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Svenekite, Ca[AsO_2(OH)_2]_2, a new mineral from Jachymov, Czech Republic

机译:Svenekite Ca [AsO_2(OH)_2] _2,来自捷克共和国Jachymov的新矿物

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Svenekite (IMA 99-007), Ca[AsO_2(OH)_2]_2, is a rare supergene arsenate mineral occurring in the Geschieber vein, Jachymov ore district, Western Bohemia, Czech Republic. It grows directly on the granite rocks and occurs isolated from other arsenate minerals otherwise common in Jachymov. Svenekite usually forms clear transparent coatings composed of indistinct radiating to rosette-shaped aggregates up to 3 mm across. They are composed of thin lens- or bladed-shaped crystals, usually 100—150 urn long. Svenekite is transparent to translucent and has a white streak and a vitreous lustre; it does not fluoresce under ultraviolet light. Cleavage is very good on {010}. The Mohs hardness is ~2. Svenekite is biaxial, non-pleochroic. The refractive indices are a' = 1.602(2), y' = 1.658(2). The empirical formula of svenekite (based on As + P + S = 2 a.p.f.u., an average of 10 spot analyses) is (Ca_(1.oo)Mg_(o.o1))[AsO_2(OH)_2]_(1.96)[PO_2(OH)_2]_(o.o3)(SO_4)_(o.o1) The simplified formula is Ca[AsO_2(OH)_2]_2 and requires CaO 17.42, As_2O_5 71.39, H_2O 11.19, total 100.00 wt.%. Raman and infrared spectroscopy exhibit dominance of O—H vibrations and vibration modes of distorted tetrahedral AsO_2(OH)_2 units. Svenekite is triclinic, space group PI, with a = 8.5606(5), b = 7.6926(6), c = 5.7206(4) A, a = 92.605(6), p = 109.9002(6), y = 109.9017(6)°, and V= 327.48(4) A3, Z= 2, D_(calo) = 3.26 g-cm~(-3). The a:b:c ratio is 0.7436:1:1.1082 (for single-crystal data). The six strongest diffraction peaks in the X-ray powder diffraction pattern are [d (A)/I(%)/(hkl)]: 3.968(33)(2l0); 3.766(35)(2ll); 3.697(49)(101); 3.554(100)(020); 3.259(33)(220); 3.097(49)(121). The crystal structure of svenekite was refined from single-crystal X-ray diffraction data to R_1 = 0.0250 based on 1309 unique observed, and to wR_2 = 0.0588, for all 1588 unique reflections (with GOF_(a11) = 1.20). The structure of svenekite consists of sheets of corner-sharing CaO_8 polyhedra and AsO_2OH_2 groups, stacked parallel to (001). Adjacent sheets are linked by hydrogen bonds. The svenekite structure possesses very short symmetrical hydrogen bonds (with the D—H lengths -1.22 A). The mineral is named to honour Jaroslav Svenek, the former curator of the mineralogical collection of the National Museum in Prague, Czech Republic.
机译:Svenekite(IMA 99-007)Ca [AsO_2(OH)_2] _2是一种稀有的超基因砷酸盐矿物,存在于捷克共和国西波西米亚Jachymov矿区的Geschieber脉中。它直接生长在花岗岩岩石上,并与其他Jachymov中常见的砷酸盐矿物隔离存在。堇青石通常形成透明的透明涂层,该涂层由模糊不清的辐射形成为最大3 mm宽的玫瑰状聚集体。它们由薄片状或叶片状晶体组成,通常长100-150微米。堇青石透明至半透明,具有白色条纹和玻璃光泽。它不会在紫外线下发出荧光。 {010}上的切割非常好。莫氏硬度为〜2。堇青石是双轴的,非疏油性的。折射率为a'= 1.602(2),y'= 1.658(2)。闪锌矿的经验公式(基于As + P + S = 2 apfu,平均10次斑点分析)为(Ca_(1.oo)Mg_(o.o1))[AsO_2(OH)_2] _(1.96) [PO_2(OH)_2] _(o.o3)(SO_4)_(o.o1)的简化公式为Ca [AsO_2(OH)_2] _2,需要CaO 17.42,As_2O_5 71.39,H_2O 11.19,总量为100.00 wt。 %。拉曼光谱和红外光谱显示出OH振动和扭曲的四面体AsO_2(OH)_2单元的振动模式。 Svenekite是三斜晶系,空间群PI,a = 8.5606(5),b = 7.6926(6),c = 5.7206(4)A,a = 92.605(6),p = 109.9002(6),y = 109.9017(6 )°,并且V = 327.48(4)A3,Z = 2,D_(calo)= 3.26 g-cm〜(-3)。 a:b:c之比为0.7436:1:1.1082(对于单晶数据)。 X射线粉末衍射图中六个最强的衍射峰为[d(A)/ I(%)/(hkl)]:3.968(33)(2l0); [d(A)/ I(%)/(hkl)]: 3.766(35)(2ll); 3.697(49)(101); 3.554(100)(020); 3.259(33)(220); 3.097(49)(121)。基于所有观察到的1588次唯一反射(GOF_(a11)= 1.20),基于观察到的1309次唯一反射,细晶石的晶体结构从单晶X射线衍射数据精炼为R_1 = 0.0250,以及wR_2 = 0.0588。闪锌矿的结构由角共享的CaO_8多面体和AsO_2OH_2基片平行于(001)堆叠而成。相邻的薄片通过氢键连接。闪锌矿结构具有非常短的对称氢键(DH长度为-1.22 A)。矿物的名字是为了纪念Jaroslav Svenek,他是捷克共和国布拉格国家博物馆矿物学收藏的前馆长。

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