Residual CO2 imaged with X‐ray micro‐tomography

By S. Iglauer, A. Paluszny, C. Pentland, Martin J. Blunt. 2011

324 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Environmental Engineering, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/989c8e689c17ebb5a38f00fbafbbb18d77babc11

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In Environmental Chemistry

In Environmental Engineering

In Ocean Engineering

Citations in the corpus

Pore‐scale trapping of supercritical CO2 and the role of grain wettability and shape (2013, background): “Core-scale experiments and pore-network flowmodels suggest that this capillary trapping in saline aquifers ranges from 10% to 90% of the total injected volume of CO2 [Bachu and Bennion, 2008; Iglauer et al., 2011; Krevor et al., 2012; Pentland et al., 2011; Suekane et al., 2008].”
Pore-scale contact angle measurements at reservoir conditions using X-ray microtomography (2014, background): “Recent advances in microtomography have allowed for the noninvasive imaging of fluid distributions in rocks at conditions of pressure, temperature and salinity representative of oil reservoirs and saline aquifers [24–26].”
Multi-scale x-ray computed tomography analysis of coal microstructure and permeability changes as a function of effective stress (2016, methodology): “However, recent developments in the area of x-ray micro-computed tomography (microCT) applied in core analysis (e.g. Iglauer et al., 2011; Lebedev et al., 2014; Rahman et al., 2016) enable the application of effective stresses to a sample while it is imaged in-situ in 3D at high resolution.”
Real-time 3D imaging of Haines jumps in porous media flow (2013, background): “J Colloid Interface Sci 377(1):406–415.”
Capillary trapping for geologic carbon dioxide storage - From pore scale physics to field scale implications (2015, background): “Iglauer et al. (2011) and Andrew et al. (2013, 2014b) used an X-ray transparent carbon fibre core holder to maintain high temperatures (50–70◦C) and pressures (around 10 MPa) in the fluids; these conditions are typical of many storage aquifers.”
From connected pathway flow to ganglion dynamics (2015, unknown): “While we have a good view on the initial and final states of this process [Andrew et al., 2013; Murison et al., 2014; Iglauer et al., 2011; Pak et al., 2015; Chaudhary et al., 2013; Deng et al., 2014], it is far less clear how we actually arrive from an initially connected pathway flow to trapped…”