Pore types and structure in shales
have a significant impact on
shale gas accumulation and shale reservoir quality. Based on data
from the Wufeng-Longmaxi formation, this paper presents an in-depth
investigation of pore types and structure in shales, including a detailed
analysis of pore features and controlling factors of pore development.
During this study, the researchers used eight testing techniques,
including scanning electron microscopy (SEM) after Ar-ion milling,
total organic carbon (TOC), thermal maturity, thin-section identification,
X-ray diffraction, mercury intrusion, pulse decay porosity and permeability,
and low-temperature N2 adsorption. The study identified
five types of reservoir spaces in Wufeng-Longmaxi shales, including
organic pores, interparticle pores, intercrystalline pores, dissolved
pores, and microfractures, among which organic pores and interparticle
pores were the most common types. The test results suggested that
the pore diameters were predominantly 5–20 nm and 5–10
μm. The findings also indicated that the pore throats were narrow
and the pore connectivity was relatively good. The porosity and permeability
were generally low, with the former measured at 1.27% on average and
the latter at 0.0116 mD. The controlling factors of pore development
in the Wufeng-Longmaxi shale were mainly thermal maturity, TOC, and
mineral components. TOC had a positive correlation with the specific
surface area. TOC was associated with samples with the lowest clay
content, and the Brunauer–Emmett–Teller (BET) specific
surface area was correlated with TOC content. The clay mineral content
was negatively correlated with porosity, indicating a clear controlling
role in pore development by TOC and clay mineral content. In addition,
a favorable thermal maturity could contribute to the pore development
in the study area.