Archive General | archaeometallurgy
Jan 17 2014

how to do slag microscopy – sample cutting

Bastian Asmus
cross-section-cut-sample

This shows a cross section through a sample.  On a micro-scale the cutting surface of a samples is shattered by the cutting process. This areas needs to be removed for samples to be representative of the find.

This is part two of the series on slag microscopy and will deal with sample cutting. Part one was on the macroscopic description and documentation of the sample. Of course these steps may equally employed to mount samples other than slag.

The following things are needed for this:

  • a circular diamond blade cutter / tile cutter
  • ultrasonic bath
  • IMS
  • safety goggles
  • ear protection
  • lab coat or an apron Continue reading

Dec 18 2013

earliest tin-bronze discovered

Bastian Asmus

Another superlative from in Pločnik in Serbia: This time the team of the Rise of Metallurgy project has found evidence for the earliest known tin-bronze. The recovered artefact, a thin sheet bronze fragment, is at least 6500 years old and consists of a copper-tin alloy with 11 wt% tin, and a number of minor elements . Archaeologists call copper alloys with zinc brass, all others are often labelled as bronze. In order to clarify that it is bronze in the sense of the modern definition, in archaeological texts it is often referred to  as tin-bronze. Alloys with arsenic are called in the rest of the best arsenical copper. Continue reading


Nov 4 2013

Gossan or the iron cap

Bastian Asmus


Gossan is a term from mineral economics. The gossan may also be called iron cap. This is so because it denotes a concretion of iron hydroxides that has formed on top of sulphide mineral vein, where it reaches the surface. It forms during the supergene sulphide ore enrichment, when weakly acid surface water perloctaes through the mineral deposit. Many sulphide ores are oxidised in this process and brought into solution:

    \[ H_2 O + CO_2 & \pfeil H_2 CO_3 \]

Gossan or the iron cap

Schematic view of a sulphide vein. You can see the oxidation zone, consisting of the gossan, the leached zone and the oxidised zone. The reducing zone consists of the enrichment zone and the area of ​​primary mineralization. Significantly modified after Evans (1992) and Ottaway (1994).

 

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