【2h】

Studies of Excess Heat and Convection in a Water Calorimeter

机译:水热量计中的过量热和对流的研究

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

To explain a difference of 0.5 % between the absorbed-dose standards of the National Institute of Standards and Technology (NIST) and the National Research Council of Canada (NRCC), Seuntjens et al. suggest the fault lies with the NIST water calorimeter being operated at 22 °C and the method with which the measurements were made. Their calculations show that this difference is due to overprediction of temperature rises of six consecutive 60Co radiation runs at NIST. However, the consecutive runs they refer to were merely preliminary measurements to determine the procedure for the NIST beam calibration. The beam calibration was determined from only two consecutive runs followed by water circulation to re-establish temperature equilibrium. This procedure was used for measurements on 77 days, with 32 runs per day. Convection external to the glass cylindrical detector assembly performed a beneficial role. It aided (along with conduction) in increasing the rate of excess heat transported away from the thin cylindrical wall. This decreased the rate of heat conducted toward the axially located thermistors. The other sources of excess heat are the: (1) non-water materials in the temperature probe, and (2) exothermic effect of the once-distilled water external to the cylinder. Finite-element calculations were made to determine the separate and combined effects of the excess heat sources for the afterdrift. From this analysis, extrapolation of the measured afterdrifts of two consecutive runs to mid radiation leads to an estimated over-prediction of no more than about 0.1 %. Experimental measurements contradict the calculated results of Seuntjens et al. that convective motion (a plume) originates from the thermistors operated with an electrical power dissipation as low as 0.6 μW, well below the measured threshold of 50 μW. The method used for detecting a plume was sensitive enough to measure a convective plume (if it had started) down to about the 10 μW power level. Measurements also contradict the NRCC calculations in predicting the behavior of the NIST afterdrifts.
机译:为了解释美国国家标准技术研究院(NIST)和加拿大国家研究委员会(NRCC)的吸收剂量标准之间存在0.5%的差异,Seuntjens等人(2007年)。提示故障出在NIST水热计在22°C下操作以及进行测量的方法。他们的计算表明,这种差异是由于对NIST连续六次连续的 60 Co辐射的温度升高的预测。但是,它们所指的连续运行仅仅是初步测量,以确定NIST光束校准的程序。仅通过两次连续运行确定光束校准,然后进行水循环以重新建立温度平衡。该程序用于77天的测量,每天运行32次。玻璃圆柱探测器组件外部的对流起到了有益的作用。它有助于(以及传导)增加了从薄圆柱壁带走的多余热量。这降低了向轴向定位的热敏电阻传导的热量。多余热量的其他来源是:(1)温度探头中的非水材料,以及(2)气缸外部曾经蒸馏过的水的放热作用。进行了有限元计算,以确定了多余的热源对后漂的影响。根据该分析,将两次连续运行的测得的漂移漂移外推至中辐射会导致估计的过度预测不超过约0.1%。实验测量结果与Seuntjens等人的计算结果相矛盾。对流运动(羽状流)源自热敏电阻,其工作功耗低至0.6μW,远低于测得的50μW阈值。用于检测羽状流的方法足够灵敏,可以测量低至约10μW功率水平的对流羽状流(如果已开始)。在预测NIST漂移后的行为时,测量结果也与NRCC计算相矛盾。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号