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Estimation of atmospheric total organic carbon (TOC) - paving the path towards carbon budget closure

机译:大气总有机碳(TOC)估算 - 铺设碳预算封闭的路径

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The atmosphere contains a rich variety of reactive organic compounds, including gaseous volatile organic carbon (VOCs), carbonaceous aerosols, and other organic compounds at varying volatility. Here we present a novel and simple approach to measure atmospheric non-methane total organic carbon (TOC) based on catalytic oxidation of organics in bulk air to carbon dioxide. This method shows little sensitivity towards humidity and near 100% oxidation efficiencies for all VOCs tested. We estimate a best-case hourly precision of 8 ppbC during times of low ambient variability in carbon dioxide, methane, and carbon monoxide (CO). As proof of concept of this approach, we show measurements of TOC + CO during August-September 2016 from a coastal city in the southwest United Kingdom. TOC + CO was substantially elevated during the day on weekdays (occasionally over 2 ppm C) as a result of local anthropogenic activity. On weekends and holidays, with a mean (standard error) of 102 (8) ppb C, TOC + CO was lower and showed much less diurnal variability. TOC + CO was significantly lower when winds were coming off the Atlantic Ocean than when winds were coming off land if we exclude the weekday daytime. By subtracting the estimated CO from TOC + CO, we constrain the mean (uncertainty) TOC in Atlantic-dominated air masses to be around 23 (+/- = 8) ppbC during this period. A proton-transfer-reaction mass spectrometer (PTR-MS) was deployed at the same time, detecting a large range of organic compounds (oxygenated VOCs, biogenic VOCs, aromatics, dimethyl sulfide). The total speciated VOCs from the PTR-MS, denoted here as Sum(VOC), amounted to a mean (uncertainty) of 12 (+/- = 3) ppbC in marine air. Possible contributions from a number of known organic compounds present in marine air that were not detected by the PTR-MS are assessed within the context of the TOC budget. Finally, we note that the use of a short, heated sample tube can improve the transmission of organics to the analy
机译:大气层含有丰富的反应性有机化合物,包括气态挥发性有机碳(VOC),碳质气溶胶和其他有机化合物,在不同的挥发性下。在这里,我们提出了一种基于批量空气中的有机物催化氧化到二氧化碳的有机物催化氧化来测量大气非甲烷总有机碳(TOC)的新颖和简单的方法。该方法对所有测试的VOC的湿度和接近100%氧化效率的敏感性很小。在二氧化碳,甲烷和一氧化碳(CO)的低环境变异期间,我们估计了8 ppbc的最佳情况每小时精度。作为这种方法的概念证明,我们在2016年8月至2016年8月至2016年9月的沿海城市展示了TOC + CO的测量。由于局部人为活动,TOC + CO在白天(偶尔超过2ppm C)的日期基本上升高。在周末和假期,具有102(8)个PPB C的平均值(标准误差),TOC + CO较低,并显示出较少的昼夜变异性。当风从大西洋脱离大西洋时,TOC + CO显着降低,如果我们排除白天白天,风在陆地上的陆地。通过从TOC + CO中减去估计的CO,我们在此期间将大西洋主导的空气群体中的平均值(不确定性)TOC限制为大约23(+/-& = 8)PPBC。同时展开质子转移反应质谱仪(PTR-MS),检测大量的有机化合物(含氧VOC,生物转霉,芳烃,二甲基硫醚)。来自PTR-MS的总指标VOC,这里表示为SUM(VOC),其在海洋空气中为12(+/- = 3)PPBC的平均值(不确定性)。在TOC预算的背景下评估来自PTR-MS未检测到的海洋空气中存在的许多已知有机化合物的可能贡献。最后,我们注意到使用短,加热的样品管可以改善有机物的传播到分析

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