scholarly journals Integration of High Temperature Gas Reactors with in Situ Oil Shale Retorting

2012 ◽  
Vol 61 (1T) ◽  
pp. 452-457
Author(s):  
Eric P. Robertson ◽  
Michael G. McKellar ◽  
Lee O. Nelson
1998 ◽  
Vol 69 (7) ◽  
pp. 2618-2621 ◽  
Author(s):  
George Meitzner ◽  
Simon R. Bare ◽  
Deborah Parker ◽  
Hyung Woo ◽  
Daniel A. Fischer

2008 ◽  
Vol 595-598 ◽  
pp. 501-509
Author(s):  
Damien Kaczorowski ◽  
Gouenou Girardin ◽  
S. Chamousset

Nickel base alloys 617 and 230 are promising candidates for the Intermediate Heat eXchanger (IHX) of GenIV Very High Temperature gas cooled Reactors. The capability to maintain an oxide layer as an efficient barrier against corrosion under mechanical loading is investigated through SEM in situ tensile test. The mechanical properties of external oxide layers are so compared between the two alloys. Cracks and spallation are observed. Few differences could be observed between these two alloys when pre oxidized in impure helium.


Geophysics ◽  
1984 ◽  
Vol 49 (10) ◽  
pp. 1701-1707 ◽  
Author(s):  
William Daily

Geophysical tomographs (geotomographs) were made of two underground oil‐shale retorts: (1) the Occidental Oil Shale Inc. miniretort constructed for ignition tests at the demonstration mine at Logan Wash, Colorado; and (2) the Geokinetics Oil Shale Inc. Retort 25 near Vernal, Utah. These experiments demonstrate that geotomography may be a valuable diagnostic tool for underground oil‐shale retorting processes. At the Geokinetics in‐situ retort, the technique delineated the zones of high permeability in a cross‐section of the retort. At the Occidental modified in‐situ miniretort, the technique imaged the high temperature zone of the retort with a spatial resolution of about 2 m, and showed its temporal development over a period of eleven days.


Author(s):  
Eben Mulder ◽  
Dawid Serfontein ◽  
Eberhard Teuchert

In this article an advanced fuel cycle for pebble bed reactors is introduced that can safely and efficiently incinerate pure reactor-grade Pu [Pu(LWR)], thereby fulfilling the bulk of the GNEP waste incineration requirements. It is shown below that the very high fissile content of the Pu(LWR)-fuel enables it to convert practically all of the 240Pu to 241Pu and incinerate it. Since the fuel contains no 238U, no fresh 239Pu is produced. The 239Pu is reduced in-situ by 99.5% and the 240Pu by 97.6%. The only significant fissile isotope remaining is 241Pu, however, it will decay with a half life of 14.4 years to the fertile 241Am by β-decay.


2006 ◽  
Author(s):  
Mohammed Badri Al-Otaibi ◽  
Hisham A. Nasr-El-Din ◽  
Abdullah Mohammad Al Moajil

Geophysics ◽  
1984 ◽  
Vol 49 (8) ◽  
pp. 1288-1300 ◽  
Author(s):  
Stephen F. Somerstein ◽  
Mike Berg ◽  
David Chang ◽  
Hwang Chung ◽  
Hal Johnson ◽  
...  

Cross‐borehole, radio‐frequency geotomographs were made across two different‐sized, operating, experimental, underground, in‐situ, oil‐shale retorts. The tomographs taken of the smaller retort were of a plane 16.7 m wide by 18.0 m high bisecting the retort. The measurements were taken at a frequency of 25 MHz and showed excellent correlation of high signal attenuation with the high‐temperature zones. Measured attenuation coefficients (inverse skin depth) at 25 MHz ranged from [Formula: see text] across the cool, unrubbled, sill‐pillar, and between [Formula: see text] for the high‐temperature 370–700° C zone. Image resolution was approximately 1 m. The signal attenuation across the lower retort region was also found to correlate well with the movement and concentration of condensed water. The conventional algebraic deconvolution method (ART) was modified for limited perspective and finite beam width, and gave results which were in good agreement with thermocouple data. The measurements made on the larger retort were taken over a period of 33 days of retort burn and mapped the attenuation coefficients in a vertical plane 90 m wide by 48 m high at a frequency of 1.5 MHz. At this frequency, attenuation coefficients in the cool, dry retort regions were between 0.12 and [Formula: see text], while regions containing a high moisture content had coefficients of from 0.15 to [Formula: see text]. In the regions encompassing the retorting and combustion zones, attenuation coefficients were between 0.15 and [Formula: see text]. Some additional effects on the attenuation measurements were observed due to nearby thermocouple piping. The movement of the contours of attenuation coefficient with time followed temperature changes, though the paucity of thermocouples in the tomographic plane only allowed a marginal correlation to be made. Overall results suggest that radio‐frequency geotomography can be a useful tool for mapping in‐situ moisture concentrations and temperature fronts in an operating in‐situ oil‐shale retort.


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