Phosphate mineral slurry is a mixture of dry phosphate and water. It is the raw material to be exploited to produce fertilizers and phosphoric acid. The phosphate slurry is processed to produce phosphorus (P), which is one of the three main nutrients most used in fertilizers (the other two are nitrogen and potassium), and the most important macronutrients essential for the growth and development of a plant. It is a building block of deoxyribonucleic acid (DNA) and ribonucleic acid (RNA) in plant cells and is responsible for energy storage and transfer. Plants acquire all their P from fertilizers in the soil (Holford 1997).
The quality of the phosphate slurry is checked regularly in the laboratory during all the treatment processes using conventional analytical methods (Gaft et al. 2007). These methods are expensive, time-consuming and generate hazardous waste. An online X-ray fluorescence technique (XRF) analysis system could overcome these drawbacks and allow a rapid chemical analysis of the phosphate slurry. A few studies have demonstrated the potential of the XRF technique to analyze dry phosphate rock (Issahary and Pelly 1982; Addas et al. 1995; Safi et al. 2006; Hasikova et al. 2014). However, there is a lack of information on the analysis of phosphate slurry using the XRF technique.
This article will explore some challenges of analyzing phosphate slurry using the XRF technique. These challenges are related to the physical parameters of the slurry, namely particle size and water content. These parameters affect the accuracy of XRF measurements and more specifically in the case of slurry. Indeed, analyzing the slurry is a challenging process compared to solids analysis, one of these challenges is the absorption of X-rays by the water.
XRF is a rapid technique for quality control of mineral samples (Rose et al. 1986). The time required to analyze a sample can be reduced from hours (in the case of conventional analysis methods) to minutes (in the case of XRF) (Perring and Andrey 2003). Like many other techniques, XRF has some limitations regarding the analysis of light elements (Al-Eshaikh et al. 2016). In the case of phosphate slurry, the particle size of the sample and the water content may affect the accuracy of the XRF measurements. (Melquiades et al. 2011; Kalnicky and Singhvi 2001; Laperche 2005; Clark et al. 1999; Ge et al. 2005; Kido et al. 2006; Tjallingii et al. 2007; Parsons et al. 2013; Weindorf et al. 2014). When analyzing samples with different particle size distribution and light elements or having analytes with long-wave characteristic lines (e.g., Si, Al), peak intensities can be attenuated by 30% (Mzyk et al. 2002). F. Demir et al. (2008) studied the effect of particle size distribution on XRF measurements of cement samples with different grain sizes. The results show a difference between the maximum intensities of the \({K}_{\alpha }\) peaks which can reach 17%, depending on the particle size of the sample analyzed. In another study, samples of different grain sizes extracted from the Nile River in Egypt were analyzed with the XRF technique. The results show that the XRF intensities of \({K}_{\alpha }\) radiation can increase or decrease when decreasing grain size and depending on the atomic number of the analyte. For small particle size samples, the characteristic radiation penetration depth increases, and therefore the probability of the particle size effect on the characteristic radiation decreases (Shaltout et al. 2011). Presence of water in a slurry and its capability to absorb x-ray could affect the accuracy of the XRF measurements as well, and can also causes diffusion of primary radiation from excitation sources, resulting in a decrease of the intensity of the characteristic X-rays and an increase of the intensity of the X-rays scattered in the fluorescence spectrum (Ge et al. 2005). Three certified reference materials with different water contents were analyzed with the XRF technique. The measurements show that the elements identified by the \({L}_{\alpha }\) spectral line with the highest Z atomic number were more affected by the water content than the elements identified by the \({K}_{\alpha }\) line with the lowest Z. Ti, Cr and Fe were not significantly influenced by water content, while the Sr was the most affected (Santana et al. 2019). In some cases, the influence of water can be corrected by calculating the attenuation coefficients for each measured element (Schneider et al. 2016).
The work presented in this article is part of a project to develop an online XRF analyzer to control the quality of phosphate slurry directly on the production line. Particle size and water content are parameters that can adversely affect XRF measurements. Several studies have addressed the effect of these two parameters in the case of XRF analysis of other materials. However, the case of XRF analysis of phosphate slurry has not been reported in the literature, mainly because of the following parameters such as the specific chemical composition, mineralogical structure and other characteristics of the sample being analyzed. In this study, we investigate the effect of these two parameters for the analysis of phosphate slurry with XRF. We analyzed 07 samples of phosphate slurry with different particle sizes (from 106 µm to 425 µm) and 16 samples with different water content ranging from 30–60%. Based on the obtained data, we will propose new formulas to correct the concentration considering the particle size distribution and water content. Also, solutions are envisaged in the future to obtain these data in real-time with a view to implementing an XRF online analyzer system for phosphate slurry.