Fr. Hauer et Cn. Spencer, Phosphorus and nitrogen dynamics in streams associated with wildfire: A study of immediate and longterm effects, INT J WILDL, 8(4), 1998, pp. 183-198
Stream nutrient data were collected both during a wildfire and over a subse
quent five-year period. Sampling was from a series of paired watersheds loc
ated within and outside of the wildfire. Phosphorus and nitrogen concentrat
ions increased from 5 to 60 fold over background levels during the first fe
w days of the month-long wildfire with maximum recorded concentrations as h
igh as 135 mu g/L soluble reactive phosphorus, 261 mu g/L ammonium, and 61
mu g/L nitrate. Total phosphorus and total nitrogen during this same time p
eriod increased up to 206 mu g/L and 349 mu g/L, respectively. Nutrient con
centrations declined to background levels (<5-10 mu g/L) within a few weeks
after the fire. Over the following five years we observed dissolved nutrie
nt concentrations reaching >40 mu g/L soluble reactive phosphorus and >125
mu g/L nitrate in impacted streams, concentrations >5 fold over those obser
ved in control streams. In high gradient watersheds, all nutrients were eas
ily transported to the streams with most notable impact during the early ye
ars after the fire. In less steep terrain, soluble reactive phosphorus conc
entrations were significantly higher 3 to 5 years after the fire, which als
o corresponded to relatively high spring hydrographs. In contrast, nitrogen
compounds were observed to be significantly higher in concentration in fir
e impact streams in the years immediately following the fire. We attribute
these differences in the rate of nutrient loads to be the result of the dif
ferent mobilization mechanisms of phosphorus and nitrogen and the different
soil and geomorphic settings of the watersheds drained by the different st
reams.