首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Quantification of seep-related methane gas emissions at Tommeliten, North Sea
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Quantification of seep-related methane gas emissions at Tommeliten, North Sea

机译:北海Tommeliten的与渗出有关的甲烷排放量的量化

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Tommeliten is a prominent methane seep area in the Central North Sea. Previous surveys revealed shallow gas-bearing sediments and methane gas ebullition into the water column. In this study, the in situ methane flux at Tommeliten is re-assessed and the potential methane transport to the atmosphere is discussed, with regards to the hydrographic setting and gas bubble modeling. We have compiled previous data, acquired new video and acoustic evidence of gas bubble release, and have measured the methane concentration, and its C-isotopic composition in the water column. Parametric subbottom sonar data reveal the three-dimensional extent of shallow gas and morphologic features relevant for gas migration. Five methane ebullition areas are identified and the main seepage area appears to be 21 times larger than previously estimated. Our video, hydroacoustic, subbottom, and chemical data suggest that ~1.5×10!6molCH_4/yr (~26tonsCH_4/yr) of methane gas is being released from the seepage area of Tommeliten. Methane concentration profiles in the vicinity of the gas seeps show values of up to 268nM (~100 times background) close to the seafloor. A decrease in δ~(13)C-CH_4 values at 40m water depth indicates an unknown additional biogenic methane source within the well oxygenated thermocline between 30 and 40m water depth. Numerical modeling of the methane bubbles due to their migration and dissolution was performed to estimate the bubble-derived vertical methane transport, the fate of this methane in the water column, and finally the flux to the atmosphere. Modeling indicates that less than ~4% of the gas initially released at the seafloor is transported via bubbles into the mixed layer and, ultimately, to the atmosphere. However, because of the strong seasonality of mixing in the North Sea, this flux is expected to increase as mixing increases, and almost all of the methane released at the seafloor could be transferred into the atmosphere in the stormy fall and winter time.
机译:Tommeliten是北海中部一个重要的甲烷渗透区。先前的调查显示,浅层含气沉积物和甲烷气沸腾进入水柱。在这项研究中,重新评估了Tommeliten的原位甲烷通量,并讨论了有关水文环境和气泡建模的潜在甲烷向大气的传输。我们收集了以前的数据,获得了气泡释放的新视频和声音证据,并测量了水柱中的甲烷浓度及其C同位素组成。参数化的底部声纳数据揭示了浅层气体的三维范围和与气体运移相关的形态特征。确定了五个甲烷沸腾区域,主要的渗流面积似乎比先前估计的大21倍。我们的视频,水声,底部和化学数据表明,从Tommeliten的渗流区释放出了约1.5×10!6molCH_4 / yr(约26tonsCH_4 / yr)的甲烷气体。气体渗漏附近的甲烷浓度曲线显示,靠近海底的甲烷浓度最高可达268nM(约为背景的100倍)。在水深40m处δ〜(13)C-CH_4值降低表明在水深30至40m之间的含氧温床中有未知的其他生物甲烷源。对甲烷气泡由于其迁移和溶解而进行了数值模拟,以估算气泡衍生的垂直甲烷传输,该甲烷在水柱中的命运以及最终通向大气的通量。模型表明,最初在海底释放的气体中,只有不到〜4%的气体通过气泡进入混合层,最终到达大气。但是,由于北海混合的强烈季节性,预计这种流量会随着混合的增加而增加,并且在暴风雨的秋季和冬季,几乎所有在海底释放的甲烷都可能转移到大气中。

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