Summary
Low-salinity (lowsal) waterflooding has been evaluated for increased oil
recovery (IOR) at the Snorre field. Coreflooding experiments and a single-well
chemical tracer-test (SWCTT) field pilot have been performed to measure the
remaining oil saturation after seawaterflooding and after lowsal flooding.
The laboratory coreflooding experiments conducted at reservoir and
low-pressure conditions involved core material from the Upper and Lower
Statfjord and Lunde formations. The core material from the Statfjord formations
gave incremental recovery in the order of 2% of original oil in place (OOIP) by
injection of diluted seawater. Similar amounts were produced during following
NaCl-based lowsal injections. The same trend was observed in the high- and
low-pressure experiments. No significant response to lowsal flooding was
observed for Lunde cores. No response was normally observed during alkaline
injection.
The SWCTT field pilot was carried out in the Upper Statfjord formation. The
average oil saturations after seawater injection, after lowsal seawater
injection, and after a new seawater injection were determined; no significant
change in the remaining oil saturation was shown. The measured in-situ value of
remaining oil saturation after seawaterflooding was in agreement with previous
special core analysis (SCAL) experiments.
The measured effect of tertiary lowsal flooding from core experiments was in
agreement with the SWCTT. Both measurements indicated only low or no effect
from lowsal injection.
It has been suggested that lowsal flooding has a potential for improved oil
recovery in all clayey sandstone formations containing crude oil. The results
from this work indicate that the initial wetting condition is a crucial
property for the effect of lowsal injection.
© 2011. Society of Petroleum Engineers
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History
- Original manuscript received:
4 June 2010
- Meeting paper published:
25 April 2010
- Revised manuscript received:
28 September 2010
- Manuscript approved:
17 November 2010
- Published online:
31 March 2011
- Version of record:
6 April 2011