Abstract

Phosphogypsum (CaSO4·2H2O) waste is produced in large amounts during phosphoric acid (H3PO4) production. Minor quantities are utilized in construction or agriculture, while most of the material is stockpiled, creating an environmental challenge to prevent pollution of natural waters. In principle, the gypsum waste could be used to capture several hundred Mt of carbon dioxide (CO2). For example, when gypsum is converted to ammonium sulfate ((NH4)2SO4) with ammonia (NH3) and CO2, also solid calcium carbonate (CaCO3) is generated. The ammonium sulfate can be utilized as a fertilizer or in other mineral carbonation processes that use magnesium silicate-based rock as feedstock, while calcium carbonate has various uses as e.g. filler material. The reaction extent of the described process was studied by thermodynamic modeling and experimentally as a function of reactant concentrations and temperature. Other essential properties such as purity and quality of the solid products are also followed. Conversion efficiencies of >95% calcium from phosphogypsum to calcium carbonate are obtained. Scalenohedral, rhombohedral and prismatic calcite particles can be produced, though the precipitates contain certain contaminants such as rare earth metals and sulfur from the gypsum. A reverse osmosis membrane cartridge is also tested as an alternative and energy-efficient method of concentrating the ammonium sulfate salt solution instead of the traditional evaporation of the process solution.

Highlights

  • Phosphogypsum (PG) is a waste material generated during production of phosphoric acid (H3PO4) from phosphate rock rich in apatite [Ca5(PO4)3OH] via reaction with sulfuric acid (H2SO4)

  • Long-term stockpiling causes a risk of pollution to natural waters primarily in form of increased eutrophication and is, not a preferred, Mineral Carbonation of Phosphogypsum Waste

  • This paper studies the production of AS and CC salts using both theoretical modeling and laboratory-scale experiments

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Summary

Introduction

Phosphogypsum (PG) is a waste material generated during production of phosphoric acid (H3PO4) from phosphate rock rich in apatite [Ca5(PO4)3OH] via reaction with sulfuric acid (H2SO4). PG consists primarily of calcium sulfate dihydrate, CaSO4·2H2O (Table 1). 100–280 Mt/year PG is produced, 85% of which is stockpiled for long-term storage without further treatment (Choura et al, 2012). Depending on the origin of the apatite rock, PG may be slightly radioactive, or it may, for instance, contain some rare earth metals. Together with the huge amount produced, these contaminants often hinder efficient utilization of PG in construction and other industrial applications. Long-term stockpiling causes a risk of pollution to natural waters primarily in form of increased eutrophication and is, not a preferred, Mineral Carbonation of Phosphogypsum Waste

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