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 51:1033-1041 (1987)
© 1987 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Fisher, F. M.
Right arrow Articles by Whitford, W. G.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Fisher, F. M.
Right arrow Articles by Whitford, W. G.
Agricola
Right arrow Articles by Fisher, F. M.
Right arrow Articles by Whitford, W. G.

Nitrogen Mineralization in a Desert Soil: Interacting Effects of Soil Moisture and Nitrogen Fertilizer1

F. M. Fisher, L. W. Parker, J. P. Anderson and W. G. Whitford2

ABSTRACT

The responses of N mineralization to two patterns of supplemental water, N fertilizer, and a drying-wetting episode were examined in order to evaluate the effects of variation in timing and intensity of natural precipitation on N availability. Field plots received either 6 mm water/week or 25 mm water/month with or without 10 g N m–2. Samples were collected three times from July 1984 to March 1985 and incubated in the lab for 28 d. The effects of drought were simulated by drying soil at 35°C for 28 d followed by 168-d leaching incubations. Supplemental water reduced 28-d mineralization by 22% in soils collected during dry and moderate soil moisture conditions (July 1984, October 1984) but had no effect on soils collected during a moist period (March 1985). Nitrogen fertilizer had no effect on 28-d mineralization in soils from July but increased 28-d mineralization by 58% in soils from October and March. Air-drying increased mineralization rates across all field treatments during the first 14 d of the 168-d leaching incubations. Mineralization rates were lower in soils from watered plots in both the air-dry and field-moist treatments. Air-drying interacted with both the water and N treatments by increasing watering effects and decreasing fertilizer N effects. The observed drying effects appear to be a net result of several processes that, on the whole, tend to increase N availability. Mineralization rates in both experiments were lower in 6 mm/week soils than in 25 mm/month soils which, in turn, were lower than unwatered controls. We hypothesize that increased moisture availability eventually leads to losses of mineralizable N as initially rapid mineralization converts organic N to inorganic forms that are readily lost from the soil.


NOTES

1 Contribution from the Dep. of Biology and the Jornada LTER program, New Mexico State Univ., Las Cruces, NM 88003.

2 College Assistant Professor, former College Assistant Professor, Research Assistant, and Professor, respectively.

Received for publication October 24, 1986.


This article has been cited by other articles:


Home page
Soil Sci.Home page
H. Van Miegroet, M. T. Hysell, and A. D. Johnson
Soil Microclimate and Chemistry of Spruce-Fir Tree Islands in Northern Utah
Soil Sci. Soc. Am. J., July 1, 2000; 64(4): 1515 - 1525.
[Abstract] [Full Text]


Home page
ScienceHome page
W. H. Schlesinger, W. H. Schlesinger, J. F. Reynolds, G. L. Cunningham, L. F. Huenneke, W. M. Jarrell, R. A. Virginia, and W. G. Whitford
Biological Feedbacks in Global Desertification
Science, March 2, 1990; 247(4946): 1043 - 1048.
[Abstract] [PDF]




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 © 1987 by the Soil Science Society of America.