首页> 外文期刊>American Mineralogist >Hydrothermal synthesis and crystal chemistry of the new strontium uranyl selenites, Sr[(UO2)3(SeO3)2O2]*4H2O and Sr[UO2(SeO3)2]
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Hydrothermal synthesis and crystal chemistry of the new strontium uranyl selenites, Sr[(UO2)3(SeO3)2O2]*4H2O and Sr[UO2(SeO3)2]

机译:新型锶铀酰亚硒酸盐Sr [(UO2)3(SeO3)2O2] * 4H2O和Sr [UO2(SeO3)2]的水热合成和晶体化学。

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摘要

The reaction of UO3 with SeO2 in the presence of SrCl2• 6H2O and Sr(OH)2• 8H2O in supercritical water at 425 °C for 3 d results in the formation of the new strontium uranyl selenites, Sr[(UO2)3(SeO3)2O2]•4H2O (1) and Sr[UO2(SeO3)2] (2). The single crystal X-ray structures of type 1 and type 2 were solved by direct methods and refined by full-matrix least-squares methods. Crystallographic data (193 K): (1), monoclinic, space group C2/m, a = 17.014(2), b = 7.0637(7), and c = 7.1084(7) Å, ß = 100.544(2)°, Z = 2, R(F) = 0.0361 for 79 parameters with 1132 reflections with I > 2(I), wR2 = 0.0998 for all data; (2), triclinic, space group P, a = 5.6722(4), b = 6.7627(5), and c = 11.2622(8) Å, = 104.698(1)°, ß = 93.708(1)°, = 109.489(1)°, Z = 2, R(F) = 0.0373 for 110 parameters with 1902 reflections with I > 2(I), wR2 = 0.0856 for all data. The structure of type 1 contains two-dimensionalsheets with the same topology as those found in guilleminite, Ba[(UO2)3(SeO3)2O2]•3H2O, and marthozite, Cu[(UO2)3(SeO3)2O2](H2O)8. Sr2+ cations and H2O groups occur between the layers. In contrast, the structure of type 2 contains one-dimensional ribbons with Sr2+ cations residing between them. This compound is isostructural with its Ca2+-containing analog.
机译:在SrCl 2 6H 2 存在下,UO 3 与SeO 2 的反应在425°C 的超临界水中连续3 d的sub> O和Sr(OH) 2 •8H 2 O导致形成新锶铀酰 硒沸石,Sr [(UO 2 3 (SeO 3 2 O 2 ]•4H 2 O(1)和Sr [UO 2 (SeO 3 )< sub> 2 ] (2)。通过直接方法解决了类型1和 2的单晶X射线结构,并通过全矩阵最小二乘法 方法进行了改进。晶体学数据(193 K):(1),单斜晶,空间 群C2 / m,a = 17.014(2),b = 7.0637(7),c = 7.1084(7) Å,ß= 100.544(2)°,Z = 2,R(F)= 0.0361 对于79个参数具有1132次反射且I> 2(I),wR 2 = 0.0998(对于所有数据); (2),三斜度,空间群P,a = 5.6722(4),b = 6.7627(5),c = 11.2622(8) Å,= 104.698(1)°,ß= 93.708 (1)°, = 109.489(1)°,Z = 2,R(F)= 0.0373对于110个参数的 1902反射,I> 2(I),对于所有数据,wR 2 = 0.0856。 类型1的结构包含二维片状结构,其拓扑结构与guilleminite Ba [(UO 2 < / sub>) 3 (SeO 3 2 O 2 ]•3H 2 O, 和马洛石,Cu [(UO 2 3 (SeO 3 2 < / sub> O 2 ](H 2 O) 8 。 Sr 2 + 阳离子和 H 2 O基团在层之间出现。相比之下,类型2的结构 包含一维带,它们之间存在Sr 2 + 阳离子。该化合物是等结构的 及其含Ca 2 + 的类似物。

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    《American Mineralogist》 |2004年第7期|00000976-00000980|共5页
  • 作者单位

    Department of Chemistry, Auburn University, Auburn, Alabama 36849, U.S.A.;

    Department of Chemistry, Auburn University, Auburn, Alabama 36849, U.S.A.;

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