Neutron Scattering Measurements of Carbon Dioxide Adsorption in Pores within the Marcellus Shale: Implications for Sequestration

• Published in: Environmental science & technology Vol. 51; no. 11; pp. 6515 - 6521
• Main Authors: Stefanopoulos, Konstantinos L, Youngs, Tristan G. A, Sakurovs, Richard, Ruppert, Leslie F, Bahadur, Jitendra, Melnichenko, Yuri B
• Format: Journal Article
• Language: English
• Published: United States American Chemical Society 06.06.2017
• Subjects: Adsorption; Carbon Dioxide; Carbon monoxide; Carbon sequestration; Densification; Diffraction; Gas recovery; Geology; Laboratories; Measurement; Natural gas; Neutron Diffraction; Neutron scattering; Neutrons; Pores; Porosity; Research facilities; Scattering; Scattering, Small Angle; Shale; Shale gas
• ISSN: 0013-936X; 1520-5851
• DOI: 10.1021/acs.est.6b05707

Shale is an increasingly viable source of natural gas and a potential candidate for geologic CO2 sequestration. Understanding the gas adsorption behavior on shale is necessary for the design of optimal gas recovery and sequestration projects. In the present study neutron diffraction and small-angle neutron scattering measurements of adsorbed CO2 in Marcellus Shale samples were conducted on the Near and InterMediate Range Order Diffractometer (NIMROD) at the ISIS Pulsed Neutron and Muon Source, STFC Rutherford Appleton Laboratory along an adsorption isotherm of 22 °C and pressures of 25 and 40 bar. Additional measurements were conducted at approximately 22 and 60 °C at the same pressures on the General-Purpose Small-Angle Neutron Scattering (GP-SANS) instrument at Oak Ridge National Laboratory. The structures investigated (pores) for CO2 adsorption range in size from Å level to ∼50 nm. The results indicate that, using the conditions investigated densification or condensation effects occurred in all accessible pores. The data suggest that at 22 °C the CO2 has liquid-like properties when confined in pores of around 1 nm radius at pressures as low as 25 bar. Many of the 2.5 nm pores, 70% of 2 nm pores, most of the <1 nm pores, and all pores <0.25 nm, are inaccessible or closed to CO2, suggesting that despite the vast numbers of micropores in shale, the micropores will be unavailable for storage for geologic CO2 sequestration.