SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 55:670-675 (1991)
© 1991 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 Grossl, P. R.
Right arrow Articles by Inskeep, W. P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Grossl, P. R.
Right arrow Articles by Inskeep, W. P.
Agricola
Right arrow Articles by Grossl, P. R.
Right arrow Articles by Inskeep, W. P.

Precipitation of Dicalcium Phosphate Dihydrate in the Presence of Organic Acids

Paul R. Grossl and William P. Inskeep*

Department of Plant and Soil Science, Montana State Univ., Bozeman, MT 59717-0002

* Corresponding author.

ABSTRACT

Inhibition of dicalcium phosphate dihydrate (DCPD) precipitation rate by organic acids may play an important role in controlling phosphate activity and availability in P-fertilized soils. The precipitation rate of DCPD was measured at pH 5.7 and 25 °C in the absence and presence of organic acids common to soil solutions using a seeded crystal growth method. Forward rate constants (kf) were determined from an integrated form of the second-order rate law expression: rate = kfS[Ca2+][HPO2-4]{gamma}22, where brackets represent concentrations, S is the surface area (m2 L–1), and {gamma}2 is the divalent ion activity coefficient calculated from the Davies equation. The average kf (L2 mol–1 m–2 s–1) for DCPD precipitation without organic acids was 9.7 ± 0.5. Additions of 0.26 to 2.06 mM C as humic acid and 1.1 to 3.3 mM C as fulvic acid resulted in induction periods lasting 2.0 to 632 and 1.5 to 10 min, respectively, prior to subsequent precipitation of DCPD. This indicates that DCPD precipitation was able to overgrow adsorbed humic and fulvic acids. Rates of DCPD precipitation were determined in the presence of humic, fulvic, citric, and tannic acids at concentrations ranging from 0.26 to 9.0 mM total soluble C (CTS). The highest levels of humic, fulvic, citric, and tannic acids added were 2.05, 7.8, 8.0, and 9.0 mM CTS, which resulted in decreased kf values of 1.1, 0.1, 0.6, and 2.1 L2 mol–1 m–2 s–1, respectively. Precipitation was inhibited by adsorption of these organic acids onto DCPD surfaces blocking sites acting as nuclei for new crystal growth. Adsorption characteristics of these organic acids were related to their functional-group content and size. The ability of DCPD to precipitate on seed crystals with adsorbed C may explain the kinetically favored formation of DCPD vs. more thermodynamically stable octacalcium phosphate (OCP) and hydroxyapatite (HAP), where precipitation rates are more strongly inhibited by soluble C.


NOTES

Contribution of the Montana State Univ. Agric. Exp. Stn. Journal no. J-2561.

Received for publication April 6, 1990.


This article has been cited by other articles:


Home page
Soil Sci.Home page
C. Saavedra, J. Velasco, P. Pajuelo, F. Perea, and A. Delgado
Effects of Tillage on Phosphorus Release Potential in a Spanish Vertisol
Soil Sci. Soc. Am. J., January 1, 2007; 71(1): 56 - 63.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
M. Kalbasi and K. G. Karthikeyan
Phosphorus Dynamics in Soils Receiving Chemically Treated Dairy Manure
J. Environ. Qual., November 1, 2004; 33(6): 2296 - 2305.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
C. L. Mackowiak, P. R. Grossl, and B. G. Bugbee
Beneficial Effects of Humic Acid on Micronutrient Availability to Wheat
Soil Sci. Soc. Am. J., November 1, 2001; 65(6): 1744 - 1750.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
E. Valsami-Jones
Mineralogical controls on phosphorus recovery from wastewaters
Mineralogical Magazine, October 1, 2001; 65(5): 611 - 620.
[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 © 1991 by the Soil Science Society of America.