Empirical relationship for predicting radiocesium inventory and concentration in forest soils from ambient dose equivalent rates under quasi-equilibrium conditions
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Updated: Jul 10, 2026

Measuring Fluxes of Mineral Nutrients and Toxicants in Plants with Radioactive Tracers
Published on: August 22, 2014
Wataru Sakashita1, Yoshiki Shinomiya2, Tadashi Sakata3
1Center for Forest Restoration and Radioecology, Forestry and Forest Products Research Institute (FFPRI), 1 Matsunosato, Tsukuba, Ibaraki, 305-8687, Japan; Department of Forest Soils, FFPRI, 1 Matsunosato, Tsukuba, Ibaraki, 305-8687, Japan.
Abstract:
Following the Fukushima Daiichi Nuclear Power Plant accident, radiocesium (134Cs and 137Cs) cycling between forest trees and soils has approached a quasi-equilibrium state. In forest radioecology, efforts are increasingly being made to generalize soil-to-tree aggregated transfer factors (Tag), defined as the 137Cs activity concentration in aboveground tree tissues divided by the total soil 137Cs inventory, across diverse sites. However, Tag estimation requires time- and resource-demanding measurements of 137Cs inventory in forest soils. Therefore, we proposed a practical and efficient method for estimating soil 137Cs inventory using ambient dose equivalent rate (Ḣ∗(10)) as an alternative indicator. We established an empirical relationship between Ḣ∗(10) (1 m above ground) and 137Cs inventory based on data collected from 14 sites in Fukushima Prefecture in 2023, including both evergreen coniferous and deciduous broad-leaved forests. The relationship followed a power-law form: 5.86 × 105 × Ḣ∗(10)0.874. Its predictions, based on Ḣ∗(10), were validated using measurements at 11 independent study sites made in 2024, not included in the model development. This empirical relationship is expected to facilitate the more time- and cost-efficient collection of Tag data across diverse forest ecosystems. In addition, using orthogonal regression, we determined the upper 95% safety limit for estimating radiocesium activity concentration in forest soils using Ḣ∗(10). This upper limit is expected to help reduce the probability that concentrations estimated using Ḣ∗(10) exceed the thresholds specified in forest decontamination and forestry operation guidelines.
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