JEQ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 7:580-588 (1978)
© 1978 American Society of Agronomy, Crop Science Society of America, and 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
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Tiedemann, A. R.
Right arrow Articles by Anderson, T. D.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Tiedemann, A. R.
Right arrow Articles by Anderson, T. D.
Agricola
Right arrow Articles by Tiedemann, A. R.
Right arrow Articles by Anderson, T. D.

Stream Chemistry and Watershed Nutrient Economy Following Wildfire and Fertilization in Eastern Washington1

A. R. Tiedemann, J. D. Helvey and T. D. Anderson2

ABSTRACT

During the first 3 years after a severe wildfire in 1970, maximum concentrations of nitrate-N (NO3-N) in stream water increased from prefire levels of <0.016 to 0.$6 mg/liter on a burned, unfertilized watershed and to 0.54 and 1.47 mg/liter on two watersheds that were burned and fertilized. Maximum NO3-N concentration in the stream from an unburned watershed was 0.066 mg/liter. Since NO3-N levels in the stream from the burned-only watershed were similar to burned-fertilized watersheds, increased levels appear to be primarily a result of increased nitrification. Organic N concentrations in streamflow were nearly doubled during the second year after fire compared to prefire levels.

Concentrations of total phosphorus (T-P) in streams from one burned and two burned-fertilized watersheds were 1.5 to 3 times greater than from an unburned watershed. Combined concentrations of Ca, Mg, K, and Na in streams prior to fire ranged from 12.0 to 14.9 mg/liter. Concentrations declined to 7.4–10.5 mg/liter in streams from burned and burned-fertilized watersheds during the second year after fire (1972) because of dilution resulting from increased discharge and were still less in 1975 than prefire levels (8.4 to 12.7 mg/liter).

Average inputs of N, P, and the four cations during the 5 years of study were 1.23, 0, and 3.56 kg/ha per year. Yearly N input from precipitation was sufficient to balance solution losses in three of the five postfire years. Cation losses in solution greatly exceeded precipitation inputs in all years.

Relative to background conditions and levels observed in the control stream, the fire exerted protracted impacts on the chemistry of these streams. Results however, indicate that fire and fertilization exerted negligible effects on chemical water quality for municipal use.

Key Words: streams • forest fire effects • fertilization (plants) urea • ammonium sulfate • nutrients (plants)


NOTES

1 Contribution from USDA For. Serv., Pacific Northwest For. and Range Exp. Stn., Forest Hydrology Lab., Wenatchee, WA 98801.

2 Principal Range Scientist, Principal Hydrologist, and Chemist, respectively.

Received for publication October 12, 1977.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Copyright © 1978 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.