Interference Sources and Elimination Methods for the Determination of Selenium in Soil and Water Sediment by Atomic Fluorescence Spectrometry
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摘要: 原子荧光光谱法(AFS)具有灵敏度高、结构简单、容易操作等优点,但目前测定土壤和沉积物中的硒等元素的标准方法所采用的消解过程繁琐,易产生干扰。沸水浴可以把土壤和水系沉积物中硒提取完全,本文根据样品中元素丰度和仪器性能,将AFS测定Se的干扰分为Cu和Pb两大类,根据实验提出在水浴消解液加入浓盐酸(不宜加入硫脲-抗坏血酸),通过增加溶液酸度和Cl-浓度,即保持样品中盐酸浓度高于23%,可抑制Cu2+还原为Cu0和Pb4+生成PbH4,有效降低了Cu的负干扰和Pb的正干扰,提高了AFS测定Se的精密度和准确度。本方法测定Se的检出限为0.008mg/kg,测试标准物质的相对标准偏差为0.5%~11%,相对误差为-16.3%~9.5%;比行业标准HJ 680—2013的检出限(0.01mg/kg)、精密度(0.79%~23.1%)和准确度等技术指标更佳。Abstract:
BACKGROUNDAtomic Fluorescence Spectrometry (AFS) has advantages of high sensitivity, simple structure and easy operation, but the digestion process of the standard analysis method for determination of Se in soil is cumbersome and readily produces interference. OBJECTIVESTo evaluate the applicability of Se determination in soil and sediment by water bath digestion/AFS, and uncover the main interference and elimination methods. METHODSBased on the standard method of GB/T 22105-2008, boiling water bath of aqua regina was used to digest Se in soil and sediment. Four treatments, including Fe3+, concentrated hydrochloric acid, Fe3+with concentrated hydrochloric acid, and water bath solution, were used to eliminate the interference of Cu2+ and Pb4+. RESULTSThe detection limit of Se by this method was 0.008mg/kg, the relative standard deviation of the test reference materials was 0.5%-11%, and the relative error was -16.3%-9.5%, better than the detection limit (0.01mg/kg), precision (0.79%-23.1%) and accuracy of the industry standard HJ 680-2013. CONCLUSIONSAccording to the experiment, it is proposed to add concentrated hydrochloric acid to the water bath digestion solution without adding thiourea-ascorbic acid. By increasing the acidity and Cl- concentration of the solution and keeping the concentration of hydrochloric acid in the sample higher than 23%, the reduction of Cu2+ to Cu0 and Pb4+ to form PbH4 can be inhibited. The negative interference of Cu and the positive interference of Pb are effectively reduced, and the precision and accuracy of Se measured by AFS are improved. -
Key words:
- soil /
- sediment /
- water bath digestion /
- selenium /
- Atomic Fluorescence Spectrometry /
- interference elimination
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表 1 标准物质中硒测定结果
Table 1. Determination results of selenium in certified reference materials of soils and sediments
标准物质编号 标准物质采样地区 Se认定值
(mg/kg)Se含量6次测定平均值
(mg/kg)RSD
(%)平均相对误差
(%)ΔlgC(GBW) GBW07406 广东阳春多金属矿区黄色红壤 1.34±0.17 1.440 4.3 7.5 0.031 GBW07430 珠江三角洲 0.51±0.05 0.477 2.4 -6.5 0.029 GBW07451 山东日照市黄海滩涂沉积物 0.11±0.02 0.093 11.0 -15.5 0.073 GBW07453 广东阳江市南海滩涂沉积物 0.20±0.03 0.174 6.4 -13.0 0.060 GBW07455 安徽五河淮河沉积物 0.14±0.02 0.129 4.6 -7.9 0.036 GBW07456 江苏张家港长江沉积物 0.29±0.04 0.285 6.6 -1.7 0.008 GBW07457 湖南益阳市湘江沉积物 0.44±0.05 0.459 0.5 4.4 0.018 GBW07307a 辽宁开源铅锌矿区 (0.26) 0.251 4.9 -3.5 0.015 GBW07311 湖南柿竹园多金属矿区 0.20±0.05 0.219 7.1 9.5 0.039 GBW07312 广东阳春多金属矿区 0.25±0.03 0.241 4.8 -3.6 0.016 GBW07362 青海拉水下铜镍矿区 0.24±0.02 0.201 3.8 -16.3 0.077 表 2 不同方式处理土壤及水系沉积物硒的测定结果
Table 2. Analytical results of selenium in soil and sediment pretreated with different methods
样品处理方式 Fe3+含量 盐酸浓度
(%)③GBW07453 GBW07311 GBW07312 测定值
(mg/kg)认定值
(mg/kg)测定值
(mg/kg)认定值
(mg/kg)测定值
(mg/kg)认定值
(mg/kg)铁盐 0.83x%+1.17%
(1.20%)6.25 0.179 0.171 0.175 0.20±0.03 0.502 0.463 0.448 0.20±0.05 0.324 0.310 0.330 0.25±0.03 上清液 x%①(0.04%)② 7.50 0.162 0.163 0.172 0.20±0.03 0.341 0.331 0.340 0.20±0.05 0.178 0.185 0.176 0.25±0.03 盐酸-铁盐 0.86x%+1.00%
(1.03%)19.6 0.170 0.164 0.166 0.20±0.03 0.328 0.339 0.339 0.20±0.05 0.288 0.298 0.300 0.25±0.03 盐酸 0.83x%(0.03%) 22.9 0.165 0.161 0.168 0.20±0.03 0.230 0.232 0.229 0.20±0.05 0.245 0.253 0.254 0.25±0.03 注:①x%为样品中溶出的Fe3+含量,②括号内取值为所有土壤及水系沉积物中Fe2O3中位数5.00%折算后Fe3+含量,③未考虑消解过程盐酸损失。 表 3 硫脲-抗坏血酸和浓盐酸处理方式对硒测试的影响
Table 3. Effects of treatment with thiourea-ascorbic acid and hydrochloric acid on selenium in soil sample
样品类型 标准物质编号 标准物质采样地区 Se认定值
(mg/kg)浓盐酸处理 硫脲-抗坏血酸处理 Se测定值
(mg/kg)回收率
(%)Se测定值
(mg/kg)回收率
(%)GBW07402 内蒙四子王旗和白云鄂博栗钙土 0.16±0.03 0.131 82.0 0.034 21.4 GBW07408 陕西洛川黄土 0.10±0.01 0.083 80.0 0.013 13.0 土壤 GBW07423 洪泽湖沉积物 0.15±0.03 0.131 87.5 0.012 8.00 GBW07430 珠江三角洲 0.51±0.05 0.454 88.9 0.049 9.61 GBW07456 江苏张家港长江沉积物 0.29±0.03 0.276 95.1 0.059 20.4 GBW07386 江西省南昌市扬子洲 0.30±0.01 0.268 89.4 0.036 12.0 GBW07312 广东阳春多金属矿区 0.25±0.03 0.273 109 0.101 40.2 GBW07318 四川西昌多种火成岩和沉积岩分布区 (0.15) 0.178 119 0.085 56.5 水系沉积物 GBW07364 新疆吐鲁番小热泉子铜矿区 1.55±0.34 1.54 99.2 0.277 17.9 GBW07366 江西德兴银山多金属矿区 0.69±0.08 0.704 102 0.113 16.3 GBW07383 湖南汝城花岗岩区 0.652±0.066 0.618 94.8 0.100 15.3 GBW07384 江西资溪花岗岩区 0.261±0.028 0.223 85.3 0.047 17.9 -
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