JEQ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Abstract Freely available
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (37)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Singh, S. P.
Right arrow Articles by Harris, W. G.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Singh, S. P.
Right arrow Articles by Harris, W. G.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Singh, S. P.
Right arrow Articles by Harris, W. G.
Related Collections
Right arrow Soil Mineralogy
Right arrow Industrial Waste
Right arrow Heavy Metals
Right arrow Soil Pollution
Right arrow Soil Chemistry

Heavy Metal Interactions with Phosphatic Clay

Sorption and Desorption Behavior

S. P. Singha, L. Q. Ma*,b and W. G. Harrisb

a Soil Science Division, Univ. of Idaho, Moscow, ID 83844-2339
b Soil and Water Science Dep., Univ. of Florida, Gainesville, FL 32611-0290



View larger version (19K):

[in a new window]
 
Fig. 1. Langmuir sorption isotherms of Pb+2, Cd+2, and Zn+2 on phosphatic clay (A) and their linear fittings (B) after the transformation using the Langmuir equation.

 


View larger version (17K):

[in a new window]
 
Fig. 2. Relationships between sorbed metals and final pH (A), and between sorbed metals and total Ca concentrations in the final solution (B) after 24 h of metal interaction with phosphatic clay.

 


View larger version (24K):

[in a new window]
 
Fig. 3. X-ray diffraction patterns of phosphatic clay before Pb sorption (A) and after Pb sorption (B). Mineral abbreviations: s (smectite), pa (polygorskite), k (kaolinite), q (quartz), py (pyromorphite), and a (apatite).

 


View larger version (120K):

[in a new window]
 
Fig. 4. Scanning electron microscopy (SEM) back scattered electron image (BSI) micrograph of pyromorphite in aqueous Pb-treated phosphatic clay showing cluster of lath-like pyromorphite crystals.

 


View larger version (129K):

[in a new window]
 
Fig. 5. Energy dispersive X-ray spectroscopy (EDS) dot-mapping of pyromorphite particle in aqueous Pb-treated phosphatic clay. (A) Selected pyromorphite crystal. (B) Presence of Pb in pyromorphite. (C) Presence of P in pyromorphite. (D) Absence of Ca in pyromorphite.

 





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Copyright © 2001 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.