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The mechanism of enhancement/inhibition of quartz toxicity induced by iron is still unclear. Here the amount of iron on a fibrogenic quartz (Qz) was increased by wet impregnation (Fe(NO3)30.67 and 6.7 wt %). X-ray diffraction (XRD), XRF diffuse reflectance, UV−vis, and infrared (IR) spectroscopies revealed dispersed ferric ions, and hematite aggregates at the higher loading. Surface features relevant to pathogenicity and cell responses were compared not only to the original quartz but also to reference quartz DQ12. Surface charge (ζ-potential) was more negative on the original and low-loaded specimen than on the high-loaded one. DQ12 had a less negative ζ-potential than Qz, ascribed to the absence of aluminium present in Qz (1.7 wt %). All quartz specimens were able to generate HO•radicals, iron-loaded samples being more reactive than original quartz. Iron deposition inhibited the rupture of a C−H bond. All quartzes were phagocytized by alveolar macrophages (AMΦ cell line NR8383) to the same extent, irrespective of their surface state. Conversely, iron loading increased AMΦ viability (evaluated by cytotoxicity and induction of apoptosis). Qz was found to be much less cytotoxic than DQ12. The induction of oxidative stress and inflammatory responses (evaluated by HO-1 mRNA expression and TNF-α mRNA and protein expression) revealed a reduction in inflammogenicity upon iron loading and a more inflammogenic potency of DQ12 ascribed to undissociated SiOH interacting via H-bonding with cell membrane components. The results suggest that besides aluminium also iron at the quartz surface may have an inhibitory effect on adverse health responses. [ABSTRACT FROM AUTHOR]

To understand the effect of the commercial processing of diatomaceous earths (DEs) on their ultimate surface structure and potential toxicity, we investigated the influence of the industrial processing and the nature of the deposit. Two flux calcined specimens from different deposits, DE/1-FC and DE/2-FC, and the simply calcined sample DE/1-C, from the same deposit as DE/1-FC, were compared in both their bulk and their surface properties. X-ray diffraction (XRD) analysis in a heating chamber revealed the presence of cristobalite in all samples, more abundant on the flux calcined ones. The crystal lattice is probably imperfect, as the α−β transition, visible by XRD in DE/1-FC and DE/2-FC, is not detected by differential scanning calorimetry. Progressive etching with HF solutions suggests that most of the crystalline phase is at the core and not at the outer region of the samples. The combined use of spectroscopic (UV−vis and IR) and calorimetric techniques (heat of adsorption of water as a measure of hydrophilicity) reveals that DE/1-FC and DE/2-FC particles have an external layer of glass, absent in DE/1-C, where iron impurities act as network-forming and sodium ions as modifier species, with few patches of a hydrophobic phase, the latter relatable to a heated pure silica phase. When tested on a macrophage cell line (MH-S) in comparison with appropriate positive and negative controls (an active and an inactive quartz dust, respectively), only DE/1-C exhibited a cell damage and activation similar to that of active quartz (measured by lactate dehydrogenase release, peroxidation of membrane lipids and synthesis of NO). It is likely that the presence of a vitreous phase mitigates or even eliminates the cellular responses of silica in DE. [ABSTRACT FROM AUTHOR]