Ascertaining the pore geometry and wettability characteristics
of tight shales is of great significance for revealing the mechanisms
of occurrence, migration, and production of shale resources. Taking
the Bossier Shale collected from Well A, East Texas, USA, as an example,
the pore geometry and wettability behavior in a broad nm−μm
scale pore spectrum were quantified based on integrated techniques,
including water immersion porosimetry (WIP), mercury intrusion porosimetry
(MIP), (ultra)small-angle X-ray scattering [(U)SAXS], contact angle,
and liquid spontaneous imbibition (SI). Mainly owing to differences
in the sample sizes used, data interpretation, as well as the detectable
pore type (e.g., connected or not) and pore diameter ranges among
different methods, sample porosities derived from WIP, MIP, and (U)SAXS
were quite different, which range from 7.70 to 13.34%, 5.12 to 9.52%,
and 2.48 to 6.44%, respectively. Therefore, a comparison of the porosities
derived from different methods must be handled with utmost care. Additionally,
although (U)SAXS is an effective technique for detecting both connected
and non-connected pores, the fraction of non-connected pores could
be underestimated by directly comparing the pore size distribution
derived from (U)SAXS and MIP tests. This is because the sample sizes
used for and pore information reflected by these two methods are different.
Furthermore, the studied Bossier Shales exhibited various contact
angle values and imbibition behaviors when using differently polarized
liquids, revealing their mixed-wet characteristics. Comprehensively
considering the differences in contact angle, imbibition slope, and
imbibed liquid volume, three sub-categories of wettability behavior,
with respect to more oil-wet, more water-wet, and intermediate mixed-wet,
were qualitatively identified.