Elsevier

Quaternary Geochronology

Volume 30, Part B, October 2015, Pages 369-373
Quaternary Geochronology

Research paper
OSL chronology of traditional zinc smelting activity in Yunnan province, southwest China

https://doi.org/10.1016/j.quageo.2015.05.011Get rights and content

Abstract

The production of zinc has played an important role in both the technological and the economic history of ancient china. However, the lack of studies on zinc smelting remains with convincing chronology limits our understanding on the history of zinc production.

Our recent field survey in Yunnan province, southwest china, has discovered zinc-smelting sites in Qiaojia County. The location is in the Jinsha River Valley, which has abundant lead, zinc, copper and mineral coals. Large numbers of crucible and slags were excavated, which indicates a large scale of zinc production in the region. A profile of 10 layers containing slag pellets altered with fluvial sediments presents clear evidence of a series of zinc smelting events. The ages of both the fluvial sediment and slag layers have been obtained using luminescence dating. Detailed chronology indicates that large scale of zinc production in this area can be traced back to late Qing Dynasty (AD 1854).

Introduction

Zinc (Boiling temperature: 907 °C) was a difficult and enigmatic metal in the antique world. It immediately volatilizes and reoxidizes when people attempt to reduce the zinc ore in an open furnace. The earliest use of zinc is to make brass, an alloy of zinc and copper. Brass was manufactured by heating zinc-bearing copper ore and charcoal to 1000 °C in a sealed crucible to directly dissolve zinc vapor into the copper (Craddock, 1978). Regular production of unalloyed zinc occurred relatively late in metallurgical history. In China, smelting of zinc was achieved based on the principle of distillation by ascending vapors (Hu and Han, 1984, Mei, 1990, Zhou, 1996). Recent studies suggest that regular zinc production in China is known to have begun in the16th Century AD in the Chongqing region (Zhou, 2007, Zhou et al., 2012). Zinc was mainly used for making brass coins and copper-bearing artefacts in the late Ming (AD 1368–1644) and Qing (AD 1644–1911) Dynasties (Zhou, 2012). The Chinese mining and smelting of zinc have a significant impact not only on the domestic economy, but also on European industrial production via exporting (Craddock and Hook, 1997).

Early studies by historians of metallurgy, mainly based on historical records and analyses of brass coins, provide us a time outline since the late Ming Dynasty (Zhang, 1925, Zhao, 1984, Zhou and Fan, 1993, Zhou, 2001). A recent case study of ancient zinc smelting sites in Chongqing analyzed production remains directly relates to older zinc smelting with an established chronology (Zhou et al., 2012). A brief outline of general temporal and regional distribution of zinc production is provided. Geological surveys focusing on traditional zinc production since the early 20th century have identified several zinc smelting sites in Hezhang, Guizhou, in 1954 (Xu, 1986); in Huize, Yunnan, in 1939; in Weining, Guizhou, in 1940; and in Huili, Sichuan, in 1941 (summarized in Mei, 1990). The sites documented by historians and geologists are mostly located in the Chuan-Dian-Qian region, a triangle-shaped area surrounded by Sichuan, Yunnan and Guizhou Provinces. The region is known to have an abundance of zinc and lead ores, coal, and other resources for zinc production (Zhou, 1997). However, lack of studies on zinc smelting sites with convincing chronology limit our understanding on the history of zinc production in this region. This paper presents the results of our recent survey to explore the history of traditional zinc smelting in this area.

Section snippets

Sampling

The sampling site is in Qiaojia County, located about 310 km south of Kunming city in Yunnan (Fig. 1a), southwest China. The mountain region has abundant resources of various ores, including copper, zinc, lead and coal mines, which support the mining and smelting activities. Our archaeological survey led to the discovery of several zinc-smelting sites close to the Jinsha River, including buried slags and hundreds of ceramic crucibles showing large-scale smelting activities in the past (Fig. 1

Methods

The tubes of OSL samples were opened under subdued red light in the laboratory. Surface samples at both ends of tubes were used for measurements of water content, radionuclide concentrations and other proxies. Only the central part of the sediment was used for OSL dating to avoid any incidental exposure to light during sampling and transportation. Chemical treatments using 10% hydrochloric acid and 10% hydrogen peroxide solution were employed to remove carbonates and organic materials

Results and discussion

The samples showed good behavior in OSL measurements, with good recycling ratios and dose recovery. This suggests that samples in the study site are suitable for OSL dating. The obtained OSL ages, together with the De values, environmental dose rates and other data used for age calculations are summarized in Table 1. The OSL ages in the profile are in stratigraphic order within the errors. Ages are calculated using the weighted mean of all aliquots of each sample and data is converted to

Acknowledgments

The authors are grateful to Professor James Burton for the help in improving the manuscript. The research was supported by National Natural Science Foundation of China (Grant No. 41073004 and Grant No. 41303080) and China Postdoctoral Science Foundation (Grant No. 2013T60618 and Grant No. 2012M521236). We thank the anonymous reviewer, who provided very helpful commentary and suggestions that improved the manuscript.

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