Nickelpicromerite, K^sub 2^Ni(SO^sub 4^)^sub 2^6H2O, a new picromerite-group mineral from Slyudorudnik, South Urals, Russia

• Published in: Mineralogy and petrology 2015-04, Vol.109 (2), p.143
• Main Authors: Belogub, Elena V, Krivovichev, Sergey V, Pekov, Igor V, Kuznetsov, Aleksey M, Yapaskurt, Vasiliy O, Kotlyarov, Vasiliy A, Chukanov, Nikita V, Belakovskiy, Dmitry I
• Format: Article
• Language: English
• Subjects: Anions; Cations; Crystals; Gypsum; Minerals; Mountains; Nickel; Pyrite; Sulfides
• ISSN: 0930-0708; 1438-1168
• DOI: 10.1007/s00710-014-0360-4

A new picromerite-group mineral, nickelpicromerite, K^sub 2^Ni(SO^sub 4^)^sub 2^·6H2O (IMA 2012-053), was found at the Vein #169 of the Ufaley quartz deposit, near the town of Slyudorudnik, Kyshtym District, Chelyabinsk area, South Urals, Russia. It is a supergene mineral that occurs, with gypsum and goethite, in the fractures of slightly weathered actinolite-talc schist containing partially vermiculitized biotite and partially altered sulfides: pyrrhotite, pentlandite, millerite, pyrite and marcasite. Nickelpicromerite forms equant to short prismatic or tabular crystals up to 0.07 mm in size and anhedral grains up to 0.5 mm across, their clusters or crusts up to 1 mm. Nickelpicromerite is light greenish blue. Lustre is vitreous. Mohs hardness is 2-2½. Cleavage is distinct, parallel to {10-2}. D ^sub meas^ is 2.20(2), D ^sub calc^ is 2.22 g cm^sup -3^. Nickelpicromerite is optically biaxial (+), [alpha]=1.486(2), [beta]=1.489(2), γ=1.494(2), 2V^sub meas^ =75(10)°, 2V^sub calc^ =76°. The chemical composition (wt.%, electron-microprobe data) is: K^sub 2^O 20.93, MgO 0.38, FeO 0.07, NiO 16.76, SO3 37.20, H2O (calc.) 24.66, total 100.00. The empirical formula, calculated based on 14 O, is: K^sub 1.93^Mg^sub 0.04^Ni^sub 0.98^S^sub 2.02^O^sub 8.05^(H2O)^sub 5.95^. Nickelpicromerite is monoclinic, P2^sub 1^/c, a=6.1310(7), b=12.1863(14), c=9.0076(10) Å, [beta]=105.045(2)°, V=649.9(1) Å^sup 3^, Z=2. Eight strongest reflections of the powder XRD pattern are [d,Å-I(hkl)]: 5.386-34(110); 4.312-46(002); 4.240-33(120); 4.085-100(012, 10-2); 3.685-85(031), 3.041-45(040, 112), 2.808-31(013, 20-2, 122), 2.368-34(13-3, 21-3, 033). Nickelpicromerite (single-crystal X-ray data, R=0.028) is isostructural to other picromerite-group minerals and synthetic Tutton's salts. Its crystal structure consists of [Ni(H2O)^sub 6^]^sup 2+^ octahedra linked to (SO^sub 4^)^sup 2-^ tetrahedra via hydrogen bonds. K^sup +^ cations are coordinated by eight anions. Nickelpicromerite is the product of alteration of primary sulfide minerals and the reaction of the acid Ni-sulfate solutions with biotite.