Spatial and Temporal Distributions in Sandy Soils with Seepage Irrigation: I. Ammonium and Nitrate

Tomato (Lycopersicon esculentum Mill.) in southwest Florida is typically grown on fumigated, raised beds with polyethylene mulch under seepage irrigation. An average grower's N rate currently exceeds the University of Florida's Institute of Food and Agricultural Sciences (UF-IFAS) recommen...

Full description

Saved in:
Bibliographic Details
Published inSoil Science Society of America journal Vol. 73; no. 3; pp. 1044 - 1052
Main Authors Sato, Shinjiro, Morgan, Kelly T, Ozores-Hampton, Monica, Simonne, Eric H
Format Journal Article
LanguageEnglish
Published Madison Soil Science Society 01.05.2009
Soil Science Society of America
American Society of Agronomy
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Tomato (Lycopersicon esculentum Mill.) in southwest Florida is typically grown on fumigated, raised beds with polyethylene mulch under seepage irrigation. An average grower's N rate currently exceeds the University of Florida's Institute of Food and Agricultural Sciences (UF-IFAS) recommendation (224 kg N ha-1 maximum). Excess nutrients are subject to runoff and leaching, which raises environmental concerns in Florida watersheds. A field study was conducted to elucidate N spatial distribution in tomato beds during the 2006 spring and winter growing seasons with 224 and 358 kg N ha-1 rates. Ammonium N was highest for both seasons during 0 to 1 wk after planting (WAP) at the 0- to 10-cm depth in the fertilizer band, but rarely moved vertically. Lateral movement of NH4+-N was observed through 7 WAP, however, probably due to diffusion. Nitrate N at 0 to 10 cm in the band peaked during 3 to 4 WAP, indicating about 3 wk of nitrification in the spring; however, this process was shortened to 1 to 2 wk in the winter, probably due to greater bacterial activity with warmer temperatures in the beginning of the winter than the spring (average 8°C in the first 3 wk). Both lateral and vertical movements of NO3(-)-N were observed in the spring, even at the 20- to 30-cm depth. A rise and subsequent fall of the water table level during 5 to 8 WAP particularly enhanced NO3(-)-N downward movement, which was attributed to greater diffusivity of NO3(-)-N than NH4+-N. Minimizing water table fluctuations and applying a reduced N rate are critical to reduce NO3(-)-N leaching loss.
Bibliography:http://dx.doi.org/10.2136/sssaj2008.0206
All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. Permission for printing and for reprinting the material contained herein has been obtained by the publisher.
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 14
ObjectType-Article-2
content type line 23
ObjectType-Article-1
ObjectType-Feature-2
ISSN:0361-5995
1435-0661
DOI:10.2136/sssaj2008.0206