14656
Title Of Article Chaper
Über das Ionenaustchverhalten von Feuersteinen
Title Of Journal Book
Acta Praehistorica et Archaeologica
Volume
44147
Pages
35-36
Publisher City
Berlin
Language Of Text
German
Literature Type
Serial
Literature Level
Analytic
Abstract
In general flint is believed to consist of microcrystalline alpha-quartz. Closer investigation reveals a very complex structure of pseudohexagonal plates forming grains. These plates consist of even smaller particles held together by monolayers of water. The question arises, where in this structure the impurities, in total up to 3%, are situated. Iron for instance cannot be removed by different concentrated acids. So it cannot be outside the plates. On the other hand iron is leached out by soft solvents such as solutions of ammonia and salt. So the impurities must be located between the monolayers. Measurements of the grain size of different sorts of flint were carried out by x-ray diffraction. Investigations like this play a part in the understanding of weathering of flint artifacts and their colors. -- AATA
pub_id
14656
Title Translation
On the ion exchange behavior of flint