Previous studies have suggested that Davis tube (DT) experiment can used to study wet low intensitymagnetic separation (WLIMS) for magnetic iron ores. But DT process has never been used to mapWLIMS process, specifically in a geometallurgical framework. This thesis work is a step towardsfulfilling this gap by studying the Davis tube experiment performed on 13 different samples fromLeveäniemi iron ore deposit. The methodology adapted to map WLIMS concentrate quality includesstudy and analysis of feed, DT and WLIMS. Analyses were made using experimental data, processingdata using some analytical tools, some data-processing tools and post processing tools. For coveringthe geometallurgical aspect the analysis was done for both elements and minerals. The results fromthis study has reviled that DT can be used to predict WLIMS concentrate quality to an acceptablelevel of confidence. Furthermore, results show that a combination of DT and WLIMS informationproduce very accurate and highly reliable models for predicting and mapping WLIMS concentratequality. This work serves as the first step towards studying an unexplored field pertaining to magneticiron ore concentrate and has opened door to possible future work that could take this work a stepfurther. Supplementing this study with more data from different sample is required not only tovalidate the model but also to make it better. A better modal mineralogy of the samples is needed tounlock the full potentials of mineralogical modelling approach used in this work. / <p>I am a graduate from the of Erasmus Mundus masters in Georesource Engineering, 2017.</p> / Primary Resource Efficiency by Enhanced Prediction (PREP)

The Leveäniemi iron oxide apatite (IOA) deposit, mined by LKAB, is located in Norrbotten, northern Sweden. The deposit has a partially more complex mineralogy than the neighbouring and more famous IOA deposits of Kiirunavaara and Malmberget. The Leveäniemi deposit contains comparatively more ore containing both magnetite and hematite but also maghemite and with slightly different trace element chemistry of the iron oxide minerals. Hematite is currently not considered a valuable mineral in the Svappavaara mineral processing and in the magnetite concentrate titanium and vanadium are considered to be penalty elements. Ore samples were collected from selected drill cores and from these polished thin sections were prepared that were investigated by optical microscopy, EPMA, and FE-SEM-EDS. Investigations focused on iron oxide mineralogy and mineral chemistry with special consideration to titanium and vanadium as those elements are considered deleterious in subsequent blast furnace or direct reduction processes. Investigations revealed that magnetite is the predominant mineral with secondary hematite being the second most abundant iron oxide mineral. In the investigated samples vanadium concentration in magnetite ranges from 0.12 to 0.32% V2O3 with higher concentrations in the southern part of the deposit. No such conclusions regarding spatial distribution could be done for titanium. Furthermore, the investigations indicated that alteration from primary magnetite to secondary hematite does not significantly affect the trace element chemistry of the minerals. Titanium in iron oxides occurs as either inclusions or lamellae of titanium oxide minerals. Vanadium in iron oxides occur as a substitution element and does not occur in stochiometric vanadium minerals. It is considered unfeasible to lower the content of these deleterious elements by physical separation methods. / Leveäniemi är en järnoxid-apatitfyndighet (IOA) i Norrbotten som bryts av LKAB. Fyndigheten har en delvis mer komplex mineralogi än de närliggande och mer kända IOA-fyndigheterna Kiirunavaara och Malmberget. Leveäniemifyndigheten innehåller jämförelsevis mer malm innehållande både magnetit och hematit men även maghemit samt med något annorlunda spårämneskemi i järnoxidmineralen. Hematit anses inte i nuläget vara ett värdemineral i Svappavaaras malmförädling och i magnetitekoncentratet anses titan och vanadin utgöra straffelement. Malmprov togs från utvalda borrkärnor och från dessa tillverkades polerade tunnslip som undersöktes med optisk mikroskopering, EPMA och FE-SEM-EDS. Undersökningarna var fokuserade på järnoxidernas mineralogi och mineralkemi med speciellt fokus på titan och vanadin då grundämnena anses vara skadliga i efterföljande masugns- eller direktreduktionsprocesser. Undersökningarna visade att magnetit är det dominerade mineralet med sekundär hematit som det näst vanligaste förekommande järnoxidsmineralet. I de undersökta proven varierade vanadinhalten från 0,12% till 0,32% V2O3 med högre halter i fyndigheten södra delar. Inga liknande slutsatser angående rumsliga fördelningen av titan kunde göras. Vidare så indikerade undersökningarna att omvandling från primär magnetit till sekundär hematit inte nämnvärt påverkar spårämneskemin i mineralen. Titan i järnoxider förekommer antingen som inneslutning eller lameller av titanoxidsmineral. Vanadin i järnoxider förekommer som ett substitutionselement och förekommer inte som stökiometriska vanadinmineral. Det anses inte vara tekniskt eller ekonomiskt möjligt att sänka halterna av dessa skadliga grundämnen med hjälp av fysiska separationsmetoder.

In a particle based geometallurgical model, the behavior of the particles can be used for forecast the products and quantify the performance of the different ore types within a deposit. The particle tracking is an algorithm developed by Lamberg and Vianna 2007 whose aim is to balance the liberation data in a mineral processing circuit composed by several processing units. Currently, this tool is being developed for the HSC Chemistry software by Outotec.The objective of this study is to understand and evaluate the particle tracking algorithm in a geometallurgical test for iron ore. To achieve this objective, the liberation data is balanced in a Davis tube test circuit. A total of 13 samples from Leveäniemi iron ore were process in a Davis tube circuit.The magnetite is the main mineral in the Leveäniemi iron ore samples. Its high recovery in the Davis tube circuit along with the V, Ti and Mn suggest that these elements are present in the magnetite lattice. These penalty elements in the iron concentrates cannot be avoided at the stage of mineral concentrations.The washing effect of the Davis tubes controlled by the rotational and longitudinal agitation of the tube perturb the particles agglomeration between the pole tips of the electromagnet. A higher agitation frequency and amplitude will wash away most of the gangue minerals and also fine grained magnetite.In this work, the particle tracking is depicted and implemented in a magnetic separation circuit for high liberated material. The liberation data was balanced in a way that the particle classes can be followed through circuit and their recoveries can be calculated. Nevertheless, the algorithm requires further validation and analysis of its limitations in terms of resolution and reproducibility.