ISO 18589-3:2023
Current
The latest, up-to-date edition.
Measurement of radioactivity in the environment — Soil — Part 3: Test method of gamma-emitting radionuclides using gamma-ray spectrometry
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English, French
27-07-2023
This document specifies the identification and the measurement of the activity in soils of a large number of gamma-emitting radionuclides using gamma spectrometry. This non-destructive method, applicable to large-volume samples (up to about 3l), covers the determination in a single measurement of all the γ-emitters present for which the photon energy is between 5keV and 3MeV.
Generic test method and fundamentals using gamma-ray spectrometry are described in ISO20042.
This document can be applied by test laboratories performing routine radioactivity measurements as a majority of gamma-emitting radionuclides is characterized by gamma-ray emission between 40keV and 2MeV.
The method can be implemented using a germanium or other type of detector with a resolution better than 5keV.
This document addresses methods and practices for determining gamma-emitting radionuclides activity present in soil, including rock from bedrock and ore, construction materials and products, pottery, etc. This includes such soils and material containing naturally occurring radioactive material (NORM) or those from technological processes involving Technologically Enhanced Naturally Occurring Radioactive Materials (TENORM) (e.g. the mining and processing of mineral sands or phosphate fertilizer production and use) as well as of sludge and sediment. This determination of gamma-emitting radionuclides activity is typically performed for the purpose of radiation protection. It is suitable for the surveillance of the environment and the inspection of a site and allows, in case of accidents, a quick evaluation of gamma activity of soil samples. This might concern soils from gardens, farmland, urban or industrial sites that can contain building materials rubble, as well as soil not affected by human activities.
When the radioactivity characterization of the unsieved material above 200μm or 250μm, made of petrographic nature or of anthropogenic origin such as building materials rubble, is required, this material can be crushed in order to obtain a homogeneous sample for testing as described in ISO18589‑2.
DocumentType |
Standard
|
Pages |
35
|
PublisherName |
International Organization for Standardization
|
Status |
Current
|
Supersedes |
Standards | Relationship |
PN-EN ISO 18589-3:2024-07 | Identical |
VDE 0493-4-5893:2024-08 | Identical |
DIN EN ISO 18589-3:2024-08 | Identical |
SS-ISO 18589-3:2023 | Identical |
SN EN ISO 18589-3:2024 | Identical |
DS/EN ISO 18589-3:2024 | Identical |
NS-EN ISO 18589-3:2024 | Identical |
UNI EN ISO 18589-3:2024 | Identical |
DS/ISO 18589-3:2023 | Identical |
SS-EN ISO 18589-3:2024 | Identical |
UNE-EN ISO 18589-3:2024 | Identical |
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