Abstract

This study reports the natural radioactivity of characteristic rocks found in the historic Jeroným Mine of the Czech Republic as measured under the laboratory conditions. The rocks analyzed included granites and schists weathered to varying degrees and collected from different levels of the underground workings of the Jeroným Mine. The mine itself has been subject to metal extraction (mainly tin and tungsten) since the sixteenth century and has recently been developed as a cultural and scientific attraction open to the public. Activity concentrations of 40K, 232Th and 238U were measured from nine rock samples using gamma-ray spectrometry. The activity concentrations of 40K varied from 595 Bq kg−1 to 1244 Bq kg−1, while 232Th varied from 25 Bq kg−1 to 55 Bq kg−1. The activities associated with 238U ranged from 46 Bq kg−1 to 386 Bq kg−1. The measured activities were used to estimate two radiation hazard indices typically applied to building materials, the activity concentration index I and the external hazard index Hex. Mean respective values of 1.02 and 0.77 for I and Hex indicate that the rocks found in the Jeroným Mine meet radiological safety standards for building materials and do not pose a risk to potential tourists and staff.

Highlights

  • The historic Jeroným Mine is located near the former Čistá municipality in the Sokolov District of the Czech Republic (Fig. 1)

  • The locality is a part of a protected landscape, the Slavkovsky Les Mountains, which border the Bohemian Massif

  • The present study reports laboratory gamma-ray spectrometry measurements of natural radioactivity levels from characteristic rocks samples found in the mine

Read more

Summary

Introduction

The historic Jeroným Mine is located near the former Čistá municipality ( known as Lauterbach Stadt) in the Sokolov District of the Czech Republic (Fig. 1). The long term subsurface mining activities and other human impacts have led to the designation of the Jeroným Mine as a National Heritage Site open to the public as part of the greater Czech Bavarian Jeopard. The Jeroným Mine accesses metamorphosed rocks belonging to the Slavkov mantle crystalline complex and Variscan granites of the Ore Mountains pluton. The area sampled occurred near the contact of major geological units, the Ore Mountain and Tepla-Barrandium megablock which formed at around 265 Ma. The immediate surroundings as well as the Jeroným Mine itself include altered acidic granites hosting prominent Variscan tin-tungsten mineralization.

Materials and methods
Results and discussion
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call