APPLICATIONS OF THE CONTINUOUS-FLOW STIRRED-CELL (CFSC) TECHNIQUE .2.THE ADSORPTION BEHAVIOR OF NA, CS, SR, CU, NI AND PB ON HUMIC ACIDS

Citation
K. Randle et Eh. Hartmann, APPLICATIONS OF THE CONTINUOUS-FLOW STIRRED-CELL (CFSC) TECHNIQUE .2.THE ADSORPTION BEHAVIOR OF NA, CS, SR, CU, NI AND PB ON HUMIC ACIDS, European journal of soil science, 46(2), 1995, pp. 303-315
Citations number
24
Categorie Soggetti
Agriculture Soil Science
ISSN journal
13510754
Volume
46
Issue
2
Year of publication
1995
Pages
303 - 315
Database
ISI
SICI code
1351-0754(1995)46:2<303:AOTCS(>2.0.ZU;2-U
Abstract
The first part of this paper deals with the sorption of Na, Cs, Sr, Ni , Cu and Pb on two humic fractions derived from a soil. The sorption d ata for individual elements were obtained using the continuous-flow st irred-cell (CFSC) technique, in which the metal sorptive solution is p umped through a cell containing a known mass of the humic acid retaine d by a filter and the solution emerging from the cell was analysed by either atomic absorption spectrometry (Cu, Ni and Pb) or by the combin ed use of radioisotope dilution and gamma-ray spectroscopy (Na, Cs and Sr). Sorption isotherms were determined at two flow rates. It was fou nd that, in general, the sorption isotherms for all the metals studied could be described by the Langmuir equation and parameters derived fr om the fitted line provided information on the metal-humate binding st rengths and the maximum amount of metal sorbed per unit mass of humic acid. Caesium showed anomalous behaviour at certain flow rates in both its sorption and desorption behaviour. In the second part of the pape r we discuss the sequential sorption and desorption of one metal by an other on the same humic fraction, using Na, Cs, Zn and Cd. The aim was to elucidate the nature of the binding process when several metals we re competing simultaneously for the functional groups on the humic aci ds. In addition, at the end of the experiment, the humic material was isolated and analysed by gamma-ray spectroscopy to determine the metal s still bound in this fraction. Some tentative conclusions concerning the nature of the metal-humate complexes are made on the basis of thes e data.