Bronze age artifacts, physical links between us and people alive 3000
years ago, have long been closely examined with physics-based instruments
such as x-ray crystallography and mass spectrometry.
Now scrutiny of microchemical surface properties of such ancient bronze
in some respects surpasses the diagnostic information gained by previous
bulk-phase studies. Ernesto Paparazzo of the Instituto di Stuttura della
Materia in Rome (paparazzo@ism.rm.cnr.it, 39-06-4993-4153), and his
colleagues at the Pacific Northwest National Lab and Oxford, have looked
at an early-first-millennium BCE belt from Syria with scanning auger
microscopy (SAM), a process in which specific elements in a material
can be identified when electrons with characteristic energies are knocked
out of atoms by an incoming electron beam.
Bronze is an alloy of copper and tin---generally a mixture of about
85% copper and 10% tin, with minor amounts of other metals being also
possible (e.g., zinc, lead, etc.). Metals put back into the earth naturally
rust but unequally, leading in the case of bronze to "decuprification,"
that is, the disproportionate detachment of copper atoms from the bronze.
With their SAM device, the researchers have studied this process, and
have characterized the microchemistry of the bronze at a level of spatial
resolution as good as 15 nm, the best yet achieved for the analytical
study of an archeomaterial. They can inventory the invasion of silicates
into the alloy from surrounding soil during the burial phase and even
spot alloy inhomogeneities introduced by the smith during the manufacturing
phase. (Paparazzo et
al., Journal of Vacuum Science and Technology A, July 2001.)