Thèse (D.Ress.Min.) -- Université du Québec à Chicoutimi, programme extensionné à l'Université du Québec à Montréal, 2003. / Bibliogr.: f. 267-278. Document électronique également accessible en format PDF. CaQCU

Thesis (Ph.D.)(Metallurgical Engineering)--University of Pretoria, 2005. / Includes summary. Includes bibliographical references.

Thesis(Ph.D.(Physics)) -- University of Limpopo, 2020 / Surface properties of pyrite (FeS2), chalcopyrite (CuFeS2), galena (PbS) and sphalerite (ZnS) most thermodynamically stable surfaces have been studied using first priniciples density functional theory. The most stable surfaces showed the highest surface exposure as it covered a higher percentage of the surface area on morphologies. The interaction of water with such sulphide surfaces was also investigated; the structures of sulphide minerals surfaces were changed in the presence H2O molecules. The surfaces of FeS2 and ZnS relax most while those of CuFeS2 and PbS surfaces change slightly in the presence of H2O molecules. The results on the effect of chain length of DTPs and DTCs on the enthalpies of adsorption on pyrite, galena, chalcopyrite and sphalerite have shown that an increase in chain length of the DTPs resulted in an increase in the enthalpies of adsorption trend for pyrite, galena and sphalerite. This is an important observation since the ligand is the same in all cases and therefore the effect is due to the role of the alkyl group Moreover, we noted a decrease of enthalpies of adsorption with an increase of DTCs chain lengths on pyrite, galena, chalcopyrite and sphalerite. The effect of the branching of the hydrocarbon chain length of the dithiocarbamates on the enthalpy of adsorption of pyrite was investigated. The results show that the configuration of the alkyl chain length of the same carbon number has an influence on the enthalpy of adsorption. Furthermore, the results indicate that there was minimal enthalpy of adsorption when DeDTP was dosed to galena, chalcopyrite and sphalerite minerals as compared to DeDTC and ethyl xanthate. On the other hand, the enthalpies of adsorption of DeDTP on pyrite were very high which represented a greater exothermic reaction than for any of the DeDTC and ethyl xanthate. The bond distance between thiol collector and the surface is consistent with the corresponding calculated adsorption energies. The Mulliken population of S-Fe/S-Pb/S-Zn bond for the adsorption of eX on CuFeS2 surface are high compared to PbS and ZnS surfaces, which indicated that there is a strong covalent bond between S and Fe atoms as compared to S-Pb and Pb-Zn bonds. Such observations are consistent with results of other thiol collectors. It was seen that the Mulliken atomic charges populations of CuFeS2, PbS and ZnS surface layers are different before and after DTPs adsorption. The charges of Fe atom reduce, which indicates that the Zn and Pb atoms become more positive and the Fe atom becomes more negative. In addition, there are changes in the charges of S atoms in ZnS and PbS surface layers before and after H2O absorption, suggesting that the presence of water would affect the adsorption of thiol collector. The densities of states (DOS) of the thiol collectors on surfaces of sulphide minerals have shown a strong hybridisation between the S 3p-orbital HOMO, metals (Fe, Pb, Zn) 3d-orbital for pyrite and chalcopyrite, 6p-orbital for galena and (3d and 4s)-orbitals for sphalerite. The collector S 3p-orbital reduces to zero states on the surfaces of Fe, Pb and Zn atoms. The Fe-S bond population for DeDTP is lower than that of DispDTP and DbDTP in pyrite, respectively. For chalcopyrite the DeDTP Fe-S population is higher than both DispDTP and DbDTP: similar trends were observed for Pb-S and Zn-S, however, the Pb-S bonding was less covalent as compared to the Fe S in chalcopyrite. The DTPs Fe-S bond population is generally higher in chalcopyrite than in pyrite. Mulliken charges analysis indicated that the DTPs S atoms lost charges and the metals gained with a decreasing DTPs chain length for pyrite: a similar trend was observed for chalcopyrite. The DTPs gained electrons from galena and sphalerite surface. For DTCs pyrite and chalcopyrite surface Fe atoms gain more electrons in the presence of DeDTP than other DTPs, while galena and sphalerite lost most electrons in the presence of DbDTC than other DTCs. As for xanthate, the Mulliken bond charges indicated that the S atoms and the metals lost charges, suggesting that some charges reside at the internuclear region between the metals and sulphurs (M– S). These show that electron charges are collector and mineral dependent; collector would be an electron acceptor or donor depending on the mineral makeup. A comparison of the computational results, isothermal titration calorimetry (ITC) and microfloatation experiments for the interaction of DeDTP, DeDTC and eX with pyrite and galena was made. The calculated adsorption energies between thiol collectors and mineral surfaces were always more exothermic than the experimentally determined ones. In computational calulations, water adsorption was found to reduce the reactivity of Fe and Pb atom for the interaction with thiol collectors and bring the adsorption energies closer to the magnitude of the experimental values. FeS2 (100) surface heat of adsorption depict similar trends to experimental recoveries from microfloation for DeDTP, DeDTC and eX, while FeS2 (111) heats of adsorptions for DeDTP and DeDTC are consistent with ITC experimental results. Lastly, calculated DeDTP and DeDTC adsorptions on the PbS (100) are also consistent with experimental recoveries. / National Research Foundation (NRF), South African Minerals of Metal Institution (SAMMRI) and University of Limpopo (UL)

A dissertation submitted to the Faculty of Engineering and the Built Environment, University of the Witwatersrand, Johannesburg, in fulfilment of the requirements for the degree of Master of Science in Chemical Engineering, 2016 / In South Africa, the need for water treatment is increasing, especially in the mining sector. As active water treatment technologies are expensive, the mining sector has an increasing need for passive water treatment technology, with low maintenance and operating costs, yet efficient water treatment ability. Literature on passive water treatment suggests that these systems only offer a narrow range of treatment capabilities. Therefore, hybrid water treatment systems could be a solution to low-cost water treatment in South Africa. The Degrading Packed Bed Reactor (DPBR) is one of the units comprising the hybrid treatment group. The DPBR’s main action is to convert sulfates into sulfides and alkalinity. In practice, the main drawback of the DPBR is clogging. Clogging lessens the amount of Acid Mine Drainage (AMD) that comes into contact with Sulfur Reducing Bacteria (SRB) in the DPBR, thereby reducing the efficiency of the bioreactor. In this study, six small-scale DPBRs were constructed. Each was classified according to its unique organic source (manure, straw, vegetable food processing waste, wood shavings, chicken litter and a combined sample with layers of all the carbon sources). Synthetic AMD was fed through the six bioreactors for a period of three months. From the small-scale DPBRs, the permeability, sulfate, iron and pH of the exit samples were measured. On average, the carbon sources removed 50 % of the sulfates and 98 % of the iron from the fed AMD. The different carbon sources showed no significant difference between each other in terms their sulfate and iron removal. The range between the best performing carbon source and the poorest performing carbon source, in terms of sulfate removal, was 17%. For iron removal, the range between the best and poorest performing carbon sources was only 2%. It was found that the permeability of the carbon sources played a larger role in the efficiency of the DPBR than the type of carbon source used. Manure is highly effective in terms of pH improvement, sulfate and iron removal. However, this is at the expense of permeability, as its packing clogs very rapidly. Compost and straw have excellent permeabilities which do not change significantly over long timeframes. This is, however, at the expense of the remedial ability of the packing materials. The combined reactor, in every instance, offers a good compromise between these different behaviours. / GR2016

Downhole sampling of unboiled liquid at 1350 and 1500 m depth in the seawater-dominated Reykjanes high-temperature geothermal system in Iceland shows that metal concentrations measured at surface are minimum values due to mineral precipitation in the wells; by analogy of similar tectonic setting, host rocks and fluid composition, the metal concentrations measured in many black smoker vents at the seafloor are also minima. Fluids in the Reykjanes geothermal system react with mid-ocean ridge basalt at temperatures as high as 346°C and contain Fe 9-140 ppm, Cu 14-17 ppm, Zn 5-27 ppm, Pb 120-290 ppb, 1-6 ppb Au, and 28-107 ppb Ag. Fluids discharged at surface from the same wells have orders of magnitude lower metal concentrations due to precipitation caused by boiling and vapor loss during depressurization. Upstream of the orifice plate at high pressure (40 bar, 252°C) the precipitates consist mainly of sphalerite and chalcopyrite with a trace of galena and bornite. At the orifice plate of old wells, the pressure decreased sharply to 11 bar (188°C), resulting in abundant deposition of amorphous silica together with minor sphalerite and traces of chalcopyrite. In new wells the pressure at the orifice plate decreases to 22 bar (220°C); this pressure decrease and concomitant boiling causes deposition of fine-grained bornite-digenite solid solution together with sphalerite and galena on the fluid flow control valve. In high-pressure wells (average wellhead pressure 45-35 bar) most metals (mainly as sphalerite) are deposited downstream of the orifice plate, with up to 950 ppm Au and 2.5 wt.% Ag. Bulk concentrations in the scales vary between 15-60 wt.% upstream and downstream of the orifice plate and diminish from there. Iron increases up well from 8 to ~20 wt.% and decreases downstream of the orifice plate from 6 to 2 wt.% at the separation station; Cu downhole is ~3 wt.% but increases to 25 wt.% on the fluid flow control valve and then decreases; Pb downhole 100s ppm but at the wellhead is ~3 wt.%, increasing to 15 wt.% at the fluid flow control valve, then decreasing sharply from there.

Downhole sampling of unboiled liquid at 1350 and 1500 m depth in the seawater-dominated Reykjanes high-temperature geothermal system in Iceland shows that metal concentrations measured at surface are minimum values due to mineral precipitation in the wells; by analogy of similar tectonic setting, host rocks and fluid composition, the metal concentrations measured in many black smoker vents at the seafloor are also minima. Fluids in the Reykjanes geothermal system react with mid-ocean ridge basalt at temperatures as high as 346°C and contain Fe 9-140 ppm, Cu 14-17 ppm, Zn 5-27 ppm, Pb 120-290 ppb, 1-6 ppb Au, and 28-107 ppb Ag. Fluids discharged at surface from the same wells have orders of magnitude lower metal concentrations due to precipitation caused by boiling and vapor loss during depressurization. Upstream of the orifice plate at high pressure (40 bar, 252°C) the precipitates consist mainly of sphalerite and chalcopyrite with a trace of galena and bornite. At the orifice plate of old wells, the pressure decreased sharply to 11 bar (188°C), resulting in abundant deposition of amorphous silica together with minor sphalerite and traces of chalcopyrite. In new wells the pressure at the orifice plate decreases to 22 bar (220°C); this pressure decrease and concomitant boiling causes deposition of fine-grained bornite-digenite solid solution together with sphalerite and galena on the fluid flow control valve. In high-pressure wells (average wellhead pressure 45-35 bar) most metals (mainly as sphalerite) are deposited downstream of the orifice plate, with up to 950 ppm Au and 2.5 wt.% Ag. Bulk concentrations in the scales vary between 15-60 wt.% upstream and downstream of the orifice plate and diminish from there. Iron increases up well from 8 to ~20 wt.% and decreases downstream of the orifice plate from 6 to 2 wt.% at the separation station; Cu downhole is ~3 wt.% but increases to 25 wt.% on the fluid flow control valve and then decreases; Pb downhole 100s ppm but at the wellhead is ~3 wt.%, increasing to 15 wt.% at the fluid flow control valve, then decreasing sharply from there.

published_or_final_version / Earth Sciences / Doctoral / Doctor of Philosophy

M. Tech. Metallurgical Engineering. / Aims to provide a mineralogical basis for understanding the galvanic dissolution and interaction of sulphide ores in presence of hydrogen peroxide using electrochemical technique. The research aim to achieve the following objectives: study the mineralogical characteristics of different sulphide ores ; study the sulphuric acid dissolution behaviour of the sulphide ores in the presence of hydrogen peroxide and to investigate the interaction of the mineralogy on the ores and hydrogen peroxide during dissolution.

No description available.

Downhole sampling of unboiled liquid at 1350 and 1500 m depth in the seawater-dominated Reykjanes high-temperature geothermal system in Iceland shows that metal concentrations measured at surface are minimum values due to mineral precipitation in the wells; by analogy of similar tectonic setting, host rocks and fluid composition, the metal concentrations measured in many black smoker vents at the seafloor are also minima. Fluids in the Reykjanes geothermal system react with mid-ocean ridge basalt at temperatures as high as 346°C and contain Fe 9-140 ppm, Cu 14-17 ppm, Zn 5-27 ppm, Pb 120-290 ppb, 1-6 ppb Au, and 28-107 ppb Ag. Fluids discharged at surface from the same wells have orders of magnitude lower metal concentrations due to precipitation caused by boiling and vapor loss during depressurization. Upstream of the orifice plate at high pressure (40 bar, 252°C) the precipitates consist mainly of sphalerite and chalcopyrite with a trace of galena and bornite. At the orifice plate of old wells, the pressure decreased sharply to 11 bar (188°C), resulting in abundant deposition of amorphous silica together with minor sphalerite and traces of chalcopyrite. In new wells the pressure at the orifice plate decreases to 22 bar (220°C); this pressure decrease and concomitant boiling causes deposition of fine-grained bornite-digenite solid solution together with sphalerite and galena on the fluid flow control valve. In high-pressure wells (average wellhead pressure 45-35 bar) most metals (mainly as sphalerite) are deposited downstream of the orifice plate, with up to 950 ppm Au and 2.5 wt.% Ag. Bulk concentrations in the scales vary between 15-60 wt.% upstream and downstream of the orifice plate and diminish from there. Iron increases up well from 8 to ~20 wt.% and decreases downstream of the orifice plate from 6 to 2 wt.% at the separation station; Cu downhole is ~3 wt.% but increases to 25 wt.% on the fluid flow control valve and then decreases; Pb downhole 100s ppm but at the wellhead is ~3 wt.%, increasing to 15 wt.% at the fluid flow control valve, then decreasing sharply from there.