两种中子通量热化程度不同的辐照设施的裂变径迹定年zeta标定常数的直接比较

Seong-Cheon Shin , Susumu Nishimura
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引用次数: 5

摘要

Zeta (ζ)常数是用锆石、磷灰石和榍石年龄标准测定的,用于裂变径迹定年的系统校准。相同的晶体在两个中子通量热化程度明显不同的设施中进行了双重检查:韩国原子能研究所(KAERI) TRIGA III反应堆的辐照坑-6 (IP-6)和京都大学研究反应堆(kor -1)的石墨气动管(GrPn), Au的Cd比分别为12.5和~ 200。最终单一加权平均ζ基线的误差(2σ)为:来自KAERI IP-6的SRM612为324.5±7.9,CN1为110.9±2.7,CN2为118.8±2.9;KUR GrPn的SRM612、CN1和CN2分别为333.7±8.5、109.0±2.8和119.5±3.1。两个设施的最终结果表明,尽管在误差(2σ)范围内大致一致,但CN1和CN2的ζ值在ζs上具有极好的一致性,而SRM612-ζ值存在差异(~ 2.8%)。KAERI IP-6中ϱdCN1/ϱdSRM612、ϱdCN2/ϱdSRM612和ϱimineral/ϱdSRM612的较低比例(~ 2.5-4%)强烈暗示了ζSRM6l2的降低。两个设施中ζCN1和ζCN2的一致性表明,矿物与CN1或CN2之间232Th/2355U比值的巨大差异可能不会显著影响热中子剂量测定,即使磷灰石与剂量计玻璃的比值差异最大。238U在超热能区和快中子能区的反应截面(n,f)大于2322Th,这也表明,无论三种矿物的Th/U比如何,在耗尽U的SRM612玻璃中所见的238U /235U比的差异可能比232Th/235U比的差异更显著地影响热中子剂量学。因此,ζSRM612的差异主要是由于在热化程度较低的KAERI IP-6中,非热中子诱导的238U裂变对热中子剂量学的贡献较大。因此,从KAERI IP-6得到的最终的ζSRM6l1精度明显降低。CN1和CN2的最终ζ基线,独立于两个设施,被推荐用于准确的裂变径道分析,优先于SRM612-ζ基线,即使在热化良好的设施,例如KUR GrPn。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Direct comparison of zeta calibration constants for fission-track dating by double-checking of two irradiation facilities with different degrees of neutron flux thermalization

Zeta (ζ) constants were determined using zircon, apatite and sphene age standards for a systematic calibration of fission-track dating. Identical crystals were double-checked in two facilities having significantly different degrees of neutron flux thermalization: Irradiation Pit-6 (IP-6) of the Korea Atomic Energy Research Institute (KAERI) TRIGA III reactor and the Graphite Pneumatic Tube (GrPn) of the Kyoto University Research Reactor (KUR-1) which have Cd ratios of 12.5 and ∼200, respectively, for Au. The final single weighted mean ζ baselines are given with errors (2σ) as: 324.5 ± 7.9 for SRM612, 110.9±2.7 for CN1 and 118.8±2.9 for CN2 from KAERI IP-6; and 333.7±8.5 for SRM612, 109.0±2.8 for CN1 and 119.5 ± 3.1 for CN2 from KUR GrPn. The final results from both facilities show anexcellent consistency in ζs for CN1 and CN2 and a discrepancy ( ∼2.8%) in SRM612-ζ values despite of a rough agreement within the error (2σ). Lower ratios (∼2.5–4%) of ϱdCN1/ϱdSRM612, ϱdCN2/ϱdSRM612 and ϱimineral/ϱdSRM612 in KAERI IP-6 strongly imply such a decrease of ζSRM6l2.

The consistency in ζCN1 and ζCN2 in both facilities implies that the large difference in 232Th/2355U ratio between the mineral and CN1 or CN2 may not significantly affect thermal neutron dosimetry, even for apatite which has the largest difference of the ratio against dosimeter glasses. The larger (n,f ) reaction cross-section of 238U than that of 2322Th in epithermal and fast neutron energy regions also suggests that the difference of 238U /235U ratio as seen in glass SRM612, which has depleted U, may affect the thermal neutron dosimetry more significantly than that of 232Th/235U ratio regardless of Th/U ratios of the three minerals. Therefore, the discrepancy in ζSRM612 results mainly from the larger contribution of 238U fission induced by non-thermal neutrons to the thermal neutron dosimetry in the less thermalized KAERI IP-6. In consequence, the final ζSRM6l1 from KAERI IP-6 is significantly less precise. The final ζ baselines for CN1 and CN2, obtained independently from both facilities, are to be recommended for accurate fission-track analyses in preference to the SRM612-ζ baseline, even in the well-thermalized facility, e.g. KUR GrPn.

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