Romero Isabel C, Toro-Farmer Gerardo, Diercks Arne-R, Schwing Patrick, Muller-Karger Frank, Murawski Steven, Hollander David J
University of South Florida, College of Marine Science, St. Petersburg, FL 33701, USA.
University of South Florida, College of Marine Science, St. Petersburg, FL 33701, USA.
Environ Pollut. 2017 Sep;228:179-189. doi: 10.1016/j.envpol.2017.05.019. Epub 2017 May 20.
The blowout of the Deepwater Horizon (DWH) drilling rig in 2010 released an unprecedented amount of oil at depth (1,500 m) into the Gulf of Mexico (GoM). Sedimentary geochemical data from an extensive area (∼194,000 km) was used to characterize the amount, chemical signature, distribution, and extent of the DWH oil deposited on the seafloor in 2010-2011 from coastal to deep-sea areas in the GoM. The analysis of numerous hydrocarbon compounds (N = 158) and sediment cores (N = 2,613) suggests that, 1.9 ± 0.9 × 10 metric tons of hydrocarbons (>C9 saturated and aromatic fractions) were deposited in 56% of the studied area, containing 21± 10% (up to 47%) of the total amount of oil discharged and not recovered from the DWH spill. Examination of the spatial trends and chemical diagnostic ratios indicate large deposition of weathered DWH oil in coastal and deep-sea areas and negligible deposition on the continental shelf (behaving as a transition zone in the northern GoM). The large-scale analysis of deposited hydrocarbons following the DWH spill helps understanding the possible long-term fate of the released oil in 2010, including sedimentary transformation processes, redistribution of deposited hydrocarbons, and persistence in the environment as recycled petrocarbon.
2010年,“深水地平线”(DWH)钻井平台发生井喷,向墨西哥湾(GoM)深处(1500米)释放了前所未有的大量石油。利用来自广阔区域(约194,000平方千米)的沉积地球化学数据,来表征2010 - 2011年沉积在GoM沿海至深海区域海底的DWH石油的数量、化学特征、分布和范围。对大量碳氢化合物(N = 158)和沉积物岩心(N = 2,613)的分析表明,在研究区域的56%沉积了1.9±0.9×10公吨的碳氢化合物(>C9饱和烃和芳烃馏分),占DWH泄漏未回收石油总量的21±10%(高达47%)。对空间趋势和化学诊断比率的研究表明,风化的DWH石油在沿海和深海区域大量沉积,而在大陆架(GoM北部的过渡区域)沉积可忽略不计。对DWH泄漏后沉积碳氢化合物的大规模分析有助于了解2010年泄漏石油可能的长期归宿,包括沉积转化过程、沉积碳氢化合物的重新分布以及作为循环石油碳在环境中的持久性。