SSSAJ Journal of Natural Resources and Life Sciences Education
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 (15)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Akhtar, M. S.
Right arrow Articles by Steenhuis, T. S.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Akhtar, M. S.
Right arrow Articles by Steenhuis, T. S.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Akhtar, M. S.
Right arrow Articles by Steenhuis, T. S.
Related Collections
Right arrow Vadose Zone Processes and Chemical Transport
Right arrow Nutrients
Right arrow Phosphorus
Soil Science Society of America Journal 67:458-470 (2003)
© 2003 Soil Science Society of America

DIVISION S-1—SOIL PHYSICS

Dissolved Phosphorus from Undisturbed Soil Cores

Related to Adsorption Strength, Flow Rate, or Soil Structure?

M. Saleem Akhtar{dagger}, Brian K. Richards, Pedro A. Medrano, Maarten deGroot and Tammo S. Steenhuis*

Dep. Bio. and Env. Eng., Cornell Univ., Ithaca, NY 14853

* Corresponding author (tss1{at}cornell.edu)

While the rapid transport of nonadsorbed chemicals is relatively well understood, preferential transport of adsorbable chemicals including P requires further study. Our objective was to characterize subsurface P transport in glaciated soils of the northeastern USA. Large intact columns from five soils with differing structures were subjected in duplicate to both synthetic acid rainfall at a low rate simulating natural rainfall, and ponded water for observing saturated flow. The rain was enriched with inorganic and organic P after baseline conditions were established. Drainage water P concentrations were measured and adsorption isotherms were determined. Type of flow was characterized using Cl breakthrough curves and visualizations of blue dye patterns. Baseline P concentrations in drainage water were 0.02 to 0.04 mg L-1. At low flow rates, P appeared in the drainage water soon after application of either inorganic or organic P for the silt loam soil (firm, moderate coarse prismatic parting to moderate medium subangular blocky structure) in which preferential flow paths carried most of the water flow. In contrast, the soils in which matrix type flow dominated (weak fine granular or weak medium subangular blocky structures) had little or no increase in drainage water P. However, under ponded conditions all soils exhibited preferential flow and rapid P breakthrough. Elevated P concentration in the drainage water could not be explained by the P adsorption strength with the possible exception of the sandy loam soil, where the outflow P concentration was consistently low. Variation in flow rate in conjunction with soil structure satisfactorily explained elevated concentrations of dissolved inorganic and organic P in drainage water from surface applied P.

Abbreviations: DOC, dissolved organic C




This article has been cited by other articles:


Home page
J. Environ. Qual.Home page
E. O. Young and R. D. Briggs
Phosphorus Concentrations in Soil and Subsurface Water: A Field Study among Cropland and Riparian Buffers
J. Environ. Qual., January 4, 2008; 37(1): 69 - 78.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
M. Mamo, S. C. Gupta, C. J. Rosen, and U. B. Singh
Phosphorus Leaching at Cold Temperatures as Affected by Wastewater Application and Soil Phosphorus Levels
J. Environ. Qual., June 7, 2005; 34(4): 1243 - 1250.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
Y.-J. Kim, C. J. G. Darnault, N. O. Bailey, J.-Y. Parlange, and T. S. Steenhuis
Equation for Describing Solute Transport in Field Soils with Preferential Flow Paths
Soil Sci. Soc. Am. J., March 1, 2005; 69(2): 291 - 300.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
L. Day
Septic Systems as Potential Pollution Sources in the Cannonsville Reservoir Watershed, New York
J. Environ. Qual., November 1, 2004; 33(6): 1989 - 1996.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
M. A. Saleque, U. A. Naher, A. Islam, A. B. M. B. U. Pathan, A. T. M. S. Hossain, and C. A. Meisner
Inorganic and Organic Phosphorus Fertilizer Effects on the Phosphorus Fractionation in Wetland Rice Soils
Soil Sci. Soc. Am. J., September 1, 2004; 68(5): 1635 - 1644.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
J. Lilienfein, R. G. Qualls, S. M. Uselman, and S. D. Bridgham
Adsorption of Dissolved Organic and Inorganic Phosphorus in Soils of a Weathering Chronosequence
Soil Sci. Soc. Am. J., March 1, 2004; 68(2): 620 - 628.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
M. S. Akhtar, M. S. Akhtar, T. S. Steenhuis, B. K. Richards, and M. B. McBride
Chloride and Lithium Transport in Large Arrays of Undisturbed Silt Loam and Sandy Loam Soil Columns
Vadose Zone J., November 1, 2003; 2(4): 715 - 727.
[Abstract] [Full Text] [PDF]




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
Journal of
Environmental Quality
Copyright © 2003 by the Soil Science Society of America.