Structural evolution of water and hydroxyl groups during thermal, mechanical and chemical treatment of high purity natural quartz

Bartłomiej A Gaweł; Anna Ulvensøen; Katarzyna Łukaszuk; Bjørnar Arstad; Astrid Marie F Muggerud; Andreas Erbe

doi:10.1039/d0ra05798c

Structural evolution of water and hydroxyl groups during thermal, mechanical and chemical treatment of high purity natural quartz

RSC Adv. 2020 Aug 5;10(48):29018-29030. doi: 10.1039/d0ra05798c. eCollection 2020 Aug 3.

Authors

Bartłomiej A Gaweł¹, Anna Ulvensøen¹, Katarzyna Łukaszuk², Bjørnar Arstad³, Astrid Marie F Muggerud², Andreas Erbe¹

Affiliations

¹ Department of Materials Science and Engineering, NTNU, Norwegian University of Science and Technology 7491 Trondheim Norway quartz-heat-treatment@the-passivists.org +47 73 594048.
² The Quartz Corp Strandveien 50 1366 Lysaker Norway.
³ SINTEF Industri Pb. 124 Blindern 0314 Oslo Norway.

Abstract

Fused silica crucibles are commonly used in the fabrication process of solar grade silicon ingots. These crucibles are manufactured from high purity natural quartz sand and as a consequence, their properties are influenced by the presence of water and hydroxyls in the raw quartz. In this work, diffuse reflectance IR, ¹H magic angle spinning NMR, and Raman spectroscopy were used to investigate the influence of thermal treatment on water and hydroxyl groups in high purity natural quartz sand. Most of the water in dry sand is present in the form of closed inclusions within the quartz grains which were detected in Raman imaging studies, even after thermally treating the samples at 600 °C. Only after heating to 900 °C did this water completely vanish, most likely as a result of rupturing of the inclusions. However, newly formed OH groups, identified as isolated and hydrogen bound OH were observed as products of the reaction between water and quartz. Similarly, liquid water was observed in NMR spectra even after treatment at 600 °C while at temperatures >900 °C, only non-interacting silanol groups were present. The comparison of the temperature dependence of the IR and NMR spectra also yields insight into the assignment of the OH stretching mode region of the IR spectrum in this system. The intensity of water related bands decreases while the intensity of OH bands first increases and then decreases with increasing temperature. The band intensity of Al-rich defects as well as the characteristic feature at 3200 cm^-1 does not follow the temperature dependence of typical water peaks. It is also shown that leaching the quartz sand in HF solution helps to remove water from inclusions, likely by forming pathways for fluid flow inside the quartz grains. Milling of the samples caused formation of an additional type of hydroxyl group, possibly due to partial amorphisation of the surfaces of the quartz grains surface during the process. The results improve the basis for a knowledge-based processes development for the processing of high purity natural quartz.