The viscosity of aqueous NaCl solutions with dissolved CO 2 was measured at conditions representing an underground aquifer at a depth of (1000 to 2000) m for the geological storage of CO 2 (i.e., (30 to 60) °C and (10 to 20) MPa at a mass fraction of NaCl between 0 and 0.03 by using a sedimenting solid particle type viscometer with an estimated uncertainty of ±2%). On the basis of this experimental data, an empirical equation for predicting this viscosity as a function of the temperature and mole fraction of CO 2 for these conditions was derived.
No takes yet. Share an insight, caveat, or question.
Bando et al. (2004) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context:
More from Journal of Chemical & Engineering Data