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Abstract

Struvite (NH4MgPO4·6H2O) is a mineral often found in urinary tracts and kidneys. Thermal decomposition using slow low heating shows that the 'kidney' stone can be decomposed at temperatures below 40°C. At this temperature both ammonia and water are evolved. If more rapid heating is employed the decomposition occurs at around 80°C. The implication of this work rests with the use of low slow heat for the decomposition of the kidney stones.

phosphate - hot stage Raman spectroscopy - infrared emission spectroscopy - high resolution thermogravimetric analysis - kidney stones - struvite

This revised version was published online in July 2006 with corrections to the Cover Date.

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