Abstract

Portland cement is the most common type of cement and one of the most important ingredients in concrete. Concrete, on the other hand, is the most used building material worldwide just behind the water with an increasing usage trend in infrastructure for the upcoming years. During the production process of cement, massive CO2 emissions are released into the environment, while large amounts of raw materials and energy are consumed. In the present study, Portland type cement was prepared in laboratory-scale by Greek Wet Fly Ash and Mill Scales, as well as conventional raw materials such as limestone, shale and lava. The experiments were conducted at 1450 °C and 1340 °C. The fired compositions were characterized by XRD, Q–XRD, optical microscopy, SEM/EDS and the concrete specimens were tested for their compressive strength. The results indicated that formation of cement clinker at lower temperatures (1340 °C) is feasible with the combined use of natural raw materials and industrial byproducts following the standard production route of cement industries. Finally, the so-obtained cement presented compressive strength values comparable to the conventional ones fired at 1450 °C.

Highlights

  • Cement is a basic building material, with a global production of 4.1 Gt/year (2020 world production) [1]

  • The cements produced in this study do not require changes in the existing production route of industries

  • The use of Portland cement has been established worldwide and there is no need to re-integrate the product into the market

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Summary

Introduction

Cement is a basic building material, with a global production of 4.1 Gt/year (2020 world production) [1]. Cement production requires raw materials rich in the oxides CaO, SiO2 , Al2 O3 and Fe2 O3. Their common abbreviations, in industry and research of cement, is C, S, A and F respectively [2–4]. In order to produce Portland cement, raw materials rich in these oxides are mixed and fired at temperatures usually up to 1450 ◦ C. The clinker of Portland cement consists mainly of 4 basic mineralogical phases; tricalcium silicate or alite (C3 S), dicalcium silicate or belite (C2 S), Tetracalcium aluminoferrite or ferrite (C4 AF) and tricalcium aluminate or celite (C3 A) [3,4]

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