微孔钛矿型相A6[B12O18][CX3]2[Dx(H2O,OH,O)6−y]的研究[j]

X. Wang , F. Liebau
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引用次数: 10

摘要

在120 ~ 200℃之间进行了水热合成,以确定具有鲸蜡石结构的半导体微孔材料的化学变异性。分子式为A6[B12O18][CX3]2[Dx(H2O,OH,O)6−y],(0≤x≤2;0≤y≤6),这是由x射线晶体结构的细化得来的。A = Li+, Na+, K+, Rb+, Cs+, Tl+, NH4+, Ca2+, Sr2+和Ba2+作为氢氧化物引入,在某些情况下作为碳酸盐引入,B = C = As3+, Sb3+和Bi3+, X = S2−,Se2−和Te2−作为元素引入。只有B = C = Sb3+和X = S2−和Se2−的合成是成功的。已知的钙钛石型相现在包括元素组合A/Sb3+/S2−与A = Na+和K+,和A/Sb3+/Se2−与A = Na+, K+, Rb+, Sr2+, Ba2+,可能还有Tl+。不同数量的Na+、Sb3+和C4+占据了蛭石型结构的D位。化学变异性可以用A+ + h2o2 + + OH−mH2ODm+ + mOH和nOH−Dn+ + nO2−的偶联取代来描述。所得到的晶体呈橙色到暗红色,与它们的半导体特性一致。
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An investigation of microporous cetineite-type phases A6[B12O18][CX3]2[Dx(H2O,OH,O)6−y] I. The cetineite structure field

Hydrothermal syntheses between 120 and 200 °C have been performed to determine the chemical variability of semiconducting microporous materials with cetineite structure. The syntheses were based on the general formula A6[B12O18][CX3]2[Dx(H2O,OH,O)6−y], (0≤×≤2; 0≤y≤6), which was derived from X-ray crystal structure refinements. A = Li+, Na+, K+, Rb+, Cs+, Tl+, NH4+, Ca2+, Sr2+, and Ba2+ were introduced as hydroxides, in some cases as carbonates, B = C = As3+, Sb3+, and Bi3+, and X = S2−, Se2−, and Te2− as elements. Only syntheses with B = C = Sb3+ and X = S2− and Se2− were successfull. Known cetineite-type phases now include the element combinations A/Sb3+/S2− with A = Na+ and K+, and A/Sb3+/Se2− with A = Na+, K+, Rb+, Sr2+, Ba2+, and probably Tl+. Variable amounts of Na+, Sb3+ and C4+ were found to occupy the D position of the cetineite-type structure. The chemical variability can be described by the coupled substitutions A+ + H2OA2+ + OH mH2ODm+ + mOH, and nOHDn+ + nO2−. The crystals obtained are orange to dark red, in agreement with their semiconducting properties.

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