Radioactivity of soils enriched with pyrogenic artefacts in the land of Pernik city, Bulgaria

IF 1.4 Q4 SOIL SCIENCE
V. Tsolova, R. Lazarova, I. Yordanova, D. Staneva
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引用次数: 0

Abstract

This article aims to study the radioactivity of soils enriched with pyrogenic artefacts and the possible enhancement of radioactive background and the dose load on the population as a result of coal mining and electricity generation in mine-energetic region Pernik, Bulgaria. Content of major radionuclides responsible for radiation loading – 238 U, 232 Th, 40 K, their progenies 226 Ra and 210 Pb, and technogenic 137 Cs was determined in fi ve soil types representative for the region. Data show that the activity (Bq kg -1 ) of 238 U, 226 Ra, 232 Th and 40 K in studied soils slightly fl uctuates around average values in Bulgarian soils, accepted as background levels in this study. The activity of 210 Pb and 137 Cs was also comparable to that established in other uncontaminated soils. The mixing of materials and artefacts containing pyrogenic carbon (coal-clayey substrate occurring in the unproductive coal strata and slag produced in the local thermal power plant) during the formation of reclaimed soils increases the content of studied radioactive elements, but the highest levels are found in soils (Cam-bisols) enriched with soot. Thus, a typical anthropogenic enhancement of radiation background was observed but it is also not hazardous to the population. Gamma radiation emanating from studied soils is below the recommended values and vary from 0.23 to 0.57 for external hazard index, and from 0.29 to 0.61 mSv y -1 for outdoor annual effective dose. The established interlink between 210 Pb activity and pyrogenic carbon content show that 210 Pb could be used as a marker of the recent deposition of pyrogenic carbon formed during the coal combustion and other activities emitting pyrogenic carbon-containing aerosols.
保加利亚佩尼克市土地上富含热原人工制品的土壤的放射性
本文旨在研究富含热原人工制品的土壤的放射性,以及由于保加利亚佩尼克矿区的煤矿开采和发电而可能增强的放射性本底和对人口的剂量负荷。测定了具有代表性的5种土壤类型的主要放射性核素238 U、232 Th、40 K及其子代226 Ra、210 Pb和技术源137 Cs的含量。数据显示,研究土壤中238 U、226 Ra、232 Th和40 K的活度(Bq kg -1)在保加利亚土壤的平均值附近略有波动,该平均值在本研究中被接受为背景水平。210 Pb和137 Cs的活性也与其他未受污染的土壤相当。在再生土壤的形成过程中,含有热原碳(非生产煤层中的煤粘土基质和当地热电厂产生的矿渣)的物质和人工制品的混合增加了所研究的放射性元素的含量,但在富含煤烟的土壤(cami -bisols)中发现的含量最高。因此,观察到典型的人为辐射本底增强,但对人口也没有危害。所研究土壤发出的伽马辐射低于建议值,外部危害指数在0.23至0.57之间,室外年有效剂量在0.29至0.61毫西弗/ 1之间。210 Pb活度与热原碳含量之间的相互联系表明,210 Pb可作为煤燃烧过程中形成的热原碳沉积和其他活动释放含热原碳气溶胶的标志。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Soil Science Annual
Soil Science Annual SOIL SCIENCE-
CiteScore
2.50
自引率
6.70%
发文量
0
审稿时长
29 weeks
期刊介绍: Soil Science Annual journal is a continuation of the “Roczniki Gleboznawcze” – the journal of the Polish Society of Soil Science first published in 1950. Soil Science Annual is a quarterly devoted to a broad spectrum of issues relating to the soil environment. From 2012, the journal is published in the open access system by the Sciendo (De Gruyter).
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