Marcelo Avena

Prof. Marcelo Avena

orcid

Research Focus & Metrics

Academic Career Length

12Years (2015-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
1 October 2019 in Journal of Environmental Chemical Engineering
Verified
Journal Article
Closed access
JOJulian Ortiz Otalvaro
Julian Ortiz Otalvaro
MAMarcelo Avena
Marcelo Avena
MBMaximiliano Brigante
Maximiliano Brigante

1 June 2020 in Advances in Colloid and Interface Science
Verified
Journal Article
Closed access
LKLuuk Koopal
Luuk Koopal
WTWenfeng Tan
Wenfeng Tan
MAMarcelo Avena
Marcelo Avena

1 February 2016 in Chemosphere
Verified
Journal Article
Closed access
JAJeison Manuel Arroyave
Jeison Manuel Arroyave
CWCarolina C. Waiman
Carolina C. Waiman
GZGraciela P. Zanini
Graciela P. Zanini
MAMarcelo Avena
Marcelo Avena

25 May 2015 in Environmental Chemistry
Verified
Journal Article
Closed access
PDF file
NKNanci Kloster
Nanci Kloster
MAMarcelo Avena
Marcelo Avena
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. 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.

1 January 2021 in Journal of Environmental Management
Verified
Journal Article
Closed access
FMFlorencia M. Onaga Medina
Florencia M. Onaga Medina
MAMaría B. Aguiar
María B. Aguiar
MPMaría E. Parolo
María E. Parolo
MAMarcelo Avena
Marcelo Avena

1 June 2018 in Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy
Verified
Journal Article
Closed access
JAJeison Manuel Arroyave
Jeison Manuel Arroyave
VPVirginia Puccia
Virginia Puccia
GZGraciela P. Zanini
Graciela P. Zanini
MAMarcelo Avena
Marcelo Avena