2002
DOI: 10.1016/s0045-6535(01)00206-5
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Comparison between fractionation and bioavailability of trace elements in rhizosphere and bulk soils

Abstract: Rhizosphere is a microbiosphere and has quite different chemical, physical and biological properties from bulk soils. A greenhouse experiment was performed to compare the difference of fractionation and bioavailability of trace elements Cr, Ni, Zn, Cu, Pb and Cd between rhizosphere soil and bulk soil. In the meantime, the influence of air-drying on the fractionation and bioavailability was also investigated by using wet soil sample as a control. Soils in a homemade rhizobox were divided into four zones: rhizos… Show more

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Cited by 148 publications
(80 citation statements)
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“…The properties of the rhizosphere are different from those of bulk soil in terms of a range of biochemical, chemical and physical processes that occur as a consequence of root growth, water and nutrient uptake, respiration and rhizodeposition (Wang et al 2002;Hinsinger et al 2005). Field data support the hypothesis that exudation of organic ligands may contribute to enhanced solubility and replenishment of metals in the rhizosphere of hyperaccumulating species (Wenzel et al 2003).…”
Section: Introductionmentioning
confidence: 85%
“…The properties of the rhizosphere are different from those of bulk soil in terms of a range of biochemical, chemical and physical processes that occur as a consequence of root growth, water and nutrient uptake, respiration and rhizodeposition (Wang et al 2002;Hinsinger et al 2005). Field data support the hypothesis that exudation of organic ligands may contribute to enhanced solubility and replenishment of metals in the rhizosphere of hyperaccumulating species (Wenzel et al 2003).…”
Section: Introductionmentioning
confidence: 85%
“…Means in final row for amounts of Cu release in each extractant from the bulk and the rhizosphere soil followed by the different letters are significantly different (P < 0.01); DTPA-TEA -diethylenetriaminepentaacetic acid-triethanolamine Table 4. Coefficient of determination (R 2 ) and standard error of the estimate (SE, mg/kg) of various kinetic models for Cu release in diethylenetriaminepentaacetic acid-triethanolamine (DTPA-TEA) and citric acid (2003) and Wang et al (2002), the different chemical and biological conditions of the rhizosphere soil can change Cu fractions and therefore amounts of release of Cu. The best supporting evidence for any equation used to describe the kinetics of Cu release is the comparison of the amount of Cu desorption with plant indices on soils with a range of Cu supply.…”
Section: Resultsmentioning
confidence: 99%
“…In this study, a homemade rhizobox (Wang et al 2002) was used to plant wheat. The rhizobox was divided into three sections: a central zone or rhizosphere zone (30 mm in length), which was surrounded by nylon cloth (300 mesh), and left and right non-rhizosphere zones (bulk soils) (50 mm in length).…”
Section: Methodsmentioning
confidence: 99%
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“…The rhizosphere also affects the availability of heavy metals. Early studies have indicated that there is higher concentration of exchangeable and carbonate bound Cr, Ni, Zn, Cu, Pb and Cd in the rhizosphere than in bulk soil (Wang et al, 2002). Root -induced changes in the rhizosphere are important factors controlling nutrient dynamics in this zone and thus the mineral nutrition of plants.…”
Section: Introductionmentioning
confidence: 99%