The basic triggering mechanism underlying induced seismicity traces back to the mid‐1960s
that relied on the process of pore‐fluid pressure diffusion. The last decade has experienced …

Dissolution and precipitation reactions are the primary mechanisms that occur when a rock
(ie, a mineral assemblage) is in contact with a fluid out of equilibrium. They play a critical …

This study investigates fines migration and mineral reactions as a mechanism for CO 2
residual trap**. We perform imbibition experiments using a sintered glass core and seven …

Abstract To investigate CO 2 Capture, Utilization, and Storage (CCUS) in sandstones, we
performed three 150° C flow-through experiments on K-feldspar-rich cores from the Eau …

Hydrothermal flow experiments of single-pass injection of CO 2-charged brine were
conducted on nine dolomite cores to examine fluid–rock reactions in dolomite reservoirs …

Four reactive flow‐through laboratory experiments (two each at 0.1 mL/min and 0.01 mL/min
flow rates) at 150° C and 150 bar (15 MPa) are conducted on intact basalt cores to assess …

Water injection into an aquifer is generally motivated by one of three objectives: disposal,
managed aquifer recharge (MAR), or aquifer storage and recovery (ASR). Any of these …

Several studies suggest that CO 2-based geothermal energy systems may be operated
economically when added to ongoing geologic CO 2 sequestration. Alternatively, we …

Four flow-through experiments at 150° C were conducted on intact cores of basalt to assess
alteration and mass transfer during reaction with CO 2-rich fluid. Two experiments used a …

Quantitatively assessing seismic attenuation caused by fluid pressure diffusion (FPD) in
partially saturated rocks is challenging because of its sensitivity to the spatial fluid …