Shakeup over sacred blood.Thixotropy thixotropy /thix·ot·ro·py/ (thik-sot´rah-pe) the property of certain gels of becoming fluid when shaken and then becoming semisolid again.thixotrop´ic thix·ot·ro·py n. -- the property that lets toothpaste ooze OOZE - Object oriented extension of Z. "Object Orientation in Z", S. Stepney et al eds, Springer 1992. when squeezed out of its tube and yet not drip off the toothbrush -- may explain a centuries-old miracle. Blood, once congealed con·geal v. con·gealed, con·geal·ing, con·geals v.intr. 1. To solidify by or as if by freezing: "My aim . . . was to take the Hill by storm before . . . , tends to stay that way. But when religious leaders handle a vial believed to contain the blood of St. Januarius, the dark brown substance begins to flow. Periodic demonstrations of this effect have drawn crowds to Naples since 1389, notes Luigi Garlaschelli, an organic chemist of the University of Pavia History The University of Pavia is one of the oldest universities in Europe. An edict issued by King Lotarius quotes a higher education institution in Pavia as already established 825 A.D. in Italy. In the Oct. 10 NATURE, Garlaschelli and two other Italian researchers propose that medieval alchemists An alchemist was a person versed in the art of alchemy, an ancient branch of natural philosophy that eventually evolved into chemistry and pharmacology. Alchemy flourished in the Islamic world during the Middle Ages, and then in Europe from the 13th to the 18th centuries. could have created a thixotropic substance that looked like blood by mixing water and salt with a mineral called molysite. Thixotropic materials exist as gels until a mechanical stress -- such as picking up or tilting their containers -- makes them flow. To explore this possibility, Garlaschelli searched through the scientific literature and discovered that about 70 years ago, researchers demonstrated thixotropy in an iron hydroxide alloy. He reproduced their work by mixing a ferric chloride compound with calcium carbonate calcium carbonate, CaCO3, white chemical compound that is the most common nonsiliceous mineral. It occurs in two crystal forms: calcite, which is hexagonal, and aragonite, which is rhombohedral. in water, then separating out the iron hydroxide that formed. By adding salt to a solution of this alloy, he created a dark brown gel. "It looks exactly like the samples in Naples," he told SCIENCE NEWS. All of these materials were available five centuries ago, including ferric chloride, found near Mt. Vesuvius in the form of molysite, he says. While noting that the Catholic Church forbids opening the sacred vials and analyzing their contents, Garlaschelli and his colleagues write: "Our replication of the phenomenon seems to render this sacrifice unnecessary." |
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