Second update on compounds with kröhnkite-type chains

Second update on compounds with kröhnkite-type chains
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具有 kröhnkite 型链的化合物的第二次更新

DOI:
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发表时间:
2005
期刊:
影响因子:
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通讯作者:
M. Fleck
M. Fleck
中科院分区:
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文献类型:
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作者:
U. Kolitsch;M. Fleck

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本文报道了五种新合成的复盐二水合物的单晶X-射线衍射结构。以下三种硒酸盐(VI)、硫酸盐(VI)和铬酸盐(VI)化合物都含有克氏-[Na 2Cu(SO 4)2 · 2 H2O]-型无限四面体-八面体链:K2Zn(SeO4)2 ·2H2O(a = 5.571(1),B = 6.586(1),c = 7.458(2)π,α = 111.14(3),β = 96.35(3),γ = 106.15(3)°,V = 238.26(8)π 3,R(F)= 0.037,空间群P-1,no.2,Z = 1),K_2Co(SO_4)_2·2H_2O(a = 5.327(1),B = 6.566(1),c = 7.256(2)π,α = 110.74(3),β = 95.00(3),γ = 107.02(3)°,V = 221.72(8)π 3,R(F)= 0.037,空间群P-1,no.2,Z = 1),Rb_2Cd(CrO_4)_2·2H_2O(a = 6.852(1),B = 7.706(2),c = 11.362(2)°,α = 73.07(3),β = 75.11(3),γ = 69.63(3)°,V = 529.88(18)° 3,R(F)= 0.026,空间群P-1,no.2,Z = 2)。其余两种化合物,同型重铬酸盐K2 Co(Cr2 O 7)2 · 2 H2O和Cs2 Cd(Cr2 O 7)2 · 2 H2O的晶体结构(a = 6.801(1)/7.368(1),B = 7.723(1)/8.051(2),c = 7.814(1)/8.047(2)°,α = 89.23(3)/88.68(3),β = 81.05(3)/81.12(3),γ = 64.39(3)/63.81(3)°,V = 364.93(14)/422.66(16)3,R(F)= 0.022/0.025,空间群P-1,no. 2,Z = 1)与克氏石型化合物的结构密切相关;结构中含有Cr2 O 7基团,具有与克氏石型含氧盐中XO 4基团相同的桥接作用。这两种重铬酸盐与它们的K-Zn-和K-Cd-类似物是同型的,尽管Cs_2Cd(Cr_2O_7)_2·2H_2O中的氢键方案完全不同。描述了这五个新化合物的原子排列,并指出了它们的特殊之处。关于我们先前提出的分类,讨论了与其他克陨石型和类矿物和化合物的结构关系(Fleck等人,2002年; Fleck和Kolitsch,2003年)。化合物Rb 2Cd(CrO 4)2 · 2 H2O代表第一个克朗斯特型铷化合物和第一个具有结构类型D的铬酸盐。Cs2 Cd(Cr2 O 7)2 · 2 H2O是已知的第一个含有类铬榴石链的铯化合物。
Abstract The crystal structures of five new synthetic double salt dihydrates have been determined from single-crystal X-ray diffraction data. The following three selenate(VI), sulphate(VI) and chromate(VI) compounds all contain kröhnkite-[Na2Cu(SO4)2 · 2 H2O]-type infinite tetrahedral-octahedral chains: K2Zn(SeO4)2 · 2 H2O (a = 5.571(1), b = 6.586(1), c = 7.458(2) Å, α = 111.14(3), β = 96.35(3), γ = 106.15(3)°, V = 238.26(8) Å3, R(F) = 0.037, space group P-1, no. 2, Z = 1), K2Co(SO4)2 · 2 H2O (a = 5.327(1), b = 6.566(1), c = 7.256(2) Å, α = 110.74(3), β = 95.00(3), γ = 107.02(3)°, V = 221.72(8) Å3, R(F) = 0.037, space group P-1, no. 2, Z = 1), Rb2Cd(CrO4)2 · 2 H2O (a = 6.852(1), b = 7.706(2), c = 11.362(2) Å, α = 73.07(3), β = 75.11(3), γ = 69.63(3)°, V = 529.88(18) Å3, R(F) = 0.026, space group P-1, no. 2, Z = 2). The crystal structures of the two remaining compounds, the isotypic dichromates K2Co(Cr2O7)2 · 2 H2O and Cs2Cd(Cr2O7)2 · 2 H2O (a = 6.801(1)/7.368(1), b = 7.723(1)/8.051(2), c = 7.814(1) /8.047(2) Å, α = 89.23(3)/88.68(3), β = 81.05(3)/81.12(3), γ = 64.39(3)/63.81(3)°, V = 364.93(14)/422.66(16) Å3, R(F) = 0.022/0.025, space group P-1, no. 2, Z = 1) are closely related to those of kröhnkite-type compounds; the structure contains Cr2O7 groups assuming the same bridging role that XO4 groups have in kröhnkite-type oxysalts. Both dichromates are isotypic with their K—Zn- and K—Cd-analogues although the hydrogen bonding scheme in Cs2Cd(Cr2O7)2 · 2 H2O is completely different. The atomic arrangements of the five new compounds are described and unusual features are pointed out. Structural relations with other kröhnkite-type and -like minerals and compounds are discussed with respect to our previously proposed classification (Fleck et al., 2002; Fleck and Kolitsch, 2003). The compound Rb2Cd(CrO4)2 · 2 H2O represents both the first kröhnkite-type rubidium compound and the first chromate with structure type D. Cs2Cd(Cr2O7)2 · 2 H2O is the first caesium compound known to contain kröhnkite-like chains.