SPE Projects, Facilities & Construction
Volume 6,
Number 4,
December 2011,
pp. 158-165
Summary
Carbon dioxide (CO2) sequestration in saline aquifers has been
proposed as one of the most practical options for reducing CO2
emissions into the atmosphere. Massive CO2 injection into an aquifer
would alter the geochemical equilibrium between the rock-forming minerals and
the formation water. In this work, a novel and simple predictive tool is
presented to estimate the formation of calcium carbonate (CaCO3)
scaling as a function of pH, temperature, ionic strength of the solution,
calcium cation concentration, bicarbonate anion concentration, and
CO2 mole fraction when the water mixture is saturated with a gas
containing CO2 to evaluate the effect of solution conditions on the
tendency and extent of precipitation. The proposed simple method covers
concentrations of calcium cation or bicarbonate anion in the range of 10 to 10
000 mg/L, with temperature ranging between 5 and 90°C, total ionic strength
ranging between 0.1 and 3.6, and pH values ranging between 5.5 and 8. The
predicted values are found to be in good agreement with the reported data, with
average absolute deviations being less than 2.6%. The proposed tool is superior
because of its accuracy and clear numerical background based on the Vandermonde
matrix, wherein the relevant coefficients can be retuned quickly if more data
become available in the future. The simple predictive tool proposed in the
paper can be of immense practical value for engineers and researchers to have a
quick check on the formation of calcium carbonate scaling when the water
mixture is saturated with a gas containing CO2 at various conditions
without opting for any experimental measurements. In particular, process
engineers would find the proposed method to be user friendly, involving no
complex expressions and presenting transparent calculations.
© 2011. Society of Petroleum Engineers
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History
- Original manuscript received:
6 August 2010
- Meeting paper published:
6 June 2010
- Revised manuscript received:
5 January 2011
- Manuscript approved:
4 April 2011
- Published online:
10 November 2011
- Version of record:
16 December 2011