the problem
Why the continuum fails at the nanoscale.
Unconventional reservoirs – organic-rich shales, tight gas sands, and other nanoporous
formations – host a significant fraction of domestic hydrocarbon production but operate in a
regime where the classical assumptions of subsurface flow break down. When pore diameters
approach the nanometer scale, the continuum description of fluid flow becomes invalid:
molecular interactions between fluid and pore walls dominate over bulk fluid-fluid
interactions, slip flow and Knudsen diffusion become significant transport mechanisms, and
apparent permeability becomes a function of fluid type, pressure, and temperature, not
geometry alone.
Why pore-scale physics matters.
Shale and tight-rock systems are dominated by pore networks below the resolution of
conventional petrophysical tools. Hydrocarbon storage, deliverability, and connectivity
all live in the nano- and micro-scale fabric of organic matter, clay platelets, and
microfracture networks – features that traditional plug-scale measurements average away.
From shales to critical minerals.
We bring extensive published expertise in the multi-scale characterization, image-based
modeling, and pore-scale simulation of nanoporous reservoir rocks. The methodology developed
for shales now extends to critical-mineral systems through our active research program.
The imaging, modeling, and simulation workflow is the same; the
rocks, the fluids, and the reactions differ. The fundamental insight is shared: in any porous
system where pore geometry, mineral composition, and dynamic alteration co-determine fluid
behavior, the predictive framework must be derived from the pore scale.