Abstract

This study assessed the possibility of using polymethylhydrosiloxane (PMHS)-treated fly ash cenospheres (FCS) for formulating a thermally insulating and thermal shock (TS)-resistant cementitious blend with calcium aluminate cement. To prevent FCS degradation in an alkaline cement environment at high temperatures, the cenospheres were pre-treated with sodium metasilicate to form silanol and aluminol groups on their surface. These groups participated in a dehydrogenation reaction with the functional ≡Si–H groups within PMHS with the formation of siloxane oxygen-linked M-FCS (M: Al or Si). At high hydrothermal temperatures of 175 and 250 °C, some Si–O–Si and SiCH3 bonds ruptured, causing depolymerization of the polymer at the FCS surface and hydroxylation of the raptured sites with the formation of silanol groups. Repolymerization through self-condensation between the silanol groups followed, resulting in the transformation of siloxane to low crosslinked silicon-like polymer as a repolymerization-induced product (RIP) without carbon. The RIP provided adequate protection of FCS from pozzolanic reactions (PR), which was confirmed by the decline in zeolites as the products of PR of FCS. Cements with PMHS-treated FCS withstood both hydrothermal and thermal temperature of 250 °C in TS tests, and they also showed improved compressive strength, toughness, and water repellency as well as decreased thermal conductivity. The lubricating properties of PMHS increased the fluidity of lightweight slurries.

Highlights

  • To identify the reaction products and establish mechanisms of the reactions at three different hydrothermal temperatures, we studied the following systems: fly ash cenospheres (FCS)/SMS, PMHS/SMS, and PMHS/FCS/SMS

  • The pattern of the FCS-SMS cured at 85 ◦ C was identical to that of FCS, suggesting that no crystalline reaction products formed at that temperature

  • The two major crystalline compounds of FCS were mullite (3Al2O32SiO2) and quartz (SiO29).ofThe pattern of the FCS-SMS cured at 85 °C was identical to that of FCS, suggesting that no crystalline reaction products formed at that temperature

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Summary

Introduction

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. The use of generating or storage geothermal systems for stabilizing the electric grid, increasing its flexibility, and providing energy on demand presents a possibility of flexible and renewable energy generation and storage. The geothermal environments of storage reservoirs can range from rock and sand formations to hot confined aquifers over the bedrock heated by magma. For a robust long-term performance, the geothermal reservoir must be able to withstand repeated thermal stresses during the injection and production of heated fluids. Since the most economical heat-recovery systems require high-temperature carrier fluids, the thermal shocks may be significant.

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