“…Previous works (Wilson, 2016;Oluyemi, 2014;Mohamed and Nasr-El-Din, 2013;Denney, 2013;Bybee, 2010;Egermann et al, 2010;Tomson et al, 2008;Metcalf and Devine, 2004) studied the effects of interaction between chemicals like hydrochloric acid (HCl), carbon dioxide (CO2), brine and water (H2O), diethylenetriamine penta (methylene phosphonic acid) (DETPMP), 2,2 bis(4-hydroxyphenyl)-4-methylpentane (BHPMP) and the formation rock on the strength and petrophysical properties of sandstone and carbonate rocks. These studies were carried out to: (i) determine the mechanisms involved in the chemistry of water flow back in the water/shale interaction (Wilson, 2016); (ii) establish a fundamental knowledge on the behaviour of carbonate and clastic rocks in the presence of scale inhibitor (Oluyemi, 2014;Tomson et al, 2008); (iii) investigate the effect of CO2-carbonate rock interaction on the strength and petrophysical properties of the rock (Mohamed and Nasr-El-Din, 2013;Denney, 2013;Egermann et al, 2010); (iv) investigate wellbore integrity as it relates to CO2 migration during CO2/cement/brine interactions (Bybee, 2010); and (v) assess rock strength after acid fracture treatment using HCl (Metcalf and Devine, 2004).…”