Pedogenic Chromium and Nickel Partitioning in Serpentine Soils along a Toposequence
To elucidate the properties of pedogenic Cr and Ni in serpentine soils in terms of mobilization, three pedons on the shoulder (Entisol), backslope (Inceptisol), and footslope (Alfisol) along a toposequence in eastern Taiwan were examined for metal partitioning and their geochemical origins. The anal...
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Published in | Soil Science Society of America journal Vol. 75; no. 2; pp. 659 - 668 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Madison
Soil Science Society
01.03.2011
Soil Science Society of America American Society of Agronomy |
Subjects | |
Online Access | Get full text |
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Summary: | To elucidate the properties of pedogenic Cr and Ni in serpentine soils in terms of mobilization, three pedons on the shoulder (Entisol), backslope (Inceptisol), and footslope (Alfisol) along a toposequence in eastern Taiwan were examined for metal partitioning and their geochemical origins. The analysis combined bulk soil analysis by selective sequential extraction (SSE) with mineralogical methods, including x‐ray diffraction (XRD) and scanning electron microscopy/energy dispersive x‐ray spectroscopy (SEM/EDX) analyses. Experimental results showed that Cr and Ni were mainly concentrated in chromites and silicates, respectively, and were gradually exposed by weathering of the parent materials. The SEM/EDX analysis indicated that chemical modification of the chromites was more prevalent near the soil surface and that the chemical modification increased as available Cr content increased from the shoulder to the footslope. Landscape position was the most important factor in controlling the trends in Ni and Cr fractions. The footslope accumulated more total Cr and Ni than the shoulder and backslope. Additionally, the soil on the footslope received more effective precipitation as run‐on water from upslope and was potentially more leached than the soils on the other landscape positions. The accumulation of clay and dithionite‐citrate‐bicarbonate (DCB) extractable Fe (Fed) and the increase of exchangeable Ca/Mg ratio correlated with the increased total labile pools of Cr and Ni in the soil from the shoulder and backslope to the footslope. However, the concentrations of acid soluble, reducible, and oxidizable fractions (total labile pool) of Ni were higher than those of Cr, indicating that Ni was more available than Cr in all soils tested by the SSE procedures. |
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Bibliography: | All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. Permission for printing and for reprinting the material contained herein has been obtained by the publisher. |
ISSN: | 0361-5995 1435-0661 |
DOI: | 10.2136/sssaj2010.0007 |