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 44:559-565 (1980)
© 1980 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 Google Scholar
Google Scholar
Right arrow Articles by Savant, N. K.
Right arrow Articles by De Datta, S. K.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Savant, N. K.
Right arrow Articles by De Datta, S. K.
Agricola
Right arrow Articles by Savant, N. K.
Right arrow Articles by De Datta, S. K.

Movement and Distribution of Ammonium-N Following Deep Placement of Urea in a Wetland Rice Soil1

N. K. Savant and S. K. De Datta2

ABSTRACT

The vertical distribution of NH4+-N following subsurface placement of different forms of urea was studied in incubated, undisturbed wetland soil cores. For prilled urea, supergranule urea, and prilled urea in mudballs placed at the 10-cm depth, peak concentration of NH4+-N was near the placement site and decreased with time, whereas after placement of sulfurcoated urea (SCU-21) at the same depth, peak concentration of NH4+-N increased over a period of 4 weeks. With time, the NH4+-N tended to move downward more than upward from the placement sites, probably because of the mass flow of percolating water.

In another experiment, the movement and spatial distribution of NH4+-N were studied following application of 2-g supergranules of urea (SGU) and sulfur-coated supergranules of urea (SC-SGU) at a depth of 10 cm in transplanted and cultivated wetland fallow plots. After 2 weeks, NH4+-N concentration gradient for SGU was 1,850 to 32 µg N/cm3 wet soil, over a distance of 10–12 cm from the placement site. The corresponding gradient for SC-SGU was 287 to 32 µg N/cm3 wet soil, over a distance of 5–7 cm from its placement site. For SGU in transplanted plots, the concentration gradient decreased steadily through 8 weeks, whereas for SC-SGU it increased during the first 4 weeks and then decreased. The disappearance of NH4+-N with time and distance from the site of application is attributed to diffusive transport or convective transport, or both, and root-sink effect. The general movement of NH4+-N was downward > lateral > upward. The apparent benefits of deep placement of urea in a wetland rice soil are discussed.


NOTES

1 Contribution from the Dep. of Agronomy, The Int. Rice Res. Inst., Los Baños, Laguna, Philippines.

2 Postdoctoral Research Fellow and Head, respectively, Dep. of Agronomy, The Int. Rice Res. Inst., Los Baños, Laguna (mail address: P. O. Box 933, Manila), Philippines.

Received for publication July 16, 1979. Accepted for publication January 2, 1980.







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 © 1980 by the Soil Science Society of America.