Desorption rate of glyphosate from goethite as affected by different entering ligands: hints on the desorption mechanism

2017 ◽  
Vol 14 (5) ◽  
pp. 288 ◽  
Author(s):  
Jeison M. Arroyave ◽  
Carolina C. Waiman ◽  
Graciela P. Zanini ◽  
Wenfeng Tan ◽  
Marcelo J. Avena

Environmental contextGlyphosate is a heavily used herbicide that is mobilised in soil and sediments through adsorption–desorption processes from the surface of mineral particles. We demonstrate that the desorption rate of glyphosate from goethite, a ubiquitous mineral, is nearly independent of the concentration and nature of the substance that is used to desorb it. The results elucidate the desorption mechanism and are relevant to understand and predict the environmental mobility of glyphosate. AbstractThe desorption kinetics of glyphosate (Gly) from goethite was studied in a flow cell using attenuated total reflectance Fourier-transform infrared spectroscopy. Because Gly forms an inner-sphere surface complex by coordinating to Fe atoms at the goethite surface, the desorption process is actually a ligand-exchange reaction, where Gly is the leaving ligand and water molecules or dissolved substances are the entering ligands. A series of possible entering ligands that can be found in nature was tested to evaluate their effect on the desorption kinetics of Gly. Contrarily to expectations, the desorption rate was quite independent of the entering ligand concentration. Moreover, the identity of this ligand (phosphate, citrate, sulfate, oxalate, EDTA, thiocyanate, humic acid, water) had only a small effect on the value of the desorption rate constant. By analogy with the reactivity of transition metal complexes in solution, it is concluded that the rate is mainly controlled by the breaking of the Fe–Gly bond, through a dissociative or a dissociative interchange mechanism. The results are relevant in understanding and predicting the environmental mobility of Gly: irrespective of the identity of the entering ligand, Gly will always desorb from iron (hydr)oxides in nature at nearly the same rate, simplifying calculations and predictions enormously. The importance of studying desorption kinetics using mineral surfaces and environmentally relevant molecules is also highlighted.

Soil Science ◽  
1988 ◽  
Vol 146 (4) ◽  
pp. 221-231 ◽  
Author(s):  
J. J. T. I. BOESTEN ◽  
L. J. T. VAN DER PAS

2019 ◽  
Vol 17 (2) ◽  
pp. 371-380 ◽  
Author(s):  
Mohamed El messoudi ◽  
Aicha Boukhriss ◽  
Omar Cherkaoui ◽  
M’hammed El kouali ◽  
Said Gmouh

1993 ◽  
Vol 99 (9) ◽  
pp. 7190-7197 ◽  
Author(s):  
C. R. Carlson ◽  
W. F. Buechter ◽  
F. Che‐Ibrahim ◽  
E. G. Seebauer

Energies ◽  
2019 ◽  
Vol 12 (20) ◽  
pp. 4013 ◽  
Author(s):  
Norbert Skoczylas ◽  
Anna Pajdak ◽  
Mariusz Młynarczuk

The paper presents the results of studies on sorption and CO2 desorptions from coals from two Polish mines that differed in petrographic and structural properties. The tests were carried out on spherical and plane sheet samples. On the basis of the sorption tests, the effective diffusion coefficient was calculated on the plane sheet samples based on a proper model. Similar tests were performed on the spherical samples. Mathematical model results for plane sheet samples were compared with the most frequently chosen model for spherical samples. The kinetics of CO2 desorption from plane sheet samples were compared with the kinetics of sample shrinkage. In both samples, the shrinkage was about 0.35%. The size change kinetics and CO2 desorption kinetics significantly differed between the samples. In both samples, the determined shrinkage kinetics was clearly faster than CO2 kinetics.


Soil Science ◽  
2011 ◽  
Vol 176 (11) ◽  
pp. 582-588 ◽  
Author(s):  
Chang Yoon Jeong ◽  
H. Magdi Selim

Sign in / Sign up

Export Citation Format

Share Document