{"title":"Monitoring greenhouse gases in comandante ferraz antarctic station, King George Island","authors":"L. Marani, P. C. Alvalá","doi":"10.4322/APA.2014.022","DOIUrl":null,"url":null,"abstract":"This document presents the results of the monitoring of Greenhouse Gases (GHG) at Brazilian Antarctic Station Comandante Ferraz (EACF). The samples were taken near the Ozone and Meteorology Modules, weather conditions, such as direction and intensity of the wind, being annotated. For measurements of the concentration of GHG, a collection system that used a diaphragm pump, with samples of air being stored in stainless steel cylinders, was used. Concentrations of gases of interest in the samples collected were determined by the ozone gas chromatography laboratory, in São José dos Campos/SP. Furthermore, a continuous infrared monitor (model LI-820 Licor Gas Analyzer) was installed in the Ozone Module. There was great stability of the concentration values obtained by liquor, in that the average for these records were 378.8 ± 2.0 ppm (parts per million by volume), very close to that reported at NOAA’s (National Oceanic and Atmospheric Administration) polar station (385 ppm). Analyses of nitrous oxide (N2O) collected in the cylinders in the months of January to March 2010 resulted in an average of 334.7 ± 2.0 ppb (parts per billion by volume), very close to that reported by NOAA as a global average (323 ppb), however it was noted that this value was virtually constant in all samples, which reflected in low standard deviation, revealing an offset in our pattern to be given in subsequent samples. Samples collected in cylinders in the same period and analyzed for methane showed an average 1,791.4 ± 38.0 ppb. This value is higher than expected for the region (1,750 ppbv). However there was a wide variability in the samples (represented by the standard deviation) reflecting local sample point, mainly in the samples collected near the station. CO data did not pass in the validation tests, mainly due to their long storage time. As the CO is reactive and can undergo alteration inside the cylinder through other compounds, the storage time led to reactions inside the cylinders, causing the invalidation of the samples for this gas.","PeriodicalId":169975,"journal":{"name":"INCT-APA Annual Activity Report","volume":"41 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"INCT-APA Annual Activity Report","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4322/APA.2014.022","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
This document presents the results of the monitoring of Greenhouse Gases (GHG) at Brazilian Antarctic Station Comandante Ferraz (EACF). The samples were taken near the Ozone and Meteorology Modules, weather conditions, such as direction and intensity of the wind, being annotated. For measurements of the concentration of GHG, a collection system that used a diaphragm pump, with samples of air being stored in stainless steel cylinders, was used. Concentrations of gases of interest in the samples collected were determined by the ozone gas chromatography laboratory, in São José dos Campos/SP. Furthermore, a continuous infrared monitor (model LI-820 Licor Gas Analyzer) was installed in the Ozone Module. There was great stability of the concentration values obtained by liquor, in that the average for these records were 378.8 ± 2.0 ppm (parts per million by volume), very close to that reported at NOAA’s (National Oceanic and Atmospheric Administration) polar station (385 ppm). Analyses of nitrous oxide (N2O) collected in the cylinders in the months of January to March 2010 resulted in an average of 334.7 ± 2.0 ppb (parts per billion by volume), very close to that reported by NOAA as a global average (323 ppb), however it was noted that this value was virtually constant in all samples, which reflected in low standard deviation, revealing an offset in our pattern to be given in subsequent samples. Samples collected in cylinders in the same period and analyzed for methane showed an average 1,791.4 ± 38.0 ppb. This value is higher than expected for the region (1,750 ppbv). However there was a wide variability in the samples (represented by the standard deviation) reflecting local sample point, mainly in the samples collected near the station. CO data did not pass in the validation tests, mainly due to their long storage time. As the CO is reactive and can undergo alteration inside the cylinder through other compounds, the storage time led to reactions inside the cylinders, causing the invalidation of the samples for this gas.
本文介绍了巴西南极科考站费拉兹科考站(EACF)温室气体监测的结果。样品是在臭氧和气象模块附近采集的,天气条件,如风的方向和强度,被注释。为了测量温室气体的浓度,使用了一个使用隔膜泵的收集系统,空气样本被储存在不锈钢圆筒中。收集的样品中感兴趣的气体浓度由臭氧气相色谱实验室测定,在 jos dos Campos/SP。此外,在臭氧模块中还安装了一个连续红外监测器(LI-820型Licor气体分析仪)。通过液体获得的浓度值具有很大的稳定性,因为这些记录的平均值为378.8±2.0 ppm(百万分之一体积),非常接近NOAA(国家海洋和大气管理局)极地站报告的浓度(385 ppm)。对2010年1月至3月在气瓶中收集的一氧化二氮(N2O)的分析结果平均为334.7±2.0 ppb(十亿分之一体积),非常接近NOAA报告的全球平均值(323 ppb),但值得注意的是,该值在所有样品中几乎是恒定的,这反映在低标准偏差中,揭示了我们的模式将在后续样品中给出的偏移。同一时期在气瓶中收集的样品和分析的甲烷显示平均为1,791.4±38.0 ppb。这一数值高于该地区的预期值(1750 ppbv)。然而,反映当地样本点的样本(以标准差表示)存在很大的变异性,主要是在站点附近收集的样本。CO数据在验证测试中没有通过,主要是由于其存储时间过长。由于一氧化碳是活性的,并且可以通过其他化合物在钢瓶内发生变化,因此储存时间导致钢瓶内发生反应,导致该气体的样品失效。