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Metal sorption at mineral water interfaces may involve various molecular level processes, including adsorption (the formation of mononuclear surface complexes), precipitation (the formation of secondary metal precipitates), and absorption (the incorporation of metal ions into the sorbent lattice) [3, 4].
Once exuded, PS participate in rhizosphere processes including adsorption, degradation, and mobilization of iron and other metals.
Rapid modulation between 150 and 450 °C exerts kinetic control over transient processes, including adsorption, desorption, diffusion, and reaction phenomena, which are important for charge transfer occurring in transduction processes and the observed response times.
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Physical processes include adsorption, chelation ion exchange, membrane filtration, and coagulation.
The microscopic model of the thin film growth process includes adsorption and migration processes.
The deposition process includes adsorption and migration processes and it is modeled via kinetic Monte Carlo simulation on a triangular lattice with vacancies and overhangs allowed to develop inside the film.
In a nut shell, physical chemical process, includes adsorption, coagulation/flocculation and chemical oxidation, is commonly used when the biological process is hindered due to excessive presence of refractory compounds in leachate.
Several chemical processes may be involved in biosorption, including adsorption, ion exchange processes and covalent binding.
Effects of the experimental parameters, including adsorption time, initial dye concentration, temperature, and pH value were studied to optimize the adsorption process.
Relevant processes include hydration (adsorption of water), hydroxylation (adsorption of H+ and OH- ions), oxidation (combination of oxygen, with loss of electrons to weathering agents), and reduction (depletion of combined oxygen).
Geochemical simulations of the one-dimensional transport of the Pb2+, considering removal processes including: ion-exchange, adsorption and complexation; the concomitant release of exchangeable cations (Ca2 +, Mg2 +, Na+, and K+) and the changes in pH were subsequently performed using the geochemical model PHREEQC.
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