Coupling of methoxy group with organic matter during methanolysis of heavy hydrocarbon using oil shale as an example

Author(s):  
Zhenghua Lu ◽  
Zhenyu Liu ◽  
Xiaosheng Zhao ◽  
Yachuan Guo ◽  
Qingya Liu
2018 ◽  
Vol 480 (1) ◽  
pp. 611-614
Author(s):  
D. A. Bushnev ◽  
N. S. Burdelnaya ◽  
I. V. Goncharov ◽  
V. V. Samoylenko ◽  
M. A. Veklich

1992 ◽  
Vol 18 (4) ◽  
pp. 511-519 ◽  
Author(s):  
B. Jovančićević ◽  
D. Vitorović ◽  
M. Šaban ◽  
H. Wehner
Keyword(s):  

Geosciences ◽  
2020 ◽  
Vol 10 (9) ◽  
pp. 337
Author(s):  
Hanane Sghiouri El Idrissi ◽  
Abderrahim Samaouali ◽  
Younes El Rhaffari ◽  
Salah El Alami ◽  
Yves Geraud

In this work, we study the variability of the lithological composition and organic matter content of samples were taken from the different layers M, X and Y of the Timahdit oil shale in Morocco, in order to experimentally analyze the impact of this variability on petrophysical measurements. The objective of this study is to predict the properties of the layers, including their thermal conductivity, thermal diffusivity, porosity and P and S wave velocities. The results of the study of the impact of the organic matter content of the samples on the petrophysical measurements show that, regardless of the organic matter content, thermal conductivity and diffusivity remain insensitive, while P and S wave velocities decrease linearly and porosity increases with increasing organic matter content. On the other hand, the study of the organic matter variability content is consistent with the velocity ratio, so can be used as an organic matter indicator of the layers. Conductivity and thermal diffusivity are almost invariant to the variability of the organic matter.


2020 ◽  
Vol 60 (9) ◽  
pp. 991-997
Author(s):  
E. Yu. Kovalenko ◽  
A. V. Petrov ◽  
I. S. Korol’ ◽  
T. A. Sagachenko ◽  
R. S. Min ◽  
...  

2019 ◽  
Vol 33 (2) ◽  
pp. 859-867 ◽  
Author(s):  
Qing Liu ◽  
Yucui Hou ◽  
Weize Wu ◽  
Yupeng Wang ◽  
Qian Wang ◽  
...  
Keyword(s):  

1980 ◽  
Vol 20 (1) ◽  
pp. 44 ◽  
Author(s):  
A.C. Hutton ◽  
A.J. Kantsler ◽  
A.C. Cook ◽  
D.M. McKirdy

The Tertiary oil-shale deposits at Rundle in Queensland and of the Green River Formation in the western USA, together with Mesozoic deposits such as those at Julia Creek in Queensland, offer prospects of competitive recovery cost through the use of large-scale mining methods or the use of in situ processing.A framework for the classification of oil shales is proposed, based on the origin and properties of the organic matter. The organic matter in most Palaeozoic oil shales is dominantly large, discretely occurring algal bodies, referred to as alginite A. However, Tertiary oil shales of northeastern Australia are chiefly composed of numerous very thin laminae of organic matter cryptically-interbedded with mineral matter. Because the present maceral nomenclature does not adequately encompass the morphological and optical properties of most organic matter in oil shales, it is proposed to use the term alginite B for finely lamellar alginite, and the term lamosites (laminated oil shales) for oil shales which contain alginite B as their dominant organic constituent. In the Julia Creek oil shale the organic matter is very fine-grained and contains some alginite B but has a higher content of alginite A and accordingly is assigned to a suite of oil shales of mixed origin.Petrological and chemical techniques are both useful in identifying the nature and diversity of organic matter in oil shales and in assessing the environments in which they were formed. Such an understanding is necessary to develop exploration concepts for oil shales.


2000 ◽  
Vol 31 (9) ◽  
pp. 787-798 ◽  
Author(s):  
Sylvie Derenne ◽  
Claude Largeau ◽  
Alice Brukner-Wein ◽  
Magdolna Hetenyi ◽  
Gérard Bardoux ◽  
...  

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