CO2 degassing from a Spanish natural analogue for CO2 storage and leakage: Implications on 222Rn mobility

Abstract The Ganuelas-Mazarron Tertiary basin (SE Spain) hosts a deep saline CO 2 -rich aquifer from which CO 2 escapes occurs. Consequently, this basin is considered as a natural analogue for CO 2 storage and leakage. Recent studies performed in wellheads showed a close association between CO 2 and 222 Rn, therefore suggesting a further investigation of this association, particularly in diffuse escapes from soils. For that, concentrations of CO 2 and 222 Rn in soils, at ∼1 m depth, were measured by using the TRT-SEG04 and RM-2 Radon devices, respectively. These measurements were performed on areas with high density of lineament intersections, since they could be structural weakness zones and consequently favourable pathways for these gases. Moreover, the measurements were correlated with their corresponding geological cross-sections. The results allowed to conclude that: i) both gases only show a significant correlation in faulted zones and/or wellheads; ii) the CO 2 leakages could be doubly dangerous (toxicity and radioactivity of the associated 222 Rn); and iii) the Neogene marly cap-rock of the basin acts as a sealing formation against CO 2 and 222 Rn leakages. Finally, it can be also stated that 222 Rn can be used as an alert of CO 2 escapes from both CO 2 natural reservoir and CO 2 deep geological storage.