Combining hydraulic
fracturing with lateral drilling has allowed
for economical hydrocarbon production from unconventional formations.
Nevertheless, beyond hydraulic fracturing, our understanding of how
hydrocarbons are stored and transported from the stimulated volume
of a reservoir is still limited. Source rocks consist of organic materials
finely dispersed within an inorganic matrix. Despite their small size,
these organic pockets are capable of storing significant amounts of
hydrocarbon due to their large surface area. The extent of the source
rock’s storage capacity is determined by several factors, including
the natural fracture abundancy, organic material content, type, and
level of maturity. The petrophysical properties of organic materials,
also known as kerogens, are subject to a high degree of uncertainty.
Kerogens are difficult to isolate experimentally, which hinders accurate
petrophysical analysis. The objective of this research was to use
a molecular modeling approach to explore the petrophysical characteristics
of kerogen. Kerogen macromolecules of different types and maturity
levels were recreated via a computational platform. Then nanoporous
structures representing these kerogens were obtained and characterized.
Several elemental parameters, including porosity, density, pore size
distribution, and adsorption capacity were closely delineated. The
kerogen properties were found to correlate with the kerogen type and
thermal maturity level. Kerogen type III showed the highest storage
capacity, followed by types II and I, in a descending order. Moreover,
in the same type of kerogen, a general trend of increasing storage
capacity was observed as the maturity level increased. Methane adsorption
capacity was modeled as a function of kerogen porosity. A transition
flow regime was found to be the predominant mechanism. Such observations
have significant implications for reservoir-scale modeling of unconventional
resources.