石墨炉原子吸收光谱法测定全血中铅的不确定度评定

根据《测量不确定度评定与评定表示指南》(JJF 1059-1999)建立了石墨炉原子吸收光谱法测定全血中铅不确定度的数学模型,分析了测试过程中不确定度的来源,并对各不确定度分量进行量化。本次测量的合成相对不确定度值为0.047 3,其中最大的分量是样品消化前处理重复测定引入的,其不确定度分量值为0.04。本次全血中铅测定结果为(130.7±12.4)μg/L,k=2,即测定结果置信水平为95%。     

测定水中挥发酚的测量不确定度评定

分析了采用预蒸馏的4-氨基安替比林萃取光度法，测定水中挥发酚过程中产生测量不确定度的主要来源．通过实例介绍了配制标准溶液、标准曲线拟合、重复性测量、分光光度计仪器等引入的各不确定度分量的量化计算方法．经合成计算出测定水中挥发酚的扩展不确定度为0．001mg／L．测量结果表示为（0．011±0．001）mg／L（=2）．     

测量土壤中多溴联苯和多溴联苯醚含量不确定度评定

通过对气相色谱-质谱联用法测定土壤中多溴联苯和多溴联苯醚类化合物含量的不确定度进行评定,分析了测量过程中引入的不确定度来源,求出各不确定度分量,最后合成标准不确定度并计算相对扩展不确定度。结果表明,各化合物最大的不确定度分量是方法回收率,约占50%~90%,方法相对扩展不确定度为0.12~0.20。     

硝酸银标准滴定溶液的不确定度评定

在掌握JJF1059-1999的基础上，对硝酸银标准滴定溶液浓度的不确定度进行评定，主要从方法概述、确定测量中不确定度的来源、建立数学模型、计算相对标准不确定度分量、合成相对标准不确定度、扩展不确定度等入手，详细介绍了硝酸银标准滴定溶液的不确定度评定过程。     

火焰原子吸收法测定水样铅含量的不确定度评定

实验室认可和资质认定都要求检测实验室具备评定测量不确定度的能力,现依据JJF1059-1999《测量不确定度评定与表示》,对火焰原子吸收法测定水样中铅含量进行不确定度评估,分析测定过程中不确定度来源,量化不确定度分量,求出合成不确定度和扩展不确定度,给出测定结果的表示式。     

热电厂锅炉排放烟尘监测的测量不确定度评定

在理解JJF1059-1999《测量不确定度评定与表示》的基础上,对按照国家标准GB5468-1991《锅炉烟尘测试方法》和GB/T16157-1996《固定污染源排气中颗粒物测定与气态污染物采样方法》规定的测定方法,监测热电厂锅炉排放烟尘的测量结果不确定度进行了评定.通过对影响测量结果的系统效应、随机效应产生的不确定度分量的分析和量化评估,计算得到相对合成标准不确定度为10%,扩展不确定度U为6.4 mg/m3(k=2).     

固体吸附/热脱附-气相色谱法测定环境空气中苯系物的不确定度评定

建立固体吸附/热脱附-气相色谱法测定环境空气中苯系物的不确定度评定方法,分析测定过程中不确定度的来源,进行各不确定度分量的评估,并给出合成相对标准不确定度和扩展不确定度。     

石墨炉原子吸收法测定土壤中镉的不确定度评定

评定了石墨炉原子吸收法测定土壤样品中镉的测量不确定度。在测定过程中,对样品称量、水分测定、样品消解、样品定容、标准溶液配制、标准曲线拟合等影响不确定度的分量进行了评定。按照《测量不确定度评定与表示》(JJF 1059.1—2012)的规定进行合成,给出了扩展不确定度,镉含量结果的表示式为(0.115±0.015)mg/kg,k=2。     

热解吸—气相色谱法测定室内空气中TVOC不确定度的评定

《测量不确定度表示指南》[简称（GUM）]采用当前国际通行的观点和方法，使涉及测量的技术领域和部门可以用统一的准则对测量结果及其质量进行评定、比较和表示．在环境监测中使用GUM不仅是不同学科之间交往的需要，也是全球市场经济发展的需要．讨论了室内空气中总挥发性有机物的测量不确定度的产生原因及其评定方法．在不确定度的所有可能来源中找出主要来源，分析其不确定度分量是一种可行的评定方法．     

厂界噪声测量的不确定度评定

阐述了厂界噪声测量的不确定度来源和对不确定度分量的评定,并且对不确定度分量评定中有关的内容进行了实例计算,为测量的不确定度在环境监测领域中的评定提供了参考.     

两种消解法测定沉积物总磷的对比

通过过硫酸钾消解法与HClO₄-H₂SO₄消解法对土壤和水系沉积物的标准物质,以及三峡水库沉积物未知样品中的总磷含量进行测定,并对检测结果进行对比,分析过硫酸钾消解法测定沉积物总磷的可行性。结果表明,在标准样品中,HClO₄-H₂SO₄消解法的检测结果是标准值的83%~100%,并且所有结果均在其不确定度范围之内;过硫酸钾消解法的检测结果仅达到标准值的19%~42%,超出其不确定度范围,不能作为有效数据。在未知样品中,过硫酸钾消解法检测结果也远低于HClO₄-H₂SO₄消解法检测结果,只达到后者的32%~52%。由此可见,过硫酸钾消解法测定沉积物或土壤中总磷,仍需要进一步的研究,以达到符合实际的检测结果。     

火焰原子吸收法测定水中铁、锰含量的不确定度评定

从样品消解、分析、计算全过程对火焰原子吸收法测定水中铁、锰进行分析,根据JJF 1059-1999对其测量不确定度进行评定。结果表明,测定水中铁的不确定度主要来源于消解过程、标准溶液及配制、重复测定样品;测定水中锰的不确定度主要来源于消解过程、工作曲线拟合、标准溶液及配制。水中铁、锰含量的结果可分别表示为：（2.58±...     

SI-traceable certification of Cu, Cr, Cd and Pb in sediment and fly ash candidate reference materials

Many fields in environmental analytical chemistry deal with very low limits and thresholds as set by governmental legislations or transnational regulations. The need for the accuracy, comparability and traceability of analytical measurements in environmental analytical chemistry has significantly increased and total uncertainties are even asked for by accreditation bodies of environmental laboratories. This paper addresses achieving these goals to guarantee accuracy, quality control, quality assurance or validation of a method by means of certified reference materials. The assessment of analytical results in certified reference materials must be as accurate as possible and every single step has to be fully evaluated. This paper presents the SI-traceable certification of Cu, Cr, Cd and Pb contents in geological and environmentally relevant matrices (three sediments and one fly ash sample). Certification was achieved using isotope dilution (ID) ICPMS as a primary method of measurement. In order to reduce significantly the number of analytical steps and intermediate samples a multiple spiking approach was developed. The full methodology is documented and total uncertainty budgets are calculated for all certified values. A non-element specific sample digestion process was optimised. All wet chemical digestion methods examined resulted in a more or less pronounced amount of precipitate. It is demonstrated that these precipitates originate mainly from secondary formation of fluorides (essentially CaF2) and that their formation takes place after isotopic equilibration. The contribution to the total uncertainty of the final values resulting from the formation of such precipitates was in general < 0.1% for all investigated elements. Other sources of uncertainty scrutinised included the moisture content determination, procedural blank determination, cross-contamination from the different spike materials, correction for spectral interferences, instrumental background and deadtime effects, as well as the use of either certified values or IUPAC data in the IDMS equation. The average elemental content in the sediment samples was 30-130 micrograms g-1 for Pb, 0.5-3 micrograms g-1 for Cd and 50-70 micrograms g-1 for Cu. Cr was measured in one sample and was about 60 micrograms g-1. The concentrations in the fly ash sample were up to 2 orders of magnitude higher. Expanded uncertainty for the investigated elements was about 3% (coverae factor k = 2) except for Cr, (measured by high resolution ICPMS), for which the expanded uncertainty was about 7% (k = 2).     

水中挥发酚的测量不确定度评定

建立了分光光度法测定水中挥发酚的合成标准不确定度的数学模式，它由质量的标准测量不确定度和体积的标准测量不确定度组成。应用一个实例对这两部分标准不确定度的分量作了详尽的分析和计算，得出测量扩展不确定度结果。     

便携式GC-MS测定气体样品中6种典型VOCs的不确定度评定

以便携式GC-MS测定气体样品中6种典型挥发性有机物(VOCs)组分(苯、1,1,2-三氯乙烷、四氯乙烯、乙苯、间二甲苯和1,3,5-三甲基苯)为例,应用不确定度理论,从检测过程和计算方法的角度分析了影响测量不确定度的各种因素:标准气体定值、标准气体稀释、工作曲线的非线性及重复性测定。对各测量不确定度分量进行计算和评定,同时采用稳健统计方法对测定结果进行准确度评价。结果表明:采用便携式GC-MS测定气体样品中VOCs不确定度的主要影响因素是标准气体定值和工作曲线的非线性,其次是重复性测定,标准气体稀释引入的不确定度较小。当VOCs组分含量为200 nmol/mol浓度水平时,测量扩展不确定度为14～17 nmol/mol,测量相对扩展不确定度为7.1%～9.2%(k=2,置信水平为95%),相对误差为1.5%～4.0%。     

水中总氮测定方法存在问题的研究及改进

碱性过硫酸钾消解紫外分光光度法测定水中总氮采用的消解器皿是玻璃比色管,易造成空白偏高、结果偏低等问题。采用双圆柱状的消解杯对水样进行消解。结果表明,消解杯消解水中总氮,线性相关系数均大于0.999,检出限为0.05 mg/L,相对标准偏差小于5%,相对误差为0.88%~1.00%;改进后的消解器皿具有较好的精密度和准确度,能够更加准确测定水中总氮的含量。     

土壤氨氮、亚硝酸盐氮、硝酸盐氮的测定试料保存实验

对测定土壤中氨氮、亚硝酸盐氲、硝酸盐氲的试料保存条件和时间进行研究。结果表明，在4℃、避光保存的条件下，试料可以保存7d，而各组份浓度值基本保持不变。其中，氨氮的本底试料值相对标准偏差为2．86％，加标试料值相对标准偏差为2．88％，加标回收率为85．8％～101％；亚硝酸盐氮加标量为0．5μg试料值相对标准偏差为3．55％，加标量为4．0μg试料值相对标准偏差为2．93％；硝酸盐氮与亚硝酸盐氮总量的本底试料值相对标准偏差为7．02％，加标试料值相对标准偏差为4．56％，加标回收率为82．6％～104％。     

Validation of a diffusive sampler for NO2

A diffusive sampler for NO2, Willems badge, was validated in laboratory experiments and field tests. The collecting reagent for NO2 in the sampler is triethanolamine, and the analysis is based on a modified colorimetric method, the Saltzman method. The analysis was performed by a flow injection analysis (FIA) technique. The sampling rate for the sampler was determined to be 40.0 ml min-1. There was no effect of NO2 concentration or relative humidity on sampling rate, and the influence of sampling time was found to be small. The detection limit was 4 micrograms m-3 for a 24 h sample. The capacity is high enough to allow sampling of 150 micrograms m-3 for 7 days, which is twice the recommended Swedish short-term (24 h) guideline value as a 98-percentile over 6 months. In field tests, the sampler performed well, even at wind speeds higher than 2 m s-1, and at low temperatures. The overall uncertainty of the method was 24%. The sensitivity and capacity of the method also make it suitable for personal sampling for 2-8 h in working environments.     

Assessment of uncertainty of NO2 measurements by the chemiluminescence method and discussion of the quality objective of the NO2 European Directive

Hereafter, an assessment of the ability of the chemiluminescence method to measure ambient NO2 with an accuracy within 15%, as requested by the data quality objective of European directive 1999/30/CE, is presented. In general, uncertainty is evaluated using the response to reference materials or by means of inter-comparisons used to determine some statistics like repeatability, reproducibility and calibration bias. These are incomplete approaches and the method of the Guide to the Expression of Uncertainty in Measurement, advised by the Directive, should be preferred. In fact, even if it requires a large data set, it allows the relative influence of all possible sources of uncertainty to be studied. The extent of NO2 uncertainty is mainly dependent on the level of NO. It is decreased by NOx and the correlation between NOx and NO. Furthermore, the uncertainty budget reveals that the contribution of accuracy of calibration standard, linearity, converter efficiency and drift of the analyser between calibration checks to the overall uncertainty is less important than the contribution of interference, mainly humidity and PAN in rural areas. The relative expanded uncertainty of the NO2 hourly average exceeds 30% for NO2 concentrations lower than 40 microg m(-3). Nevertheless, the data quality objective of 15% is reached for 200 microg m(-3), the hourly limit value of the European directive. On the contrary, at the limit value on the annual average, 40 microg m(-3), the data quality objective is not met if NO is higher than 100 microg m(-3). However, the data quality objective could be reached by correcting the measurements with the bias due to interference.     

程序控温石墨消解-原子荧光法测定土壤中总砷

采用程序控温石墨全自动消解仪消解土壤样品，原子荧光光谱法测定总砷。通过试验确定原子荧光光度计的最佳工作条件，使得该方法在2.00μg／L ～20.0μg／L 范围内线性良好，检出限为0.025 mg／kg，加标回收率在96.0％～10^5％之间，RSD为1.9％～3.3％。用该方法与国标法同时测定土壤标准样品和实际样品，结果无显著差异。