SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 53:1057-1061 (1989)
© 1989 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
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 Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hinedi, Z. R.
Right arrow Articles by Chang, A. C.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Hinedi, Z. R.
Right arrow Articles by Chang, A. C.
Agricola
Right arrow Articles by Hinedi, Z. R.
Right arrow Articles by Chang, A. C.

Solubility and Phosphorus-31 Magic Angle Spinning Nuclear Magnetic Resonance of Phosphorus in Sludge-Amended Soils

Zeina R. Hinedi*

Soil Science Dep., 2169 McCarty Hall, Univ. of Florida, Gainesville, FL 32611

Andrew C. Chang

Dep. of Soils and Environmental Sciences, Univ. of California, Riverside, CA 92521

*Corresponding author.

ABSTRACT

The solubility of P in two sludge-amended soils was studied. Solubility and activity ratio diagrams for P in sludge-amended soils were constructed and were compared with those of selected Ca-P, Fe-P, and Al-P minerals. The solid phase controlling P solubility in the sludge-amended soils appeared to be a carbonated apatite formed through coprecipitation. The 31P magic angle spinning nuclear magnetic resonance (31P MAS NMR) examinations confirmed that P in the sludge-amended soils was in form of calcium phosphate. The resonant peak [at isotropic chemical shift ({delta}lso) = 3.1 ppm] is indicative of an apatitic calcium phosphate environment characterized by carbonate substitution. Additionally, pyrophosphate was detected by the presence of a peak at {delta}lso = –9 ppm.


NOTES

Contribution from Dep. of Soil and Environmental Sciences, Univ. of California, Riverside.

Received for publication June 15, 1988.


This article has been cited by other articles:


Home page
J. Environ. Qual.Home page
R.W. McDowell, L.M. Condron, N. Mahieu, P.C. Brookes, P.R. Poulton, and A.N. Sharpley
Analysis of Potentially Mobile Phosphorus in Arable Soils Using Solid State Nuclear Magnetic Resonance
J. Environ. Qual., March 1, 2002; 31(2): 450 - 456.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1989 by the Soil Science Society of America.