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Soil Humic Acid and Arsenite Binding by Isothermal Titration Calorimetry and Dynamic Light Scattering: Thermodynamics and Aggregation

2022; RELX Group (Netherlands); Linguagem: Inglês

10.2139/ssrn.4167606

1556-5068

Mirjana Marković, Đuro Čokeša, Svjetlana Radmanović, Nebojša Potkonjak, Snezana M. Serbula,

Clay minerals and soil interactions

Arsenite-humic acid binding process was investigated using the Isothermal Titration Calorimetry (ITC), Dynamic Light Scattering and Laser Doppler Electrophoresis techniques. The ITC data were successfully (R 2 =0.996-0.936) interpreted by applying the MNIS model, enabling thermodynamic parameters to be determined. The MNIS model was adjusted to the arsenite-HA binding process assuming that hydrogen bonding is the dominant type of interaction in the system. Negative enthalpy change values indicated the arsenite-HAs binding as an exothermic process. Negative ΔG values (-(26.83-27.00) kJ mol -1 ) pointed out to spontaneous binding reaction, leading to the formation of the arsenite-HA complexes. The binding constants values ((7.57-5.02) 10 5 M -1 ) clearly demonstrate pronounced binding affinity. As ΔS values are obviously positive but close to zero, and ΔH>ΔS, the reaction can be considered enthalpy driven. Reaction heats and DH values (-(18.96-15.64) kJ mol -1 ) confirmed hydrogen bonds as the most ascendant interaction type in the arsenite-HA complex. Negative zeta potential values (-45 to -20 mV) had shown that arsenite-HA aggregates remained negatively charged in the whole molar charge ratio range. The HAs' aggregate size change is evident but not particularly pronounced (Z av =50-180 nm). It can be speculated that aggregation during the titration process is not expressive due to repulsive forces between negatively charged arsenite-HA particles. Thermodynamic and reaction parameters clearly indicated that arsenite-HA complexes are formed at common soil pH values, confirming the possible influence of humic acids on increased As mobility and its reduced bioavailability.