화학공학소재연구정보센터
Inorganic Chemistry, Vol.60, No.1, 195-205, 2021
Characterization of and Structural Insight into Struvite-K, MgKPO4 center dot 6H(2)O, an Analogue of Struvite
Struvite-K (MgKPO4 center dot 6H(2)O) is a magnesium potassium phosphate mineral with naturally cementitious properties, which is finding increasing usage as an inorganic cement for niche applications including nuclear waste management and rapid road repair. Struvite-K is also of interest in sustainable phosphate recovery from wastewater and, as such, a detailed knowledge of the crystal chemistry and high-temperature behavior is required to support further laboratory investigations and industrial applications. In this study, the local chemical environments of synthetic struvite-K were investigated using high-field solid-state Mg-25 and K-39 MAS NMR techniques, alongside P-31 MAS NMR and thermal analysis. A single resonance was present in each of the Mg-25 and K-39 MAS NMR spectra, reported here for the first time alongside the experimental and calculated isotropic chemical shifts, which were comparable to the available data for isostructural struvite (MgNH4PO4 center dot 6H(2)O). An in situ high-temperature XRD analysis of struvite-K revealed the presence of a crystalline-amorphous-crystalline transition that occurred between 30 and 350 degrees C, following the single dehydration step of struvite-K. Between 50 and 300 degrees C, struvite-K dehydration yielded a transient disordered (amorphous) phase identified here for the first time, denoted delta-MgKPO4. At 350 degrees C, recrystallization was observed, yielding beta-MgKPO4, commensurate with an endothermic DTA event. A subsequent phase transition to gamma-MgKPO4 was observed on further heating, which reversed on cooling, resulting in the alpha-MgKPO 4 structure stabilized at room temperature. This behavior was dissimilar from that of struvite exposed to high temperature, where NH4 liberation occurs at temperatures >50 degrees C, indicating that struvite-K could potentially withstand high temperatures via a transition to MgKPO4.