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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Variability-lifetime relationship for organic trace gases: A novel aid to compound identification and estimation of HO concentrations
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Variability-lifetime relationship for organic trace gases: A novel aid to compound identification and estimation of HO concentrations

机译:有机微量气体的寿命关系:化合物鉴定和HO浓度估算的新方法

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In this study we report aircraft-borne measurements of organic species made during March 1998 in Surinam, an unpolluted region on the northeast coast of South America Measurements included the following: CO by tunable diode laser; a wide variety of organics including acetone, acetonitrile, and isoprene by proton transfer mass spectrometry (PTR-MS); and nonmethane hydrocarbon measurements by gas chromatography-flame ionization detection. Here we compare the standard deviation of the natural logarithm of the mixing ratio (Sigma_1nX) to the estimated lifetime of these species. This relationship has been used to support identification of masses measured by the PTR-MS; ascertain the consistency and quality of hydrocarbon measurement data; and to provide information concerning sinks of important trace species. A selection of the data is used to indirectly determine an average HO concentration of 2.0 X 10(5) molecules cm(-3) along the back trajectory for air encountered during the Large-Scale Biosphere-Atmosphere Experiment in Amazonia-Cooperative LBA Airborne Regional Experiment (LBA-CLAIRE) measurement campaign between 0-1 km over the tropical rain forest. The lower than expected HO concentration derived could have been caused by significant atmospheric or oceanic photochemical production of acetone and MEK along the back trajectory. [References: 54]
机译:在这项研究中,我们报告了1998年3月在苏里南(Surinam)进行的机载有机物测量,苏里南(Surinam)是南美东北海岸的一个未被污染的区域。测量包括以下内容:可调谐二极管激光器产生的一氧化碳。质子转移质谱法(PTR-MS)可以检测多种有机物,包括丙酮,乙腈和异戊二烯;和非甲烷碳氢化合物的气相色谱-火焰电离检测。在这里,我们将混合比(Sigma_1nX)的自然对数的标准偏差与这些物种的估计寿命进行比较。这种关系已被用来支持对PTR-MS测量质量的鉴定。确定碳氢化合物测量数据的一致性和质量;并提供有关重要痕迹物种汇的信息。数据的选择用于间接确定在亚马逊合作LBA机载区域的大型生物圈-大气实验期间遇到的空气沿回弹轨迹的平均HO浓度为2.0 X 10(5)分子cm(-3)在热带雨林上0-1公里之间进行实验(LBA-CLAIRE)测量活动。低于预期的HO浓度可能是由于沿后向轨迹在大气或海洋中大量丙酮和MEK的光化学产生所致。 [参考:54]

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