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Formula: Fe3+16O16(OH)9.6(SO4)3.2.10H2O
Valence: Fe3+16O16(OH)9.6(S6+O4)3.2.10H2O
Hydrated sulphate
Crystal system: Tetragonal
Specific gravity: 3.88 calculated
Hardness: 1 to 2
Streak: Yellow
Colour: Brownish yellow
Solubility: Rapid dissolution in cold, 5 M hydrochloric acid or in ammonium oxalate at pH 3 (strongly acid)
Environments
Schwertmannite is a secondary mineral precipitated
by waters of pH 3 to 4.5 and high in iron sulphate content from the surface oxidation of metal sulphides.
Associated minerals include goethite,
jarosite, natrojarosite,
ferrihydrite and sulphides
(HOM).
Localities
Rotbachl, Rotbachlspitze, Pfitsch pass, Finkenberg, Schwaz District, Tyrol, Austria. After being frequently
identified in precipitates from acid mine waters, a fully natural occurrence of schwertmannite has been
found in a small steam draining a pyritic
schist at the Pfitscher Joch. The characteristics of specimens from
this location are in full agreement with those of synthetic samples and samples from acid mine waters described
elsewhere. This natural occurrence also demonstrates the genetic relationship between schwertmannite,
jarosite and
goethite/ferrihydrite as
products of pyrite oxidation, which is governed mainly the sulphate and
iron concentrations of the stream
(EJM 7.547-552).
At the type locality, Pyhäsalmi Mine, Pyhäjärvi, North Ostrobothnia, Finland, schwertmannite occurs as a
poorly crystalline, yellowish brown, ochreous precipitate from acid, sulphate-rich waters. It typically consists
of needles 2 to 4 nm thick and 60 to 90 nm long, which are in spherical to ellipsoidal aggregates 200 to 500 nm
across.
Schwertmannite is known synthetically and from more than 40 localities in Europe, North America and
Australia. All occurrences are related to the surface or near-surface oxidation of metal sulphides; optimum
conditions for formation are pH 3 to 4.5 (acid) and S04 concentrations of 1000 to 3000 mg/L. Typical
associates are jarosite,
natrojarosite, goethite
and ferrihydrite
(AM 80.845-850).
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