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Spatial distribution of arsenic and heavy metals in willow roots from a contaminated floodplain soil measured by X-ray fluorescence spectroscopy

delete2011-07-01
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PRE
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D
Dana Zimmer *
J
Jens Kruse
C
Christel Baum
C
Camelia N. Borca
M
Michael Laue
G
Gerd Hause
M
Meissner, Ralph
P
Peter Leinweber
DOI:10.1016/j.scitotenv.2011.06.038delete
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Abstract

Abstract

En 中文
Under changing redox conditions some plants create plaques at their root surface, which may affect the mobility and uptake of As and heavy metals but it is unknown to what extent this also holds true for willows in contaminated floodplain soils. Therefore, willow roots were sampled from a phytoremediation trial in the contaminated floodplain of the river Elbe (Germany), cryofixed, freeze-dried, and cross sections were mapped for the distribution of As, Ca, Cu, Fe, K, Mn, Ni, S and Zn by synchrotron based X-ray fluorescence spectroscopy. The elements Ca, Cu, Ni, S and Zn were concentrated in the aerenchymatic tissue, and not associated with Fe and Mn. Mixed Fe Mn plagues covered the surface of the willow roots and As was accumulated in these plagues. The observed association pattern between As and Fe was explained by the different sorption/desorption properties of As(III) and As(V). The Cu and Zn intensities were not associated with the intensity of Fe in the plaque, which seems to be a willow-specific difference compared to other wetland plants. These results suggested that willows are especially suited to stabilize low-phytoextractable elements like Cu and As in their roots and rhizosphere. Thus, short rotation coppicing of willows may be a practical approach to mitigate the adverse effects of floodplain soil contamination. (C) 2011 Elsevier B.V. All rights reserved.
Keywords:
Plaques
Salix caprea x viminalis
Element mapping
XRF
Cryofixation
Rhizosphere
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Science of The Total Environment cover
Science of The Total Environment
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M
Martin Luther University Halle Wittenberg
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University of Rostock
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swiss federal institutes of technology domain
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Paul Scherrer Institute
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