The distribution and association of trace elements in the bitumen, kerogen and pyrolysates from New Albany oil shale
The distribution and association of trace elements in bitumen, kerogen and pyrolysates from New Albany oil shale were investigated using instrumental neutron activation analysis (INAA), x-ray diffraction (XRD), electron microprobe x-ray fluorescence (EMP-XRF), liquid chromatography, ultra-violet spectroscopy and mass spectrometry. The kerogen was found to contain several HCl/HF resistant minerals (determined by XRD), including pyrite, marcasite, chalcopyrite, rutile, and anatase, and the neoformed mineral ralstonite. Kerogens (prepared at UNOCAL, CA) which were fractionated in an aqueous ZnBr[sub 2] solution were found to contain [approximately]20% less acid-resistant minerals than traditional' HCl/HF isolated kerogens and were contaminated with Zn and Br. Kerogens (prepared at the University of Munich) treated with SnCl[sub 2]/H[sub 3]PO[sub 4] at 150-270[degrees]C (Kiba) and/or SnCl[sub 2]/HCl at 110[degrees]C were found to contain <10% of their original pyrite/marcasite (FeS[sub 2]), but were contaminated with large amounts of Sn. The Kiba treatment also appeared to demetallate Ni(II) and VO(II) porphyrins. The inorganic and organic associations of trace elements in New Albany kerogen were studied by analysis of kerogen fractions and a mineral residue ([approximately]85% FeS[sub 2]) obtained through density separations. The degree of association of several elements (As, Co, Mn, Mo, Ni, Sb, and Se) with FeS[sub 2] was determined through the analysis of individual mineral grains by EMP-XRF and by analysis of the mineral residue treated with dilute HNO[sub 3] to remove FeS[sub 2]. These studies indicated that essentially all of the V and [approximately]95% of the Ni present in New Albany kerogen is organically associated. Methods which are designed to account for the inorganic associations of trace elements in kerogens, including methods based on physical methods of separation, chemical removal of FeS[sub 2], EMP-XRF and low temperature ashing, are compared.
- Research Organization:
- Washington State Univ., Pullman, WA (United States)
- OSTI ID:
- 7197938
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
040500* -- Oil Shales & Tar Sands-- Properties & Composition
ALKALINE EARTH METALS
ANTIMONY
BITUMENS
BITUMINOUS MATERIALS
CALCIUM
CARBONACEOUS MATERIALS
CHEMICAL ANALYSIS
ELEMENTS
ENERGY SOURCES
FOSSIL FUELS
FUELS
KEROGEN
MANGANESE
MATERIALS
MATTER
METALS
MOLYBDENUM
NICKEL
OIL SHALES
ORGANIC COMPOUNDS
ORGANIC MATTER
OTHER ORGANIC COMPOUNDS
PYROLYSIS PRODUCTS
QUANTITATIVE CHEMICAL ANALYSIS
ROCKS
SEDIMENTARY ROCKS
SELENIUM
SEMIMETALS
SHALES
TAR
TRANSITION ELEMENTS
VANADIUM
ZINC