Preparation and characterization of ferrous oxalate cement—A novel acid‐base cement

• Published in: Journal of the American Ceramic Society Vol. 104; no. 2; pp. 1120 - 1131
• Main Authors: Luo, Zhongqiu, Ma, Yue, He, Huan, Mu, Weihong, Zhou, Xintao, Liao, Wenyu, Ma, Hongyan
• Format: Journal Article
• Language: English
• Published: Columbus Wiley Subscription Services, Inc 01.02.2021
• Subjects: Acids; Borax; Cement; Chemical reactions; Compressive strength; Copper; copper slag; Ferrous ions; ferrous oxalate cement; Iron oxides; Oxalic acid; reaction mechanism; Reaction mechanisms; Room temperature; setting; Slag; strength
• ISSN: 0002-7820; 1551-2916
• DOI: 10.1111/jace.17511

Ferrous oxalate cement (FOC), a new type of acid‐base cement, is prepared at room temperature through reactions between iron‐rich copper slag (CS) and oxalic acid (OA). In this work, the influences of precursor proportions, including the copper slag‐to‐oxalic acid mass ratio (CS/OA), borax‐to‐cement mass ratio (B/C), and water‐to‐cement mass ratio (W/C), on the setting behavior and compressive strength of FOC paste are investigated. Furthermore, the evolutions of pH and ions concentrations are traced to understand the reaction mechanism of FOC. The results show that the compressive strength decreases with an increase in W/C; when W/C is fixed, with an increase in CS/OA, the compressive strength first increases and then decreases, giving an optimal value. The compressive strengths of specimens at 3, 7, and 28 days can reach 33, 41, and 55 MPa, respectively, under the optimal conditions (CS/OA = 3.6, B/C = 0.03, and W/C = 0.18). The setting time is also a function of W/C and CS/OA, and can be extended by adding borax. Iron oxalate hydrate (FeC2O4·2H2O) has been identified as the exclusive hydration product of FOC due to the chemical reaction between Fe2SiO4 or Fe3O4 contained in CS and OA solution. At the initial stage of reaction, OA is dissolved to release protons, HC2O4− and C2O42−, which facilitate the dissolution of Fe2SiO4 and Fe3O4 and the release of Fe2+ in the aqueous phase. Then the Fe2+ ions combine with HC2O4− and C2O42− to precipitate FeC2O4·2H2O, acting as the cementitious phase to bond the unreacted CS particles.