Determining Liquid Carry Over in Gas Condensate Production Facilities and Assessing the Flow Regime in the Gas Sweetening Carbon Dioxide Amine Units Offshore on the Sleipner Platform in the North Sea

2000 ◽  
Author(s):  
Waleed J. Georgie ◽  
Jan I. Nilsen ◽  
Trygve Håland ◽  
Erik Solheim ◽  
Chris J. Lyth
2014 ◽  
Vol 63 ◽  
pp. 7280-7289 ◽  
Author(s):  
Marit J. Mazzetti ◽  
Ragnhild Skagestad ◽  
Anette Mathisen ◽  
Nils H. Eldrup

2007 ◽  
Vol 106 (1-2) ◽  
pp. 161-173 ◽  
Author(s):  
L.-S. Schiettecatte ◽  
H. Thomas ◽  
Y. Bozec ◽  
A.V. Borges

2018 ◽  
Vol 607 ◽  
pp. 187-205 ◽  
Author(s):  
O Henriksen ◽  
A Christensen ◽  
S Jonasdottir ◽  
BR MacKenzie ◽  
KE Nielsen ◽  
...  

2021 ◽  
pp. 1-22
Author(s):  
Saeed Ghanbari ◽  
Eric J. Mackay ◽  
Gillian E. Pickup

Summary Carbon dioxide (CO2) enhanced oil recovery (EOR) has long been practiced in the US as an efficient mean for enhancing oil production. Many of the US CO2-EOR developments have been designed horizontally. This is because of a viscous-dominated CO2 flow regime that is prevalent in these developments driven by thin and low-permeability reservoirs. Reservoirs and fluid properties are different in the North Sea. Pays are usually thicker with better petrophysical properties. Lighter oils can also be found in North Sea reservoirs. This suggests that a dissimilar flow regime might prevail CO2 displacements in the North Sea developments, which could favor a dissimilar CO2-EOR process design. This study thus compares CO2 flow regimes between several North Sea and US reservoirs. We use scaling analysis to characterize and compare CO2 flow regimes between these two classes of reservoirs. Scaling analysis characterizes CO2 displacement in each reservoir system using three dimensionless numbers: gravity, effective aspect ratio, and mobility ratio. Displacement experiments conducted in stochastically generated permeability fields, under exactly matched magnitudes of the derived dimensionless numbers, reveal the prevailing CO2 flow regime in each reservoir system. Results of scaling analysis indicate that CO2 flooding in the North Sea reservoirs can be generally characterized with a larger gravity number, smaller effective aspect ratio, and smaller mobility ratio than the average US CO2 flooded reservoirs. Flow regime analysis indicates that unlike the majority of the US CO2 flooded reservoirs, CO2 flow regimes tend to be more gravity-dominated in the North Sea class of reservoirs. CO2 flow regimes in the North Sea systems are expected to suffer from a higher degree of instability because of thicker North Sea pays, which limit effective crossflow. Understanding the differences and characteristics of CO2 flow regimes in the North Sea prospects can help operators design their CO2 flooding more efficiently, which could increase the recovery factor (RF) as well as address CO2 storage requirements, a necessary consideration for CO2-EOR deployment in the North Sea.


2016 ◽  
Vol 8 (1) ◽  
pp. 561-570 ◽  
Author(s):  
Jon Gluyas ◽  
Simon Mathias ◽  
Salim Goudarzi

AbstractIn 2015, the North Sea petroleum province was 50 years old. The celebrations were short lived because oil prices and gas prices were in free fall. The demand from the UK market had outstripped demand back in 2005 and, 10 years on, falling production and increasing operating expenditure, when coupled with falling prices, had brought the North Sea to crisis point. Many fields became unprofitable and companies began to close down. In an effort to avert the developing crisis, this work examines what options exist for better utilizing the North Sea industry, be that monetizing co-produced fluids or using the pore space once occupied by petroleum for waste products such as carbon dioxide. We briefly examine: the possibility of utilizing heat from the co-produced fluids for power generation; extracting gases and ores from co-produced fluids; and evaluation of the role that carbon dioxide could play in enhanced oil and gas recovery, as well as its ultimate long-term storage in geological deep storage.


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