The Maturing
Fretwell, Nick, Pierre Baux,
Total E&P UK PLC,
The Alwyn North Field is located on
the western side of the Viking Graben of the
The Carnian to Rhaetian
Upper Lunde gross succession is up to 800m thick. The
Alwyn reservoirs are 2-10m thick fluvial sandstones
deposited as ephemeral and perennial channels with splay and lake margin
deposits within a dominant floodplain paleosol
environment. The sands are heavily and variably cemented with calcite and
chlorite and most permeability results from secondary porosity generation in
the burial environment. Production from thin sands comes from over 10 stratigraphic intervals spanning over 400m thickness of
sequence, but is constrained by reduced reservoir quality at depth. Most
production to date is from two intervals where channels are preferentially
laterally and vertically connected suggesting constrained valley-fill
deposition following periods of overall incision. These intervals are
significantly depleted even in downdip locations over
2km from the main crestal producers.
To assess
remaining recoverable reserves, our approach uses numerous 3D geomodel realisations that have
been constrained and fully conditioned by a rigorous analysis of historical
well performance data. These models are used to assess incremental reserves
benefits from multilateral well designs and fracturation
techniques, to prolong Alwyn Field life.