Abstract:In the past years, several corpses that remained intact in the course of history were found in the Chehrabad salt mine of Zanjan Province, Iran and were made use to conduct several interdisciplinary studies to answer the questions of this paper. As we may know, archeological findings are always exposed to destruction. The rate of destruction depends variably on the organic or mineral substances and materials, as well as the environmental factors. In the environments with saline soils like the archeological site of Chehrabad, the destruction rate makes it necessary to adopt a new approach for the study of destruction and protection of the data. Therefore, the six samples of the rock salt taken from this site were analyzed by XRF method and psychrometric tests. The results show that the different saline compositions and environmental conditions are effective in the protection or destruction of organic or mineral components. In addition, we concluded that the high purity of rock salt at this site (more than 99.5%) and the very low moisture content of the environment were involved in the mummification of the buried corpses immediately after they were buried and thus prevented the activity of bacteria and other microorganisms that were the cause of decay.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
customersupport@researchsolutions.com
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
This site is protected by reCAPTCHA and the Google Privacy Policy and Terms of Service apply.
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.