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iron ii chloride dihydrate is a water soluble crystalline iron source. It is the precursor to hydrated iron (III) oxides which are magnetic pigments. It is also used as a reducing agent in organic synthesis reactions. It is available in a variety of forms, including high purity, submicron and nanopowders.
The dihydrate crystal structure has been determined at 298degK by single-crystal x-ray intensity analysis, with the iron ii and chlorine ions bonded in an isomorphous fashion to the chloride ion. The structure is a close analogue to that of the related lawrencite mineral (Fe, Ni)Cl2