Loading…
Materials selection for dew-point corrosion in geothermal fluids containing acid chloride
[Display omitted] •General corrosion, pitting and stress corrosion cracking characterization of a large number of stainless steel, nickel alloys and titanium alloys.•Material selection criteria for geothermal energy production.•Definition corrosion susceptibility maps for corrosion resistant alloys...
Saved in:
Published in: | Geothermics 2017-09, Vol.69, p.139-144 |
---|---|
Main Authors: | , , , , , |
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!
|
Summary: | [Display omitted]
•General corrosion, pitting and stress corrosion cracking characterization of a large number of stainless steel, nickel alloys and titanium alloys.•Material selection criteria for geothermal energy production.•Definition corrosion susceptibility maps for corrosion resistant alloys and titanium alloys.
The paper is aimed to the evaluation of the corrosion behavior of corrosion resisting alloys (CRAs) in geothermal fluids operating at the dew point.
Several test series were carried out in geothermal production sites of Tuscany (Italy) under continuous flow. The vapor was extracted directly from the main flow and it was conveyed in an experimental device designed to simulate dew point conditions.
Nine martensitic stainless steel, one precipitation hardening stainless steel with martensitic structure, two ferritic extra low interstitial (ELI) stainless steels, four duplex (austenitic-ferritic) stainless steel, five austenitic stainless steels, six nickel alloys/super austenitic stainless steels, four titanium alloys were tested.
The main forms of corrosion were general corrosion, localized corrosion (pitting and crevice) and stress corrosion cracking. Corrosion maps are presented as a function of PREN index, chromium, molybdenum and nickel content. |
---|---|
ISSN: | 0375-6505 1879-3576 |
DOI: | 10.1016/j.geothermics.2017.05.010 |