2001
DOI: 10.1016/s0016-7037(00)00602-5
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Cadmium and copper release kinetics in relation to afforestation of cultivated soil

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Cited by 76 publications
(42 citation statements)
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“…This showed that the release of soil metals was controlled by the contents of total organic carbon to a great extent, and was similar to the results of Strobel, Hansen, Borggaard, Andersen, and Raulund-Rasmussen (2001) and Tipping et al (2003). Special low values of coefficient a for Cu indicated that Cu was highly associated with soil organic matter and not released into soil solution.…”
Section: Discussionsupporting
confidence: 80%
“…This showed that the release of soil metals was controlled by the contents of total organic carbon to a great extent, and was similar to the results of Strobel, Hansen, Borggaard, Andersen, and Raulund-Rasmussen (2001) and Tipping et al (2003). Special low values of coefficient a for Cu indicated that Cu was highly associated with soil organic matter and not released into soil solution.…”
Section: Discussionsupporting
confidence: 80%
“…Vários trabalhos relatam que a dessorção de Cd, tanto em solos quanto em óxidos sintéticos (por exemplo, goethita), diminui com o aumento do pH (Christensen 1989;Backes et al, 1995;Strobel et al, 2001). Entretanto, a comparação entre trabalhos é dificultada pela grande diversidade de soluções extratoras neles usadas [como,por exemplo,DTPA,CaCl 2 ,HCl,Ca(NO 3 ) 2 ].…”
Section: Resultsunclassified
“…Dissolved organic carbon is the most mobile fraction of organic ligands that exist in soils and may assist in the transfer of metals through soil as organic complexes (Cao et al, 2003); greater concentrations of aromatic and phenolic compounds will produce soluble metal-organic complexes (Tapia et al, 2010;Vaca-Paulín et al, 2006). Copper mobility has been shown to increase with increasing DOC concentration and pH (Temminghof et al, 1997;Strobel et al, 2001), whilst Zhou and Wong (2001) reported that application of soluble organic carbon from sewage sludge reduced Cu sorption in soil due to development of soluble complexes, with the effect being greater at higher pH. There were no significant differences in pore water Zn and Mn concentrations compared to controls (Figs S4 and S5).…”
Section: Micronutrient Mobility and Dissolved Organic Carbonmentioning
confidence: 99%