scholarly journals ISOTOPIC-HELIUM AND CARBON-HELIUM INDICATORS OF THE DEEPNESS OF THE PROCESSES OF OIL-GAS GENERATION AND OIL-GAS ACCUMULATION

Author(s):  
A.N. Dmitrievsky ◽  
B.M. Valyaev ◽  
I.S. Dremin
Author(s):  
Geylani M. Panakhov ◽  
Eldar M. Abbasov ◽  
Sayavur I. Bakhtiyarov ◽  
Dennis A. Siginer

A relative motion of different phases leads to formation of certain forces at the interface of transported fluid and pipe walls. In the non-isothermal flow case a thermal interaction between the phases will affect the flow velocity, the pressure and the temperature distributions in variable cross section pipes. Laboratory experiments were conducted in order to study the effects of the gas generation at the pipe walls on the hydrodynamic characteristics of the two-phase oil/gas flow. It is shown that a throughput capacity of the pipe is affected by the temperature difference between the oil and the pipe walls. At certain temperature difference value (∼3°C) the pipe capacity reached a maximum value.


2020 ◽  
Vol 79 ◽  
pp. 103341
Author(s):  
Adebanji Kayode Adegoke ◽  
Mohammed Hail Hakimi ◽  
Wan Hasiah Abdullah ◽  
El-Khedr Ibrahim ◽  
Babangida M. Sarki Yandoka ◽  
...  

2020 ◽  
Vol 117 ◽  
pp. 104412
Author(s):  
Martin Stockhausen ◽  
Roberto Galimberti ◽  
Rouven Elias ◽  
Lea Di Paolo ◽  
Lorenz Schwark

2013 ◽  
Vol 295-298 ◽  
pp. 2736-2739
Author(s):  
Hai Yan Hu

Overpressure is often encountered in the Jurassic tight and the overpressure is closely associated with gas generation. The pressure transfer from the over-pressurized mudstones to adjacent tight sandstones might occur through overpressure induced-fractures. The fine-grained coal containing Jurassic sandstone is sensitive to compaction, and the porosity decreases dramatically with the increase of overlying load. As gas migrates into the tight sandstones, it must overcome the capillary pressure which is greater than the hydrostatic pressure. The gas charging pressure in the tight sandstone must be higher than the capillary pressure, resulting in an overpressure buildup within the tight sandstones. Gas shows, low permeability and strong diagenesis in the overpressure of the tight sandstone system have been observed. Additionally, capillary seals are identified as playing an important role in the mechanism of the overpressure formation in tight sandstone reservoirs. Overpressure might be a driving force to create induced fractures in the interval, which has applications for crossing-formation migration and gas accumulation.


2019 ◽  
Vol 16 (4) ◽  
pp. 713-728 ◽  
Author(s):  
Liu-Wen Xia ◽  
Jian Cao ◽  
Ming Wang ◽  
Ju-Lei Mi ◽  
Ting-Ting Wang

2021 ◽  
pp. 255-261
Author(s):  
Yang Keming ◽  
Chen Zhaoguo ◽  
Gong Ming ◽  
Wu Yajun
Keyword(s):  

2014 ◽  
Vol 962-965 ◽  
pp. 234-237
Author(s):  
Ming Xue Zhang ◽  
Xu Tang Zheng

Since the discovery of business flow in volcanic rocks of Yingcheng formation, the deep volcanic rocks of Songliao basin have become another advantaged target for oil-gas exploration. To reproduce the the development process of oil-gas generation, migration and accumulation, accurately calculating the oil-gas accumulation time is a very important work. To minimize the error, we must seriously study the regional tectonic evolution history and recover the eroded thickness. According to the actual situation of the study area, trend method can be used to recover the top eroded thickness of volcanic rocks in Yingcheng formation. Finally we get the maximum eroded thickness in the basin is between 120 m to 240 m, located in the southeastern basin.


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