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A Novel Tandem of Thermal Desorption Carbon Analyzer and Off-Axis Integrated Cavity Output Spectroscopy for Aerosol Stable Carbon Isotope Ratio Measurement

机译:新型串联式热解吸碳分析仪和离轴集成腔输出光谱仪,用于气溶胶稳定碳同位素比测量

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A novel approach for measurement of stable carbon isotopic ratio of atmospheric aerosols was developed by tandem operation of two instruments: a Sunset Organic Carbon-Elemental Carbon (OC-EC) analyzer and an online Carbon Dioxide Stable Isotope Analyzer (LGR, CCIA-36d). Sensitivity, accuracy and measurement uncertainty of the CCIA was comprehensively investigated using the standard reference CO2 gas with known concentration and isotopic ratio. Drift in CCIA measurement due to varying CO2 and water vapor concentration was evaluated and a humidity stabilizer was designed and developed to control the water vapor concentration of exhaust gas flow from OC-EC prior to entering the CCIA. A Keeling approach was applied to separate the ratio in the samples from the mixture of PM sample-produced CO2 and reference gas and we developed a protocol to derive the isotopic composition of the particle samples. A lithium carbonate standard (in powder form) from National Institute of Standards and Technology (NIST) was used to validate measurement of δ13C ratios by CCIA. Offline measurement on ambient aerosol and diesel exhaust aerosols produced comparable results of isotopic ratio with literature values. This study demonstrates the utility of this tandem operation for carbon isotopic measurement of atmospheric particles with better than 1.0‰ precision as a cost-effective alternative of conventional Isotopic Ratio Mass Spectrometer (IR-MS).
机译:通过两种仪器的串联操作,开发了一种测量大气气溶胶稳定碳同位素比的新方法:日落有机碳-元素碳(OC-EC)分析仪和在线二氧化碳稳定同位素分析仪(LGR,CCIA-36d) 。使用已知浓度和同位素比的标准参比二氧化碳气体,对CCIA的灵敏度,准确性和测量不确定度进行了全面研究。评估了由于CO2和水蒸气浓度变化引起的CCIA测量漂移,并设计并开发了一种湿度稳定剂,以控制进入CCIA之前来自OC-EC的废气流的水蒸气浓度。应用Keeling方法从PM样品产生的CO2和参考气体的混合物中分离样品中的比例,我们开发了一种协议来导出颗粒样品的同位素组成。美国国家标准技术研究所(NIST)的碳酸锂标准品(粉末形式)用于验证CCIA对δ13C比的测量。离线测量环境气溶胶和柴油机废气气溶胶的同位素比值结果与文献值相当。这项研究证明了这种串联操作的实用性,它是传统同位素比质谱仪(IR-MS)的一种经济高效的替代方法,具有优于1.0‰的精度,可用于测量大气颗粒的碳同位素。

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