While
hydrate formation conditions are commonly present in natural
gas offshore production, where hydrates can cause undesirable blockages,
the natural reserves of CH4 hydrate on the seafloor have
been studied as a potential energy source. Different applications
for these crystalline structures are also being developed due to their
gas storage capacity. Hence, understanding the hydrate growth phenomenon
may lead to alternative operational procedures to avoid blockages,
explore natural reserves, and develop new gas storage technologies.
However, despite the literature advances to describe hydrate equilibrium
states, the formation dynamics of these solids are still obscure.
A generic model capable of including the thermodynamic factor in the
growth is fundamental to better describe the phenomenon in all these
scenarios. Therefore, we propose a new model for hydrate growth kinetics
using reaction chemical affinity as a driving force. This model is
based on nonequilibrium thermodynamics, clarifying conceptually relevant
but rarely investigated problems. DeDonder’s affinity allows
the inclusion of nonideal thermodynamic factors for all hydrate-forming
components in the growth model, explicitly relating the thermodynamic
behavior of hydrate formation to the kinetics. The definition of a
coupling factor between reaction and diffusion makes it necessary
to estimate only the reaction constant of the model. We show that
the model accurately describes the experimental data by evaluating
the reaction-diffusion limiting conditions on the growth rate of CH4 hydrate in freshwater. Depending on the pressure, the chemical
affinity-based model confirms that reaction and diffusion mechanisms
govern methane hydrate growth. Lastly, we verify that including water
activity in the driving force alters the growth dynamics even for
systems close to ideality.