DETERMINATION of RA-226, TH-232, K-40 and CS-137 ACTIVITIES in SOILS and BEACH SANDS and RELATED EXTERNAL GAMMA DOSES in ARIKLI MINERALIZATION AREA (AYVACIK/TURKEY)

G. lcan Top, Yüksel Örgün, Ismail Ercüment Ayazll, Murat Belivermiş, Zekiye Karaclk, Györgyi Kampfl

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)

Abstract

Uranium mineralization areas may jeopardize public health and surrounding natural life. In the current study for radioactivity and geochemical analyses, 43 soil, 5 rock and 10 beach sand samples were collected in and around Arlkll (Ayvaclk, Turkey) uranium mineralization area. Radioactivity levels in the soils (up to Ra-226: 629, Th-232: 240, K-40: 3669 Bq/kg) were found higher than the that of beach sands. Besides, radioactivity of the beach sand samples is found at normal levels (avg: Ra-226: 31, Th-232: 31, K-40: 542 Bq/kg) when compared to worldwide average soil. Dose values indicate that the region have ~three times higher average gamma radioactivity than the corresponding world average although measured gamma doses ranged up to 687 nGy/h. The high measured values are related to uranium mineralization, alteration zones, faults and Arlkll tuff.

Original languageEnglish
Pages (from-to)137-154
Number of pages18
JournalRadiation Protection Dosimetry
Volume193
Issue number3
DOIs
Publication statusPublished - 1 Mar 2021

Bibliographical note

Publisher Copyright:
© 2021 The Author(s) 2021. Published by Oxford University Press. All rights reserved. For Permissions, please email: [email protected].

Funding

This research was supported by the Scientific Research Projects Unit of Istanbul Technical University (project number: MGA-2018-41483).

FundersFunder number
Istanbul Teknik ÜniversitesiMGA-2018-41483

    Fingerprint

    Dive into the research topics of 'DETERMINATION of RA-226, TH-232, K-40 and CS-137 ACTIVITIES in SOILS and BEACH SANDS and RELATED EXTERNAL GAMMA DOSES in ARIKLI MINERALIZATION AREA (AYVACIK/TURKEY)'. Together they form a unique fingerprint.

    Cite this