Bojanowski R, Radecki Z, Piekoś R
Institute of Oceanology, PAS, ul. Powstanców Warszawy 55, 81-712 Sopot, Poland.
ScientificWorldJournal. 2002 Jul 9;2:1891-905. doi: 10.1100/tsw.2002.821.
A simple and rapid method has been developed to determine 226Ra in rocks, soils, and sediments. Samples are decomposed by fusion with lithium metaborate and the melt is dissolved in a solution containing sulfates and citric acid. During the dissolution, a fine suspension of mixed barium and radium sulfates is formed. The microcrystals are collected on a membrane filter (pore size 0.1 microm) and analysed in an alpha spectrometer. Application of a 133Ba tracer enables us to assess the loss of the analyte, which only rarely exceeds 10%. All analytical operations, beginning from sample decomposition to source preparation for alpha spectrometry, can be accomplished within 1 or 2 h. With uranium determination, the filtrate is spiked with a 232U tracer and passed through a column loaded with a Dowex AG (1 x 4) anion-exchange resin in the sulfate form. Interfering elements are eluted with dilute sulfuric acid followed by concentrated hydrochloric acid. Uranium is eluted with water, electrodeposited on silver discs, and analysed in the alpha spectrometer. The method was tested on reference soil and sediment materials and was found to be accurate within the estimated uncertainties.
已开发出一种简单快速的方法来测定岩石、土壤和沉积物中的镭-226。样品通过与偏硼酸锂熔融分解,熔体溶解在含有硫酸盐和柠檬酸的溶液中。溶解过程中会形成硫酸钡和硫酸镭的混合细悬浮液。微晶收集在膜过滤器(孔径0.1微米)上,并在α光谱仪中进行分析。使用钡-133示踪剂使我们能够评估分析物的损失,其损失很少超过10%。从样品分解到α光谱分析源制备的所有分析操作都可以在1或2小时内完成。测定铀时,向滤液中加入铀-232示踪剂,然后通过装有硫酸根形式的Dowex AG(1×4)阴离子交换树脂的柱子。用稀硫酸然后用浓盐酸洗脱干扰元素。铀用水洗脱,电沉积在银盘上,并在α光谱仪中进行分析。该方法在参考土壤和沉积物材料上进行了测试,发现在估计的不确定度范围内是准确的。