Loading…

Corrosion of carbon steel and the passivating properties of corrosion films formed under high-PT geothermal conditions

Corrosion is a major obstacle to a safe implementation of geotechnical applications. Using a novel approach that includes vertical scanning interferometry (VSI) and electrochemical impedance spectroscopy (EIS) we discuss time-dependent carbon steel corrosion and film formation at geothermally releva...

Full description

Saved in:
Bibliographic Details
Published in:The Science of the total environment 2019-08, Vol.677 (C), p.307-314
Main Authors: Mundhenk, Niklas, Knauss, Kevin G., Bandaru, Siva R.S., Wonneberger, Robert, Devine, Thomas M.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Corrosion is a major obstacle to a safe implementation of geotechnical applications. Using a novel approach that includes vertical scanning interferometry (VSI) and electrochemical impedance spectroscopy (EIS) we discuss time-dependent carbon steel corrosion and film formation at geothermally relevant temperatures (80–160 °C) in CO2-saturated mildly acidic NaCl brine. Iron dissolution kinetics follows a logarithmic rate at 80 and 160 °C and a linear rate at 120 °C. At 80 °C, high initial corrosion rates (first 24 h) generate H2 at a minimum rate of 12 μmol h−1 cm−2 and lead to the formation of a continuous ~100 μm thick porous corrosion film. It exhibits a duplex structure with a crystalline outer FeCO3 layer and an inner layer composed of a skeletal network of Fe3C impregnated with FeCO3. Being an electrical conductor we hypothesize the Fe3C to strongly enhance corrosion rates by providing additional cathodic sites. Pseudo-passivity due to an anodic film-forming reaction (presumably Fe-oxide) was observed at 120 and 160 °C, soon followed by the initiation of pitting at 120 °C. Steady-state corrosion rates at 160 °C are at least one order of magnitude lower than for 120 °C. Our experimental approach demonstrated potential for general applicability in studying corrosion-related phenomena. [Display omitted] •Iron dissolution kinetics follows a logarithmic rate at 80 °C and a linear rate at 120 °C.•Fe3C-catalyzed corrosion causes significant H2 generation at 80 °C.•Formation of FeCO3 film lowers corrosion rate substantially at 80 °C.•Localized corrosion at 120 °C & substantially lower uniform corrosion at 160 °C.
ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2019.04.386