文章摘要
王琳,王睿,郑循华,张丽娟.气相转化-化学发光法测定土壤中的亚硝态氮[J].农业环境科学学报,2017,36(9):1916-1924.
气相转化-化学发光法测定土壤中的亚硝态氮
A gas phase conversion-chemiluminescence method for detecting nitrite concentrations in soils
投稿时间:2017-02-28  
DOI:10.11654/jaes.2017-0238
中文关键词: 亚硝态氮  气相化学发光法  土壤  一氧化氮
英文关键词: nitrite  chemiluminescence  soil  nitric oxide
基金项目:国家自然科学基金项目(41303060,41675144);大气边界层物理与大气化学国家重点实验室开放课题
作者单位E-mail
王琳 河北农业大学资源与环境科学学院, 河北 保定 071000
中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室, 北京 100029 
 
王睿 中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室, 北京 100029 wangrui@mail.iap.ac.cn 
郑循华 中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室, 北京 100029
中国科学院大学地球科学学院, 北京 200049 
 
张丽娟 河北农业大学资源与环境科学学院, 河北 保定 071000  
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中文摘要:
      试验探究了将亚硝态氮(NO2-)还原转化为一氧化氮(NO)气体与化学发光法检测NO相结合的方法(气相转化-化学发光法,简称NC法)对土壤NO2-含量测定的适用性。在室温条件下,采用浓度为50%的冰醋酸提供酸性条件,以抗坏血酸为还原剂,将NO2-还原为NO气体,生成的NO被高纯氮气载入化学发光法氮氧化物分析仪的NO检测通道,实时记录NO信号值并积分信号峰面积,通过已知NO2-浓度系列的标准曲线,确定样品中的NO2-浓度。结果显示:NO信号值的峰面积与样品的NO2-浓度显著正相关(P<0.01),线性检测范围为2~500 μg·L-1(以纯N计,下同),检出限为2 μg·L-1,对土壤NO2-浓度的检出限为10 μg·kg-1(以水土比为5:1计),优于比色法的检出限15 μg·kg-1;重复测定10次50 μg·L-1标准溶液的峰面积变异系数为1.2%,精度为1.2 μg·L-1(95%置信区间),对应的土壤NO2-浓度检测精度为6 μg·kg-1,优于比色法的检测精度11 μg·kg-1;检测已知浓度NO2-的回收率为90%~97%。与比色法相比,NC法测定酸性土壤NO2-浓度的准确度相当,精度更优,但该方法测定碱性土壤NO2-浓度的结果偏高,可能是碱性土壤中大量的Ca2+、SO42-和CO32-对测定有干扰,而且NC法测定NO2-浓度的分析时间较比色法长,单个样品需8~15 min。
英文摘要:
      A chemiluminescence method that detects nitric oxide(NO) combined with the conversion from nitrite to NO for measuring soil nitrite concentrations is reported. The applicability of the method is evaluated by comparing it with the colorimetry method. The chemiluminescence method involves a reaction system consisting of 50% glacial acetic acid and ascorbic acid in the purge vessel. At room temperature, samples containing nitrite were injected into the purge vessel and nitrite was stoichiometrically reduced to NO by ascorbic acid under these acidic conditions. The produced NO was swept with pure nitrogen gas into the NO analyzer and the data was recorded while chemiluminescence signals were generated. The concentration of nitrite in the samples was calculated by the curve between the peak areas of the NO signals and the corresponding standard nitrite concentrations. The results showed that peak areas of chemiluminescence signals were linearly positively correlated with the nitrite concentrations in the range of 2 to 500 μg·L-1(P<0.01). The lowest detection limit of this method was 2 μg·L-1, equivalent to10 μg·kg-1 in soil(water:soil=5:1), lower than that of the colorimetry method(15 μg·kg-1). This method had a good precision of 1.2 μg·L-1 within 95% confidence interval by repeating the measurements of standard nitrite concentration of 50 μg·L-1 for ten times. The corresponding precision for soil nitrite concentration(6 μg·kg-1) was also better than that of colorimetry(11 μg·kg-1). The recovery rates were in the range of 90%~97%. Compared to the colorimetry, the chemiluminescence method had the same accuracy for detecting nitrite concentrations in acid soils, but it overestimated the concentrations in alkaline soil because of the existence of Ca2+, SO42-, and CO32- in alkaline soil. Moreover, the analysis times for each soil nitrite sample were approximately 8~15 min, which is time-consuming comparing to the colorimetry method.
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