Abstract

Mineral carbonation is considered to be the most stable mechanism for the sequestration of CO2. This study comprises a comparative review of the effect of ball milling on the CO2 uptake of ultramafic/mafic lithologies, which are the most promising rocks for the mineralization of CO2. Samples of dunite, pyroxenite, olivine basalt and of a dolerite quarry waste material were previously subjected to ball milling to produce ultrafine powders with enhanced CO2 uptake. The optimum milling conditions were determined through selective CO2 chemisorption followed by temperature-programmed desorption (TPD) experiments, revealing that the CO2 uptake of the studied lithologies can be substantially enhanced via mechanical activation. Here, all these data are compared, demonstrating that the behavior of each rock under the effect of ball milling is predominantly controlled by the mineralogical composition of the starting rock materials. The ball-milled rock with the highest CO2 uptake is the dunite, followed by the olivine basalt, the pyroxenite and the dolerite. The increased CO2 uptake after ball milling is mainly attributed to the reduction of particle size to the nanoscale range, thus creating more adsorption sites per gram basis, as well as to the structural disordering of the constituent silicate minerals.

Highlights

  • The alleviation of the environmental impacts caused by the increasing levels of human CO2 emissions represents one of the greatest challenges of this century

  • The comparative study of the effect of ball milling on the CO2 adsorption properties of a dunite, a pyroxenite, an olivine basalt and a dolerite quarry waste material revealed the following:

  • Ball milling can be used for the development of ultrafine mafic/ultramafic powders with substantially enhanced CO2 uptake compared to the initial rock materials

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Summary

Introduction

The alleviation of the environmental impacts caused by the increasing levels of human CO2 emissions represents one of the greatest challenges of this century. The development of efficient technologies for carbon capture and storage (CCS) is crucial to alleviate the ongoing climate problem. This has stimulated research on the potential use of rocks that are abundant throughout the world for the removal of CO2 from the atmosphere [3,4,5,6]. Mineral carbonation is a CCS technology that was initially proposed by Seifritz [7], which includes the conversion of CO2 into carbonate minerals [8,9,10] It requires the participation of divalent cations (Ca, Mg and Fe) that are mostly found in ultramafic and mafic rocks.

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