The Vasa's New Battle

The sulfuric acid threat to the Vasa

Outbreak of sulfate salts

During the wet summer in 2000 the relative humidity on several occasions reached levels higher than 65% in the Vasa Museum. An increasing number of white and yellowish salts started to precipitate inside the ship and on artefacts in the magazine.

A beam with salt formations A chest fromt the Vasa
Salt formation on a beam below the Vasa's galley in the hold (S4, see below) and on a chest in the magazine       Photos: M. Sandström, and the Vasa Museum

In February 2001 chemists were invited to a meeting at the Vasa Museum to discuss the problems. With a Guiner-Hägg camera, we could identify crystalline salts on the surfaces. The most common precipitate inside the Vasa was found to be the yellow-coloured natrojarosite, NaFe3(SO4)2(OH)6, an iron(III) sulfate that sometimes appears greenish on moist wood. Other commonly occurring salts are small bluish-white crystals of the iron(II) sulfate melanterite, FeSO4·7H2O, and ordinary white gypsum (calcium sulfate, CaSO4·2H2O. Also, crystalline elemental sulfur (consisting of ring-shaped S8 molecules) was found on some surfaces, mostly in the hold (Sandström 2001).

Side view of the Vasa

Common crystalline salts on the Vasa's surfaces:

Jarosite Melanter
Jarosite: NaFe3(SO4)2(OH)6 Melanterite: FeSO4·7H2O
Gypsum calsium sylfate S8 crowns
Gypsum calcium sulfate: CaSO4·2H2O Elemental sulfur (S8 crowns)

More information with molecules and minerals visualized in 3-D can be found in the homepage of: The Virtual Museum of Minerals and Molecules.