Phosphate-intercalated Ca–Fe-layered double hydroxides: Crystal structure, bonding character, and release kinetics of phosphate

The nitrate-form of Ca–Fe-layered double hydroxide (Ca–Fe-LDH) was synthesized via co-precipitation method, and its phosphate-intercalates were prepared by ion-exchange reaction. According to X-ray diffraction analysis, the Ca–Fe-LDH–NO3− compound and its H2PO4−-intercalate showed hexagonal layered structures, whereas the ion-exchange reaction with HPO42− caused a frustration of the layer ordering of LDH. Fe K-edge X-ray absorption spectroscopy clearly demonstrated that the Ca–Fe-LDH lattice with trivalent iron ions was well-maintained after the ion-exchange with HPO42− and H2PO4−. Under acidic conditions, phosphate ions were slowly released from the Ca–Fe-LDH lattice and the simultaneous release of hydroxide caused the neutralization of acidic media. Fitting analysis based on kinetic models indicated a heterogeneous diffusion process of phosphates and a distinct dependence of release rate on the charge of phosphates. This study strongly suggested that Ca–Fe-LDH is applicable as bifunctional vector for slow release of phosphate fertilizer and for the neutralization of acid soil.

Graphical abstractWe synthesized phosphate-intercalated Ca–Fe-LDH materials that can act as bifunctional inorganic vectors for the slow release of phosphate fertilizer and also the neutralization of acid soil. Fitting analysis based on kinetic models indicated a heterogeneous diffusion process of phosphates and a distinct dependence of release rate on the charge of phosphates.Figure optionsDownload full-size imageDownload as PowerPoint slideResearch Highlights► The phosphate forms of Ca–Fe-layered double hydroxide (Ca–Fe-LDH) were synthesized via co-precipitation method. The crystal structure, bonding character, and release kinetics of phosphate of the phosphate-intercalates were investigated. These Ca–Fe-LDH materials are applicable as bifunctional vector for slow release of phosphate fertilizer and for the neutralization of acid soil.