Plant and Soil

, Volume 359, Issue 1–2, pp 71–83 | Cite as

Hyperaccumulation of nickel by Alyssum corsicum is related to solubility of Ni mineral species

  • Tiziana CentofantiEmail author
  • Matthew G. Siebecker
  • Rufus L. Chaney
  • Allen P. Davis
  • Donald L. Sparks
Regular Article



Past studies have demonstrated that hyperaccumulators absorb Ni from the same labile pools in soil as normal plant species. This study investigated whether the Ni hyperaccumulator plant Alyssum corsicum possesses distinct extraction mechanisms for different Ni species present in soils. Different Ni species have different solubilities and potential bioavailabilities to roots.


Uptake of Ni in shoots of A. corsicum was analyzed after four weeks of plant growth in nutrient solution with 17 different Ni compounds or soils.


The results indicate that Ni uptake is related to Ni solubility and plant transpiration rate. The most soluble compounds had the highest Ni uptake, with the exception of Ni3(PO4)2, Ni phyllosilicate, Ni-acid birnessite which showed a low solubility but a relatively high plant uptake and transpiration rate. In serpentine soils and insoluble NiO plant transpiration rate was high but uptake was very low and statistically comparable to the control.


It appears that Ni uptake is driven by convection, which depends on the initial concentration of Ni in solution and the plant transpiration rate.


Ni minerals Alyssum Hyperaccumulators Ni solubility 



The authors would like to thank Dr. G. Echevarria for providing the garnierite and limonite soils from Brazil and Dr. C. Green for carrying out the ICP analyses.

Supplementary material

11104_2012_1176_MOESM1_ESM.pdf (284 kb)
ESM 1 (PDF 283 kb)


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Copyright information

© Springer Science+Business Media B.V. 2012

Authors and Affiliations

  • Tiziana Centofanti
    • 1
    • 3
    Email author
  • Matthew G. Siebecker
    • 2
  • Rufus L. Chaney
    • 3
  • Allen P. Davis
    • 1
  • Donald L. Sparks
    • 2
  1. 1.Department of Civil and Environmental EngineeringUniversity of MarylandCollege ParkUSA
  2. 2.Environmental Soil Chemistry Research Group, Department of Plant and Soil SciencesUniversity of DelawareNewarkUSA
  3. 3.US Department of Agriculture, Agricultural Research ServiceEnvironmental Management and Byproduct Utilization LaboratoryBeltsvilleUSA

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