scholarly journals Environmental assessment: tar sand in situ steam injection experiment

1979 ◽  
Author(s):  
1981 ◽  
Vol 103 (4) ◽  
pp. 296-300
Author(s):  
S. M. Farouq Ali ◽  
J. Ferrer

Thermal recovery models for oil recovery consist of steam injection and in-situ combustion simulators. At the present time, steam injection simulators have been developed to a point where it is possible to reliably simulate portions of a fieldwide flood. Cyclic steam stimulation simulation still entails a number of questionable assumptions. Formation parting cannot be simulated in either case. In-situ combustion simulators lack the capability for front tracking. Even though the models are rather sophisticated, process mechanism description and input data are inadequate.


2020 ◽  
Vol 192 ◽  
pp. 107267
Author(s):  
Yang Zheng ◽  
Guanglun Lei ◽  
Chuanjin Yao ◽  
Jingang Fu ◽  
Long Wang ◽  
...  

2013 ◽  
Vol 16 (03) ◽  
pp. 333-344 ◽  
Author(s):  
Y.. Hamedi Shokrlu ◽  
T.. Babadagli

Summary Studies on the application of transition-metal catalysts for heavy-oil or bitumen in-situ upgrading were conducted in the absence of a porous medium, mainly measuring the characteristics of heavy oil in reaction with metal ions at static conditions with the help of a magnetic stirrer. Metal species in ionic form are not soluble in oil phase. Therefore, metal particles, as inhomogeneous catalysts, are considered in this paper. Furthermore, dynamic tests in porous media are needed to clarify the injection possibility of the metal particles and their effect on in-situ upgrading of heavy oil. Injection of metal particles may deteriorate the recovery process by damaging porous media because of attractive forces such as van der Waals and electrostatic forces between particles and porous rock. A better understanding of these forces and their importance in the retention of particles is required. In this paper, the catalysis effect of pure nanometer-sized nickel during steam-injection application was compared with that of an industrial catalyst such as micron-sized Raney nickel. The changes in the viscosity, refractive index, and asphaltene content were measured after each test to analyze the catalysis effects. Nickel nanoparticles showed a better catalysis compared with Raney nickel. The approximate optimum concentration of the catalysts was determined. Then, the catalysis effect of nickel nanoparticles was studied in the presence of sandpack as a porous medium. The results showed accelerated catalysis in presence of the sands. Also, nickel nanoparticles improved the oil recovery factor. The next phase of this paper studies the injectivity and transport of nickel particles. The injected suspension was stabilized by use of xanthan gum polymer and ultrasonication. The effect of solution pH, which controls the magnitude of the repulsive electrostatic forces, was clarified. Stabilization of the metal particles’ suspension was studied at different pH values through zeta-potential measurements. Also, the zeta potential of the recovered suspensions was studied to confirm the stability of the suspension during travel through the porous medium. Depending on the size, particles carry different charges and have different settling velocities. Therefore, the stabilization pH and dispersant concentration were different from one sample to another. The results of the injectivity tests confirmed the lower retention and better injectivity of nanoparticles in comparison with micron-sized particles.


2020 ◽  
Author(s):  
Shuhei Tsuji ◽  
Koshun Yamaoka ◽  
Ryoya Ikuta

Abstract We developed a method to detect changes in attenuation in transfer functions obtained by precisely controlled artificial seismic sources, namely Accurately Controlled Routinely Operated Signal System (ACROSS), and applied it to monitor the temporal changes for in-situ data collected by previous studies. Our method, together with the usage of the ACROSS sources, is less susceptible to change in noise level to which conventional methods such as envelope calculation suffer. The method utilizes the noise level that is independently estimated in the frequency domain. Thus, we can eliminate the influence of the noise by subtracting it from the observed signal. To test the performance, we applied this method to a dataset obtained at Awaji Island, Japan from 2000 to 2001. We detected the changes in amplitude with several causes including ground motion in an earthquake and water injection experiment. At the 2000 Western Tottori earthquake (MW = 6.6, Epicenter distance of 165 km), a sudden decrease in amplitude up to 5% followed by gradual recovery are clearly observed. These coseismic changes in amplitude are consistent with the opening of fluid-filled cracks as proposed by previous studies. We convert the amplitude change into ΔQ-1, which gives similar values as reported by previous studies using natural earthquakes. Increases in amplitude up to 5% associated with water injection experiments are also observed. During these experiments, the amplitude increased several days after the beginning of the injection and recovered to the previous level. This may be the result of a stress increase caused by the injection followed by a saturation increase by water diffusion.


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