Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Vadose Zone Journal Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
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 Derby, N. E.
Right arrow Articles by Knighton, R. E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

ORIGINAL RESEARCH

Long-Term Observations of Vadose Zone and Groundwater Nitrate Concentrations under Irrigated Agriculture

Nathan E. Derbya,*, Francis X. M. Caseya and Raymond E. Knightonb

a Dep. of Soil Science, North Dakota State Univ., Fargo, ND 58105-5638
b USDA-CSREES, Washington, DC 20250

Correspondence: * Corresponding author (nathan.derby{at}ndsu.edu).

Received for publication 1 October 2007. Proper N management for agricultural production is critical to minimize groundwater contamination with NO3. For 18 yr, research was conducted to observe NO3–N concentrations in the vadose zone, groundwater, and subsurface drainage under sprinkler-irrigated, primarily corn (Zea mays L.) production. Potato (Solanum tuberosum L.) and soybean [Glycine max (L.) Merr.] were also grown intermittently on the site. The lysimeter leachate NO3–N concentration increased to 156 mg L–1 under corn production within 1 yr after the initiation of irrigation (at the onset of the study), then decreased to <10 mg L–1 during a 6-yr period of best-management N fertility management for corn. The average yearly lysimeter NO3–N concentration fluctuated between 8 and 117 mg L–1 during the study. Nitrate concentrations in the shallow groundwater followed a similar time series trend as leachate concentrations, but with lower concentrations and lagging about 1 yr. Subsurface drainage NO3–N concentrations were much lower but followed the same trend as the shallow groundwater. An N balance indicated higher net N mineralization after the initiation of irrigation and the years after potato production. Fertilizer N application rates and yearly weather conditions, which affected crop vigor and N uptake, combined to affect the fall residual soil NO3. Fall soil NO3 from 0- to 1.8-m depth was the most significant factor influencing the leachate NO3–N concentration each year during the study (r2 = 0.76).

Abbreviations: GDD, growing degree days • NBAL, nitrogen balance







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Soil Science Society of America