For decades, scientists and resource managers have known that wildfires affect forest soils, evidenced, in part, by the erosion that often occurs after a fire kills vegetation and disrupts soil structure. But, the lack of detailed knowledge of forest soils before they are burned by wildfire has hampered efforts to understand fire's effects on soil fertility and forest ecology.
A new study led by the Pacific Northwest (PNW) Research Station addresses this critical information gap and represents the first direct evidence of the toll wildfire can take on forest soil layers. It draws on data from the 2002 Biscuit Fire, which scorched some 500,000 acres in southwest Oregon, including half of a pre-existing study's experimental plots, which had been studied extensively before the fire. The result was a serendipitous and unprecedented opportunity to directly examine how wildfire changes soil by sampling soils before and after a wildfire.
"Losing our experiment in the fire was hard, but the opportunity to better understand fire as a dominant ecosystem process has been very exciting," said Bernard Bormann, a research forest ecologist with PNW Research Station and the study's lead investigator. "This study, covering over 300 acres, provided nearly 400 soil sampling points as well as extensive tree and understory plots to use in our analysis."
Bormann—along with study co-author and Western Washington University professor Peter Homann and colleagues from the PNW Research Station and Oregon State University—conducted chemical analyses on soil samples collected before and after the fire. They found that the combustion of the organic layer at the soil's surface, including woody debris, caused intense, 1,300 °F-plus temperatures, which, in turn, displaced considerable amounts of carbon and nitrogen from the underlying mineral soil layer and left mostly ash behind. What was more surprising to the researchers was how these organic materials may have been lost. Some carbon and nitrogen were lost as gases—consisting mostly of carbon dioxide, nitrogen dioxide, and water vapor—and some in an inch of fine mineral-soil particles, which disappeared and left behind a crust of rocks.
"Altogether, we documented losses of more than 10 tons per acre of carbon and between 450 to 620 pounds per acre of nitrogen," Bormann said. "The loss of topsoil and combustion of organic materials together led to losses that are higher than most previous estimates."
The loss of topsoil and carbon from soil can negatively affect a range of processes, Bormann said, including nutrient retention and water infiltration. In the absence of special nitrogen-fixing plants, which are capable of converting atmospheric nitrogen into nitrogen compounds for growth, losses of nitrogen in the order of what he and his colleagues documented would require at least a century to be reversed.
Equally disconcerting is the role these released organic materials might have on the atmosphere, especially in the face of a warming climate. The burning of soil by wildfire may contribute to global warming, in the short term, by releasing carbon as a greenhouse gas and, in the long term, by reducing soil productivity through losses of organic matter and nutrients. With less productive soils, Bormann said, a forest will not grow as quickly nor reabsorb as much carbon as before a burn—a process critical to mitigating the accumulation of atmospheric carbon, which traps heat in the atmosphere and can, thus, raise temperatures.
"Our findings suggest that forest managers should carefully consider the effects of wildfire on soils when planning to reduce fuels, suppress future fires, and help trees and habitat recover after fire," Bormann said.
The above story is based on materials provided by USDA Forest Service, Pacific Northwest Research Station. Note: Materials may be edited for content and length.
- Bernard T. Bormann, Peter S. Homann, Robyn L. Darbyshire, and Brett A. Morrissette. Intense forest wildfire sharply reduces mineral soil C and N: the first direct evidence. Canadian Journal of Forest Research, 38(11): 2771%u20132783 (2008) DOI: 10.1139/X08-136
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