How large is our CO2 storage capacity assessment error? Analyzing the magnitude of error in the effective capacity calculation propagated from uncertainties in the thermophysical conditions in the aquifer, the case of the Israeli Jurassic saline aquifer

2019 ◽  
Vol 82 ◽  
pp. 19-37 ◽  
Author(s):  
R. Calvo ◽  
R. Taragan ◽  
R. Rosenzweig
Author(s):  
Zheming Zhang ◽  
Ramesh Agarwal

With recent concerns on CO2 emissions from coal fired electricity generation plants; there has been major emphasis on the development of safe and economical Carbon Dioxide Capture and Sequestration (CCS) technology worldwide. Saline reservoirs are attractive geological sites for CO2 sequestration because of their huge capacity for sequestration. Over the last decade, numerical simulation codes have been developed in U.S, Europe and Japan to determine a priori the CO2 storage capacity of a saline aquifer and provide risk assessment with reasonable confidence before the actual deployment of CO2 sequestration can proceed with enormous investment. In U.S, TOUGH2 numerical simulator has been widely used for this purpose. However at present it does not have the capability to determine optimal parameters such as injection rate, injection pressure, injection depth for vertical and horizontal wells etc. for optimization of the CO2 storage capacity and for minimizing the leakage potential by confining the plume migration. This paper describes the development of a “Genetic Algorithm (GA)” based optimizer for TOUGH2 that can be used by the industry with good confidence to optimize the CO2 storage capacity in a saline aquifer of interest. This new code including the TOUGH2 and the GA optimizer is designated as “GATOUGH2”. It has been validated by conducting simulations of three widely used benchmark problems by the CCS researchers worldwide: (a) Study of CO2 plume evolution and leakage through an abandoned well, (b) Study of enhanced CH4 recovery in combination with CO2 storage in depleted gas reservoirs, and (c) Study of CO2 injection into a heterogeneous geological formation. Our results of these simulations are in excellent agreement with those of other researchers obtained with different codes. The validated code has been employed to optimize the proposed water-alternating-gas (WAG) injection scheme for (a) a vertical CO2 injection well and (b) a horizontal CO2 injection well, for optimizing the CO2 sequestration capacity of an aquifer. These optimized calculations are compared with the brute force nearly optimized results obtained by performing a large number of calculations. These comparisons demonstrate the significant efficiency and accuracy of GATOUGH2 as an optimizer for TOUGH2. This capability holds a great promise in studying a host of other problems in CO2 sequestration such as how to optimally accelerate the capillary trapping, accelerate the dissolution of CO2 in water or brine, and immobilize the CO2 plume.


2011 ◽  
Vol 5 (2) ◽  
pp. 318-326 ◽  
Author(s):  
Toyokazu Ogawa ◽  
Shigetaka Nakanishi ◽  
Takumi Shidahara ◽  
Tadahiko Okumura ◽  
Eiji Hayashi

2015 ◽  
Vol 20 (2) ◽  
pp. 239-245 ◽  
Author(s):  
Joongseop Hwang ◽  
Soohyun Baek ◽  
Hyesoo Lee ◽  
Woodong Jung ◽  
Wonmo Sung

2013 ◽  
Vol 734-737 ◽  
pp. 1905-1909
Author(s):  
Xiao Yi Yang ◽  
Yan Feng Liu ◽  
Jian Jun Wang

Carbon Capture and Storage (CCS) is one of the effective means to reduce the carbon dioxide concentration in atmosphere. Deep saline aquifer is the most potential storage sites because of its wide spread and the huge storage capacity. The storage capacity of deep saline aquifer was determined by hydrogeological parameters of the assessed aquifer. Spatial discretization method based on the geostatistical method takes account of the spatial variability of hydrogeological parameters involved in capacity assessment, which applied by inputting the value of hydrological parameters of every cell and calculating the storage capacity of each cell. The total storage capacity in assessed area was the summation of all cells. In the Central Depression of Songliao Basin, the theoretical carbon dioxide storage capacity of deep saline aquifers was estimated as 81.80Gt with spatial discretization method. Compared with the other methods, this method can reflect the spatial characteristics of the carbon dioxide storage capacities and was more precise.


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