A thesis submitted for the degree of Doctor of Philosophy in the Faculty of Science at the University of the Witwatersrand. / The present thesis is divided into three parts. The study described in Part I arose out of a request by the Chamber of Mines Mining Research Laboratory to the National Institute for Metallurgy to undertake a preliminary study of whether it would be feasible, in Witwatersrand conglomerates, to carry out rapid delimitation of areas rich in gold and/or uranium at the rock face, a procedure which would permit areas of rich ore to be removed selectively by means of the "rock-cutter". The approach adopted in this study was essentially geochemical, while conventional mineralogical techniques (macro-auto radiographs , thin section and polished section analyses) provided a control. The samples were drawn from the Vaal Reef at Hartebeestfontein and Zandpan and from the Ventersdorp Contact Reef at Venterspost, and were analysed quantitatively for gold, silver, uranium, pyrite, muscovite, pyrophyllite, chlorite, quartz, iron, potassium, nickel, titanium, zirconium and chromium. The intensity of the interrelationships between the elements and minerals analysed for was examined statistically by means of correlation covariance and factor analysis programmes written for an IBM 360/50 digital computer. A sympathetic relationship -- defined as significant positive correlation (with a correlation coefficient r> 0. 7) -- was found to exist between gold and uranium in both the Vaal Reef and Ventersdorp Contact Reef samples. These findings suggest that gold and uranium can be removed Simultaneously by means of the rock-cutter, and that radioactivity can be used as an indicator for on-site delimitation of areas rich in gold. In the course of the study described in Part I, it became evident that little detailed mineralogical work had ever been done on the phyllosilicates occurring in the Witwatersrand System. Accordingly, certain phyllosilicates from Witwatersrand conglomerate bands and other sources were examined in detail, this study being described in Part II of the present thesis. This study called for detailed chemical, optical, X-ray crystallographic, infra-red, differential thermal and thermogravimetric analyses, the results of which are presented. The findings were examined in the light of variolls classification schemes that have bep proposed for the phyllosilicates. This investigation revealed the need for a universally acceptable system of classification for the phyllosilicates, which should preferably be drawn up under the auspices of the International Mineralogical Association to avoid the confusion that exists at present. Part III of the present thesis is devoted to a discussion and description of various analytical techniques that had to be modified or developed to meet th8 requirements of the studies described in Parts I and II. The techniques described include: (1) An X-ray diffraction method which was developed for the quantitative analysis of pyrite, muscovite, pyrophyllite, chlorite and quartz in crushed ore from Witwatersrand conglomerates. This method makes use of novacul iie as an external standard and of binary mixtures as analytical standards, and had a mean absolute error of 1. 1 %. This method may be expanded to permit analysis of an n-component mixture. (2) A whole rock pressed powder technique of X-ray fluorescence analysis which was used for the quantitative determination of iron, potassium, nickel, titanium, zirconium and chromium. This method makes use of internstional rock standards as external standards. Six computer programmes used for the computation of the analytical results and in the statistical and crystallographic calculations are also presented in Part III. / AC2017

The relationship between soil properties and micromorphological features was studied in six Alfisol and six Spodosol profiles from Southern Ontario. The total porosity of the soil material was largely related to the size, shape and conformation of the soil voids in thin sections, while the differential development of plasma fabric could be used to discern a sequence of degrees of weathering which was also expressed by various mineralogical and physico-chemical indices. The relative proportions of soil constituents in thin sections was successfully used to indicate the existing textural discontinuities in five of the profiles studied. The elementary structure of soil thin sections is considered the most important micromorphological feature in the investigation of the degree of B horizon development in both Alfisol and Spodosol profiles. / Thesis / Doctor of Philosophy (PhD)

Η επεξεργασία των νικελιούχων λατεριτικών μεταλλευμάτων της χώρας μας για την παραγωγή σιδηρονικέλιου στη Λάρυμνα συνοδεύεται με την εκπομπή 200000t/y λεπτομερούς σκόνης που συλλέγεται στα συστήματα αντιρρύπανσης των περιστροφικών κάμινων (Π/Κ), μέσης περιεκτικότητας 1.2-1.5% σε Ni και 4-5% σε C. Η διατριβή αυτή συνέβαλε στην ανάπτυξη μεθόδου ανακύκλωσης της σκόνης αυτής με απευθείας αναγωγική της τήξη σε ηλεκτρική κάμινο συννεχούς ρεύματος (DC-HEP) με εμφυσησή της μέσω του κεντρικού διάτρητου γραφιτικού ηλκετρόδιου. Την προκαταρκτική θεωρητική διερεύνηση και τις εργαστηριακές προδοκιμές ακολούθησαν βιομηχανικές δοκιμές στην κάμινο 125t DC-HEP στη χαλυβουργία Georgsmarienhutte της Γερμανίας, όπου έλαβε χώρα τήξη 70t σκόνης και 2.5t φιλομερούς μεταλλεύματος.Η ανάκτηση Ni ήταν πολύ υψηλή 93-99%. Παρήχθησαν χάλυβες χαμηλής κραμάτωσης σε σε Ni καθώς και ποικίλοι τύποι σκωρίας προς διερεύνηση της χρήσης τους στην παραγωγή σύνθετων τσιμέντων Portland και σκωριωτσιμέντων. Πραγματοποιήθηκε μεταλλουργική αξιολόγηση των δοκιμών και αναπτύχθηκε μοντέλο προσομοίωσης της αναγωγικής τήξης της σκόνης. / The tratment of the laterite nickel ferrous ores in Hellas for the production of ferronickel at Larymna is associated with the emission of 200000t/y of fine dust collected in the gas cleaning systems of the rotary kilns (R/Ks), with 1.2-1.5% and 4-5% . Average Ni and C contents respectively . This thesis contributed to the development of a method for the recycling of this dust by means of its direct reduction smelting in a DC-HEP furnace (Direct Current-Hollow Electrode Powder) by its injection through the central hollow graphite electrode. The preliminary theoretical study and the laboratory trials were followed by industrial heat campaigns in the 12st DC-HEP furnace at georgsmarienhutte steelwork in Germany, where around 70t of dust and 2.5t of ore fines were smelted. The Ni-recovery was very high 93-99.9%. Low Nickel alloyed steel grades were produced and various slag types for the investigation of their utilization for the production of composite-portland cements and slag cements. The metallurgical evaluation of the trials was performed and model for the dust reduction smelting process was developed.