While studying trace elements in sediments, I became involved in researching their partitioning between the water column and the sediments (Kd), their speciation in the solid phase (referred to as particulate speciation by Tessier in his 1979 article), and the processes of adsorption.
There are various adsorption isotherms, but they can all be generalized by considering localized adsorption sites that exhibit a Langmuirian isotherm. All of these sites have the Boltzmann distribution of adsorption energies. In my opinion, there is no better approach than the generalized Langmuirian isotherm model for describing adsorption. Unfortunately, this concept has very few proponents.
This generalized approach is not only important for studying adsorption but also for mineral dissolution, reaction kinetics, investigating the interactions of plant exudates with minerals in the soil, understanding the transport of trace elements by rivers worldwide, studying the interactions between phytoplankton and trace elements (uptake), and comprehending interface chemistry.
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