Nitrogen Content in Floodwater of Drill-Seeded, Delayed Flood Rice Following Urea Fertilization.

Monday, February 2, 2009: 11:00 AM
Westin Peachtree Plaza, International Room C
Alice J. Enochs1, Trenton L. Roberts1, Nathan A. Slaton1, Richard J. Norman2, Charles E. Wilson Jr.3, Donna Frizzell3 and James Branson3, (1)University of Arkansas, Fayetteville, AR
(2)Crop, Soil, and Environmental Sciences, University of Arkansas, Fayetteville, AR
(3)Rice Research & Extension Center, University of Arkansas, Stuttgart, AR
Nitrogen (N) fertilizer has the potential to enter surface waters via runoff from rice [Oryza sativa (L.)] fields.  This study was conducted to determine the days after fertilizing with urea that floodwater should be held to minimize N loss via runoff.  The effects of fertilizer N rate, fertilizer N application time, and floodwater temperature on the extent and persistence of urea, ammonium, and nitrate in rice floodwater were examined with a dry-seeded, delayed flood cultural system at Stuttgart, AR on a Dewitt silt loam (fine, smectic, thermic Typic Albaqualf).  Preflood N fertilizer persisted in the floodwater for more than one week after application and flooding, while midseason N fertilizer remained for 5 days.  Increased N fertilizer rate and decreased floodwater temperature appears to lengthen the persistence of N in rice floodwater.  Recommendations regarding the length of time floodwater should be held after fertilization with urea may need to account for these factors.