Gypsum is an economically important mineral, extensively used as the commercial construction material Plaster of Paris, with a global production of around 100 billion kilogrammes per year, researchers said.
It is a ubiquitous mineral on the Earth's surface, and is also found on the surface of Mars. Despite its importance, until now researchers have not understood how gypsum grows from ions in solutions.
The formation of gypsum, from concentrated aqueous solutions of calcium sulfate, was thought to be a simple, single-step process.
Researchers examined the process using time resolved synchrotron-based X-ray scattering at Diamond Light Source in the UK and identified and quantified each of the 4 steps of the formation process, highlighting specially that the initial moments in the reaction chain are of particular importance, because they determine the final properties of gypsum.
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In this 1st step, tiny sub-3 nanometres elongated particles form the primary building blocks (bricks). In subsequent steps these bricks aggregate, self-assemble and rearrange themselves, and finally transform to gypsum crystals.
"Since plaster is normally produced by the energy-intensive heating of gypsum, such an approach would drastically reduce the cost of production, and significantly decrease the carbon footprint of the industry," Stawsky said.
"We know that gypsum is naturally found on Mars, so applying our current finding will also help us understand and predict the hydrological conditions at the time of gypsum formation on other planets," said Liane G Benning from University of Leeds.