field has been on production since 1983. Production of oil is from intra-Kimmeridge Clay Formation age turbidite sandstones. The individual lobes of the turbidites are generally fining-up, or have fine tops. Waterflood production tends to sweep the lower part of the units very effectively, thus leaving an unswept oil target at the top of many flow units. An enhanced oil recovery (EOR) scheme has been implemented on the Magnus Field by bringing gas, which had no access to a market, from the Foinaven and Schiehallion fields West of Shetland. Because the gas is mainly methane it is taken via the Sullom Voe Terminal (SVT) on the Shetland Islands where it is enriched by injecting higher molecular weight gases. This enrichment improves the effectiveness of the EOR process at Magnus. The scheme adds value not only at the Magnus Field but also to the West of Shetland fields and at SVT. The gas can also be used as fuel to replace diesel at SVT, bringing environmental benefits.

Publisher

Geological Society of London

Subject

Fuel Technology,Energy Engineering and Power Technology,Geology,Geochemistry and Petrology

Reference7 articles.

1. DTI IOR 2003. World Wide Web Address: http://ior.rml.co.uk/, Issue 6 October 2003 contains an article ‘Magnus Miscible WAG EOR Project’.

2. DTI ‘SHARP’ 2003. Sustainable Hydrocarbons Additional Recovery Programme. World Wide Web Address: http://www.dti-sharp.co.uk/.

3. Haajizadeh R. 2001. Modelling Miscible WAG Injection EOR in the Magnus Field. Paper SPE, 66378.

4. Lee, Sheng-Tai et al. 2001. Optimising Miscible Injectant (MI) Composition for Gas Injection projects. Paper SPE 71606.

5. Genetic sequence stratigraphy for the North Sea Late Jurassic and Early Cretaceous: distribution and prediction of Kimmeridgian–Late Ryazanian reservoirs in the North Sea and adjacent areas

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