Wettability is the fundamental parameter that influences
the productivity
of hydrocarbon reservoirs. The knowledge of this regarding shale formation
is yet inadequate; thus, detailed analysis is essential for successful
development of such reservoirs. The Early Cretaceous Sembar formations
in the Lower Indus Basin, Pakistan, is considered as the key target
for energy exploration; however, it exhibits large uncertainties due
to the lack of data availability. Sembar shales hold significant hydrocarbon
volumes rich in organic content; however, prior to this, no comprehensive
research has been conducted to quantify the wetting behavior of these
shales. Thus, precise information about the wetting behavior of Sembar
shale formations is essential, as it is influenced by many factors.
Therefore, in this study, we examined the wettability of Sembar shale
samples by performing a suit of contact angle (CA) measurements. The
CA measurements on shale samples were performed using different salt
types (NaCl, KCl, MgCl2, and Reef Salt) and concentrations
of 0.1 M and 0.5 M under ambient pressures and varying temperatures
(25–50 °C). The CA was measured via air–brine and
air–oil under prevailing pressure and temperature conditions.
Subsequently, the sample morphology and surface topography were examined
via field emission scanning electron microscopy and atomic force microscopy,
respectively. The mineral compositions were obtained via X-ray diffraction
studies. The results clearly show that the Sembar shale possesses
a mixed wetting behavior. Under dry surfaces, they have large affinity
to oil and deionized water in which the droplet spreads quickly on
the sample surfaces. Conversely, the samples aged with n-decane and NaCl brines exhibited higher CAs than the untreated samples.
Additionally, the CA measured by changing temperatures led to an increase
for all brine droplets; the CA further increased as the concentrations
of salts increased from 0.1 to 0.5 M. We then discussed the possible
reasons for the discrepancy in CA values due to temperature changes
and brine concentrations. Moreover, the CA was measured corresponding
to the surface roughness from which it appears that it merely affects
the wettability of these shale samples. However, the present study
results lead to an improved understanding of the wettability of Sembar
shale of the Lower Indus Basin in Pakistan.