18 research outputs found
Evaluation of the chemical composition and structure of asphaltenes from there offshore brazilian biodegrades heavy oils
Asphaltenes fractions were extracted and purified from three heavy Brazilian oils. Their mass compositions of C, H, N, Ni and V were obtained from elemental analysis and S and O atomic percentages from EDS. The H/C ratios showed high degree of unsaturation, while the O atomic percentages indicated more pronounced biodegradation effects on two samples. Quantitative data on N, Ni, and V and semi-quantitative data on S were related to oils origins. The structural data of asphaltenes were explored by combining Fourier transform infrared spectroscopy (FTIR) and proton nuclear magnetic resonance (1H NMR). The oil with the lower degree of biodegradation contained asphaltenes with a lower level of condensed aromatic rings and longer aliphatic chain substituents. The asphaltenes obtained from the two most biodegraded oils showed similarities of polar groups and the presence of carboxylic functions, as well as lower contents of aliphatic substituents. The quality and quantity of occluded hydrocarbons were assessed after the mild oxidation of the separated asphaltenes fractions. It was suggested that the severe biodegradation which altered these structures may also be responsible to affect their occluded hydrocarbons
Digital Outcrop Model Generation from Hybrid UAV and Panoramic Imaging Systems
The study of outcrops in geosciences is being significantly improved by the enhancement of technologies that aims to build digital outcrop models (DOMs). Usually, the virtual environment is built by a collection of partially overlapped photographs taken from diverse perspectives, frequently using unmanned aerial vehicles (UAV). However, in situations including very steep features or even sub-vertical patterns, incomplete coverage of objects is expected. This work proposes an integration framework that uses terrestrial spherical panoramic images (SPI), acquired by omnidirectional fusion camera, and a UAV survey to overcome gaps left by traditional mapping in complex natural structures, such as outcrops. The omnidirectional fusion camera produces wider field of view images from different perspectives, which are able to considerably improve the representation of the DOM, mainly where the UAV has geometric view restrictions. We designed controlled experiments to guarantee the equivalent performance of SPI compared with UAV. The adaptive integration is accomplished through an optimized selective strategy based on an octree framework. The quality of the 3D model generated using this approach was assessed by quantitative and qualitative indicators. The results show the potential of generating a more reliable 3D model using SPI allied with UAV image data while reducing field survey time and complexity
Pearson Correlation Coefficient Applied to Petroleum System Characterization: The Case Study of Potiguar and Reconcavo Basins, Brazil
This study applied the Pearson correlation coefficient and principal component analysis as tools for unsupervised qualitative petroleum system evaluation techniques. A total of 252 oil samples (32 features per sample) representative of two Brazilian sedimentary basins (Recôncavo and Potiguar) were used to classify them according to their respective degrees of maturation and origin. The large initial set of variables comprises data on δ13C composition, saturate, aromatic, polar compound fractions, and the techniques reduced biomarkers to the most important variables, maintaining the global pattern of variance. The results were efficient in discriminating different petroleum systems from lacustrine, marine, and mixing sources, as observed in the studied accumulations from the Lower Cretaceous sediments of the Recôncavo and Potiguar basins. The methodology proved to be very useful to vene better characterize the petroleum systems. This methodology can be applied to analyze a large amount of oil samples, using simple software and spending relatively less time
Evaluation of the effects of the simulated thermal evolution of a Type-I source rock on the distribution of basic nitrogen-containing compounds
Geochemical Considerations from the Carboniferous Unconventional Petroleum System of SW Iberia
The Baixo Alentejo Flysch Group (BAFG) is an important stratigraphic unit that covers
over half of the South Portuguese Zone (SPZ) depositional area, and it is composed by three main
tectono-stratigraphic units: the MĂ©rtola, Mira, and Brejeira formations. All of these formations
contain significant thicknesses of black shales and have several wide areas with 0.81 wt.%, 0.91 wt.%,
and 0.72 wt.% average total organic carbon (TOC) (respectively) and thermal maturation values
within gas zones (overmature). This paper is considering new data from classical methods of organic
geochemistry characterization, such as TOC, Rock–Eval pyrolysis, and organic petrography, to
evaluate the unconventional petroleum system from the SPZ. A total of 53 samples were collected.
From the stratigraphical point of view, TOC values seem to have a random distribution. The Rock–
Eval parameters point out high thermal maturation compatible with gas window (overmature zone).
The samples are dominated by gas-prone extremely hydrogen-depleted type III/IV kerogen, which
no longer has the potential to generate and expel hydrocarbons. The petrographic analyses positioned
the thermal evolution of these samples into the end of catagenesis to metagenesis (wet to dry gas
zone), with values predominantly higher than 2 %Ro (dry gas zone). The presence of thermogenic
hydrocarbon fluids characterized by previous papers indicate that the BAFG from SPZ represents a
senile unconventional petroleum system, working nowadays basically as a gas reservoir
Preservation Factors during Cretaceous Oceanic Anoxic Events in the Espírito Santo Basin, Southeast Brazil
The oceanic anoxic events (OAEs) are characterized by enhanced accumulation of organic matter in marine sediments. However, there is still an ongoing debate regarding the interplay between production and preservation during these events. Moreover, few studies provide quantitative estimations of primary productivity and/or the amount of carbon preserved during the OAEs. Here, we used geochemical data from multiple wells located at the Espírito Santo Basin that cover the intervals of events OAE1d and OAE2 to provide quantitative estimates of preservation factors. Our results show enhanced preservation during OAEs compared to modern conditions and a stronger preservation during OAE1d compared to OAE2 in the Espírito Santo Basin. The amount of preserved carbon could reach up to 8.6% during OAE1d, depending on the productivity of the system. In addition, we show that such improvement in preservation is linked to the bottom water with low-O2 concentrations and not due to fast burial caused by high sedimentation rates. Our findings are extremally relevant for organic carbon and source rock modelling studies since model simulations need quantitative estimations
Preservation Factors during Cretaceous Oceanic Anoxic Events in the EspĂrito Santo Basin, Southeast Brazil
The oceanic anoxic events (OAEs) are characterized by enhanced accumulation of organic matter in marine sediments. However, there is still an ongoing debate regarding the interplay between production and preservation during these events. Moreover, few studies provide quantitative estimations of primary productivity and/or the amount of carbon preserved during the OAEs. Here, we used geochemical data from multiple wells located at the EspĂrito Santo Basin that cover the intervals of events OAE1d and OAE2 to provide quantitative estimates of preservation factors. Our results show enhanced preservation during OAEs compared to modern conditions and a stronger preservation during OAE1d compared to OAE2 in the EspĂrito Santo Basin. The amount of preserved carbon could reach up to 8.6% during OAE1d, depending on the productivity of the system. In addition, we show that such improvement in preservation is linked to the bottom water with low-O2 concentrations and not due to fast burial caused by high sedimentation rates. Our findings are extremally relevant for organic carbon and source rock modelling studies since model simulations need quantitative estimations
Late Cretaceous cyclostratigraphy and astrochronology based on Natural Gamma Ray of the well-log ES-1 drilled at the EspĂrito Santo basin (western South Atlantic)
NGR is a geophysical acquisition made by Petrobras at the time of well drilling. Petrobras acquired natural gamma-ray (NGR) data for well ES-1 measured between 1880.6 and 5405.7 m
Late Cretaceous cyclostratigraphy for the subtropical western South Atlantic, EspĂrito Santo Basin
Well-log data was acquired in a Late Cretaceous section of the EspĂrito Santo basin (western South Atlantic). Cyclostratigraphic techniques were used to explore the eventual pacing of orbital cycles in the deposition of sequences. The frequency ratio method was used to interpret the orbital cycles and based on this a long-eccentricity signal was interpreted and extracted to create a floating time-scale. Using a seismic horizon associated Cretaceous-Paleogene transition, a strong shift in the natural gamma-ray data was anchored to an age of 66.0 Ma producing an anchored astronomical time-scale placed between late Albian and early Ypresian