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- W2361673160 abstract "Degassing experiments of volcanic rocks and gas source analysis of the Changdedong CO2 reservoir show the following:at temperature of 250℃,the degassing amounts of volatiles from volcanic rocks range from 0.0299 to 0.0790 mL/g,of which the CO2 amounts are 0.0218 to 0.0706 mL/g (viz.0.429-1.387wt%);the volatile components consist predominantly of CO2 with reducing gases such as H2,CO and CH4 and minor low-carbon alkanes,and there are an inverse relationship between the CO2 content and total hydrocarbon content,a negative correlation between the CO2 degassing amount and SiO2 content and a positive correlation between the CO2 degassing amount and alkali content of rocks;the amount and rate of CO2 degassing from basic rocks are higher than those of intermediate and acid rocks.The genetic model of the Changdedong CO2 reservoir is self-generation and self-accumulation,and the CO2 gas is mainly CO2 derived from the depth and adsorbed by volcanic rocks.With the ascent of magma,the CO2 adsorbed on joints,cleavages and crystal dislocations of volcanic rocks in the process of cooling and solidification of magma into volcanic rocks,together with residual gases in inclusions of volcanic rocks,become the main recharge sources of high-purity CO2 gas reservoirs.So the CO2 gas reservoirs are not formed by direct filling of mantle gas into the reservoirs along major faults." @default.
- W2361673160 created "2016-06-24" @default.
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- W2361673160 date "2005-01-01" @default.
- W2361673160 modified "2023-09-23" @default.
- W2361673160 title "Potential to form CO_2 reservoirs through adsorption of CO_2 by volcanic rocks and case study" @default.
- W2361673160 hasPublicationYear "2005" @default.
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