1982
DOI: 10.1002/crat.2170171223
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Investigations of Dissolving Mechanically Processed Quartz Grains

Abstract: The dissolution of polycrystalline quartz strained by compression and shear or by impact crushing in 1-N NaOH lead to different results. The defects of the impact crushed quartz grains, measured as crystallinity by X-ray methods, are not preferentially concentrated in regions near the surface. It is assumed that in this case the corners and edges of the quartz grains are preferred centers of defects.Es wurden Loseversuche in 1 n NaOH von polykristallinem Quarz nach Druck-und Scherbeanspruchung und nach Prallbe… Show more

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Cited by 14 publications
(8 citation statements)
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“…From X-ray powder diffraction investigation it follows that only the disturbed partially cristalline part of quartz dissolves and reacts with y-Al,O, forming zeolite. The zeolite formation shows the same dependence on the quartz crystallinity as in ( BERNHARD et al ;STEINIKE et al 1982) cited quartz solubility after the mechanical activation under pressure and shear stress (in a vibration mill). Further experiments were made with precipitated amorphous SiO,.…”
Section: Zeolite Formationsupporting
confidence: 67%
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“…From X-ray powder diffraction investigation it follows that only the disturbed partially cristalline part of quartz dissolves and reacts with y-Al,O, forming zeolite. The zeolite formation shows the same dependence on the quartz crystallinity as in ( BERNHARD et al ;STEINIKE et al 1982) cited quartz solubility after the mechanical activation under pressure and shear stress (in a vibration mill). Further experiments were made with precipitated amorphous SiO,.…”
Section: Zeolite Formationsupporting
confidence: 67%
“…The elementary step of the dissolution is influenced by lattice defects, e.g. bond breakings and deformation (WEYL;STEINIKE et al (1982)). Such defects could e.g.…”
Section: Introductionmentioning
confidence: 99%
“…52,112 The perturbed external amorphous layer (known as Beilby layer), which often covers quartz particles, stems from such a process. [10][11][12]113 As a consequence, the surface of a crystalline silica particle with whom cells interact is not a perfect and regular crystalline face, but rather an almost amorphous and irregular one. A scanning electron microscopy (SEM) image showing conchoidal fractures on a microscopic quartz particle obtained by ball milling of larger crystals is reported in Figure 3b.…”
Section: Filling the Gaps In The Association Between Particle Surface...mentioning
confidence: 99%
“…Since ancient times, crystallinity was considered to be the prerequisite feature for silica pathogenicity, in spite of some reports on nonpathogenic quartz dusts ,, and the general notion among mineralogists that quartz particles generated by grinding yield irregular distributions of crystallographic surfaces, expose conchoidal fractures, , and are mostly covered by an amorphous layer. The cells and tissue would have indeed been in direct contact with amorphous surfaces. Observing the occurrence of major occupations associated with silica exposure and related disasters (Table ), one feature emerges: in nearly all cases, crystalline silica (more often quartz, but also the other common polymorphs cristobalite and tridymite) was ground, crushed, or abraded.…”
Section: Variability Of Quartz Hazardmentioning
confidence: 99%
“…The mechanical activation of silica particles can result in the formation of free radicals at the surface of the particles 1–5. The reactive free radicals may initiate covalent grafting of functional components onto the surface of the silica particles 6–9.…”
Section: Introductionmentioning
confidence: 99%