The
complexity of the shale pore structure, which can be assessed
by the fractal dimension, will affect the percolation and reservoir
capability of a shale; thus, the pore structure is important for shale
reservoir evaluation. For the pore structure and fractal characteristics
of lacustrine shale to be investigated, a combination of X-ray diffraction
(XRD), total organic carbon (TOC), scanning electron microscopy (SEM),
mercury-injection capillary pressure (MICP), nuclear magnetic resonance
(NMR), and Nano-CT experiments were performed on shale samples from
the lower submember of the third member of the Eocene Shahejie Formation
(Es3
L) in the Zhanhua Depression, Bohai Bay
Basin. On the basis of fractal theory, the NMR fractal dimensions
of the analyzed shale samples were determined by the transversal relaxation
time (T
2) spectrum from the NMR experiment.
The relationships between the NMR fractal dimension and mineral content,
TOC, and pore structure parameter were discussed. The results indicate
that the pore structure of the lacustrine shale in the study area
is complex and exhibits strong heterogeneity. The pore types mainly
include intergranular pores, intragranular pores, and some dissolved
pores and microfractures. Calcite and clay are the dominant minerals,
ranging from 9 to 91% (average 52.23%) and from 1 to 48% (average
18.63%), respectively. The TOC contents are relatively high with values
from 0.06 to 9.32%. The calculated NMR fractal dimension (D) values are between 2.2544 and 2.439, which exhibit positive
correlations with TOC content, quartz content, and clay mineral content.
In contrast, a negative relationship occurs between the NMR fractal
dimension and calcite content, indicating that the development of
large, dissolved pores in shale samples could reduce the heterogeneity
of the pore size distribution. Negative correlations are observed
between the NMR fractal dimension and the T
2 cutoff value, T
2 geometric mean, porosity,
and average pore throat radius, whereas the NMR fractal dimension
exhibits a positive correlation with the displacement pressure (P
d) and has no obvious relationship with permeability.
The different relationships suggest that the NMR fractal dimension
is closely related to the pore structure; namely, the smaller the
NMR fractal dimension is, the better the pore structure is in the
shale samples. Four typical samples were chosen to verify the relationship
between the NMR fractal dimensions and the shale pore structure in
the logging profile of Well L69. Excellent application results were
obtained, suggesting that the NMR fractal dimension can be used to
indicate the effectiveness of the reservoir in the study area.