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A new piece of the puzzle: slag and ore analysis to reconstruct the prehispanic smelting technology at the Atacama Desert, Chile
Indexado
WoS WOS:001048585500001
Scopus SCOPUS_ID:85168381878
DOI 10.1186/S40494-023-01017-Z
Año 2023
Tipo artículo de investigación

Citas Totales

Autores Afiliación Chile

Instituciones Chile

% Participación
Internacional

Autores
Afiliación Extranjera

Instituciones
Extranjeras


Abstract



The Incas appropriated many local metallurgical technologies throughout the Andes, each of which had its unique peculiarities and was based on local ancestral knowledge. The widespread use of tin-bronze during the Inca expansion, the development of mining and smelting sites, as well as ethno-historical records evidence the Incas' interest in copper smelting, a key activity in the Andes since ca. 1400 BC. However, little is known about the technical parameters achieved by ancient metallurgists and the changes that occurred during the Inca expansion. In this paper, we address these changes through a case study of Copiapo valley, focusing on the Vina del Cerro site, one of the most famous Inca smelting centres of the southern Andes. Although this place was architectonically restructured by the Incas, its operations began long before the imperial expansion and used wind-powered furnaces. We analysed 19 slag and 11 copper ore samples using OM, SEM-EDS, WD-XRF, and XRD analyses. Results identified heterogeneous and viscous slags, rich in SiO2 (43 wt%) and poor in FeO (13 wt%). Copper retention was high (up to 60 wt%). Microstructural analyses indicate that slags were formed under unstable oxidising conditions, reaching temperatures that ranged between 1000 to 1100 & DEG;C. The copper produced was very pure. High-grade copper ores containing up to 69 wt% CuO were reduced at the site, combining carbonates (malachite, azurite), halides (buttgenbachite, clinoatacamite), and some sulphates (brochantite). We propose that even under the relatively unfavourable conditions for slag formation, the smelting conditions generated at Vina del Cerro were competent enough to extract metal, but not necessarily enough to form liquid slag. These conditions were facilitated by the local metallurgists' thorough knowledge of the wind flow and their ability to select the right ore. This new information contributes to understanding the efficiency of metallurgical technology and the knowledge, skills, and adaptability of the ancient metallurgists from Copiapo valley, a group that was integrated into the economic networks of the Inca Empire.

Revista



Revista ISSN
Heritage Science 2050-7445

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Disciplinas de Investigación



WOS
Chemistry, Analytical
Spectroscopy
Materials Science, Multidisciplinary
Scopus
Sin Disciplinas
SciELO
Sin Disciplinas

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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

Colaboración Institucional



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Autores - Afiliación



Ord. Autor Género Institución - País
1 Plaza Calonge, María Teresa Mujer Pontificia Universidad Católica de Chile - Chile
2 GARRIDO-ESCOBAR, FRANCISCO JAVIER Hombre Museo Nacl Hist Nat - Chile
Museo Nacional de Historia Natural Chile - Chile
3 Larreina-Garcia, David - Univ Basque Country - España
Equipo de Arqueología del Museo de la Minería del País Vasco - España

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Financiamiento



Fuente
Fondo Nacional de Desarrollo Científico y Tecnológico
Pontificia Universidad Católica de Chile
FONDECYT Projects
Museo Nacional de Historia Natural in Chile
Museo Regional de Atacama
Agencia Nacional de Investigacion ANID
Centro Nacional de Investigación sobre la Evolución Humana

Muestra la fuente de financiamiento declarada en la publicación.

Agradecimientos



Agradecimiento
This research was funded by Fondecyt projects 3200229 and 1230614 (Agencia Nacional de Investigacion ANID), and the sponsorship of the Museo Regional de Atacama, Museo Nacional de Historia Natural in Chile and the Pontificia Universidad Catolica de Chile.
We acknowledge the research funding provided by the Fondecyt projects 3200229 and 1230614 (Agencia Nacional de Investigación ANID), and the sponsorship of the Museo Regional de Atacama, Museo Nacional de Historia Natural in Chile, and the Pontificia Universidad Católica de Chile. We are also very grateful to Ana Isabel Alvaro and all the staff from the Centro Nacional de Investigación sobre la Evolución Humana (CENIEH) laboratories (Burgos, Spain) for their analyses.
This research was funded by Fondecyt projects 3200229 and 1230614 (Agencia Nacional de Investigación ANID), and the sponsorship of the Museo Regional de Atacama, Museo Nacional de Historia Natural in Chile and the Pontificia Universidad Católica de Chile.
We acknowledge the research funding provided by the Fondecyt projects 3200229 and 1230614 (Agencia Nacional de Investigación ANID), and the sponsorship of the Museo Regional de Atacama, Museo Nacional de Historia Natural in Chile, and the Pontificia Universidad Católica de Chile. We are also very grateful to Ana Isabel Alvaro and all the staff from the Centro Nacional de Investigación sobre la Evolución Humana (CENIEH) laboratories (Burgos, Spain) for their analyses.

Muestra la fuente de financiamiento declarada en la publicación.