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


     


Published online 29 June 2009
Published in Soil Sci Soc Am J 73:1393-1407 (2009)
DOI: 10.2136/sssaj2007.0432
© 2009 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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
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
Google Scholar
Right arrow Articles by Larsen, I. J.
Right arrow Articles by Schaffrath, K.
PubMed
Right arrow Articles by Larsen, I. J.
Right arrow Articles by Schaffrath, K.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Larsen, I. J.
Right arrow Articles by Schaffrath, K.
Related Collections
Right arrow Soil Erosion
Right arrow Fire
Right arrow Runoff

FOREST, RANGE & WILDLAND SOILS

Causes of Post-Fire Runoff and Erosion: Water Repellency, Cover, or Soil Sealing?

Isaac J. Larsena,*, Lee H. MacDonalda, Ethan Browna, Daniella Rougha, Matthew J. Welsha, Joseph H. Pietraszekb, Zamir Libohovac, Juan de Dios Benavides-Soloriod and Keelin Schaffratha

a Dep. of Forest, Rangeland, and Watershed Stewardship, Colorado State Univ., Fort Collins, CO 80523
b Golder Associates Inc., 18300 NE Union Hill Rd., Suite 200, Redmond, WA 98052
c Dep. of Agronomy, Purdue Univ., West Lafayette, IN 47907
d INIFAP, Centro Regional de Investigación del Pacifico Centro, Parque Los Colomos s/n, Guadalajara, Jalisco 44660, Mexico

* Corresponding author (larseni{at}u.washington.edu).

Few studies have attempted to isolate the various factors that may cause the observed increases in peak flows and erosion after high-severity wildfires. This study evaluated the effects of burning by: (i) comparing soil water repellency, surface cover, and sediment yields from severely burned hillslopes, unburned hillslopes, and hillslopes where the surface cover was removed by raking; and (ii) conducting rainfall simulations to compare runoff, erosion, and surface sealing from two soils with varying ash cover. The fire-enhanced soil water repellency was only stronger on the burned hillslopes than the unburned hillslopes in the first summer after burning. For the first 5 yr after burning, the mean sediment yield from the burned hillslopes was 32 Mg ha–1, whereas the unburned hillslopes generated almost no sediment. Sediment yields from the raked and burned hillslopes were indistinguishable when they had comparable surface cover, rainfall erosivity, and soil water repellency values. The rainfall simulations on ash-covered plots generated only 21 to 49% as much runoff and 42 to 67% as much sediment as the plots with no ash cover. Soil thin sections showed that the bare plots rapidly developed a structural soil seal. Successive simulations quickly eroded the ash cover and increased runoff and sediment yields to the levels observed from the bare plots. The results indicate that: (i) post-fire sediment yields were primarily due to the loss of surface cover rather than fire-enhanced soil water repellency; (ii) surface cover is important because it inhibits soil sealing; and (iii) ash temporarily prevents soil sealing and reduces post-fire runoff and sediment yields.

Abbreviations: CEC, cation exchange capacity • CST, critical surface tension







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 © 2009 by the Soil Science Society of America.