2008
DOI: 10.1016/j.envpol.2008.05.029
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Feasibility of phytoextraction to remediate cadmium and zinc contaminated soils

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Cited by 94 publications
(43 citation statements)
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“…Phytoextraction with hyperaccumulating plants has been suggested to be a promising technique to remediate soils contaminated with trace metals (Hammer and Keller 2003;Koopmans et al 2008;Maxted et al 2007;McGrath et al 2006;Robinson et al 1998;Schwartz et al 2003;Zhao et al 2003). Hyperaccumulating plants accumulate metals in shoots at concentrations above defined thresholds when grown in their natural habitats, i.e., 100 μg g −1 for Cd, 1000 μg g −1 for Ni, or 3000 μg g −1 for Zn, on a dry weight basis (Krämer 2010;van der Ent et al 2013).…”
Section: Responsible Editor: Elena Maestrimentioning
confidence: 99%
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“…Phytoextraction with hyperaccumulating plants has been suggested to be a promising technique to remediate soils contaminated with trace metals (Hammer and Keller 2003;Koopmans et al 2008;Maxted et al 2007;McGrath et al 2006;Robinson et al 1998;Schwartz et al 2003;Zhao et al 2003). Hyperaccumulating plants accumulate metals in shoots at concentrations above defined thresholds when grown in their natural habitats, i.e., 100 μg g −1 for Cd, 1000 μg g −1 for Ni, or 3000 μg g −1 for Zn, on a dry weight basis (Krämer 2010;van der Ent et al 2013).…”
Section: Responsible Editor: Elena Maestrimentioning
confidence: 99%
“…caerulescens (Brassicaceae, formerly Thlaspi caerulescens) is one of the most promising candidate species for Cd and Zn phytoextraction (Koopmans et al 2008;Maxted et al 2007;McGrath et al 2006;Zhao et al 2003). Three ecotypes of N. caerulescens have been described: metallicolous plants grow in soils enriched in Cd-Zn-Pb (calamine, CAL) and in serpentine sites (mostly enriched in Ni), whereas non-metallicolous (NMET) grow in uncontaminated soils (Escarré et al 2000;Meerts and van Isacker 1997;Molitor et al 2005;Reeves et al 2001).…”
Section: Responsible Editor: Elena Maestrimentioning
confidence: 99%
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“…The reactive fraction represents sorbed metals reacting with binding sites located on surfaces of soil organic matter (SOM), amorphous metal oxides, and clay and is believed to control the metal concentration in the soil solution (Weng et al 2001;Tipping et al 2003). Adsorption-desorption equilibria between the reactive metal pool in the soil-solid phase and the metal concentration in soil solution have been described with empirical solid-solution partitioning models in which pH and cation exchange capacity (CEC) were included to account for differences between soils (Römkens et al 2004;Ingwersen and Streck 2006;Meers et al 2007;Koopmans et al 2008a). Various extracts are used to determine the size of the reactive metal pools including dilute acids like 0.43 M HNO 3 (Houba et al 1997;Weng et al 2001;Tipping et al 2003), 0.1 M HCl (Colombo and van den Berg 1998), and EDTA (Clayton and Tiller 1979).…”
mentioning
confidence: 99%