By Claire Gillespie | Updated Mar 24, 2022

Iron oxide—commonly called rust—is a reddish‑brown compound that forms when iron reacts with oxygen in the presence of water or moisture. When chloride ions are present, such as in saltwater, the same reaction occurs, but the process accelerates significantly.
Rust is a form of corrosion driven by electron transfer. Saltwater, being a better electrolyte, speeds up this transfer, so iron corrodes faster than in fresh water.
Not every metal “rusts.” Aluminum, for instance, develops a thin, protective oxide layer that shields it from moisture and oxygen. Iron, on the other hand, lacks such a barrier, so it readily forms hydrated iron oxide when exposed to water and air.
Corrosion begins when iron atoms lose electrons (oxidation) while oxygen atoms gain electrons (reduction). The resulting ferrous (Fe²⁺) and ferric (Fe³⁺) ions react with water to produce iron hydroxides, which gradually lose water to form iron oxides—collectively known as rust. As the rust flakes away, fresh iron is exposed, perpetuating the cycle.
Saltwater is a superior electrolyte because it contains dissolved ions that facilitate electron flow. In an electrochemical cell, this means the anodic (iron) and cathodic (oxygen reduction) reactions occur more readily. Consequently, iron corrodes at a rate up to 10‑15 times faster in seawater than in freshwater. Even brief exposure to salt spray or high humidity can mimic this effect on metal structures.
Protective strategies include:
These methods are widely endorsed by industry standards such as ASTM G1 (Standard Practice for Corrosion Testing) and NACE SP 0101 (Corrosion Prevention of Structural Steel).