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一种用于深埋放射性污染物远程深度估计的新方法。

A Novel Method for Remote Depth Estimation of Buried Radioactive Contamination.

作者信息

Ukaegbu Ikechukwu Kevin, Gamage Kelum A A

机构信息

Engineering Department, Lancaster University, Lancaster LA1 4YW, UK.

School of Engineering, University of Glasgow, Glasgow G12 8QQ, UK.

出版信息

Sensors (Basel). 2018 Feb 8;18(2):507. doi: 10.3390/s18020507.

DOI:10.3390/s18020507
PMID:29419759
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5855003/
Abstract

Existing remote radioactive contamination depth estimation methods for buried radioactive wastes are either limited to less than 2 cm or are based on empirical models that require foreknowledge of the maximum penetrable depth of the contamination. These severely limits their usefulness in some real life subsurface contamination scenarios. Therefore, this work presents a novel remote depth estimation method that is based on an approximate three-dimensional linear attenuation model that exploits the benefits of using multiple measurements obtained from the surface of the material in which the contamination is buried using a radiation detector. Simulation results showed that the proposed method is able to detect the depth of caesium-137 and cobalt-60 contamination buried up to 40 cm in both sand and concrete. Furthermore, results from experiments show that the method is able to detect the depth of caesium-137 contamination buried up to 12 cm in sand. The lower maximum depth recorded in the experiment is due to limitations in the detector and the low activity of the caesium-137 source used. Nevertheless, both results demonstrate the superior capability of the proposed method compared to existing methods.

摘要

现有的用于掩埋放射性废物的远程放射性污染深度估计方法,要么限于2厘米以内,要么基于需要预先知道污染最大穿透深度的经验模型。这些方法在某些实际的地下污染场景中严重限制了它们的实用性。因此,这项工作提出了一种新颖的远程深度估计方法,该方法基于一个近似三维线性衰减模型,该模型利用了使用辐射探测器从掩埋有污染物的材料表面获得的多次测量结果的优势。模拟结果表明,所提出的方法能够检测出在沙子和混凝土中掩埋深度达40厘米的铯 - 137和钴 - 60污染的深度。此外,实验结果表明,该方法能够检测出在沙子中掩埋深度达12厘米的铯 - 137污染的深度。实验中记录的较低最大深度是由于探测器的局限性以及所使用的铯 - 137源的低活度。然而,这两个结果都证明了所提出的方法相对于现有方法具有卓越的能力。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/bd9ff7833c8d/sensors-18-00507-g013.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/a48eaab50808/sensors-18-00507-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/fe8bdcc94945/sensors-18-00507-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/637b95d6b8e0/sensors-18-00507-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/6d3c531e949b/sensors-18-00507-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/ff9fded33444/sensors-18-00507-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/c32e9aa113a9/sensors-18-00507-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/32f95e68bacb/sensors-18-00507-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/a80f969dddfc/sensors-18-00507-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/51a3b1ecb072/sensors-18-00507-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/18f8c2d0bbc2/sensors-18-00507-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/b43c649c8ec7/sensors-18-00507-g011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/6acce7e6f605/sensors-18-00507-g012.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/bd9ff7833c8d/sensors-18-00507-g013.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/a48eaab50808/sensors-18-00507-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/fe8bdcc94945/sensors-18-00507-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/637b95d6b8e0/sensors-18-00507-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/6d3c531e949b/sensors-18-00507-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/ff9fded33444/sensors-18-00507-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/c32e9aa113a9/sensors-18-00507-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/32f95e68bacb/sensors-18-00507-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/a80f969dddfc/sensors-18-00507-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/51a3b1ecb072/sensors-18-00507-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/18f8c2d0bbc2/sensors-18-00507-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/b43c649c8ec7/sensors-18-00507-g011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/6acce7e6f605/sensors-18-00507-g012.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ab6/5855003/bd9ff7833c8d/sensors-18-00507-g013.jpg

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本文引用的文献

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Ground Penetrating Radar as a Contextual Sensor for Multi-Sensor Radiological Characterisation.探地雷达作为多传感器放射特征描述的情境传感器
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Depth profiling 137Cs and 60Co non-intrusively for a suite of industrial shielding materials and at depths beyond 50 mm.
利用碲锌镉探测器对埋地放射性废物进行远程深度估计的模型。
Sensors (Basel). 2018 May 18;18(5):1612. doi: 10.3390/s18051612.
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Determination of the depth of localized radioactive contamination by 137Cs and 60Co in sand with principal component analysis.应用主成分分析法测定沙层中 137Cs 和 60Co 的局部放射性污染深度。
Environ Sci Technol. 2011 Oct 1;45(19):8262-7. doi: 10.1021/es201619r. Epub 2011 Sep 9.
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Profiling the depth of caesium-137 contamination in concrete via a relative linear attenuation model.通过相对线性衰减模型分析混凝土中铯-137的污染深度。
Appl Radiat Isot. 2010 Apr-May;68(4-5):631-4. doi: 10.1016/j.apradiso.2009.09.046. Epub 2009 Oct 22.