The
practice of gas reservoir development shows that tight sandstone
gas wells show an ultralow water flowback rate, even if the displacement
differential pressure is continuously increased. Scholars have studied
the influence of physical properties, pore structure, and fluid properties
on flowback efficiency, but the influence of heterogeneity on water
phase flowback is still not sufficient, especially comprehensive research
across different scales. To deal with this, we investigate the effect
of heterogeneity on fluid flow capability through centimeter core-scale
experiments and micrometer pore-scale simulations. First, on the basis
of the bounds of different pore-throat structure testing methods,
the full-scale pore size distribution (PSD) and throat size distribution
(TSD) structures are characterized by splicing. Next, we extract the
high-pressure mercury injection (HPMI) sorting coefficient and the
pixel variation coefficient of pore segmentation in scanning electron
microscopy (SEM) images as the characterization parameters of heterogeneity.
Direct experimental evidence shows that the stronger the rock heterogeneity,
the larger the sorting coefficient and variation coefficient and the
weaker the fluid mobility. It is difficult to improve the gas phase
seepage ability even with a continuously increasing displacement pressure
differential. Finally, we explored whether the reason for this phenomenon
is mainly controlled by heterogeneity. We carried out microfluidic
simulations, and the simulation results provide a good complementary
explanation for this phenomenon. The preferential flow pathway effect
induced by strong heterogeneity makes it impossible to affect the
fluid flow state by only changing the displacement pressure differential,
and it is difficult for the displacement phase to establish a new
flow channel. The findings at different scales provide unique insights
into the combined effects of pore heterogeneity and displacement pressure
differentials on fluid flow.