Parsa Bahman, Obed Reynaldo N, Nemeth William K, Suozzo Gail P
New Jersey Department of Health and Senior Services, Radioanalytical Services, P.O. Box 361, Trenton, NJ 08625-0361, USA.
Health Phys. 2005 Dec;89(6):660-6. doi: 10.1097/01.hp.0000175147.43222.88.
The current federal and New Jersey State regulations have greatly increased the number of gross alpha and radium tests for public and private drinking water supplies. The determination of radium isotopes in water generally involves lengthy and complicated processes. In this study, a new approach is presented for the determination of gross alpha, 224Ra, 226Ra, and 228Ra activities in water samples. The method includes a single sample preparation procedure followed by alpha counting and gamma-ray spectroscopy. The sample preparation technique incorporates an EPA-approved co-precipitation methodology for gross alpha determination with a few alterations and improvements. Using 3-L aliquots of sample, spiked with 133Ba tracer, the alpha-emitting radionuclides are isolated by a BaSO4 and Fe(OH)3 co-precipitation scheme. First the gross alpha-particle activity of the sample is measured with a low-background gas-flow proportional counter, followed by radium isotopes assay by gamma-ray spectroscopy, using the same prepared sample. Gamma-ray determination of 133Ba tracer is used to assess the radium chemical recovery. The 224Ra, 226Ra, and 228Ra activities in the sample are measured through their gamma-ray-emitting decay products, 212Pb, 214Pb/214Bi, and 228Ac, respectively. In cases where 224Ra determination is required, the gamma-ray counting should be performed within 2-4 d from sample collection. To measure 226Ra activity in the sample, the gamma-ray spectroscopy can be repeated 21 d after sample preparation to ensure that 226Ra and its progeny have reached the equilibrium state. At this point, the 228Ac equilibration with parent 228Ra is already established. Analysis of aliquots of de-ionized water spiked with NIST-traceable 230Th, 224Ra, 226Ra, and 228Ra standards demonstrated the accuracy and precision of this method. Various performance evaluation samples were also assayed for gross alpha as well as radium isotope activity determination using this procedure and the results were in close agreement with the assigned values. In addition, method comparison results of actual sample analyses agreed well with the ones performed using EPA-approved procedures. With a 3-L sample aliquot and 1,000-min counting time, the average gross alpha minimum detectable concentration (MDC) was about 0.002 Bq L(-1). The average MDC's for 224Ra, 226Ra, and 228Ra were 0.034 Bq L(-1), 0.017 Bq L(-1), and 0.036 Bq L(-1), respectively, based on a 3-L sample aliquot, 85% chemical yield, 40% intrinsic Ge detector, and 1,000-min count time. This method combines and simplifies the analytical procedures and reduces labor while achieving the precision, accuracy, and minimum detection limit requirements of EPA regulations.
当前的联邦法规和新泽西州法规大幅增加了对公共和私人饮用水供应中总α和镭的检测数量。水中镭同位素的测定通常涉及冗长且复杂的过程。在本研究中,提出了一种测定水样中总α、224Ra、226Ra和228Ra活度的新方法。该方法包括一个单一的样品制备程序,随后进行α计数和γ射线能谱分析。样品制备技术采用了经美国环境保护局(EPA)批准的共沉淀方法来测定总α,并做了一些改动和改进。使用3升加有133Ba示踪剂的等分试样,通过BaSO4和Fe(OH)3共沉淀方案分离发射α粒子的放射性核素。首先用低本底气流正比计数器测量样品的总α粒子活度,然后使用相同的制备好的样品通过γ射线能谱分析测定镭同位素。通过γ射线测定133Ba示踪剂来评估镭的化学回收率。样品中的224Ra、226Ra和228Ra活度分别通过它们发射γ射线的衰变产物212Pb、214Pb/214Bi和228Ac来测量。在需要测定224Ra的情况下,γ射线计数应在样品采集后2 - 4天内进行。为了测量样品中的226Ra活度,可在样品制备后21天重复进行γ射线能谱分析,以确保226Ra及其子体达到平衡状态。此时,228Ac与其母体228Ra的平衡已经建立。对加有可溯源至美国国家标准与技术研究院(NIST)的230Th、224Ra、226Ra和228Ra标准物质的去离子水等分试样进行分析,证明了该方法的准确性和精密度。还使用此程序对各种性能评估样品进行了总α以及镭同位素活度测定,结果与指定值非常吻合。此外,实际样品分析的方法比较结果与使用经EPA批准的程序所得到的结果吻合良好。对于3升样品等分试样和1000分钟的计数时间,总α的平均最低可检测浓度(MDC)约为0.002 Bq L(-1)。基于3升样品等分试样、8