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Survey Methodology for the Activation of Beamline Components in an Electrostatic Proton Accelerator 静电质子加速器中光束线元件活化的测量方法
Pub Date : 1900-01-01 DOI: 10.12950/RSM.200813
G. Yoshida, H. Matsumura, Hajime Nakamura, A. Toyoda, K. Masumoto, T. Miura, K. Sasa, T. Moriguchi
To establish a systematic guideline for accelerator decommissioning, as a case study, beamline activation of 12 MeV-proton electrostatic accelerator was investigated employing a survey meter and g -ray spectrometers. Beam loss points where reflected as high dose-rate area were identified, and generated nuclides and their activities were determined. Almost beamline components are made from stainless steel and 52 Mn and 56 Co were detected as principal induced activities. It was found that the 56 Co activity significantly contribute to the dose rate value denoted on the survey meter. From the beam operation history and the monitor currents of Faraday-cups, we revealed the beam loss on a certain point significantly reflects the 52 Mn activity on there. Induced activities of 52 Mn and 56 Co on the certain point of the beamline could be reproduced by the contact dose-rate on that point.
为了建立系统的加速器退役指导方针,以12 mev质子静电加速器为例,采用测量仪和g射线能谱仪对其束流激活进行了研究。确定了反映为高剂量率区域的光束损耗点,并确定了产生的核素及其活性。几乎束线成分由不锈钢制成,检测到52 Mn和56 Co为主要诱导活性。结果发现,56 Co的活性对测量仪上所示的剂量率值有显著影响。从法拉第杯的束流运行历史和监测电流来看,我们发现某一点上的束流损耗显著地反映了该点上的52mn活度。52 Mn和56 Co在光束线某一点上的诱导活性可以用该点上的接触剂量率来再现。
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引用次数: 2
Transfer Rates of 225Ac to Exhaust Air, Surface, and Waste Water under Chemical Operations 在化学操作下,225Ac向废气,表面和废水的传输速率
Pub Date : 1900-01-01 DOI: 10.12950/rsm.191219
T. Yamamura, K. Shirasaki, H. Kikunaga, Kojiro Nagata, Zijian Zhang, K. Washiyama, A. Toyoshima, T. Yoshimura, A. Shinohara
1) Laboratory of Alpha-ray Emitters, Institute for Materials Research, Tohoku University, Miyagi 980-8577, Japan 2) Institute for Integrated Radiation and Nuclear Science, Kyoto University, Osaka 590-0494, Japan 3) Research Center for Electron Photon Science, Tohoku University, Miyagi 982-0826, Japan 4) Radioisotope Research Center, Institute for Radiation Sciences, Osaka University, Osaka 565-0871, Japan 5) Department of Chemistry, Graduate School of Science, Osaka University, Osaka 560-0043, Japan 6) Advanced Clinical Research Center, Fukushima Medical University, Fukushima 960-1295, Japan 7) Division of Science, Institute for Radiation Sciences, Osaka University, Osaka 560-0043, Japan
1)东北大学材料研究所α射线发射体实验室,日本宫城980-8577 2)京都大学综合辐射与核科学研究所,日本大阪590-0494 3)东北大学电子光子科学研究中心,日本宫城982-0826 4)大阪大学辐射科学研究所放射性同位素研究中心,日本大阪565-0871 5)大阪大学理学院化学系,大阪560-0043日本福岛医科大学先进临床研究中心,福岛960-1295;大阪大学放射科学研究所科学部,大阪560-0043
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引用次数: 2
Examination of Low-Sodium Salts for Radiation Education 辐射教育用低钠盐的检验
Pub Date : 1900-01-01 DOI: 10.12950/RSM.200714
T. Kawano
Various materials containing the natural radioisotope potassium-40 ( 40 K) are often used for radiation education, but their radioactivity is not usually known. In the present study, low-sodium salts (LS salts) were purchased at several shopping malls in Japan, and the radioactivity of 40 K in the LS salts were calculated from the nutritional tables and cutting down rates (CDR) printed on their packages. CDR is the percentage of sodium chloride (NaCl) in common salts replaced with potassium chloride (KCl). Solid disks were fabricated from the LS salts and KCl reagent, and their radiation count rates (cps/g) were measured by GM survey meter and CsI spectrometer. In these measurements, the KCl disk was used to determine the conversion factors (Bq/cps) for determining radioactivity of 40 K in the LS salts. It was found that the experimentally obtained radioactivity generally coincides with that calculated from the nutritional tables, but it does not always coincide with that calculated from CDR.
含有天然放射性同位素钾-40 (40k)的各种材料经常用于辐射教育,但它们的放射性通常不为人所知。在本研究中,在日本的几个购物中心购买了低钠盐(LS盐),并根据其包装上印刷的营养表和削减率(CDR)计算了低钠盐中40k的放射性。CDR是氯化钾(KCl)取代普通盐中氯化钠(NaCl)的百分比。将LS盐和KCl试剂制成固体圆盘,用GM测量仪和CsI光谱仪测定其辐射计数率(cps/g)。在这些测量中,KCl圆盘用于确定转换因子(Bq/cps),以确定LS盐中40k的放射性。实验得到的放射性与营养表计算的结果基本一致,但与CDR计算的结果并不总是一致。
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引用次数: 0
137Cs Soil to Rice Transfer Factor and Soil Properties: Fukushima and Kawauchi Case Study 137Cs土壤对水稻的转移因子和土壤性质:福岛和川内案例研究
Pub Date : 1900-01-01 DOI: 10.12950/rsm.220131
W. Bekelesi, Triyono Basuki, Satoru Nakashima
The long-term migration of 137 Cs in the environment is mainly through the 137 Cs adsorbed on the dispersed soil particles of various sizes. However, the transfer of 137 Cs from soil to plant, especially rice plant, remains questionable. The objective of this study is to determine the relation among soil characteristics, 137 Cs distribution and transfer factor (TF) of 137 Cs from soil to rice. In this study paddy fields in Kawauchi and Fukushima were chosen. This is because more studies have focused only on one sampling field and there have not been much discussion comparing various fields as envisaged in this study. The results have shown that TF for Kawauchi is 5-fold higher than that of Fukushima. Physicochemical properties of the soils showed that Fukushima soil has less percentage of exchangeable 137 Cs and high percentage of exchangeable K in contrast to Kawauchi soil. These factors likely disturbed the transfer of 137 Cs from soil into the rice plant. Powder X-ray diffraction has shown that Fukushima soil is rich in micaceous minerals which also release a lot of K + to distract the 137 Cs transfer. This study suggests that the presence of micaceous minerals in the soil would be a good amendment for radiocesium-contaminated rice paddy fields in enhancing adsorption of 137 Cs in the soil. However, there is still a need to investigate adsorption kinetics of 137 Cs to ascertain higher values of TF in Kawauchi soil.
137 - Cs在环境中的长期迁移主要是通过分散在不同大小土壤颗粒上的137 - Cs吸附。然而,137cs从土壤到植物,特别是水稻植株的转移仍是一个问题。本研究的目的是确定土壤特征、137cs分布和137cs从土壤到水稻的转移因子(TF)之间的关系。本研究选取川内和福岛的稻田为研究对象。这是因为更多的研究只集中在一个采样领域,并没有像本研究设想的那样对各个领域进行太多的比较讨论。结果显示,川内市的辐射强度是福岛的5倍。土壤理化性质表明,与川内土壤相比,福岛土壤具有较低的交换性137cs百分比和较高的交换性K百分比。这些因素可能干扰了137cs从土壤向水稻植株的转移。粉末x射线衍射表明,福岛土壤富含云母矿物,同时释放大量K +分散137cs转移。该研究表明,土壤中云母矿物的存在可能是放射性污染稻田对土壤中137cs吸附的良好改良剂。然而,仍需要研究137 Cs的吸附动力学,以确定川内土壤中更高的TF值。
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引用次数: 0
Distinction of Migration of Strontium-90 and Cesium-137 for Fukushima Soil and Sediment following the Fukushima Accident 福岛核事故后土壤沉积物中锶-90和铯-137的迁移特征
Pub Date : 1900-01-01 DOI: 10.12950/rsm.220527
W. Bekelesi, Triyono Basuki, S. Higaki, Satoru Nakashima
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引用次数: 0
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Radiation Safety Management
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