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首页> 外文期刊>Atmospheric Measurement Techniques >New technique for high-precision, simultaneous measurements of CH 4 , N 2 O and CO 2 concentrations; isotopic and elemental ratios of N 2 , O 2 and Ar; and total air content in ice cores by wet extraction
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New technique for high-precision, simultaneous measurements of CH 4 , N 2 O and CO 2 concentrations; isotopic and elemental ratios of N 2 , O 2 and Ar; and total air content in ice cores by wet extraction

机译:高精度的新技术,CH 4,N 2 O和CO 2浓度的同时测量; N 2,O 2和Ar的同位素和元素比例; 湿提取物和冰芯的总空气含量

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摘要

Air in polar ice cores provides unique information on past climatic and atmospheric changes. We developed a new method combining wet extraction, gas chromatography and mass spectrometry for high-precision, simultaneous measurements of eight air components ( CH 4 , N 2 O and CO 2 concentrations; δ 15 N , δ 18 O , δ O 2 ∕N 2 and δ Ar∕N 2 ; and total air content) from an ice-core sample of ~ ?60? g . The ice sample is evacuated for ~ ?2? h and melted under vacuum, and the released air is continuously transferred into a sample tube at 10? K within 10? min . The air is homogenized in the sample tube overnight at room temperature and split into two aliquots for mass spectrometric and gas chromatographic measurements. Care is taken to minimize (1)?contamination of greenhouse gases by using a long evacuation time, (2)?consumption of oxygen during sample storage by a passivation treatment on sample tubes, and (3)?fractionation of isotopic ratios with a long homogenization time for splitting. Precision is assessed by analyzing standard gases with artificial ice and duplicate measurements of the Dome Fuji and NEEM ice cores. The overall reproducibility (1 SD) of duplicate ice-core analyses are 3.2? ppb , 2.2? ppb and 2.9? ppm for CH 4 , N 2 O and CO 2 concentrations; 0.006?‰, 0.011?‰, 0.09?‰ and 0.12?‰ for δ 15 N , δ 18 O , δ O 2 ∕N 2 and δ Ar∕N 2 ; and 0.63? mL STP ?kg ?1 for total air content, respectively. Our new method successfully combines the high-precision, small-sample and multiple-species measurements, with a wide range of applications for ice-core paleoenvironmental studies.
机译:Polar Ice Cores中的空气提供有关过去的气候和大气变化的独特信息。我们开发了一种结合湿萃取,气相色谱和质谱的新方法,用于高精度,同时测量八个空气成分(CH 4,N 2 O和CO 2浓度;δ15n,δ18O,δO2 / n 2和δAr/ n 2;和总空气含量)来自〜β60的冰核样品? G 。冰上样品被抽空〜?2? H并在真空下熔化,并且释放的空气在10℃下连续转移到样品管中? k 10岁?闵。将空气在样品管中均质化过夜在室温下,并分成两个等分试样的质谱和气相色谱测量。通过使用长时间的疏散时间,(2)捕获在样品管上的钝化处理期间氧气消耗氧气的氧气,(3),(3),在样品管上的钝化处理中吞噬温室气体分裂的均匀化时间。通过分析具有人造冰的标准气体和圆顶富士和纽约冰芯的重复测量来评估精度。重复冰核分析的整体再现性(1 SD)为3.2? PPB,2.2? PPB和2.9? PPM for CH 4,N 2 O和CO 2浓度; 0.006?‰,0.011?‰,0.09?‰和0.12≤δ15n,δ18o,δo2/ n 2和δar/ n 2;和0.63?用于总空气含量的m1 stp?1。我们的新方法成功结合了高精度,小样本和多种测量,具有广泛的冰核古环境研究应用。

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