Arsenate units (AsO4 tetrahedra) typically form the anionic framework in arsenate minerals and related compounds, while cobalt ions balance charge and coordinate to surrounding oxygens. The abundant water of crystallization resides in interstitial sites within the crystal lattice. The exact arrangement of cobalt and arsenate units, and the distribution of hydration water, is often described in crystallographic studies, but detailed structural data for this specific hydrate are not widely published in standard references. The material is expected to be relatively insoluble in water and to exhibit color characteristic of cobalt(II) salts, commonly blue or pale blue.
Compounds of this type are usually prepared by reacting a cobalt(II) salt (such as cobalt(II) nitrate or cobalt(II) chloride) with a source of arsenate under aqueous conditions, followed by controlled cooling or evaporation to encourage crystallization. Hydration water is incorporated from the solution and retained in the crystal structure. The exact synthesis parameters (pH, concentration, temperature) influence the final hydration level and crystal morphology.
Co3AsO428H2O is an inorganic solid that is typically insoluble in water. It is sensitive to dehydration upon heating; heating drives off water and can lead to decomposition to other cobalt-arsenate or oxide phases. As arsenate-containing compounds, it is toxic and should be handled with appropriate safety precautions to avoid ingestion or inhalation.