Shipwrecks, Corrosion and Conservation

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Shipwrecks, Corrosion and Conservation Summary Slides PART 5 – Jack Dengate

Sulfate Reducing Bacteria The wreck of the Titanic was found in 1985 in nearly 4000 metre deep waters.  Some parts had long red rusticles ('rust-like, icicle-like') hanging while other parts had black iron(II) sulfide.  Other parts of the Titanic had little corrosion.  Sulfate Reducing Bacteria

Sulfate Reducing Bacteria Experiments on samples collected from the wreck showed that sulfate reducing bacteria (SRB) were important in forming the red rusticles and black FeS. Sulfate Reducing Bacteria

Sulfate Reducing Bacteria Bacteria associated with the rusticles are sometimes called "iron-eating bacteria".  Two types of bacteria are found with the rusticles.  Anaerobic SRB which do not need oxygen are found on the inside.  Oxygen-dependent aerobic bacteria are found on the outside of the rusticles.  Sulfate Reducing Bacteria

Chemical reactions carried out by this combination of bacteria increase the rate of corrosion of the iron Titanic. One microbiologist has suggested that iron corrosion driven by bacterial action will completely reduce the Titanic to a huge iron-ore deposit within 100 years.

Sulfate Reducing Bacteria SRB produce the compound hydrogen sulfide (H2S) from the sulfate ions that are plentiful in sea water: SO42–   +   10H+   +  8e–       H2S    +   4H2O
 Note that the oxidation state of sulfur has been reduced from +6 in SO42– to –2 in H2S.
 This is why the anaerobic bacteria that cause this change are called sulfate reducing bacteria. Sulfate Reducing Bacteria

Sulfate Reducing Bacteria Sea water normally has a pH of about 8.  The increased solubility of CO2 with depth makes deep ocean water slightly acidic.  As the pH drops with depth in ocean water the presence of more hydrogen ions favours corrosion of metals. Sulfate Reducing Bacteria

Sulfate Reducing Bacteria Corrosion of metals produces metal ions, e.g. Fe + 2H+  -->  Fe2+  +  H2 Some metal ions produced can undergo hydrolysis (reaction with water) to produce more hydrogen ions. The SRB are able to change the H2 to 2H+ , which they then use to reduce sulfate ions to hydrogen sulfide. Sulfate Reducing Bacteria

Sulfate Reducing Bacteria The release of hydrogen ions can produce small acidic environments as low as pH 4 in some locations around a shipwreck. H2S, produced by the action of SRB is a weak acid that releases hydrogen ions and sulfide ions.; H2S ⇌ 2H+  +   S2– Sulfate Reducing Bacteria

Sulfate Reducing Bacteria The sulfide ions from the H2S can precipitate Fe2+ ions to form insoluble, black iron (II) sulfide FeS:    Fe2+  +  S2–    FeS(s)  The presence of black FeS indicates that SRB are present. The precipitation of FeS removes sulfide ions and encourages further ionisation of H2S releasing more H+. Sulfate Reducing Bacteria

Sulfate Reducing Bacteria Metal near wood on the Titanic was badly corroded.  As the wood cellulose, (C6H10O5)n, decayed, it released oxygen which stimulated the growth of aerobic bacteria.  Waste from these aerobic bacteria provided nourishment to the anaerobic SRB.  The SRB flourished and increased corrosion of the metal near wood. Sulfate Reducing Bacteria

Acidic conditions lead to an acceleration of the corrosion process compared with basic or neutral conditions. Hydrogen ions can react with non-passivating metals, such as iron. 
 Fe(s)   +   2H+     Fe2+   +   H2(g) Acidic Environments

Non-passivating metals are metals that do not have a protective oxide layer that would prevent hydrogen ions reacting with metal atoms. Metals with protective passivation layers include aluminium, chromium, titanium and tin. Lead and copper objects taken from shipwrecks have been found to be corroded. Hydrogen sulfide produced by sulfate reducing bacteria can react with just about any metal except gold. Acidic Environments