Interaction of humic acids with soil minerals: adsorption and surface aggregation induced by Ca2+
Nanci Kloster A and Marcelo Avena B C
+ Author Affiliations
- Author Affiliations
A EEA Anguil ‘Ingeniero Agrónomo Guillermo Covas’, Instituto Nacional de Tecnología Agropecuaria (INTA), ruta nacional número 5, kilómetro 580, (6326) Anguil, La Pampa, Argentina.
B Instituto de Química del Sur (INQUISUR)–Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Departamento de Química, Universidad Nacional del Sur, Avenida Alem 1253, (8000) Bahía Blanca, Argentina.
C Corresponding author. Email: mavena@uns.edu.ar
Environmental Chemistry 12(6) 731-738 https://doi.org/10.1071/EN14157
Submitted: 19 August 2014 Accepted: 16 February 2015 Published: 25 May 2015
Environmental context. Humic acids, important components of natural organic matter in soils, sediments and aquatic media, can interact with the surface of minerals affecting key environmental processes. In the presence of calcium, humic acids can also interact among themselves leading to molecular aggregates. We demonstrate that a solid mineral surface facilitates the formation of humic acid aggregates, and thus surface aggregation occurs under conditions where normal aggregation in solution does not occur.
Abstract. Humic acids (HAs) interact with the surface of mineral particles leading to the formation of clay–humic complexes that affect the transport of nutrients and contaminants in the environment, soil structure, soil erosion and carbon sequestration by soils. The interaction is influenced by the presence of multivalent ions, such as Ca2+, which enhances the uptake of HAs by the particles. This article reports the effects of Ca2+ on the interaction between a HA and a soil clay fraction, both obtained from the same soil sample. The study was performed by using zeta potential measurements, HA adsorption isotherms, Ca2+ adsorption isotherms and microscopy. The results show that at low HA concentrations and low Ca2+ concentrations HA adsorption takes place, but that at high concentrations surface aggregation and precipitation also takes place, a process that is seldom reported or analysed in the literature. HA adsorption isotherms only give the overall HA uptake by the solid but they do not allow differentiation of HA adsorption from surface aggregation. However, HA adsorption v. Ca2+ concentration plots and Ca2+ adsorption isotherms at different HA concentrations can distinguish these two processes quite clearly. In addition, surface aggregation could be undoubtedly observed with optical microscopy. Surface aggregation starts to take place at a 0.7 mM Ca2+ concentration, which is lower than the Ca2+ concentration needed to start HA aggregation in solution. This indicates that the surface of soil minerals acts as a nucleation centre for HA aggregation.
Additional keywords: carbon sequestration; humic acid precipitation; soil aggregates.
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