A Suitability Study on the Indicator Isotopes for Graphite Isotope Ratio Method (GIRM)

Jinseok Han, Junkyung Jang, Hyun Chul Lee
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引用次数: 1

Abstract

The Graphite Isotope Ratio Method (GIRM) can verify non-proliferation of nuclear weapon by estimating the total plutonium production in a graphite-moderated reactor. Using the reactor, plutonium is generated and accumulated through the 238U neutron capture reaction, and impurities in the graphite are converted to nuclides due to the nuclear reaction. Therefore, the amount of plutonium production and concentration of the impurities are correlated. However, the plutonium production cannot be predicted using only the absolute concentration of the impurities. It can only be predicted when the initial concentration of the impurities is obtained because the concentration, at a certain time, depends on it. Nevertheless, the ratios of the isotopes in an element are known regardless of the impurity of an element in the graphite moderator. Thus, the correlation between the isotope ratio and amount of plutonium produced helps predict plutonium production in a graphite-moderated reactor. Boron, Lithium, Chlorine, Titanium, and Uranium are known as indicator elements in the GIRM. To assess whether the correlation between the indicator isotope and amount of plutonium produced is independent of the initial concentration of the impurities, four different impurity compositions of graphite were used. 10B/11B, 36Cl/35Cl, 48Ti/49Ti, and 235U/238U had a consistent correlation with the cumulative plutonium production, regardless of the initial impurity concentration of the graphite, because these isotopes were not generated through the nuclear reaction of other elements. On the other hand, the correlation between 6Li/7Li and plutonium production depended on the initial concentration of the impurities in graphite. Although 7Li can be produced through the neutron capture reaction of 6Li, the (n, α) reaction of 10B was the major source of 7Li. Therefore, the initial concentration of 10B affected the production of 7Li, making Li unsuitable as an indicator element for the GIRM.
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石墨同位素比值法(GIRM)指示同位素适用性研究
石墨同位素比值法(GIRM)可以通过估算石墨慢化反应堆的钚总产量来验证核武器的不扩散。利用该反应堆,通过238U中子捕获反应生成和积累钚,石墨中的杂质由于核反应而转化为核素。因此,钚的产量和杂质的浓度是相关的。然而,钚的产量不能只用杂质的绝对浓度来预测。只有在获得杂质的初始浓度时才能预测它,因为在某一时刻的浓度取决于它。然而,无论石墨慢化剂中元素的杂质含量如何,元素中同位素的比值都是已知的。因此,同位素比率与钚产量之间的相关性有助于预测石墨慢化反应堆中的钚产量。硼、锂、氯、钛和铀是GIRM中的指示元素。为了评估指示同位素与钚产量之间的相关性是否独立于杂质的初始浓度,使用了四种不同的石墨杂质组成。10B/11B、36Cl/35Cl、48Ti/49Ti和235U/238U与累积钚产量具有一致的相关性,与石墨的初始杂质浓度无关,因为这些同位素不是通过其他元素的核反应产生的。另一方面,6Li/7Li与钚产量的相关性取决于石墨中杂质的初始浓度。虽然7Li可以通过6Li的中子俘获反应产生,但10B的(n, α)反应是7Li的主要来源。因此,10B的初始浓度影响了7Li的生成,使得Li不适合作为GIRM的指示元素。
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