Department of Geology, University of Cincinnati, 500 Geology-Physics Building, 345 Clifton Court, Cincinnati, OH, 45221, USA.
U.S. Environmental Protection Agency, National Risk Management Research Laboratory, 26 W. Martin Luther King Dr., Cincinnati, OH, 45268, USA.
Environ Pollut. 2018 May;236:247-256. doi: 10.1016/j.envpol.2018.01.076. Epub 2018 Feb 2.
Recent studies have indicated that urban streets can be hotspots for emissions of methane (CH) from leaky natural gas lines, particularly in cities with older natural gas distribution systems. The objective of the current study was to determine whether leaking sewer pipes could also be a source of street-level CH as well as nitrous oxide (NO) in Cincinnati, Ohio, a city with a relatively new gas pipeline network. To do this, we measured the carbon (δC) and hydrogen (δH) stable isotopic composition of CH to distinguish between biogenic CH from sewer gas and thermogenic CH from leaking natural gas pipelines and measured CH and NO flux rates and concentrations at sites from a previous study of street-level CH enhancements (77 out of 104 sites) as well as additional sites found through surveying sewer grates and utility manholes (27 out of 104 sites). The average isotopic signatures for δC-CH and δH-CH were -48.5‰ ± 6.0‰ and -302‰ ± 142‰. The measured flux rates ranged from 0.0 to 282.5 mg CH day and 0.0-14.1 mg NO day (n = 43). The average CH and NO concentrations measured in our study were 4.0 ± 7.6 ppm and 392 ± 158 ppb, respectively (n = 104). 72% of sites where fluxes were measured were a source of biogenic CH. Overall, 47% of the sampled sites had biogenic CH, while only 13% of our sites had solely thermogenic CH. The other sites were either a source of both biogenic and thermogenic CH (13%), and a relatively large portion of sites had an unresolved source (29%). Overall, this survey of emissions across a large urban area indicates that production and emission of biogenic CH and NO is considerable, although CH fluxes are lower than those reported for cities with leaky natural gas distribution systems.
最近的研究表明,城市街道可能是从泄漏天然气管道排放甲烷(CH)的热点地区,尤其是在天然气分配系统较旧的城市。本研究的目的是确定泄漏的污水管道是否也可能是俄亥俄州辛辛那提市街道水平 CH 和氧化亚氮(NO)的来源,该市的天然气管道网络相对较新。为此,我们测量了 CH 的碳(δC)和氢(δH)稳定同位素组成,以区分来自污水气体的生物成因 CH 和来自泄漏天然气管道的热成因 CH,并测量了先前研究中街道水平 CH 增强(104 个地点中的 77 个)以及通过调查污水格栅和公用事业井盖发现的其他地点(104 个地点中的 27 个)的 CH 和 NO 通量率和浓度。δC-CH 和 δH-CH 的平均同位素特征分别为-48.5‰±6.0‰和-302‰±142‰。测量的通量率范围为 0.0 至 282.5 mg CH day 和 0.0-14.1 mg NO day(n=43)。本研究中测量的平均 CH 和 NO 浓度分别为 4.0±7.6 ppm 和 392±158 ppb(n=104)。72%的通量测量点是生物成因 CH 的来源。总体而言,47%的采样点有生物成因 CH,而仅有 13%的采样点仅有热成因 CH。其他采样点要么是生物成因和热成因 CH 的来源(13%),相当一部分采样点的来源无法确定(29%)。总的来说,这项对大型城市地区排放的调查表明,生物成因 CH 和 NO 的产生和排放相当可观,尽管 CH 通量低于报告的天然气分配系统泄漏城市的通量。