4.7 Article

Experimental demonstration of comminution with transcritical carbon dioxide cycles

期刊

POWDER TECHNOLOGY
卷 407, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.powtec.2022.117615

关键词

Comminution; Supercritical CO2; Transcritical fluids; Limestone; CO2 recycling

资金

  1. Natural Resources Canada under the Impact Canada Crush It! Challenge [IMPACT-34]
  2. NRCan through the Impact Canada Clean Tech Stream
  3. Mitacs [IT17574]

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A new comminution technology using transcritical CO2 cycles is presented, showing potential for reducing energy consumption in rock grinding. Lab-scale experiments with limestone demonstrate the effectiveness of this method in breaking down rocks and generating finer particles.
A new comminution technology that can reduce energy consumption when compared to traditional grinding of rock is presented. The process is based on pulverization driven by transcritical CO2 cycles, resulting in tensile fracture inside the particle rather than compression from outside. Tensile strength of many rocks is approximately 10 times lower compared to compressive strength offering significant potential for saving energy. In this apparatus, comminution can occur over multiple cycles to enhance rock breakage without extracting and refeeding rock between cycles. The test rig depicts test conditions to capture and to recycle the CO2. Limestone is utilized as an example material in a lab-scale experimental apparatus. Within the apparatus, the temperature and pressure are raised to supercritical conditions. A rapid release of the CO2 into a decompression chamber results in an expansion of supercritical CO2 inside the pores and fractures rock from tension instead of compression. Results show a significant fraction of the limestone is comminuted in three consecutive CO2 pressure cycles. A majority of the resulting particles exhibit larger fragments from 5 mm to 13.2 mm. 6.2% of the feed material was directly transferred to fine material <300 mu m without many intermediate progeny particles. Initial results indicate a larger ratio of the pressure before and after burst, and longer soak times aid pulverization. A single rock is also analyzed, where it is noted that breakage occurs along visible fractures, and this behavior is noted over consecutive cycles.

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