Department of Earth Sciences, Royal Holloway, University of London, Egham TW20 0EX, UK.
Department of Earth Sciences, Royal Holloway, University of London, Egham TW20 0EX, UK.
Sci Total Environ. 2020 Mar 15;708:134600. doi: 10.1016/j.scitotenv.2019.134600. Epub 2019 Nov 3.
Baseline mobile surveys of methane sources using vehicle-mounted instruments have been performed in the Fylde and Ryedale regions of Northern England over the 2016-19 period around proposed unconventional (shale) gas extraction sites. The aim was to identify and characterise methane sources ahead of hydraulically fractured shale gas extraction in the area around drilling sites. This allows a potential additional source of emissions to atmosphere to be readily distinguished from adjacent sources, should gas production take place. The surveys have used ethane:methane (C2:C1) ratios to separate combustion, thermogenic gas and biogenic sources. Sample collection of source plumes followed by high precision δC analysis of methane, to separate and isotopically characterise sources, adds additional biogenic source distinction between active and closed landfills, and ruminant eructations from manure. The surveys show that both drill sites and adjacent fixed monitoring sites have cow barns and gas network pipeline leaks as sources of methane within a 1 km range. These two sources are readily separated by isotopes (δC of -67 to -58‰ for barns, compared to -43 to -39‰ for gas leaks), and ethane:methane ratios (<0.001 for barns, compared to >0.05 for gas leaks). Under a well-mixed daytime atmospheric boundary layer these sources are generally detectable as above baseline elevations up to 100 m downwind for gas leaks and up to 500 m downwind for populated cow barns. It is considered that careful analysis of these proxies for unconventional production gas, if and when available, will allow any fugitive emissions from operations to be distinguished from surrounding sources.
在 2016-19 年期间,针对拟议中的非常规(页岩)气开采地点,在英格兰北部的 Fylde 和 Ryedale 地区使用车载仪器对甲烷源进行了基线移动调查。目的是在该地区进行水力压裂页岩气开采之前,识别和描述甲烷源的特征。这使得在进行气体生产时,可以很容易地将潜在的额外排放源与相邻源区分开来。调查使用乙烷:甲烷(C2:C1)比值来分离燃烧、热成因气和生物成因源。对源羽流进行样本采集,然后对甲烷进行高精度 δC 分析,以分离和同位素特征化源,这增加了对活跃和封闭垃圾填埋场以及来自粪便的反刍动物嗳气之间的额外生物成因源的区分。调查表明,两个钻井地点和相邻的固定监测地点在 1 公里范围内都有牛棚和天然气网络管道泄漏作为甲烷源。这两个源可以通过同位素(牛棚的 δC 值为-67 至-58‰,而天然气泄漏的 δC 值为-43 至-39‰)和乙烷:甲烷比值(牛棚的<0.001,而天然气泄漏的>0.05)很容易区分开来。在混合良好的白天大气边界层下,这些源通常可以在顺风方向上检测到,距离天然气泄漏源高达 100 米,距离有人居住的牛棚源高达 500 米。如果有,对这些非常规生产气体的代理进行仔细分析,将允许将操作过程中的任何逸散排放与周围源区分开来。