InteractionLawbetweenCO2,RockandFormationWaterinYanchangOilfield
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    Abstract:

    To make clear the physical and chemical changes caused by CO2 flooding and geological storage ,the mineral composition of reservoir and the law of interaction between CO2,rock and formation water in Yanchang oilfield was studied by using SEM,XRD,EDS ,ICP-AES and IG. The results showed that the reservoir rock of Yanchang oilfield was composed of 18.7% quartz,18.2% potassium feldspar,30.1% plagioclase,0.5% calcite ,4.4% laumontite and 28.1% clay minerals. The average salinity of formation water was 71.34g/L with CaCl2 type ,and the pH value was 5.5. After the reaction of CO2,rock and formation water,the corrosion of rock surface became worse with increasing partial pressure of CO2. At reservoir temperature of 44℃,when the reaction pressure increased from 0 to 20MPa,the content of C element in rock surface fluctuating rose,while that of Na,K elements gradually decreased,the salinity of formation water increased from 95210 mg/L to 107063 mg/L,and the mass concentration of Na+、K+、Ca2+、HCO3-showed an increasing trend. When the reaction pressure increased from 5 to 20MPa,the corrosion rate of piece rock increased first and then decreased. When the pressure was 10MPa,the maximum corrosion rate was 0.72%. The higher pressure,the higher solubility of CO2 in water and corrosion rate was. The higher temperature and salinity ,the lower solubility of CO2 in water was. With increasing reaction pressure ,the dissolution of potassium feldspar and plagioclase in sandstone by CO2 gradually increased.

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TANG Ruijia, HUANG Chunxia, YU Huagui, JIANG Shaojing, WANG Weibo. InteractionLawbetweenCO2,RockandFormationWaterinYanchangOilfield[J]. OILFIELD CHEMISTRY,2015,32(4):515-519.

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  • Online: January 07,2016
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