ESTIMATING BAKING TEMPERATURES IN A ROMAN POTTERY KILN BY ROCK MAGNETIC PROPERTIES: IMPLICATIONS OF THERMOCHEMICAL ALTERATION ON ARCHAEOINTENSITY DETERMINATIONS

Show simple item record

dc.contributor.author Spassov S.
dc.contributor.author Hus J.
dc.date.accessioned 2024-12-07T09:08:03Z
dc.date.available 2024-12-07T09:08:03Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=14679789
dc.identifier.citation Geophysical Journal International, 2006, 167, 2, 592-604
dc.identifier.issn 0956-540X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46857
dc.description.abstract Absolute past geomagnetic field intensity determinations requiring laboratory heating are labourious and the success rate is rather low, mostly because of induced thermochemical magnetic mineral alterations. Archaeomagnetic intensity determinations are mainly limited to displaced ceramics produced in kilns. In this study, the suitability of an in situ baked structure is investigated. Different magnetic properties of baked material taken from the combustion chamber wall and floor of a Roman pottery kiln, with variable colouring, are examined in dependence on the distance to the combustion chamber. The temperature distribution is re-constructed based on rock magnetic experiments after stepwise heating. The rock magnetic temperature estimates agree fairly well with a mathematical heat conduction model demonstrating the penetration of heat into the combustion chamber wall. The rock magnetic results show that blackish- and greyish-coloured kiln parts, that had been in close contact with the fuel, during ancient kiln operation, are not suitable for intensity determinations. Although sufficiently baked, they strongly alter during laboratory heating and new remanence-carrying minerals are formed. The brownish-coloured material at a distance 65-80 mm away from the combustion chamber seems to be most suitable as its magnetic properties remain nearly unchanged during laboratory heating. Rock magnetic and modelled temperature estimates for this material consistently indicate ancient baking temperatures of about 600°C. The model demonstrates that cooling takes longer in the inner parts of the combustion chamber wall. Retarded cooling affects the blocking temperatures and hence the strength of the thermoremanent magnetization. The variability of cooling rates should be taken into account when investigating archaeointensities of specimens cut from large samples, or of samples taken from different parts of a kiln. © 2006 The Authors Journal compilation © 2006 RAS.
dc.subject ARCHAEOINTENSITY
dc.subject ARCHAEOMAGNETISM
dc.subject BELGIUM
dc.subject HEAT CONDUCTION
dc.subject ROCK MAGNETISM
dc.subject ROMAN POTTERY KILN
dc.title ESTIMATING BAKING TEMPERATURES IN A ROMAN POTTERY KILN BY ROCK MAGNETIC PROPERTIES: IMPLICATIONS OF THERMOCHEMICAL ALTERATION ON ARCHAEOINTENSITY DETERMINATIONS
dc.type Статья
dc.identifier.doi 10.1111/j.1365-246X.2006.03114.x


Files in this item

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record