Abstract

Potassium-bearing framework aluminosilicates are earth-abundant and globally available raw materials that are potential sources of potassium or aluminium. The physical chemistry of aqueous alteration of the corresponding minerals is discussed in this work, in the framework of green chemistry and engineering.

Highlights

  • Inorganic fertilizers are essential for crop production, in particular to supply nutrients such as nitrogen, phosphorus, and potassium

  • Aqueous alteration of potassium-bearing aluminosilicate minerals has been proposed as an alternative to both traditional K-fertilization and alumina production

  • This work discusses the mechanism of aqueous alteration of aluminosilicate minerals, and the chemical processes that have been proposed to date

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Summary

Introduction

Inorganic fertilizers are essential for crop production, in particular to supply nutrients such as nitrogen, phosphorus, and potassium. Al2O3 content in bauxites varies from 30 to 60 wt% and more than 85% of its global production (89 million tons in 2010) is consumed to produce aluminium, a commodity market in constant growth.[12] The current production of alumina from bauxite is through the Bayer process, which exhibits notoriously high energy and chemical consumption, along with the generation of a large amount of waste of ecological concern (e.g., “red mud”).[13] For products such as potash and alumina the transition from a conventional to a new mineral source, in particular of lower grades, is rarely economically and ecologically acceptable using traditional extraction technologies.

K-bearing tectosilicates as earth-abundant raw materials
Far-from-equilibrium dissolution in aqueous fluids
Mineral alteration in soil environment for agricultural application
Hydrothermal processing of K-bearing silicates
Classification and scope of processing schemes
Findings
Perspectives
Full Text
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