Treatment of high surface area feroxyhyte (delta'-FeOOH) with hydrogen
sulfide, at room temperature, yielded mackinawite (FeS) and amorphous
sulfur. On exposure to air, the sulfided material underwent an exothe
rmic reaction during which crystalline sulfur and an amorphous hydrate
d iron oxide species were formed. On leaving this material in air for
a period of days crystalline goethite (alpha-FeOOH) was formed. These
chemical and structural changes were accompanied by alterations in the
morphologies of the materials, all of which occurred at, or close to,
room temperature. These differences are important for two reasons. Fi
rst, they are of relevance to the sulfiding of metal oxides and second
ly they involve high-melting-point ionic lattices undergoing complete
reorganisation at close to ambient temperature.