TL;DR: In this article, the authors used a Nd-Yag laser operating at an excitation wavelength of 780 nm to obtain the Raman spectra of the basic copper sulphate minerals antlerite, brochantite, posnjakite and langite.
Abstract: The basic copper sulphates are of interest because of their appearance in many environmental situations such as copper pipe corrosion, restoration of brass and bronze objects, leaching from waste mineral dumps and the restoration of frescoes. The Raman spectra of the basic copper sulphate minerals antlerite, brochantite, posnjakite and langite are reported using a Nd-Yag laser operating at an excitation wavelength of 780 nm. In line with their crystal structures, each basic copper sulphate mineral has its own characteristic Raman spectrum, which enables their identification. Except for brochantite multiple bands are observed for the SO stretching vibration. Similarly multiple bands are observed for the antisymmetric SO and OSO bending regions. Hydroxyl deformation modes in the 730 to 790 cm-1 region are observed. The use of the HeNe laser operating at an excitation wavelength of 633 nm enabled the hydroxyl stretching bands of the minerals to be obtained. Antlerite and brochantite are characterised by hydroxyl stretching bands at 3580 and 3488 cm-1. The minerals posnjakite and langite display Raman hydroxyl-stretching vibrations at 3588 and 3564 cm-1. The Raman spectra of these two minerals show water OH-stretching bands at 3405, 3372 and 3260 cm-1. Raman spectroscopy allows the ready identification of these minerals.
TL;DR: In this article, micro-Raman spectroscopic analysis of different species of copper sulfates was carried out and it was shown that these products are most likely to be formed as the result of atmospheric corrosion of copper alloys, e.g. bronze in sulfurbearing environments.
TL;DR: The crystal structure of wroewolfeite has been solved by direct methods and refined by full-matrix least-squares to an R index of 6.7% usingTll observed (I > 2.5o\ reflections measured on a twinned crystal.
Abstract: The crystal structure of wroewolfeite, Cun(SOa[OH)6'2H2O, monoclinic, a : 6.0a5(1), b : 5.646(1), c : A.337Q)A, B :93.39(l)', / : 488.5(1)A3, space group Pc, has been solved by direct methods and refined by full-matrix least-squares to an R index of 6.7% usingTll observed (I > 2.5o\ reflections measured on a twinned crystal. The fundamental building block of the wroewolfeite structure is a [Cun(SOnXOH)rr]t- hetropolyhedral cluster that polymerizes in two dimensions by edge-sharing between octahedra to form the structure module, a [Cu4(SO4[OH)6(H2O)]' sheet that is parallel to {001}. These sheets are linked solely by hydrogen bonding, involving an additional (HrO) anion that is not directly bonded to a cation. This [Cu4(SO4XOH)6(H2O)]' sheet is also found in posnjakite and may also occur in langite. This and other related sheets may be described by the general formula [MoX,d.-.], in which M : octahedrally coordinated cation, X : complex anion, @ : simple anion (e.g' O'z-, (OH)-, (HrO)").The following structures are included: n : 0, botallackite; n : 1, wroewolfeite, langite, posnjakite; n :2, ktenasite, serpierite, devillite. The intra-module linkages and hydration states in these minerals may be interpreted in terms of the Lewis basicity/acidity of structural fragments.
TL;DR: Wroewolfeite as mentioned in this paper is a new mineral from the Loudville lead mine in Loudville, Massachusetts, U.S.A. The mineral occurs as blue, monoclinic crystals, twinned on {001}, very similar in appearance to posnjakite and langite.
Abstract: Wroewolfeite is a new mineral from the Loudville lead mine in Loudville, Massachusetts, U.S.A. The mineral occurs as blue, monoclinic crystals, twinned on {001}, very similar in appearance to posnjakite and langite. It is formed as small isolated pinacoidal crystals (up to 1.0 mm) implanted on covelline and chalcosine. There are three cleavages of equal facility of production. The cell dimensions are a 6.058 A, b 5.654 A, c 14.360 A, β 93° 28′, space group Pc or P2/c. The strongest diffraction lines (in A) are 7.152 (100), 3.581 (70), 2.628 (35), 2.004 (30), 2.431 (20), 2.379 (20), 2.278 (20). Electronmicroprobe analysis gives CuO 64.22 %, SO3 16.48 %, water by difference 19.30 %. Empirical cell contents are Cu7.88(SO4)2.00(OH)11.76.(H2O)4.22 or Cu4(SO4)(OH)6.2H2O with Z = 2. Wroewolfeite is strongly pleochroic with a light blue, β deep greenish blue, and γ, medium greenish blue. Absorption β > γ ≫ α. The mineral is biaxial with α 1.637, β 1.682, and γ 1.694, 2Vα = 53° The name is for C. Wroe Wolfe, American crystallographer, educator, and philosopher.