The effect of cysteine on the adsorption of Cd(II) by kaolinite was examined at 25°C using a low-defect kaolinite from Minas Gerais (Brazil) and a high-defect kaolinite from Berici Hills (Italy). The chemical data demonstrated that the amount of Cd–cysteine detected on kaolinite increases rapidly during the first few hours with a first-order reaction, thereafter adsorption becomes linear with time for low-defect kaolinite and slows rapidly for high-defect kaolinite. In low-ordered kaolinite, the Cd–cysteine is intercalated in the structure. Evidence of these changes was also observed by differential thermal analysis (DTA). The thermal decomposition of the Cd–cysteine adsorbed on the kaolinites was studied by analysing the evolved gases. The mass spectra of both samples show the evolution of NO (or CH3CH3, m/z = 30), CO2 (m/z = 44), and SO2 (m/z = 64) between 150 and 300°C and of H2O (m/z = 18), CO2 (m/z = 44) and SO2 (m/z = 64) in the temperature range between 400 and 700°C. The high-defect kaolinite also caused the evolution of molecular units with m/z=34 (H2S) and m/z=76 (N2O3).

Sorption of Cd-cysteine complexes by kaolinite

Medici L;
2002

Abstract

The effect of cysteine on the adsorption of Cd(II) by kaolinite was examined at 25°C using a low-defect kaolinite from Minas Gerais (Brazil) and a high-defect kaolinite from Berici Hills (Italy). The chemical data demonstrated that the amount of Cd–cysteine detected on kaolinite increases rapidly during the first few hours with a first-order reaction, thereafter adsorption becomes linear with time for low-defect kaolinite and slows rapidly for high-defect kaolinite. In low-ordered kaolinite, the Cd–cysteine is intercalated in the structure. Evidence of these changes was also observed by differential thermal analysis (DTA). The thermal decomposition of the Cd–cysteine adsorbed on the kaolinites was studied by analysing the evolved gases. The mass spectra of both samples show the evolution of NO (or CH3CH3, m/z = 30), CO2 (m/z = 44), and SO2 (m/z = 64) between 150 and 300°C and of H2O (m/z = 18), CO2 (m/z = 44) and SO2 (m/z = 64) in the temperature range between 400 and 700°C. The high-defect kaolinite also caused the evolution of molecular units with m/z=34 (H2S) and m/z=76 (N2O3).
2002
Istituto di Metodologie per l'Analisi Ambientale - IMAA
21
191
201
kaolinite
Cd-cysteine complex
adsorption
intercalation
mass spectrometry
Questo lavoro si inquadra in un filone di ricerca avente come oggetto di studio i processi di scambio ed adsorbimento tra ioni in soluzione e minerali dei suoli. Le problematiche alla base di questo filone di ricerca sono sorte in considerazione dell'aumentato interesse della comunità scientifica internazionale verso problemi di protezione ambientale. I lavori sviluppati in questo settore, si prefiggono di valutare, in base a considerazioni sperimentali e teoriche, il ruolo effettivo che alcuni minerali microcristallini hanno nel modificare le caratteristiche di soluzioni contenenti metalli pesanti e composti organici inquinanti e di chiarire come, ed in qual misura, l'interazione con queste soluzioni modifichi la struttura e le proprietà chimico-fisiche dei minerali stessi. Nell’anno 2002, Luca Medici, a seguito dei risultati di questi studi, ha conseguito il premio Panichi per le scienze mineralogiche.
5
info:eu-repo/semantics/article
262
Benincasa, E; Brigatti, Mf; Malferrari, D; Medici, L; Poppi, L
01 Contributo su Rivista::01.01 Articolo in rivista
none
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/431173
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