阿拉木图地区大气表层自然本底辐射的估计测量值

V. Dyachkov, M. Bigeldiyeva, Y. Zaripova, A. Yushkov
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引用次数: 0

摘要

地壳天然放射性辐射的氡同位素向地表散发,集中在人类环境中,对人类健康有直接影响。因此,研究地球大气表层的辐射密度分布是一个迫切的问题。在这项工作中,测量了地球大气表层氡的暴露剂量率、粒子通量和等效平衡体积活度(EEVA)。2021年4月至2021年8月,在阿拉木图地区海拔500至2500米的不同高度进行了氡和γ、β背景测量。它们使用电子辐射测量设备进行:β剂量计“RKS-01B-SOLO”;伽马剂量计“RKS-01G-SOLO”;野外氡-222“RAMON-02”辐射计。因此,建立了初步的评估方案,对大气表层氡同位素和放射性核素衰变的自然子产物的222Rn氡同位素、β和γ辐射场进行路线测量。研究结果表明,地表表层自然辐射γ和β本底的变化具有高度依赖性,随海拔高度的增加而增加。图中显示了氡在岩石和土壤上的不同活性,众所周知,这与氡的呼出有关,而且除其他外,还取决于土壤的密度。对氡EEVA的显著扰动的初步测量结果没有得到证实
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimated measurements of natural background radiation in the surface atmospheric layer of the Almaty region
The radon isotopes of natural radioactive radiation of the earth’s cru st emanating to the surface are concentrated in the human environment and have a direct impact on the people health. Due to this fact the problem of st udying the radiation di st ributions in the surface atmospheric layer of the Earth is urgent. In this work, measurements of the exposure dose rate, beta particle flux, and equivalent equilibrium volumetric activity (EEVA) of radon in the surface atmospheric layer of the Earth have been performed. Measurements of radon and gamma, beta backgrounds were carried out from April 2021 to Augu st 2021 in the Almaty region at various altitudes above sea level: from 500 to 2500 meters. They were carried out using electronic radiometric equipment: beta-dosimeter “RKS-01B-SOLO”; gamma dosimeter “RKS-01G-SOLO”; radiometer of radon-222 “RAMON-02” in the field. As a result, preliminary assessment schemes were built for route measurements of the 222Rn radon isotope, beta and gamma radiation fields from natural daughter products of decay of radon isotopes and radionuclides located in the surface atmospheric layer. As a result of this work, an altitude dependence of changes in the natural radiation gamma and beta background of the surface surface layer is presented, which grows with an increase in the surface above sea level. The different activity of radon over rocks and soils is shown, which, as is known, is associated with the exhalation of radon and which depends, among other things, on the density of the soils. The preliminary results of measurements of significant perturbations of the EEVA of radon did not
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