Thesis (Ph. D.)--University of Washington, 2000. / Vita. Includes bibliographical references (leaves 183-190).

This thesis was submitted to the Faculty of Arts and Sciences in partial fulfillment of the requirements for the degree Bachelor of Science. / Field observation at seven outcrops and subsequent polished section studies reveal that lead and zinc mineralization in the Hamilton vicinity occurred after the lithification of the host carbonates. The availability of open structures and the presence of potential reducing agents are the main controlling factors of sulphide deposition, The absence of an igneous source demands an origin of the metals from the sedimentary country rocks. Analysis of 14 shales and 12 dolomites by atomic absorption for Cu, Pb, and Zn indicates that the argillaceous rocks are potential source of the heavy metals. Furthermore, a simple leaching experiment has demonstrated that concentrated brine (sodium chloride solution) can preferentially leach lead and zinc from the shales. A mode of origin involving preferential_leaching can then adequately explain the scarcity of copper minerals in the Mississippi Valley-Type ore. It is suggested that better controlled leaching experiments at various temperatures should be done in conjunction with more extensive field work to check the plausibility of such a theory. / Thesis / Bachelor of Science (BSc)

<p> Field observation at seven outcrops and subsequent polished section studies reveal that lead and zinc mineralization in the Hamilton vicinity occurred after the lithification of the host carbonates. The availability of open structures and the presence of potential reducing agents are the main controlling factors of sulphide deposition, The absence of an igneous source demands an origin of the metals from the sedimentary country rocks. Analysis of 14 shales and 12 dolomites by atomic absorption for Cu, Pb, and Zn indicates that the argillaceous rocks are potential source of the heavy metals. Furthermore, a simple leaching experiment has demonstrated that concentrated brine (sodium chloride solution) can preferentially leach lead and zinc from the shales. A mode of origin involving preferential.leaching can then adequately explain the scarcity of copper minerals in the Mississippi Valley-Type ore, It is suggested that better controlled leaching experiments at various temperatures should be done in conjunction with more extensive field work to check the plausibility of such a theory. </p> / Thesis / Bachelor of Science (BSc)

When sulfide minerals are exposed to the oxidizing conditions of the earth's surface, their metal ions are released into solution and the S²⁻ is oxidized to either elemental sulfur or sulfate. The experiments described here used a mixed flow reactor system to determine the oxidation rates of galena and sphalerite under conditions similar to that expected in a weathering ore deposit . The specific surface area of the run solids was determined by N₂ BET procedure and the surface textures observed by SEM. The amount of Fe³⁺ converted to Fe²⁺ by the oxidation reaction was determined using an Eh electrode. Solid reaction products include, orthorhombic S(s) and anglesite (PbSO₄) from the galena oxidation and minor orthorhombic S(s) from the sphalerite oxidation. The rate equations describing the 25°C data are: dn_Fe³⁺/dt = -5.5 ± 1.1 × 10⁻³ (A)(a<sub>Fe³⁺</sub)^{1.06 ± 0.16} for galena, and dn_Fe³⁺/dt = -1.8 ± 0.3 × 10⁻⁶ (A)(a_Fe³⁺)^{0.47 ± 0.08} for sphalerite. Where dn_Fe³⁺/dt is the rate of reduction of Fe³⁺ (moles sec⁻¹), and A is the surface area of the solid (m²). The calculated E_a for galena oxidation is 48 kJ mol⁻¹ (25 - 40°C) and is 84 kJ mol⁻¹ (25 -60°C) for sphalerite oxidation. Although galena and sphalerite are both simple, cubic, monosulfides their reaction rate with ferric iron differs by about 2.5 orders of magnitude for m_Fe³⁺ = 10⁻³. / M.S.

Thesis (M.S.)--University of Missouri, School of Mines and Metallurgy, 1940. / The entire thesis text is included in file. Typescript. Title from title screen of thesis/dissertation PDF file (viewed March 9, 2010) Includes bibliographical references (p. 45-46) and index (p. 47-52).

One of the main risks that exposed and unvegetated tailings pose to the environment and human health is airborne dust that may be inhaled or ingested. In the case of Pb-bearing dust, both particle size and the identity of the Pb-hosting minerals affect the degree of risk. Finer dusts (<5µm diameter) have a higher potential of being ingested deeper into the human lung causing possible tissue damage and toxic effects. We have collected size-fractionated airborne dust and near-surface pH-neutral tailings at New Calumet Mine, Quebec, Canada, a former Pb-Zn mine. Bioaccessibility describes how much of a substance can be dissolved by body fluids and become available for absorption by the body. The most bioaccessible Pb compounds are PbCO3 (cerussite), Pb3(CO3)2(OH)2 (hydrocerussite) and PbO, followed by PbSO4 (anglesite), PbS (galena) and Pb5(PO4)3Cl (pyromorphite). Airborne dust samples were collected on the tailings piles using a PIXE Cascade Impactor which separates aerosol fractions onto nine impactor stages ranging from 16µm to 0.06µm. These stages were then analyzed by PIXE to obtain elemental concentrations. Samples of non-vegetated and vegetated near-surface tailings were collected for bioaccessibility tests as well as for total metal content, grain size distribution, and Pb speciation using ESEM and synchrotron techniques. Both airborne dust and near-surface tailings samples underwent synchrotron microanalysis including microXRD for identification of microcrystalline compounds and microXRF for element mapping and metal ratio evaluation. Despite extensive oxidation of iron sulfide minerals in the near-surface tailings, galena persists as the most abundant Pb-bearing phase in the pH-neutral tailings. However, rims of cerussite and hydrocerussite forming alteration rims on galena grains have been identified throughout the tailings. In vitro bioaccessibility testing of Pb in the tailings resulted in 0-0.05% bioaccessible Pb in lung fluid and 23-69% bioaccessible Pb in the gastric fluid. / Thesis (Master, Geological Sciences & Geological Engineering) -- Queen's University, 2012-02-28 21:09:08.432

Thesis (PhDApSc(MineralsandMaterials))--University of South Australia, 2001.

Thesis (MAppSc)--University of South Australia, 2000.

Thesis (MAppSc)--University of South Australia, 2000.

Thesis (Ph. D.)--Columbia University, 1933. / Vita. Bibliography: p. 52-53.