Abstract

The Comprehensive Nuclear-Test-Ban Treaty (CTBT) bans the testing of nuclear explosive devices underground, in the atmosphere and underwater. Two main technologies, radionuclide and seismo-acoustic monitoring, are deployed in the International Monitoring System used for the verification of the CTBT. Medical isotope production from fission-based processes is the dominant contributor to a worldwide background of radioxenon. This background can make the discrimination of nuclear tests from legitimate nuclear activities very challenging. Even if emissions from medical isotope producers experienced a large reduction, there remain other important sources of radioxenon that contribute to the global background such as research reactors and nuclear power plants. Until recently, the largest producer of medical isotopes was located in Canada, at the Canadian Nuclear Laboratories (CNL) facility. The characterization of CNL emissions and its research reactor can provide valuable information for effective verification of the CTBT.

Highlights

  • The Comprehensive Nuclear-Test-Ban Treaty (CTBT) bans the testing of nuclear explosive devices underground, in the atmosphere, and underwater

  • The aim of this study is to examine the impact on radioxenon observations in the Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO) International Monitoring System (IMS) due to medical isotope production at the Canadian Nuclear Laboratories (CNL) facility in Chalk River, Ontario

  • This paper examines the broad scale impact of medical isotope production and research reactors on radioxenon background levels

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Summary

Introduction

The Comprehensive Nuclear-Test-Ban Treaty (CTBT) bans the testing of nuclear explosive devices underground, in the atmosphere, and underwater. The Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO) is the international organization responsible for operating the global International Monitoring System (IMS) and provides an initial analysis of all IMS data through the International Data Centre (IDC). For a well-contained underground nuclear test, very little if any, particulate matter escapes to the atmosphere, with the result that the only radionuclide signature may be radioactive noble gases [1, 2]. For CTBT verification purposes, the noble gases monitored include the xenon isotopes 133Xe (t1/2 = 5.243 d) and 135Xe (t1/2 = 9.10 h) and the nuclear isomers 131mXe (t1/2 = 11.9 d) and 133mXe (t1/2 = 2.19 d). Medical isotope production has a large influence on the CTBT radioxenon monitoring network [3,4,5].

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