Determination of uranium in fertilisers using fission track method

Trace contents of uranium in various commercial fertilizers e.g. ureas, superphosphates, diammonium phosphates have been determined using fission track etch technique. The uranium content in ureas varies from .05 to 1.3 mg kg^–1 whereas in superphosphates it varies linearly with phosphate content.     

Object Kinetic Monte Carlo calculations of irradiated Fe-Cr dilute alloys: The effect of the interaction radius between substitutional Cr and self-interstitial Fe

Object Kinetic Monte Carlo models allow for the study of the evolution of the damage created by irradiation to time scales that are comparable to those achieved experimentally. Therefore, the essential Object Kinetic Monte Carlo parameters can be validated through comparison with experiments. However, this validation is not trivial since a large number of parameters is necessary, including migration energies of point defects and their clusters, binding energies of point defects in clusters, as well as the interaction radii. This is particularly cumbersome when describing an alloy, such as the Fe-Cr system, which is of interest for fusion energy applications. In this work we describe an Object Kinetic Monte Carlo model for Fe-Cr alloys in the dilute limit. The parameters used in the model come either from density functional theory calculations or from empirical interatomic potentials. This model is used to reproduce isochronal resistivity recovery experiments of electron irradiated dilute Fe-Cr alloys performed by Abe and Kuramoto. The comparison between the calculated results and the experiments reveal that an important parameter is the capture radius between substitutional Cr and self-interstitial Fe atoms. A parametric study is presented on the effect of the capture radius on the simulated recovery curves.     

东昆仑南部带磷灰石裂变径迹分析的地质意义

通过东昆仑南部带出露的上二叠统地层磷灰石裂变径迹分析,研究区内的构造演化特征。南北向剖面中4个砂岩样品的年龄为(48±3)—(89±8)Ma,径迹长度为(10.7±2.3)—(10.8±2.2)μm。裂变径迹年龄是区内逆冲演化的反映,长度分布体现了在退火带持续较长以及受隆升控制的特点。总体上具有3阶段热演化历史,约107Ma前后发生一次较为快速的冷却隆升作用,继之于约80Ma开始出现相对平静期,然后在6—12Ma进入快速冷却期,冷却速率为5.3—9.8℃/Ma或者106—196m/Ma。     

利用磷灰石裂变径迹定年方法探讨东大别山地区中、新生代构造抬升样式

利用裂变径迹定年方法对东大别山地区进行了磷灰石裂变径迹年龄值和其空间分布样式及对中新生代构造活动示踪意义的初步探讨 ,并改进了传统的径迹统计方法。结果表明 ,研究区磷灰石裂变径迹年龄值为 5 9.4± 3.4— 10 5 .6± 9.8Ma,具有跨度较大以及由东向西趋向增大的特点 ;研究区自 95Ma以来其构造抬升是缓慢且不均匀 ;晓天 -磨子潭断裂中部在第三纪可能有逆冲 ;断裂活动应是该区构造抬升的主要控制因素     

乏燃料组件非破坏性测量的叉形探测器

采用总γ和无源中子测量方法建立了叉形探测器。叉形探测器可用于后处理和贮存工厂中ＰＷＲ和ＢＷＲ型的乏燃料组件的燃耗、冷却时间、总钚和总裂变物质含量的测定。     

裂变产物在黄河泥,沙上吸附的多示踪剂法研究

使用离线γ能谱法和多示踪剂技术研究了钛的裂变产物在黄河水中泥和沙上的吸附行为，测定了９个裂变产物的吸附比，实验结果和献值进行了比较，并根据元素电子结合能进行讨论。     

福建漳州复式岩体中晶洞石榴子石的裂变径迹研究

对福建漳州复式岩体中晶洞石榴子石的裂变径迹定年进行了可行性研究，经测定确认其为含锰量甚高的锰铝榴石，铀浓度变化范围为０．２－１．８μｇ／ｇ，裂变径迹年龄为７３．４±２．１Ｍａ，诱发裂变径迹和自发理解变径变迹的长度分别为１１．５±０．７μｍ和１１．０±０．８μｍ。     

钍-铀燃料后处理中新萃取剂的研究 Ⅰ.双取代酰胺类的研究及其结构与性能的关系

合成并研究了10种双取代酰胺萃取铀、钍、裂片元素的情况,结果表明,取代己内酰胺的萃取性能优于非环状双取代酰胺。和1mol/1的TBP相比,取代己内酰胺萃取铀的能力比TBP强,萃取钍的能力和TBP接近。除OCLA外,酰胺对于铀钍的分离性能均比TBP好,酰胺对Zr-Nb的去污性能优于TBP。还初步探讨了酰胺类萃取剂结构与性能的关系。