scholarly journals Restoration of archaeological iron on the materials of excavations of burial grounds in the territory of the Tazovsky Polar Region

Author(s):  
Zlata Ivanova ◽  
2005 ◽  
Vol 436 (2) ◽  
pp. L43-L46 ◽  
Author(s):  
E. O'Shea ◽  
D. Banerjee ◽  
J. G. Doyle
Keyword(s):  

Radiocarbon ◽  
2007 ◽  
Vol 49 (1) ◽  
pp. 123-129 ◽  
Author(s):  
Yaroslav V Kuzmin

The problem of a hiatus at about 6100–5300 BP (about 4900–4200 cal BC) in the prehistoric chronology of the Cis-Baikal region in Siberia is discussed. Based on a critical evaluation of existing evidence, there was no discontinuity found in the cultural sequence between the Kitoi and Serovo/Glazkovo complexes of the Neolithic, and the proposed “hiatus” may be an artifact based on underestimation of solid data. Conventional 14C dates are presented that were generated in the 1980s to early 2000s for Cis-Baikal prehistoric burial grounds, and were later dated by the accelerator mass spectrometry (AMS).


2021 ◽  
Vol 2 (2) ◽  
pp. 274-292
Author(s):  
Sarah James ◽  
Edith Joseph

The instability of iron artefacts is rooted in salt contamination during burial and damages associated with exposure to alternative oxygen levels and high relative humidity once excavated. While a combination of chemical and mechanical treatments is utilised to remove the harmful ions (chlorides, sulphur species) and excess bulky corrosion products, these methods can be hazardous for conservation staff’s health, have limited success, or require extensive treatment times. Bio-based treatments provide a potentially greener alternative for removing damaging corrosion and creating biogenic mineral passivation layers, thus remediating concerns over costs, duration, and health and safety. Pseudomonas putida mt-2 (KT2440) is capable of utilising iron under certain conditions and for phosphating mild steel; however, applications have not been made in the cultural heritage sector. To address the potential of using bacteria for conservation purposes, Pseudomonas was assessed for both the bioremediation of salt contaminates and the production of a passivation layer suitable for iron artefacts, with specific conservation concerns in mind. Key factors for optimisation include the role of agitation, chloride content, and oxygen content on bacterial growth and biomineralisation. The initial results indicate a growth preference, not reliance, for NaCl and agitation with partial success of bioconversion of a mineral source.


Icarus ◽  
2004 ◽  
Vol 167 (1) ◽  
pp. 204-211 ◽  
Author(s):  
Tom S Stallard ◽  
Steve Miller ◽  
Laurence M Trafton ◽  
Thomas R Geballe ◽  
Robert D Joseph
Keyword(s):  

2011 ◽  
Vol 58 (1) ◽  
pp. 39-45 ◽  
Author(s):  
Guo Cheng Lv ◽  
Zi Se Wang ◽  
Li Mei Wu ◽  
Chunchun Xu

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