SPE Drilling & Completion
Volume 25,
Number 4,
December 2010,
pp. 555-563
Summary
A new hydraulic-fracturing fluid has been developed that is capable of
reaching fluid service temperatures up to 232°C. This fracturing fluid
technology uses a synthetic polymer that is crosslinkable with metal ions to
generate high viscosity. The synthetic-polymeric fracturing gel overcomes the
thermal limitations of traditional guar and derivatized guar-based fracturing
fluids. Several advancements have been made in the development of this
technology to maximize the efficiency of crosslinking and to give an effective
breaking profile, resulting in good laboratory gel cleanup in the proppant
pack. Research efforts have yielded a fracturing fluid with good fluid
stability at high temperatures to create better proppant transport and
placement in these most-demanding environments.
An integral part of this fluid is a crosslinking system that can be "tuned"
for crosslinking onset from 38 to 138°C, allowing for optimization for
particular well conditions. The crosslinking system allows the treatment
schedule to be tailored to the targeted well to help minimize frictional
pressure loss. An efficient and effective oxidative-breaker package has been
developed to give a controlled rheological break for the synthetic fluid and
provide good regained conductivity data. The new, high-temperature fracturing
technology provides a new tool to stimulate hotter, deeper hydrocarbon
resources to help maximize hydrocarbon recovery. This fracturing-fluid system
has been applied successfully in south Texas at temperatures approaching
232°C.
Laboratory rheological data that demonstrate fluid stability, crosslinking
performance, and controlled fluid breaks are presented. Dynamic fluid-loss and
regained-conductivity data are also presented to illustrate fluid cleanup in
proppant packs.
© 2010. Society of Petroleum Engineers
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History
- Original manuscript received:
29 May 2009
- Meeting paper published:
17 June 2009
- Revised manuscript received:
3 February 2010
- Manuscript approved:
12 April 2010
- Published online:
21 October 2010
- Version of record:
16 December 2010