The conductivity of an acid-etched fracture is a necessary indicator
for the stimulation of dolomite formation, which affects commercial
development. The widely accepted test method involves the use of a
small-scale conductivity cell for etching and measuring conductivity.
However, the field production reflects that the actual conductivity
does not match the measured one and is usually lower. Consequently,
the existing studies had limitations and hence the stimulation mechanism
needed to be explored further. To understand it more realistically,
a novel large-scale apparatus was used in this study to test the conductivity
of the acid-etched fracture. The use of this apparatus avoided the
near-core excessive eroding and weak heterogeneity with continuous
etching in a 1000 mm fracture. The results showed that the conductivity
was indeed dissimilar to that in small-scale tests. The morphology
of etched large-scale cores featured diversity and complexity, including
deep and punctate channels, nonuniform pitting grooves with connected
channels, and scale-shaped wavy grooves, which exactly demonstrated
the multiple morphology under the influence of carbonate heterogeneity
in real reservoirs. Moreover, the effect of increasing injection rate
led to the unique etching morphology of scale-shaped wavy and pelviform
grooves because of scouring flow and turbulence effects. The degree
of surface roughness promoted nonuniform etching along the longitudinal
and propagation direction, thus enhancing the conductivity of the
whole fracture and confirming that the field treatment limited the
pressure rather than the injection rate. The conductivity under different
acid type, acid concentration, reaction temperature, and injection
rate conditions was lower than that reported, confirming the experimental
deviation in small-scale conductivity. The proposed large-scale apparatus
test represented the acid-etched fracture conductivity more realistically,
thus proving beneficial for the development of carbonate reservoirs.