Understanding the effects of the process parameters on the distribution behaviour of antimony between metal and slag in the iron blast furnace is critical to develop a universal method of controlling temper embrittlement in commercially pure low alloy steels.

The present study was aimed at developing a new inexpensive and accurate analytical method for determining the glass content of slag and fly ash. Infrared absorption spectroscopy using an internal standard proved to be the method of choice. Both synthetic and commercial slags and fly ashes were investigated.

Under high irradiation, a fourth state of matter named plasma can be obtained. Plasmas emit electromagnetic radiation that can be recorded in the form of spectra for spectroscopic elemental analysis. With the advent of lasers in the 1960s, spectroscopists realized that lasers could be used simultaneously as a source of energy and excitation to create plasmas. The use of a laser to ignite a plasma subsequently led to laser-induced breakdown spectroscopy (LIBS), an optical emission spectroscopy capable of analyzing samples in various states (solids, liquids, gases) with minimal sample preparation, rapid feedback, and endowed with in situ capability. In this dissertation, studies of LIBS for multi-elemental analysis and geological applications are reported. LIBS was applied to cosmetic powders for elemental analysis, screening and classification based on the raw material used. Principal component analysis (PCA) and internal standardization were used. The intensity ratios of Mg/Si and Fe/Si observed in talcum powder show that these two ratios could be used as indicators of the potential presence of asbestos. The feasibility of LIBS for the analysis of gasification slags was investigated and results compared with those of inductively-coupled plasma−optical emission spectrometry (ICP-OES). The limits of detection for Al, Ca, Fe, Si and V were determined. The matrix effect was studied using an internal standard and PLS-R. Apart from V, prediction results were closed to those of ICP-OES with accuracy within 10%. Elemental characterization of outcrop geological samples from the Marcellus Shale Formation was also carried out. The matrix effect was substantially reduced. The limits of detection obtained for Si, Al, Ti, Mg, Ca and C were determined. The relative errors of LIBS measurements are in the range of 1.7 to 12.6%. Gate delay and laser pulse energy, have been investigated in view of quantitative analysis of variation of trace elements in a high-pressure environment. Optimization of these parameters permits obtaining underwater plasma emission of calcium with quantitative results on the order of 30 ppm within a certain limit of increased pressure. Monitoring the variation of the trace elements can predict changes in the chemical composition in carbon sequestration reservoir.

The topic of osmund iron is of great interest in both historical and metallurgical perspective. Between the 14th and the 17th century osmund iron was exported extensively from Sweden but it has been difficult to characterize and confirm what exactly osmund iron is. Further research should be conducted to improve the understanding of this kind of iron.   This work is primarily focused on medieval osmund iron. It is trying to determine what can be stated about their production methods and how to identify osmund pieces. A literature review was performed, to present an overview of iron production methods in medieval Europe. A metallurgical analysis was conducted on a number of osmund samples from the polish shipwreck ‘Miedsiowiec’, W5., together with samples from bar irons and iron billets from the same ship. Analysis was performed using LOM and SEM with EDS, analysing the crystallographic structure of the samples, and performing slag analysis using EDS to establish statistical trends. One of the aims was to evaluate a previously suggested hypothesis, namely that osmunds were shipped to Danzig from Stockholm, and then refined into iron bars and billets.  The studied iron bars and billets were purely ferritic with some slag inclusions. By looking at the shape of the slag inclusions, it can be stated that the bars and billets were forged differently from the osmund pieces. The osmunds were found to be made by indirect reduction as seen by the prevalence of cementite. It could not be confirmed if the bars and billets were forged by osmunds.  The osmunds showed different trace element compositions, than the iron bars and billets. The microstructure of all the osmunds varies greatly, which was to be expected. The osmunds had a higher carbon content and fewer slag inclusions. The hypothesis that osmunds were refined into iron bars and billets is not supported by the findings of this study. / Osmundjärn är av stort arkeometallurgiskt intresse, som en svensk exportvara som exporterades mellan 1300- och 1600-talet. Det är dock svårt att definitivt avgöra vad osmundjärn är för något. Det krävs därför ytterligare analyser och studier inom detta område för att förbättra vår förståelse av osmundjärn.   Denna studie behandlar upphittade medeltida osmundjärn och stångjärn i syfte att avgöra hur dessa har tillverkats. En litteraturstudie genomfördes som omfattande medeltida järntillverkningsprocesser, den existerande forskningen om osmundjärn samt relevanta forskningsmetoder. Järnproverna som erhölls kommer från den polska skeppsvraket ’Miedsiowiec’, W5. Mikrostrukturen av proverna analyserades med ljusmikroskop och en SEM-EDS analys utfördes. En föregående publicering om osmundar har föreslagit att osmundar exporterades från Stockholm till Gdansk, där de välldes och bearbetades till stångjärn. Osmundarna och stångjärnen som erhölls undersöktes också för att korrektheten i denna hypotes. Stångjärnens mikrostrukturer var ferritiska med ett flertal inneslutningar. Två av de så kallade iron billets hade anisotropiskt formad slagg, jämfört med de så kallade iron bars som hade isotropiskt format slagg. Det bedömdes att osmundarna var tillverkade i en masugn, på grund av perliten som hittades i mikrostrukturen i samtliga osmundar. Mikrostrukturen i alla osmundar varierade dock kraftigt, som väntat. Osmundarna hade också högre kolhalt, och färre slaggpartiklar. Hypotesen om att osmundar bearbetades till stångjärn stöds därför inte av resultaten som hittats i denna studie.