Due to the compact
two-dimensional interlayer pore space and the
high density of interlayer molecular adsorption sites, clay minerals
are competitive adsorption materials for carbon dioxide capture. We
demonstrate that with a decreasing interlayer surface charge in a
clay mineral, the adsorption capacity for CO
2
increases,
while the pressure threshold for adsorption and swelling in response
to CO
2
decreases. Synthetic nickel-exchanged fluorohectorite
was investigated with three different layer charges varying from 0.3
to 0.7 per formula unit of Si
4
O
10
F
2
. We associate the mechanism for the higher CO
2
adsorption
with more accessible space and adsorption sites for CO
2
within the interlayers. The low onset pressure for the lower-charge
clay is attributed to weaker cohesion due to the attractive electrostatic
forces between the layers. The excess adsorption capacity of the clay
is measured to be 8.6, 6.5, and 4.5 wt % for the lowest, intermediate,
and highest layer charges, respectively. Upon release of CO
2
, the highest-layer charge clay retains significantly more CO
2
. This pressure hysteresis is related to the same cohesion
mechanism, where CO
2
is first released from the edges of
the particles thereby closing exit paths and trapping the molecules
in the center of the clay particles.