Cederwall R T, Ricker Y E, Cederwall P L, Homan D N, Anspaugh L R
Environmental Sciences Division, Lawrence Livermore National Laboratory, Livermore, CA 94550.
Health Phys. 1990 Nov;59(5):533-40. doi: 10.1097/00004032-199011000-00005.
Historical air-sampling data measured within 320 km (200 mi) of the Nevada Test Site (NTS) have been reviewed for periods following atmospheric nuclear tests, primarily in the 1950s. These data come mostly from high-volume air samplers, with some from cascade-impactor samplers. Measurements considered here are for beta radiation from gross fission products. The resulting air-quality data base is comprised of almost 13,000 samples from 42 sampling locations downwind of the NTS. In order to compile an accurate air-quality data base for use in estimating exposure via inhalation, raw data values were sought where possible, and the required calculations were performed on a computer with state-of-the-art algorithms. The data-processing procedures consisted of (1) entry and error checking of historical data; (2) determination of appropriate background values, air-sampling volumes, and net air concentrations; and (3) calculation of integrated air concentration (C) for each sample (considering fallout arrival times). Comparing C values for collocated high-volume and cascade-impactor samplers during the Upshot-Knothole series showed similar lognormal distributions, but with a geometric mean C for cascade impactors about half that for the high-volume air samplers. Overall, the uncertainty in C values is about a factor of three. In the past, it has been assumed that C could be related to ground deposition by a constant having units of velocity. In our data bases, simultaneous measurements of air concentration and ground deposition at the same locations were not related by a constant; indeed, there was a great amount of scatter. This suggests that the relationship between C and ground deposition in this situation is too complex to be treated adequately by simple approaches.
已对内华达试验场(NTS)320公里(200英里)范围内在大气核试验之后的时间段(主要是20世纪50年代)所测得的历史空气采样数据进行了审查。这些数据大多来自大容量空气采样器,部分来自串级冲击器采样器。此处所考虑的测量针对的是总裂变产物的β辐射。由此形成的空气质量数据库由来自NTS下风处42个采样地点的近13,000个样本组成。为了编制一个准确的空气质量数据库以用于通过吸入估算暴露情况,尽可能寻找原始数据值,并在具有先进算法的计算机上进行所需的计算。数据处理程序包括:(1)历史数据的录入与错误检查;(2)确定合适的背景值、空气采样体积和净空气浓度;以及(3)计算每个样本的综合空气浓度(C)(考虑沉降到达时间)。对“向上钻洞”系列期间并置的大容量和串级冲击器采样器的C值进行比较,结果显示出相似的对数正态分布,但串级冲击器的几何平均C值约为大容量空气采样器的一半。总体而言,C值的不确定性约为三倍。过去曾假定C可以通过一个具有速度单位的常数与地面沉降相关。在我们的数据库中,同一地点的空气浓度和地面沉降的同步测量结果并非由一个常数相关联;实际上,存在大量离散数据。这表明在这种情况下,C与地面沉降之间的关系过于复杂,无法通过简单方法进行充分处理。