This study investigates the coupled roles of diffuse double layer (DDL) development and ion exchange in cation adsorption onto Na-bentonite. Batch adsorption tests and free swell tests were conducted over a wide range of initial CaCl2 molarities (0–1000 mmol/L), and both Ca2+ adsorption and Na+ release were quantified. The ion exchange dominated the Ca2+ adsorption when the equilibrium bulk Ca2+ molarity (Ce) was below 1 mmol/L, whereas the majority of Ca2+ adsorption was associated with DDL development. The measured adsorbed molality (qeCa, mmol/g) exhibited a non-monotonic trend with respect to Ce. When qeCa was normalized to adsorbed molarity (Cin, mmol/L) by accounting for the experimentally evaluated volume of DDL domain, the resulting molar adsorption isotherm exhibited a Langmuir-type correlation, indicating that the adsorption equilibrium was dependent on Langmuir equilibrium constant KL. This result emphasized that the DDL constituted a dynamic spatial domain governing cation adsorption process, while the adsorption equilibrium was governed by the correlation between Ce and Cin. This framework provides a physically consistent interpretation of DDL development and ion exchange to the cation adsorption onto bentonite, thereby advancing the mechanistic understanding of clay-water interactions relevant to bentonite-based barrier systems in geoenvironmental engineering.
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