Temperature dependence of the Fricke dosimeter and spur expansion time in the low-LET high-temperature radiolysis of water up to 350°C: A Monte-Carlo simulation study
Temperature dependence of the Fricke dosimeter and spur expansion time in the low-LET high-temperature radiolysis of water up to 350°C: A Monte-Carlo simulation study
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在高达 350°C 的低 LET 高温水辐射分解中,Fricke 剂量计和杂散膨胀时间的温度依赖性:蒙特卡罗模拟研究
DOI:
10.1039/c1cp20293f
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发表时间:
2011
期刊:
影响因子:
--
通讯作者:
Y. Katsumura and J-P. Jay-Gerin
中科院分区:
文献类型:
--
作者:
S. Sanguanmith;Y. Muroya;T. Tippayamontri;J. Meesungnoen;M. Lin;Y. Katsumura and J-P. Jay-Gerin
Monte-Carlo simulations of the radiolysis of the ferrous sulfate (Fricke) dosimeter with low-linear energy transfer (LET) radiation (such as 60Co γ-rays or fast electrons) have been performed as a function of temperature from 25 to 350 °C. The predicted yields of Fe2+ oxidation are found to increase with increasing temperature up to ∼100–150 °C, and then tend to remain essentially constant at higher temperatures, in very good agreement with experiment. By using a simple method based on the direct application of the stoichiometric relationship that exists between the ferric ion yields so obtained G(Fe3+) and the sum {3 [g(e−aq + H˙) + g(HO2˙)] + g(˙OH) + 2 g(H2O2)}, where g(e−aq + H˙), g(HO2˙), g(˙OH), and g(H2O2) are the primary radical and molecular yields of the radiolysis of deaerated 0.4 M H2SO4 aqueous solutions, the lifetime (τs) of the spur and its temperature dependence have been determined. In the spirit of the spur model, τs is an important indicator for overlapping spurs, giving the time required for the changeover from nonhomogeneous spur kinetics to homogeneous kinetics in the bulk solution. The calculations show that τs decreases by about an order of magnitude over the 25–350 °C temperature range, going from ∼4.2 × 10−7 s at 25 °C to ∼5.7 × 10−8 s at 350 °C. This decrease in τs with increasing temperature mainly originates from the quicker diffusion of the individual species involved. Moreover, the observed dependence of G(Fe3+) on temperature largely reflects the influence of temperature upon the primary free-radical product yields of the radiolysis, especially the yield of H˙ atoms. Above ∼200–250 °C, the more and more pronounced intervention of the reaction of H˙ atoms with water also contributes to the variation of G(Fe3+), which may decrease or increase slightly, depending on the choice made for the rate constant of this reaction. All calculations reported herein use the radiolysis database of Elliot (Atomic Energy of Canada Limited) and Bartels (University of Notre Dame) that contains all the best currently available information on the rate constants, reaction mechanisms, and g-values in the range 20 to 350 °C.