Loading…

Accumulation of arsenic and zinc in the rhizosphere of wetland plants

Iron oxyhydrides precipitate in the rhizosphere of wetland plants by oxidation, and are called ironplaque. Zinc and arsenic content of the soil in contact with the rhizosphere and in bulk soil near two species of wetland plants, Halimione portulacoides and Spartina anglica, were determined. Iron con...

Full description

Saved in:
Bibliographic Details
Published in:Bulletin of environmental contamination and toxicology 1995-07, Vol.55 (1), p.154-161
Main Authors: Otte, M.L. (University College Dublin, Belfield, Dublin, Ireland.), Kearns, C.C, Doyle, M.O
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Iron oxyhydrides precipitate in the rhizosphere of wetland plants by oxidation, and are called ironplaque. Zinc and arsenic content of the soil in contact with the rhizosphere and in bulk soil near two species of wetland plants, Halimione portulacoides and Spartina anglica, were determined. Iron concentrations of the soils were not different for each species, but the iron content of the rhizosphere soil was lower than that of the bulk soil. Zinc content of rhizosphere soil was greater than that of bulk soil for both species. Arsenic concentrations were higher in soil near H. portulacoides Rhizosphere soil had more arsenic than bulk soil for both species, however. Iron and zinc concentrations in the ironplaque were similar for both species. Arsenic content of ironplaque was greater in S. anglica.
ISSN:0007-4861
1432-0800
DOI:10.1007/bf00212403