环境中子通量随水土深度的变化

K. Komura, N. K. Ahmed, A.H.El-Kamel, M. Yousef
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引用次数: 2

摘要

作为生物环境中中子通量研究的一部分,通过197 Au(n, (cid:1)) 198 Au相互作用在金中引起的放射性,测量了慢中子随水和土壤深度的变化。在0 ~ 100 cm的淡水和20 ~ 400 cm的海水中进行的测量表明,热中子通量在10 cm左右出现峰值,然后随着水深的增加逐渐降低。海水中的深度剖面与淡水中的深度剖面几乎相同。在0~ 60 cm的土壤中,热中子通量在5 cm处达到峰值,在10~30 cm范围内呈肩状下降,随着深度的增加,热中子通量逐渐迅速下降到60 cm。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variation of Environmental Neutron Flux with the Depth of Water and Soil
As a part of interest in the study of the neutron flux in biological environments, variations of slow neutrons with depth of water and soil were measured through the radioactivity induced in gold by 197 Au(n, (cid:1) ) 198 Au interaction. The measurements made for 0-100 cm in fresh water and 20-400 cm in sea water showed that the thermal neutron flux showed peak at around 10 cm depth and then gradually decreased with depth in water. The depth profiles in seawater were almost the same profile as freshwater. In the case of soil made for 0-60 cm, thermal neutron flux showed a peak at 5 cm then through a shoulder-like decrease during 10~30 cm range and decreased with depth gradually rapidly to 60 cm.
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