科索沃北部和梅托希亚环境中放射性核素的元素浓度和土壤到苔藓的转移因子

L. Gulan, T. Jakšić, B. Milenkovic, J. Stajic
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引用次数: 3

摘要

本文研究了科索沃米特罗维察和祖宾波托克市地区放射性核素元素浓度和土壤向苔藓转移因子。12个土壤和苔藓样本。于2018年5月收集。根据土壤和苔藓样品中放射性核素的元素浓度,计算了放射性核素:226Ra、232Th、40and 137Cs的转移因子。为了指出苔藓吸收放射性核素的不同方式,进行了分析。根据计算的传递因子和分析,认为土壤是天然放射性核素的主要来源,其在苔藓中的浓度是由于土壤颗粒的再悬浮而产生的,而土壤和苔藓样品中的人工放射性核素则是由于大气干湿沉降而存在的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ELEMENTAL CONCENTRATIONS AND SOIL-TO-MOSS TRANSFER FACTORS OF RADIONUCLIDES IN THE ENVIRONMENT OF NORTH KOSOVO AND METOHIJA
This paper deals with investigations of elemental concentrations and soil-to-moss transfer factors of radionuclides in area of municipalities Kosovska Mitrovica and Zubin Potok. Twelve samples of soil and moss Hypnum cupressiforme Hedw. were collected during May 2018. Transfer factors of radionuclides: 226Ra, 232Th, 40Kand 137Cs were calculated with regard to elemental concentrations of radionuclides in soil and moss samples. Analysis was done in order to indicate the different ways of adopting radionuclides by mosses. According to calculated transfer factors and analysis, authors concluded that the soil is dominant source of natural radionuclides and their concentration in moss occurred due to resuspension of soil particles, while artificial 137Cs is present in soil and moss samples as a consequence of atmospheric dry and wet deposition.
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