OIL YIELD AND BULK GEOCHEMICAL PARAMETERS OF OIL SHALES FROM THE SONGLIAO AND HUADIAN BASINS, CHINA: A GRADE CLASSIFICATION APPROACH

Oil Shale ◽  
2013 ◽  
Vol 30 (3) ◽  
pp. 402 ◽  
Author(s):  
P SUN ◽  
Z LIU ◽  
R GRATZER ◽  
Y XU ◽  
R LIU ◽  
...  
1980 ◽  
Vol 17 (1) ◽  
pp. 13-21
Author(s):  
C. William Keighin

Inter- and intra-laboratory comparison of Fischer assay data and testing of these data by correlation analysis indicate good correlation but varied amounts of scatter in the data. The scatter seems to be due to both mechanical and analytical factors; it is possible that non-uniform sample preparation is a dominant factor in causing scatter, but variable analytical results are also apparent. The range in precision of the Fischer assay data is generally small and probably does not seriously affect the accuracy of the calculated shale-oil resources. It is highly desirable to have an accurate and uniform assay method to determine the oil yield of oil shales. If inter- or intra-laboratory precision is to be maintained, it is imperative that sample preparation and analytical conditions are uniform and closely supervised.


1980 ◽  
Vol 17 (9) ◽  
pp. 1315-1321 ◽  
Author(s):  
K. Rajeshwar ◽  
J. DuBow ◽  
R. Thapar

Laboratory measurements on the radio-frequency (10–103 MHz) electrical behavior of Green River oil shales were carried out using an automated frequency domain technique. Data are presented which show the variation of the relative dielectric constant (ε′), dielectric loss (ε″), and loss tangent (tan δ) with shale oil yield, frequency, temperature, and water content. The magnitude of these electrical parameters is shown to be sensitive to water content and possibly to varve geometry. The ε′ values tend to decrease and tan δ increases with increasing oil yield for shales subjected to prior thermal treatment at ~110 °C for 1–2 weeks. A systematic variation is observed in the degree of scatter and in the extent of correlation of tan δ and ε′ as a function of oil yield with each subsequent thermal treatment cycle. The manner in which variations in shale water content and (or) varve geometry influence the magnitude of the measured dielectric parameters is illustrated by duplicate measurements on samples with identical organic content. Such effects are shown to be important at low measurement frequencies (< 200 MHz). The temperature dependence of ε′ and ε″ is seen to be weak in the range 25–250 °C and appears to be largely dominated by temperature-induced changes in the water content of the shale.


Fuel ◽  
1988 ◽  
Vol 67 (5) ◽  
pp. 733-734 ◽  
Author(s):  
Leslie S. Dale ◽  
Christian E. Matulis
Keyword(s):  
X Ray ◽  

Oil Shale ◽  
2012 ◽  
Vol 29 (3) ◽  
pp. 206
Author(s):  
I JOHANNES ◽  
H LUIK ◽  
J A BOJESEN-KOEFOED ◽  
L TIIKMA ◽  
N VINK ◽  
...  

Energy ◽  
1999 ◽  
Vol 24 (9) ◽  
pp. 761-781 ◽  
Author(s):  
J.O. Jaber ◽  
S.D. Probert ◽  
P.T. Williams
Keyword(s):  

Fuel ◽  
1986 ◽  
Vol 65 (7) ◽  
pp. 1028-1029 ◽  
Author(s):  
Moubin Choudhury ◽  
Karen F. Rheams ◽  
James W. Harrell

1921 ◽  
Vol 3 (6supp) ◽  
pp. 569-570
Author(s):  
L. C. Kakkick
Keyword(s):  

2020 ◽  
Vol 42 (4) ◽  
pp. 33-49
Author(s):  
O.V. CHEPIZHKO ◽  
V.V. YANKO ◽  
V.M. KADURIN ◽  
I.M. NAUMKO ◽  
S.M. SHATALIN

For the first time the importance of mineralogical and lithological-petrographical ranks in the line of geological information ranks is substantiated for implementation of long-term forecasts, standard and non-standard approaches to research of physical and geochemical parameters as a basis of creation of complex system of forecast criteria and prospecting indicators of hydrocarbons within the sedimentary cover of Black sea based on the theory of global fluid-flows derivation. These criteria have different sensitivity to the object (hydrocarbon deposits) and are therefore ranked. The ranking determined the following parameters: 1) seismic data within the object, obtained by the method of deep seismic sounding, RWM SDP; 2) parameters of tectono-geodynamic structures; 3) the main characteristics of sedimentary cover and bedrock; 4) geochemical characteristics; 5) parameters of mineral complexes and fluid inclusions in mineral neoformations; 6) the value of the distribution of meiobenthos. Based on modern views of oil and gas geology, structural-tectonic and lithological-facies criteria are among the main ones. The study of the mineralogical component of sediments is made with using mineralogical, thermobarogeochemical and X-ray spectral methods. Fixation of anomalies of fluid flow at the bottom of the Black Sea as to the distribution of abiotic parameters in order to assess the prospects of oil and gas is determined by structural and tectonic features and high permeability of fluid flow; parameters of mineral complexes (minerals, facies) and genetic connections; heterogeneity of geochemical characteristics of bottom sediments; the presence of hydrocarbon inclusions in authigenic minerals of bottom sediments.


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