Abstract

Lead hydrogen arsenate PbHAsO4 and lead hydrogen phosphate PbHPO4, which can form a continuous solid solution series, have been extensively studied owing to their ferroelectric properties. PbHAsO4 has also been found to occur in weathered As- and Pb-rich outcrops and historically contaminated soils as a schultenite mineral. Although most ferroelectric studies were of substantial interest more than 30 years ago, the contamination of the Earth’s surface with toxic Pb and As remains a major concern for environmentalists. In this study, six compounds of PbHAsO4–PbHPO4 solid solution series were synthesized from aqueous solutions at ambient conditions. They were subsequently analyzed using Raman and Fourier transform infrared spectroscopy to describe their vibrational characteristics, which should help identify the series members in natural or synthetic samples in further environmental and mineralogical studies. Additionally, powder X-ray diffraction analyses were conducted to investigate the variations in the unit cell parameters along the series. The results showed linear variations in the band positions in both Raman and infrared spectra, which depend on the extent of the isomorphic substitution of (PO4)3− for (AsO4)3−. However, the bands become broader or split as a result of phosphate substitution, making it difficult to correlate the band positions with the molecular composition of an unknown phase. The X-ray diffraction data revealed linear variations of all lattice constants as a function of P. Moreover, a relevant finding of this study is the systematic deviation in the chemical compositions of the synthetic phases from the composition of aqueous solutions from which they precipitated, caused by the preferential incorporation of (AsO4)3− with respect to (PO4)3− into the structure.

Highlights

  • Lead hydrogen arsenate PbHAsO4 and its phosphate analog PbHPO4 have been extensively studied owing to their ferroelectric properties [1,2,3,4,5,6,7,8,9,10,11,12,13,14]

  • Detailed studies of the ferroelectricity of PbHAsO4 and PbHPO4 have revealed that both phases crystallize in the monoclinic crystal system [15,16,17,18,19,20,21,22,23,24,25,26]

  • Schultenite PbHAsO4 and “phosphoschultenite” PbHPO4 can form a continuous solid solution series. The results of this experi­ mental work showed that the composition of the crystallizing phases differed from that of the solutions from which the phases precipitated with preferential incorporation of (AsO4)3– with respect to (PO4)3– into the structure

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Summary

Introduction

Lead hydrogen arsenate PbHAsO4 and its phosphate analog PbHPO4 have been extensively studied owing to their ferroelectric properties [1,2,3,4,5,6,7,8,9,10,11,12,13,14]. Experimental studies have shown that both phases can form a continuous solid solution series [27,28]. Lead hydrogen arsenate has been found in Earth’s surface environments as a schultenite mineral [29,30,31,32]. The first natural occurrence of the phosphate analog of schultenite was reported in the Clara mine, central Black Forest, Ger­ many, in 2006 [35]. We refer to PbHPO4 as “phosphoschultenite”, which was first proposed by Młynarska et al [28]

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