钨酸盐

钨酸盐是指钨(VI)的含氧酸盐，其最常见的形式是WO₄^2-。钨还能够形成多酸盐，如[W₄O₁₆]^8-、[W₇O₂₄]^6-、[H₂W₁₂O₄₀]^6-等。钨和大部分元素（如P^V、As^V、Mn^II、Mn^III、Ce^IV等）可以形成杂多酸盐。[1]

钨酸盐可以在自然界中以矿物的形式存在，如白钨矿（CaWO₄）[2]、钨铁矿（FeWO₄）[3]等。

常见化合物

常见的钨酸盐有：

钨酸盐中的氧可以被过氧根取代，形成过氧钨酸盐，如黄色的W(O₂)₄^2-等。[1]硫或硒逐个至完全取代的硫（硒）代钨酸盐也是已知的，例如Cs₂WSe₄。[4]而碲代钨酸盐的报道很少。[5]

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Ferberite （页面存档备份，存于）. MinDat. [2017-2-1]
E Diemann, A Müller. Thio and seleno compounds of the transition metals with the do configuration. Coordination Chemistry Reviews， 1973. 10(1-2): 79–122. 10.1016/S0010-8545(00)80232-5
Henri Brunner, Joachim Wachter, Robert Wanninger, et al. Synthesis and X-ray Structure of [{(Cp′2Nb)2WTe4}⋅W(CO)4]·1.5C7H8, the First Organometallic Derivative of the WTe42− Anion, and of [Cp′4Nb2Te2] (Cp′ = η5-tBuC5H4). European Journal of Inorganic Chemistry, 2001. 5: 1151-1154. DOI: 10.1002/1099-0682(200105)2001:5<1151::AID-EJIC1151>3.0.CO;2-#

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