Abstract

The content of Li, B, and N is examined in ancient and modern pottery and its glazes by means of (n, p) and (n, α) reactions with thermal neutrons. Most samples exhibit a proportionality between B and Li concentrations with preferred values around 0.01 at.%. One group of pottery shows nearly constant Li abundance around 0.1 at.%, the B content varying from 10−4 at.% to 10 at.%. An explanation is given, and the individual groups of pottery are described in detail. Results for different archaeological sites of Sumerian, Babylonian, Assyrian, Phoenician and Roman provenience are presented. The data scattering of B and Li contents of samples from different places of origin varies considerably, and can be used as a measure of the economical importance of ancient centers. Local urban cultures, such as Ur, exhibit a relative data scattering around 0.2, cities with average trade relations show values around 0.4, and for the famous trade center Palmyra, 0.8 was found.The B/Li ratio of pottery indicates whether the clay used is a fresh water or a marine sediment. The B and Li contents of Euphrates pottery show systematic variations along the river valley. Several samples, found in the Mesopotamian region are highly enriched in nitrogen. This is probably due to salt precipitation in the surrounding soil after the destruction of the irrigation facilities by the Mongols in 1258.

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