Abstract
Over the past 15 years, the urate crystal has become accepted as the fundamental local factor in the pathogenesis of gout (McCarty and Hollander, 1961; McCarty, 1977). In this concept, formation of crystals is the primary event underlying all gout, with acute arthritis or the growth of tophi invariably being secondary crystal-induced responses. Clearly, the conditions leading to urate precipitation are of paramount importance to an understanding of the syndrome of gout. Crystallization in vitro is a phenomenon well understood by physical chemists, who are thus able to determine precise solubility limits for any solute in a given solvent under defined conditions of temperature and pH. Formation of urate crystals in vivo, however, is not well understood by physicians, who have found that the incidence of gout correlates poorly with the concentration of urate in human serum, and that crystals, when present, are not randomly distributed but occur preferentially at well-recognized peripheral sites.
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Simkin, P.A. (1978). Role of Local Factors in the Precipitation of Urate Crystals. In: Kelley, W.N., Weiner, I.M. (eds) Uric Acid. Handbook of Experimental Pharmacology, vol 51. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-66867-8_16
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DOI: https://doi.org/10.1007/978-3-642-66867-8_16
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