Dissolution and carbonation of mechanically activated olivine-Investigating CO2 sequestration possibilities

• Main Author: Haug, Tove Anette
• Format: Dissertation
• Language: English
• Subjects: carbonation; CO2 sequestration; CO2 storage; dissolution; geochemistry; mechanical activation; milling; Mineral processing; olivine

Mineral carbonation used for CO2 sequestration faces three main challenges: increasing the overall carbonation rate, handle large amounts of feedstock and products, and developing a practical process with commercially acceptable energy consumption. High intensity milling, also called mechanical activation, has been found to increase the extraction rate of metals in the metallurgical industry. The focus of this PhD study has been the use of mechanical activation as a pre-treatment method within mineral carbonation as applied to CO2 sequestration. Olivine was chosen due to the availability of this mineral in Norway. Experiments were conducted to determine how mechanical activation changed the specific surface area, particle size distribution and the crystallinity; and to explore how milling conditions and material characteristics were correlated with increased dissolution rates and increased extent of carbonation. A planetary mill was used in all experiments in addition to a laboratory ball mill, a pilot scale Hicom mill and a pilot scale Szegvari attritor when mechanical activation was evaluated for implementation within mineral carbonation. Finally the energy consumption during milling was evaluated in the context of CO2 sequestration. Over 60 olivine samples were prepared by milling including duplicates. Two dissolution experiments were performed, one at room conditions with 0.01 M HCl and one at 128 °C and 150 bar of CO2. The specific dissolution rates of mechanically activated samples increased up to three orders of magnitude compared to an unactivated reference sample. Crystallinity as calculated from X-ray diffractograms was the material parameter with the best correlation with the measured dissolution rates. Specific surface area was only correlated to dissolution rates for samples with relatively high crystallinity. The particle size distribution was not correlated with the measured dissolution rates. Neither the dissolution rates nor the material characteristics were directly correlated with the extent of carbonation observed in the direct carbonation experiments at 185 °C and 115 bar of CO2. The dissolution rates and crystallinity were partially correlated with the extent of carbonation obtained in the direct IV carbonation experiments performed at 128 °C and 150 bar of CO2. The interpretation was that in the 185 °C and 115 bar experiments, the extent of carbonation was mainly limited by precipitation kinetics of magnesite and silica, and was prob