TY - GEN
T1 - Water-ROCK-CO2 interaction in hot dry rock - A review
AU - Xu, Guixi
AU - Wang, Shuzhong
N1 - Publisher Copyright:
© 2017 Trans Tech Publications, Switzerland.
PY - 2017
Y1 - 2017
N2 - Recently, using CO2 as fluid to exploit thermal energy in hot dry rock has attracted the attention of researchers. The water-rock-CO2 interaction in hot dry rock CO2 will change reservoir mineral composition and physical characteristics (such as porosity and permeability) by precipitation and dissolution of mineral in artificial geothermal reservoir, which will influence the stable operation of CO2-EGS and affect the scaling and corrosion in pipes and equipment. On the other hand, water-rock-CO2 interaction is closely related to CO2 sequestration. In this paper, the interaction mechanism including phase equilibrium, mineral composition analysis, temperature and brine component, interaction region and interaction damage are summarized, which can be used as a guide for further research. We find that the water-rock-CO2 interaction analysis now is most for single factor and single mineral component. And the mechanism of reaction between single supercritical CO2 and mineral is not clear. Study about spatio-temporal evolution of mineral component and fluid component, combined with the spatio-temporal evolution of temperature and pressure, is little.
AB - Recently, using CO2 as fluid to exploit thermal energy in hot dry rock has attracted the attention of researchers. The water-rock-CO2 interaction in hot dry rock CO2 will change reservoir mineral composition and physical characteristics (such as porosity and permeability) by precipitation and dissolution of mineral in artificial geothermal reservoir, which will influence the stable operation of CO2-EGS and affect the scaling and corrosion in pipes and equipment. On the other hand, water-rock-CO2 interaction is closely related to CO2 sequestration. In this paper, the interaction mechanism including phase equilibrium, mineral composition analysis, temperature and brine component, interaction region and interaction damage are summarized, which can be used as a guide for further research. We find that the water-rock-CO2 interaction analysis now is most for single factor and single mineral component. And the mechanism of reaction between single supercritical CO2 and mineral is not clear. Study about spatio-temporal evolution of mineral component and fluid component, combined with the spatio-temporal evolution of temperature and pressure, is little.
KW - Interaction damage
KW - Interaction mechanism
KW - Interaction region
UR - https://www.scopus.com/pages/publications/85028766087
U2 - 10.4028/www.scientific.net/KEM.748.446
DO - 10.4028/www.scientific.net/KEM.748.446
M3 - 会议稿件
AN - SCOPUS:85028766087
SN - 9783035711837
T3 - Key Engineering Materials
SP - 446
EP - 450
BT - Advanced Materials and Engineering Materials VI - 6th ICAMEM
A2 - Kida, Katsuyuki
A2 - Mizobe, Koshiro
PB - Trans Tech Publications Ltd
T2 - 6th International Conference of Advanced Materials and Engineering Materials, ICAMEM 2017
Y2 - 11 March 2017 through 12 March 2017
ER -