首页|高通量试验堆G10中心孔道用于39Ar-40Ar定年辐照参数探讨

高通量试验堆G10中心孔道用于39Ar-40Ar定年辐照参数探讨

The irradiation parameters research of G10 center channel in high flux engineering test reactor for 39Ar-40Ar dating samples

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含钾岩石矿物中的 39K经反应堆快中子福照后产生 39Ar是 39Ar-40Ar法定年的前提,国内可应用于样品辐照的反应堆资源紧缺、不同类型样品辐照参数缺乏,制约我国高精度 39Ar-40Ar定年技术的发展.本次工作首次针对高通量试验堆具有高中子通量的G10中心孔道辐照参数进行探讨.通过辐照ZBH-25黑云母标准、CaF2晶体和K2SO4晶体,探讨中子通量轴向梯度变化特征、反应堆辐照孔道 39ArK产率以及副反应校正因子.结果表明,辐照14 h和35 h的J值均呈现二次线性关系分布(R2≥0.979),与中子通量余弦函数分布特征相符,中子通量梯度变化小,分别为0.88和0.45%·cm-1,表明石英管处于中子活性区轴向稳定区域,有利于准确计算待测样品辐照参数J值;孔道内 39ArK产率介于2.32×10-12~2.99×10-12(mol·h-1·%K2O)之间,高于同反应堆的外围孔道以及其他反应堆报道值;辐照K2SO4 晶体得到(40Ar/39Ar)K校正因子平均值为 2.96×10-3,诱发产生 40Ar占总 40Ar比例为(29±6)%;辐照CaF2 晶体获得(36Ar/37Ar)Ca校正因子平均值为2.54×10-4、(39Ar/37Ar)Ca校正因子平均值为7.31×10-4,诱发产生 36Ar占总 36Ar比例为(97±1)%,中子通量升高可以减小副反应校正因子计算时大气氩的干扰;ZBH-25黑云母标准物质测得的坪年龄为132.89±0.93 Ma(2σ,MSWD=0.56),与前人报道的132.7±0.6 Ma(2σ)年龄值基本一致,证明高通量试验堆G10中心孔道可以满足 39Ar-40Ar定年样品辐照要求,此孔道尤其适用于年龄老,低K/Ca比的样品辐照.
39Ar produced from 39K in potassium-containing rocks and minerals that is irradiated by fast neutrons in nuclear reactor is the basic of 39Ar-40Ar dating.There are few reactor resources for sample irradiation in China and lacked of irradiation parameters for different types of samples,which limits the development of high-precision 39Ar-40Ar dating.In this work,the irradiation parameters of G10 center channel with high neutron flux in High Flux Engineering Test Reactor(HFETR)were discussed for the first time.By irradiating biotite standard ZBH-25,calcium salt and potassium salt,the axial gradient of neutron flux,the production of 39ArK and the correction factor of interfering reaction were investigated.The results show that the J values of biotite standard ZBH-25 for 14 h and 35 h irradiation present a quadratic linear distribution(R2≥0.979),which is corresponding to the cosine function distribution of neutron flux,the neutron flux gradients are 0.88%·cm-1 and 0.45%·cm-1 which the variation is small,respectively indicating that the quartz tube is in the axially stable region of neutron flux and it is helpful to accurately calculate the J value of the sample.The production of 39ArK is 2.32×10-12 to 2.99×10-12(mol·h-1·%K2O),which is higher than the values of the outer channel of HFETR and other reactors.The average value of correction factor(40Ar/39Ar)K obtained by the irradiation of K2SO4 crystal is 2.96×10-3,and the proportion of induced 40Ar to the total 40Ar is(29±6)%,the average value of correction factor(36Ar/37Ar)Ca obtained by irradiation of CaF2 crystal is 2.54×10-4,the average value of correction factor(39Ar/37Ar)Ca is 7.31×10-4,and the proportion of induced 36Ar to the total 36Ar is(97±1)%.The correction factor results show that the increase of neutron flux can reduce the interference of atmospheric argon when calculating.The plateau age of biotite standard ZBH-25 is 132.89±0.93 Ma(2σ,MSWD=0.56),which is the same with the 132.7±0.6 Ma(2σ)age issued by previous studies.In summary,the G10 center channel in HFETR can satisfy the irradiation requirements of 39Ar-40Ar dating samples,especially is suitable for samples with old age and low K/Ca ratio.

HFETRG10 center channel39Ar-40Ar datingIrradiation parameters

石晓、刘汉彬、张佳、张建锋、韩娟、石雅静、石健

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核工业北京地质研究院,北京,100029

武昌船舶重工集团有限公司,湖北 武汉 430416

高通量试验堆 G10孔道 39Ar-40Ar定年 辐照参数

核工业北京地质研究院自主研发项目

测ZY2401

2024

世界核地质科学
核工业北京地质研究院

世界核地质科学

CSTPCD
影响因子:0.463
ISSN:1672-0636
年,卷(期):2024.41(5)