4.5 Article

Determination of in situ hydrocarbon contents in shale oil plays. Part 1: Is routine Rock-Eval analysis reliable for quantifying the hydrocarbon contents of preserved shale cores?

期刊

ORGANIC GEOCHEMISTRY
卷 170, 期 -, 页码 -

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.orggeochem.2022.104449

关键词

Shale oil; In situ hydrocarbon content; Rock-Eval; TD-GC, NMR T-1-T-2 mapping; S1 peak Dean-Stark extraction

资金

  1. National Natural Science Foundation of China [42102154, 41922015, 42072147]
  2. Postdoctoral Research Foundation of China [2021M690168]
  3. Postdoctoral Innovative Talent Support Program of Shandong Province [SDBX2021004]
  4. Fundamental Research Funds for the Central Universities [20CX06085A]
  5. Key Laboratory of Tectonics and Petroleum Resources (China University of Geosciences) [TPR-2021-02]
  6. Qingdao Postdoctoral [ZX20210070]
  7. Geological Survey of Canada's GNES (Geoscience for New Energy Supply) research program

向作者/读者索取更多资源

Accurate determination of in situ hydrocarbon content is crucial for the assessment of shale oil plays. This study found that sample preparation and analysis delay can lead to underestimation of hydrocarbon content, particularly liquid hydrocarbons. Techniques using larger rock pieces are recommended for quantifying hydrocarbon content in preserved shale samples.
An accurate determination of in situ hydrocarbon (oil) content is critical for the assessment of shale oil plays in terms of their total resources in place and recovery potential. Although correction of light hydrocarbon loss to the Rock-Eval S1 parameters on conventional core and cuttings samples has been recently attempted using preserved (e.g., sealed or pressure-preserved) cores, hydrocarbon evaporation loss during sample preparation and delay time before the actual commencement of Rock-Eval analysis has not received sufficient attention. In this study, a combination of petrophysical and geochemical techniques including Dean-Stark extraction, hydrogen nuclear magnetic resonance (1H-NMR) T1 -T2 mapping, thermal desorption-gas chromatography (TD-GC) analysis, and Rock-Eval programmed pyrolysis were used in parallel on a set of 30 preserved shale cores to determine their total hydrocarbon contents. The preserved shale cores were analyzed in large pieces (e.g., 3-5 cm in size) by the former two petrophysical methods while using fine powder (e.g., < 60 mesh) by the latter two thermal analytical methods. The total free hydrocarbon contents (equivalent of Rock-Eval S1) determined on the studied lacustrine shale samples with a Ro ranging from 1.00% to 1.51% followed the order of Dean-Stark (average 10.27 mg/g) & AP; NMR (10.34) > TD-GC (6.65) > Rock-Eval (3.93). The core crushing and grinding process required for both TD GC and Rock-Eval pyrolysis analyses was found to cause a loss of approximately 35% to the in situ hydrocarbons. In addition, Rock-Eval analysis delay time (of 5 min) could lead to another 25% reduction to the total free hydrocarbons. In combination, sample preparation and analysis delay resulted in up to 60% reduction to the Rock-Eval S1 peaks for the preserved shale cores, and a 30% loss to the liquid (C6+) hydrocarbons in particular. To the best of our knowledge, this is the first reported observation that in situ light hydrocarbon contents can be severely underestimated by Rock-Eval and TD-GC analyses using powdered forms of preserved core samples. The extents of light hydrocarbon loss in conventional cores have been underestimated using the Rock-Eval S1 difference between preserved shale and its long-duration exposed replicates. Hence, when quantifying the hydrocarbon contents of the preserved shale samples, techniques utilizing larger rock pieces are highly recommended.

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