Bismuth silicon oxide or bismuth silicate refers to an inorganic compound of bismuth, silicon and oxygen. The bismuth silicate Bi<sub>12</sub>SiO<sub>20</sub> is most commonly encountered, though others are also known. It occurs naturally as the mineral sillénite and can be produced synthetically by heating a mixture of bismuth oxide and silicon dioxide. Centimeter-sized single crystals of Bi<sub>12</sub>SiO<sub>20</sub> can be grown by the Czochralski process from the molten phase. They exhibit piezoelectric, electro-optic, elasto-optic, photorefractive and photoconductive properties, and therefore have potential applications in spatial light modulators, acoustic delay lines and hologram recording equipment. Bi<sub>12</sub>SiO<sub>20</sub> can be obtained as a whitish powder with band gap of approximately 3.2 eV starting from bismuth subcarbonate and silica in presence of ethyleneglycol. <sup>29</sup>Si solid-state NMR is used to prove that the Si(IV) cations are sharing oxygen atoms with the Bi(III) cations. The <sup>29</sup>Si chemical shift (ô) in Bi<sub>12</sub>SiO<sub>20</sub> is âÂÂ78.1 ppm. Unlike bismuth oxide, the presence of the acidic Si(IV) cations avoid the reactivity with CO<sub>2</sub>.
Other bismuth silicates are known, such as Bi<sub>4</sub>Si<sub>3</sub>O<sub>12</sub>, Bi<sub>2</sub>SiO<sub>5</sub>, and Bi<sub>2</sub>Si<sub>3</sub>O<sub>9</sub>.