Abrahamsson Katarina, Damm Ellen, Björk Göran, Bunse Carina, Sellmaier Samuel, Broström Göran, Assmann Volkmar, Dumitrascu Adela, Maciute Adele, Olofsson Niten, Pourdanandeh Milad
Department of Marine Sciences, University of Gothenburg, Medicinaregatan 7b, 413 90, Gothenburg, Sweden.
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Telegrafenberg A45, 14473, Potsdam, Germany.
Sci Rep. 2024 Jun 19;14(1):12848. doi: 10.1038/s41598-024-63449-2.
On September 26th, 2022, the detonations at the gas pipelines Nord Stream 1 and 2 resulted in some of the largest non-natural releases of methane known. The distribution of methane in the surrounding seawater and the possible effects were not apparent. To trace the pathways of methane we recorded CH concentrations and the isotopic signal (δC-CH) in seawater, and air. A week post-explosion, we detected methane concentrations up to 4 orders of magnitude above the natural Baltic Sea background. The released fossil methane created a distinct plume with δC-CH ratios differing from natural background values. The strong water stratification preserved the distribution pattern initiated by the explosion, shown by the laterally strong concentration gradient within the plume. Our analysis encompasses three stages of the explosion's impact; the initial sea-air methane release, measurements taken during our research expedition one week later, and a third stage triggered by the shift from summer to winter conditions as an outlook on how winter mixing and microbial activity will influence the plume.
2022年9月26日,北溪1号和2号天然气管道发生爆炸,导致了已知的一些规模最大的甲烷非自然泄漏。甲烷在周围海水中的分布情况以及可能产生的影响尚不明确。为了追踪甲烷的传播路径,我们记录了海水中和空气中的CH浓度以及同位素信号(δC-CH)。爆炸一周后,我们检测到甲烷浓度比波罗的海自然背景值高出4个数量级。释放出的化石甲烷形成了一个独特的羽流,其δC-CH比值与自然背景值不同。强烈的水体分层保存了由爆炸引发的分布模式,羽流内部横向的强浓度梯度就表明了这一点。我们的分析涵盖了爆炸影响的三个阶段:最初的海-气甲烷释放、一周后我们科考期间进行的测量,以及作为冬季混合和微生物活动将如何影响羽流的展望而由夏季到冬季条件转变引发的第三阶段。