Elsevier

Fuel

Volume 66, Issue 9, September 1987, Pages 1176-1184
Fuel

Main paper
Product evolution during rapid pyrolysis of Green River Formation oil shale

https://doi.org/10.1016/0016-2361(87)90054-8Get rights and content

Abstract

The devolatilization of rich (209 cm3 kg−1), rapidly heated (1000 K s−1) Green River Formation, Colorado, oil shale has been studied at temperatures from ≈ 600 to 1100K, under helium (170 kPa) and vacuum. Oil yields decrease with increasing pressure at temperatures above the 800–900 K range. This is attributed to an increased probability of condensed phase cracking reactions involving oil precursors with increased pressure. The fact that escape of the oil from shale particles is vaporization-rate limited is supported by a comparison of the molecular weights of oil collected outside the particle and that left within the particle. The measured nature of particle porosity is consistent with the view that external gas pressure can affect vaporization rates within pores. Elemental and infrared characterization of different molecular weight fractions of oil are presented.

References (41)

  • P.R. Solomon et al.

    Fuel

    (1986)
  • H. Nieh et al.

    Fuel

    (1984)
  • R.L. Braun et al.

    Fuel

    (1986)
  • R.D. Noble et al.

    Fuel

    (1982)
  • R.D. Noble et al.

    Fuel

    (1981)
  • C.C. Wang et al.

    Fuel

    (1983)
  • C.S. Wen et al.

    Fuel

    (1983)
  • P.E. Unger et al.

    Fuel

    (1984)
  • E.B. Huss et al.

    Fuel

    (1982)
  • E.M. Suuberg et al.

    Fuel

    (1985)
  • P.R. Solomon et al.

    Fuel

    (1980)
  • A.K. Burnham

    Fuel

    (1979)
    C.A. Slettevold et al.

    Lawrence Livermore National Laboratory, Report UCRL-52619

    (1978)
  • P.E. Unger et al.
  • A.K. Burnham
  • A.K. Burnham et al.

    Fuel

    (1980)
  • M. Steinberg et al.

    Am. Chem. Soc. Div. Fuel Chem. Preprints

    (1984)
  • D.R. Kahn et al.

    Am. Chem. Soc. Div. Fuel Chem. Preprints

    (1984)
  • P.H. Wallman et al.

    Am. Chem. Soc. Div. Fuel Chem. Preprints

    (1980)
  • J.H. Campbell et al.

    In Situ

    (1978)
  • A.K. Burnham et al.
  • Cited by (21)

    • Secondary cracking of volatile and its avoidance in infrared-heating pyrolysis reactor

      2018, Carbon Resources Conversion
      Citation Excerpt :

      Therefore, the modification of heating method to the cross-direction with the flow of pyrolysis products contributed the suppression of secondary reactions and the yield increase of shale oil. Many literatures have reported that vacuum pyrolysis has a potential to increase shale oil yield due to the quick extraction of the volatile from the materials and the high temperature region of the reactor [27,28]. Therefore, the pyrolysis of oil shale should be conducted under reduced pyrolysis pressure, e.g. 0.6 atm, to investigate the pyrolysis behavior under the conditions with minimized secondary reactions.

    • Experimental investigation of the role of rock fabric in gas generation and expulsion during thermal maturation: Anhydrous closed-system pyrolysis of a bitumen-rich Eagle Ford Shale

      2018, Organic Geochemistry
      Citation Excerpt :

      Carbon dioxide is commonly one of the most abundant gases generated from pyrolysis experiments, yet it is generally a trace component in produced natural gas (Andresen et al., 1994; Lewan, 1997; Kotarba et al., 2009; Kotarba and Lewan, 2013). Numerous studies have attempted to explain these observed differences between naturally and experimentally generated gas, and specific factors that have been examined include: open, semi-open, or closed-system pyrolysis techniques (Arneth and Matzigkeit, 1986; Andresen et al., 1993; Dieckmann et al., 2000; Michels et al., 2002), differences in heating procedures (Dieckmann et al., 2004) or confining pressures (Suuberg et al., 1987; Price and Wenger, 1992; Landais et al., 1994; Shuai et al., 2006; Tao et al., 2010), and the presence of various materials including: mineral matrices (Espitalié et al.,1980, 1984; Su et al., 2006; Pan et al., 2009; Holman et al., 2014), transition metals (Mango, 1992, 1996; Mango et al., 1994; Su et al., 2006; Lewan et al., 2008), and water (Hoering, 1984; Stalker et al., 1994; Lewan, 1997; Su et al., 2006; Pan et al., 2009). Another factor that has been shown to influence the products of pyrolysis experiments is the particle size of the rock sample.

    View all citing articles on Scopus

    Present address: ICI Polyurethanes, West Deptford, NJ, USA.

    View full text