Iron(II) chloride, known chemically as FeCl2, consists of a lattice structure that arises from ionic bonding. The iron ions (Fe2+) form an octahedral geometry, surrounded by six chloride ions (Cl-), which also associate with neighboring iron ions.
This arrangement creates a continuous network that extends throughout the solid, contributing to the stability and rigidity of the compound. Iron(II) chloride exhibits properties typical of ionic compounds, such as high melting points and the ability to dissolve in water producing electrolyte solutions.
- Octahedral coordination of Fe2+ and Cl- ions
- Extended three-dimensional lattice
- Characteristic ionic compound attributes