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Two-dimensional correlation analysis and multivariate time series analysis as innovative tools for the study and the comparison of the hydrocarbon distributions in marine antarctic cores

机译:二维相关分析和多元时间序列分析是研究和比较海洋南极岩心油气分布的创新工具

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In this paper we describe the use of innovative methods for the study of the hydrocarbon distribution in environmental samples such as marine sedimentary Antarctic cores. In the first and conventional step of this study, we determined by GC analysis the hydrocarbon markers which allow us to estimate the presence of biogenic, anthropogenic and petrogenic sources. These markers were the Carbon Preference Index (CPI), the Low Molecular Weight to High Molecular Weight (LMW/HMW), the pristane to phytane (Pry/Phy), the C_(17) to pristine (C_(17)/Pri) and the C_(18) to phytane (C_(18)/Phy) ratios, the presence of the so called unresolved complex mixtures (UCM), and the sum of two and three rings to the sum of higher ring (PAH(2.3)/PAH(4.6)) ratio. This part of the study showed the prevalent biogenic origin of hydrocarbons present in each sedimentary core with a minority presence of anthropogenic and pyrogenic sources of hydrocarbons. In the second and innovative step of this study we examined the GC chromatographic data sets of the cores by means of two-dimensional correlation analysis (2DC0RR) techniques such as two-dimensional mapping (2DMAP) and two-dimensional disrelation (2DDIS) analysis. The results of 2DMAP showed a more homogeneous distribution of hydrocarbons present in the inshore core whereas the offshore core showed to be highly heterogeneous. 2DDIS results confirmed these findings describing these differences as related to the presence of a wide content of hydrocarbons within the C_(20)-C_(40) range in the offshore core, depending reasonably on its specific stratigraphic and hydrologic conditions. At last, we applied Multivariate Time Series Analysis (MTSA) to study the effect of time on the spatial distribution of hydrocarbons along the sections of the cores. MTSA confirmed the different hydrological conditions present in the two sites. The innovative approach for the examination of hydrocarbon distribution by 2DC0RR and MTSA techniques allows us to retrieve information which, on the opposite, can be hardly retrieved by means of the conventional examination of GC results based on comparisons of the hydrocarbon contents and markers.
机译:在本文中,我们描述了使用创新方法研究环境样品(例如海洋沉积南极岩心)中的碳氢化合物分布的方法。在这项研究的第一步和常规步骤中,我们通过GC分析确定了烃标志物,这些烃标志物使我们能够估算出生物源,人为源和岩石成因的存在。这些标记是碳偏好指数(CPI),从低分子量到高分子量(LMW / HMW),从ane烷到植烷(Pry / Phy),从C_(17)到原始(C_(17)/ Pri)以及C_(18)与植烷的比率(C_(18)/ Phy),所谓的未解析复杂混合物(UCM)的存在以及两个和三个环的总和与较高环的总和(PAH(2.3) /PAH(4.6))比率。研究的这一部分显示了每个沉积岩心中普遍存在的烃类生物成因,而人为和热源性烃类却很少。在本研究的第二个创新步骤中,我们通过二维相关分析(2DC0RR)技术(例如二维映射(2DMAP)和二维不相关(2DDIS)分析)检查了岩心的GC色谱数据集。 2DMAP的结果表明,近海岩心中存在的碳氢化合物分布更加均匀,而近海岩心则表现出高度非均质性。 2DDIS的结果证实了这些发现,这些发现描述了这些差异与离岸核心C_(20)-C_(40)范围内广泛的碳氢化合物的存在有关,具体取决于其特定的地层和水文条件。最后,我们应用多元时间序列分析(MTSA)研究了时间对沿岩心截面的碳氢化合物空间分布的影响。 MTSA确认了这两个地点存在不同的水文条件。通过2DC0RR和MTSA技术检查碳氢化合物分布的创新方法使我们能够检索信息,相反,通过基于碳氢化合物含量和标记物比较的常规GC结果检查,很难检索到这些信息。

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