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


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 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 ISI Web of Science (3)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Lilienfein, J.
Right arrow Articles by Bridgham, S. D.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Lilienfein, J.
Right arrow Articles by Bridgham, S. D.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Lilienfein, J.
Right arrow Articles by Bridgham, S. D.
Related Collections
Right arrow Phosphorus
Right arrow Sorption/Exchange
Right arrow Volcanic Soils
Published in Soil Sci. Soc. Am. J. 68:620-628 (2004).
© 2004 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

DIVISION S-7—FOREST & RANGE SOILS

Adsorption of Dissolved Organic and Inorganic Phosphorus in Soils of a Weathering Chronosequence

Juliane Lilienfeina, Robert G. Qualls*,a, Shauna M. Uselmana and Scott D. Bridghamb

a Dep. of Environmental and Resource Sciences, MS 370, Univ. of Nevada–Reno, Reno, NV 89557
b Ecology and Evolutionary Biology, Univ. of Oregon, Eugene, OR 97403

* Corresponding author (qualls{at}unr.edu).

Leaching of dissolved organic matter (DOM) and associated nutrients can be a significant loss from developing ecosystems. We studied how the adsorption of dissolved organic P (DOP) and PO4 changes during the development of young andesitic soils and determined which soil characteristics are responsible for these changes. We sampled 77, 255, 616, and about 1200+ yr-old andesitic soils at the 0- to 10-, 30- to 40-, and 140- to 150-cm soil depths and performed adsorption isotherm analyses that were described using a modified Langmuir (for DOP) or linear equation (for PO4). We also sampled soil solution at the 10- to 20-, 40-, and 150-cm soil depths during the main snow melt period in 2001 and 2002 and analyzed it for DOP and PO4. The ability of the soils to adsorb DOP and PO4 increased with soil age. Stepwise multiple regression analyses between the adsorption capacity for DOP, or the slope of the adsorption isotherm for PO4, and several soil parameters showed that allophane concentrations control the adsorption of DOP and PO4 in these soils. Tests of preferential adsorption of DOP vs. PO4 and DOC vs. DOP showed that the adsorption strength increased in the following order: DOC < DOP < PO4. The preferential adsorption of PO4 vs. DOP and DOP vs. DOC increased significantly with increasing soil development, whereas the soil depth did not have a consistent and significant effect. Significant correlations between the null-point adsorption of DOP or PO4 and field soil solution concentrations indicated that the results obtained in laboratory experiments were applicable to field conditions. Consequently, the tendency of DOP and PO4 to leach from these andesitic soils decreases as soils and ecosystem develop.

Abbreviations: DOC, dissolved organic C • DOM, dissolved organic matter • DON, dissolved organic N • DOP, dissolved organic P • SOC, soil organic C




This article has been cited by other articles:


Home page
J. Environ. Qual.Home page
K. W. Goyne, H.-J. Jun, S. H. Anderson, and P. P. Motavalli
Phosphorus and Nitrogen Sorption to Soils in the Presence of Poultry Litter-Derived Dissolved Organic Matter
J. Environ. Qual., January 4, 2008; 37(1): 154 - 163.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
B. Gjettermann, M. Styczen, S. Hansen, O. K. Borggaard, and H. C. B. Hansen
Sorption and Fractionation of Dissolved Organic Matter and Associated Phosphorus in Agricultural Soil
J. Environ. Qual., April 5, 2007; 36(3): 753 - 763.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
T. P. McGonigle, M. L. Chambers, and G. J. White
Enrichment over Time of Organic Carbon and Available Phosphorus in Semiarid Soil
Soil Sci. Soc. Am. J., August 25, 2005; 69(5): 1617 - 1626.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
Y. Jiao, W. H. Hendershot, and J. K. Whalen
Agricultural Practices Influence Dissolved Nutrients Leaching through Intact Soil Cores
Soil Sci. Soc. Am. J., November 1, 2004; 68(6): 2058 - 2068.
[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 © 2004 by the Soil Science Society of America.