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Using fission track analysis techniques to measure plutonium isotopic ratios.

机译:使用裂变径迹分析技术测量p同位素比率。

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The alpha decay energies for the plutonium isotopes 240 and 239 are too similar for the resolution of standard alpha spectrometry detectors to differentiate the isotopes which are therefore routinely reported as a combined activity. Knowledge of the 240/239 ratio is important to understand the source and possible previous use of the plutonium. A process was investigated to measure the 240/239 ratio using a combination of alpha spectrometry and fission track analysis methods. Samples were chemically processed to isolate plutonium which was then electro-deposited on stainless steel planchettes. The activities of the samples were determined using an alpha spectrometer. The planchettes were then placed against polycarbonate detectors and the assembly was irradiated with a neutron flux. Neutrons caused the 239Pu to fission. Fission fragments entered the polycarbonate detector and caused a trail of damage. After etching the detectors, tracks were visible under a microscope from the fission fragment damage.; The mean chemical yield value for filter and soil samples was 21.7% and 9.2% respectively. The mean 240/239 ratio for four Waste Isolation Pilot Plant filters was 0.08 +/- 0.1 and 0.7 +/- 0.9 for five Rocky Flats soil samples. Due to low sample activities and low track densities the relative uncertainties for the measured samples were 0.63 and 1.07 for the Waste Isolation Pilot Plant air filter and Rocky Flats soil reference samples respectively. Uncertainty calculations and an empirical relationship of the process supported the high relative uncertainties for those samples. The primary source of uncertainty was determined to be the probabilistic nature of the fission process. Further calculations determined that the minimum relative uncertainty can be reduced to 0.042 if the track density was increased to approximately one thousand and the sample activity was 10 Bq or greater.
机译:the同位素240和239的α衰变能量对于标准α光谱检测器的分辨率而言太相似了,以致于无法区分同位素,因此通常将其报告为联合活性。了解240/239比率对于了解the的来源和以前可能的使用非常重要。研究了使用α光谱和裂变径迹分析方法相结合的方法来测量240/239的比率。对样品进行化学处理以分离p,然后将其电沉积在不锈钢小刀上。使用阿尔法光谱仪测定样品的活性。然后,将短剑放在聚碳酸酯探测器上,并用中子通量照射该组件。中子导致239Pu发生裂变。裂变碎片进入聚碳酸酯探测器,并造成一连串的损坏。蚀刻检测器后,在显微镜下可见裂变碎片损坏的痕迹。过滤器和土壤样品的平均化学产率分别为21.7%和9.2%。对于四个Rocky Flats土壤样品,四个废物隔离中试工厂过滤器的平均240/239比为0.08 +/- 0.1和0.7 +/- 0.9。由于样品活动量低和轨道密度低,废物隔离中试工厂空气过滤器和Rocky Flats土壤参考样品的被测样品的相对不确定度分别为0.63和1.07。不确定性计算和过程的经验关系支持了这些样品的较高相对不确定性。确定不确定性的主要来源是裂变过程的概率性质。进一步的计算确定,如果磁道密度增加到大约1000,并且样品活度为10 Bq或更大,则最小相对不确定度可以降低到0.042。

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