Adsorption
of surfactants in shales is not well studied. The goal
of this work is to quantify and understand surfactant adsorption in
several shale samples. Shale samples were obtained from several formations
and are referred to by the formation names; but considering the fact
that these formations are highly heterogeneous and huge, these few
samples do not represent the shales. Shales are multimineral substrates
with pores in the range of 1–300 nm. The adsorption capacity
of three surfactants (cationic, nonionic, and anionic) on an Eagle
Ford reservoir shale sample was measured. The cationic surfactant,
cetyltrimethylammonium bromide (CTAB), showed the highest adsorption
capacity in molar units, followed by anionic internal olefin sulfonate
(IOS) C15-18 and then nonionic NP-40s. CTAB also had the highest adsorption
in mass units, followed by NP-40 and then IOS. Adsorption of the anionic
surfactant onto two pure minerals (calcite and quartz) and six shales
were investigated, and all of them showed Langmuir-type sorption.
The adsorption capacity of calcite and quartz are about the same (∼1.1
mg/g of rock). The adsorption capacity of shales depends on the mineral
composition. The adsorption in Mancos outcrop and Green Shale samples
is dominated by clay, whereas that in Wolfcamp and Eagle Ford outcrop
shale samples is dominated by calcite. The adsorption in Eagle Ford
(reservoir) and Marcellus shale samples is dominated by total organic
carbon (TOC). An additive model was built to estimate the adsorption
capacity, given the mineral composition and TOC. The model shows that
organic matter and clay have the most significant impact on adsorption
per unit mass; the contribution of each shale component on adsorption
depends on its corresponding mass fraction.