In chemistry, a tungstate is a compound that contains an oxoanion of tungsten or is a mixed oxide containing tungsten. The simplest tungstate ion is WO2−4, "orthotungstate". Many other tungstates belong to a large group of polyatomic ions that are termed polyoxometalates, ("POMs"), and specifically termed isopolyoxometalates as they contain, along with oxygen and maybe hydrogen, only one other element. Almost all useful tungsten ores are tungstates.
Orthotungstates feature tetrahedral W(VI) centres with short W–O distances of 1.79 Å. Structurally, they resemble sulfates. Six-coordinate, octahedral tungsten dominates in the polyoxotungstates. In these compounds, the W–O distances are elongated.
Some examples of tungstate ions:
- HWO−4 (hydrogentungstate)
- polymeric W2O2−7 ions of various structures in Na2W2O7, Li2W2O7 and Ag2W2O7
- [W7O24]6− (paratungstate A)
- [W10O32]4− (tungstate Y)
- [H2W12O42]10− (paratungstate B) 
- α-[H2W12O40]6− (metatungstate)
- β-[H2W12O40]6− (tungstate X)
See the tungstates category for a list of tungstates.
Tungstates occur naturally with molybdates. Scheelite, the mineral calcium tungstate, often contains a small amount of molybdate. Wolframite is manganese and iron tungstate, and all these are valuable sources of tungsten. Powellite is a mineral form of calcium molybdate containing a small amount of tungstate.
Unlike chromate, tungstate is not a good oxidizer, but like chromate, solutions of tungstate condense to give the isopolytungstates upon acidification.
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