Rosa J. Key-Schwartz, Ph.D., NIOSH/DART; Paul A. Baron, Ph.D., NIOSH/DART; David L. Bartley, Ph.D., NIOSH/DART; Faye L. Rice, NIOSH/EID, and Paul C. Schlecht, NIOSH/DART

Chapter R (1994)

Rosa J. Key-Schwartz, Ph.D., NIOSH/DART; Paul A. Baron, Ph.D., NIOSH/DART; David L. Bartley, Ph.D., NIOSH/DART; Faye L. Rice, NIOSH/EID, and Paul C. Schlecht, NIOSH/DART Chapter R (1994)

Because of the complex nature of crystalline silica analysis, it is essential to have a quality assurance program which incorporates strict adherence to standardized procedures. The most important requirement should be following the analytical methods exactly as written. Any modifications made in the methods in daily laboratory practices should be accompanied by validation data demonstrating equivalency of the modified method. Other factors which are important in measurement accuracy and precision and should be tracked are sample preparation, calibration and proficiency testing.
Source: Wikisource

Rosa J. Key-Schwartz, Ph.D., NIOSH/DART; Paul A. Baron, Ph.D., NIOSH/DART; David L. Bartley, Ph.D., NIOSH/DART; Faye L. Rice, NIOSH/EID, and Paul C. Schlecht, NIOSH/DART Chapter R (1994)

Physical properties (such as specific gravity, refractive index and X-ray diffraction pattern) and toxicological properties depend on the chemical composition and the molecular structure. Silica occurs in both crystalline and non-crystalline forms. Crystalline forms are physical states in which the silicon dioxide molecules are arranged in a repetitive pattern that has unique spacing, lattice structure and angular relationship of the atoms. Crystalline silica forms (often referred to as polymorphs) include quartz, cristobalite, tridymite, keatite, coesite, stishovite and moganite [2,3,4] .
Source: Wikisource

Rosa J. Key-Schwartz, Ph.D., NIOSH/DART; Paul A. Baron, Ph.D., NIOSH/DART; David L. Bartley, Ph.D., NIOSH/DART; Faye L. Rice, NIOSH/EID, and Paul C. Schlecht, NIOSH/DART Chapter R (1994)

PHYSICAL PROPERTIES OF QUARTZ, CRISTOBALITE AND TRIDYMITE.
In nature, quartz is the crystalline form most commonly encountered and is so abundant that the term quartz is often used in place of the general term crystalline silica [6, 7] . Quartz is abundant in most rocks and soils and is also present in sand, mortar, concrete, fluxes, abrasives, construction aggregate, porcelain, paints and brick [8] .
Source: Wikisource

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