2011
DOI: 10.1016/j.ijggc.2010.11.008
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Determining the corrosive potential of CO2 transport pipeline in high pCO2–water environments

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Cited by 185 publications
(100 citation statements)
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References 21 publications
(34 reference statements)
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“…where V c is the corrosion rate of the specimen in mm/year, ∆m is the weight loss in grams, is the density of the steel in g/cm 3 , A is the exposed area in cm 2 and t is the immersion time in hours.…”
Section: Materials and Preparationmentioning
confidence: 99%
See 2 more Smart Citations
“…where V c is the corrosion rate of the specimen in mm/year, ∆m is the weight loss in grams, is the density of the steel in g/cm 3 , A is the exposed area in cm 2 and t is the immersion time in hours.…”
Section: Materials and Preparationmentioning
confidence: 99%
“…1 O 2 is particularly important in influencing corrosion mechanisms as it provides additional cathodic reaction paths for corrosion whilst also inhibiting the formation of protective iron carbonate (FeCO 3 ) which has been shown to form in water-containing supercritical CO 2 environments. [2][3][4] Furthermore, when SO 2 and O 2 are present together, the formation of sulfurous (H 2 SO 3 ) and/or sulfuric (H 2 SO 4 ) acid is permitted which can play a key role in not only the corrosion mechanisms, but also in the nature and morphology of any corrosion products formed, which may inhibit or accelerate the corrosion kinetics.…”
Section: Introductionmentioning
confidence: 99%
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“…In vapor-saturated CO 2 system, corrosion is initiated due to the condensation of water on the coupon surface as a result of small variation in pressure and temperature. Once the water condenses onto the coupon surface, it will be saturated with both CO 2 and Fe 2+ from the dissolution of the steel [27,37]. So, the corrosion phenomenon could occur in the coupon surface at vapor-saturated CO 2 condition.…”
Section: Corrosion Mechanismmentioning
confidence: 99%
“…However, the amount of dissolved CO 2 at operative depths typical for carbon sequestration into basaltic aquifers (Alfredsson et al, 2013) is in the ratio 30–70 g CO 2 per kg H 2 O (Choi & Nešić, 2011). Consequently, the large amounts of water to be injected during subsurface CO 2 storage efforts may trigger earthquakes in response to pore fluid overpressures in the vicinity of preexisting faults (Zoback & Gorelick, 2012).…”
Section: Introductionmentioning
confidence: 99%