What is the porosity of CaO

The porosity of calcium oxide (CaO) varies significantly depending on its production method, calcination temperature, and source material, but typically ranges from 30% to 60% for quicklime produced from limestone. Porosity refers to the volume fraction of void spaces within the material—essentially how much empty space exists between the solid particles. CaO produced at higher calcination temperatures (around 1000-1100°C) tends to have lower porosity and larger pore sizes, while CaO calcined at lower temperatures (around 800-900°C) generally has higher porosity with smaller, more numerous pores.

This porosity is critically important for CaO's reactivity and applications, as it directly affects the material's surface area and how readily it can react with water or other substances. Higher porosity means more surface area is available for chemical reactions, making the quicklime more reactive in slaking processes and more effective in applications like flue gas desulfurization. The pore structure also influences how quickly water can penetrate the CaO particles during hydration, affecting the rate and controllability of the exothermic reaction. In practical terms, highly porous quicklime will react more vigorously and completely with water compared to dense, low-porosity material. The porosity develops during calcination when CO2 gas is driven off from calcium carbonate, leaving behind a network of interconnected voids in the resulting CaO structure—essentially creating a solid foam-like internal architecture that makes quicklime much less dense than the original limestone.