Magnesia‐phosphate cement mortars, based on magnesia and ammonium dihydrogen orthophosphate, were prepared with water contents (measured as a weight fraction of the dry material) in the range 5% to 12%. It was shown by XRD that the major reaction product was magnesium ammonium phosphate hexahydrate (MgNH 4 PO 4 6H 2 O), also known as the mineral struvite. Evidence was also found to suggest the presence of an amorphous or poorly crystalline phase with a lower degree of hydration in materials prepared with water contents less than 8%. For higher water contents, the excess water gradually evaporated during aging to leave an interconnected fine porous structure which exhibited poor mechanical properties. An increase in the water content from 5% to 12% also led to a significant increase in the crystallite size, from around 0.5 µm to 10 µm.
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Hall et al. (1998) studied this question.
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