I . ' I ~ IE - - Johann Wolfgang DObereiner James L. Marshall, Beta Eta 1971, and Virg inia R. Marshall, Beta Eta 2003, Hof• Department of Chemistry, University of Miinch-••Bug North Texas, Denton TX 76203-5070, berg
[email protected] •Gefree n the two previous "Rediscovery of the Elements" articles'·' we followed the devel •Bayreuth Iopment of the Periodic classification of the elements, where there has been an amazing consilience of scientific law and theory, includ ing specific heat data, gas laws, valence theory, chemical behavior trends, electrochemical data, atomic theory, homologous crystalline forms, quantum theory, etc., resulting in our modem Periodic Table. ln this story'·' we have glossed over the ini tial attempts to organize the elements. When Lavoisier first recognized the true elements,' he recognized four major groups:"Elements of the body,""Nonmetallic substances,""Metals," and "Earths." The Scottish chemist Thomas Figure 1. Doberei11er never traveled outside Gen11a11y. His earlier years were spent in the Miinchberg area, Thomson, some four decades later, organized his educational travels in Dillenburg, Karlsrnhe, and Strassbourg (then part of Gennany), and his mature the 53 known elements into three classes:• years in Jena. "Supporters," whose voltaic composition result in their "attach[ing] themselves to the positive pole";"acidifiable bases," which are electropos the atomic weight for the alkaline earth in the (c) Alkalis. The average of lithium (6.94) and itive elements combining with the supporters mineral was an arithmetic mean of the previ potassium (39.10) is 23.02; sodium is 22.99. to fonn acids; and"alkalifiable bases," which are ously known atomic weights for calcium and (d) Elements "which combine with hydro electropositive elements uniting with support barium; additionally, his determined specific gen to form characteristic hydrogen acids."The ers to form alkaline compounds.