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洛杉矶大气中甲烷的来源。

On the sources of methane to the Los Angeles atmosphere.

机构信息

Division of Engineering and Applied Science, California Institute of Technology, Pasadena, California 91125, United States.

出版信息

Environ Sci Technol. 2012 Sep 4;46(17):9282-9. doi: 10.1021/es301138y. Epub 2012 Aug 20.

Abstract

We use historical and new atmospheric trace gas observations to refine the estimated source of methane (CH(4)) emitted into California's South Coast Air Basin (the larger Los Angeles metropolitan region). Referenced to the California Air Resources Board (CARB) CO emissions inventory, total CH(4) emissions are 0.44 ± 0.15 Tg each year. To investigate the possible contribution of fossil fuel emissions, we use ambient air observations of methane (CH(4)), ethane (C(2)H(6)), and carbon monoxide (CO), together with measured C(2)H(6) to CH(4) enhancement ratios in the Los Angeles natural gas supply. The observed atmospheric C(2)H(6) to CH(4) ratio during the ARCTAS (2008) and CalNex (2010) aircraft campaigns is similar to the ratio of these gases in the natural gas supplied to the basin during both these campaigns. Thus, at the upper limit (assuming that the only major source of atmospheric C(2)H(6) is fugitive emissions from the natural gas infrastructure) these data are consistent with the attribution of most (0.39 ± 0.15 Tg yr(-1)) of the excess CH(4) in the basin to uncombusted losses from the natural gas system (approximately 2.5-6% of natural gas delivered to basin customers). However, there are other sources of C(2)H(6) in the region. In particular, emissions of C(2)H(6) (and CH(4)) from natural gas seeps as well as those associated with petroleum production, both of which are poorly known, will reduce the inferred contribution of the natural gas infrastructure to the total CH(4) emissions, potentially significantly. This study highlights both the value and challenges associated with the use of ethane as a tracer for fugitive emissions from the natural gas production and distribution system.

摘要

我们利用历史和新的大气痕量气体观测结果,对加利福尼亚南海岸大气流域(即较大的洛杉矶大都市区)甲烷(CH(4))排放的估计源进行了修正。参考加利福尼亚空气资源委员会(CARB)的 CO 排放清单,每年 CH(4)的总排放量为 0.44 ± 0.15 太克。为了研究化石燃料排放的可能贡献,我们利用大气中甲烷(CH(4))、乙烷(C(2)H(6))和一氧化碳(CO)的观测值,以及在洛杉矶天然气供应中测量的 C(2)H(6)与 CH(4)的增强比值。在 ARCTAS(2008 年)和 CalNex(2010 年)飞机飞行期间观察到的大气 C(2)H(6)与 CH(4)的比值与这两个飞行期间供应给流域的天然气中这些气体的比值相似。因此,在最高限制下(假设大气 C(2)H(6)的唯一主要来源是天然气基础设施的逸散排放),这些数据与归因于盆地中大部分(0.39 ± 0.15 太克年(-1))过量 CH(4)的观点一致,即未燃烧的天然气系统损失(输送给流域客户的天然气的 2.5-6%左右)。然而,该地区还有其他 C(2)H(6)的来源。特别是,天然气渗漏以及与石油生产相关的 C(2)H(6)(和 CH(4))排放,这些排放都知之甚少,它们将减少天然气基础设施对总 CH(4)排放的推断贡献,这可能会显著降低。这项研究突出了利用乙烷作为天然气生产和分配系统逸散排放示踪剂的价值和挑战。

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