In condensed water, the free acetic acid content (HAc) is physically dissolved from the gas (or oil) phase, and this induces an overacidification of the CO2 solution. When HAc becomes the dominant acid, this increases the solubility of corrosion products, i.e. the iron content Fesat at the saturation of corrosion products in FeCO3. The empirical field thresholds of 1 and 0.1 mM HAc actually correspond to the same acidifying power as 2 and 0.2 bar of pure CO2, i.e. nearly the API limits of 1958… which nobody has ever considered as low !

In reservoir water, the free HAc is chemically produced from the total acetate content (Actot) and dissolved CO2, and this does not practically change anything on the Fesat. It just occurs that in strongly buffered waters, the HAc value in mM is always close to that of Fesat in ppm, so that the free HAc is not too bad a marker of the corrosion products solubility. Thresholds are then low because the corrosion layers can be sufficiently protective only at low Fesat.

Since the morphology and location of corrosion damage in downhole corrosion had long shown an ubiquitous effect of this solubility, as well as the more recent mechanisms on the protectiveness of corrosion layers, it is therefore suggested to replace the HAc thresholds by Fesat thresholds in the field data bases, and to look for experimental protocols in the laboratory which would be sensitive to the same Fesat thresholds as the documented experience on downhole or Top of Line corrosion.

In this respect, the famous Wytch Farm failure is not related to any acetic acid issue, but to a solubilization of corrosion products induced by a CaCO3 saturation in the gathering line. This indeed comes from an unprecedented combination of high Ca and low bicarbonate content B0 in the reservoir (high Ca/В0 ratio) and particularly low PCO2 levels in a trunk line under "full well stream transfer".

You do not currently have access to this content.