2.2

Long term consequences of a controlled slash burn and slash mastication to soil moisture and CO₂ at a southern Colorado site

William J. Massman, US Forest Service, Fort Collins, CO; and J. M. Frank, A. E. Jimenez Esquilin, M. E. Stromberger, and W. D. Shepperd

Thinning of forest stands is frequently used to reduce the risk of catastrophic fire. But thinning requires that the refuse (or slash) be removed from the site, which can be done either by burning it or by mastication and dispersal. Either method has long term consequences to the soil and to soil moisture and soil CO₂ levels. This study presents 2+ years of continuous soil moisture and CO₂ measurements at two experimental slash treatment sites within Manitou Experimental Forest in the Rocky Mountains of southern Colorado: (i) a controlled burn site and (ii) a site at which the slash was masticated and dispersed. Each experimental site has a separate control plot (with no treatment). The instrumentation was installed before each treatment (either burning or mastication). In the case of the controlled burn the soil moisture sensors had to (and did) survive temperatures exceeding 200 C. The results suggest that:

(1) The burn area tends to have higher soil moisture and lower concentrations of CO₂ than the control site. This result is consistent with the loss of plant cover, roots, and microbial biomass at the burn site, which would reduce transpiration and root and microbial respiration. This difference between treatments reaches its maximum during the late summer of 2005, approximately a year and a half after the burn, when the volumetric soil moisture at the control site is only about half of that at the burn site. As a consequence of this depletion of soil moisture at the control site, the normal gradient of CO₂ (for which CO₂ increases with depth) is virtually eliminated yielding similar and relatively low concentrations at 0.05 and 0.15 m. But the burn site appears to have sufficient moisture at the lower depth for microbial respiration to continue at levels sufficient to maintain the soil CO₂ gradient and relatively greater amounts of CO₂.

(2) Relative to the control area, the areas covered by the masticated wood chips tend to have higher soil moisture at 0.15 m depth and relatively less soil moisture at 0.05 m, and considerably higher CO₂ concentrations at both depths. This is consistent with the expectation that a layer of wood chips act as a barrier to precipitation (reducing the soil moisture at the upper level) and to the diffusional loss of water vapor (at the lower level) and the loss of CO₂ (at all levels). In addition, the chips can apparently have unusual effects on the production of soil CO₂. During mid through late March 2005 the amount of CO₂ at 0.05 m soil depth at the chip-covered areas increased from a relatively constant 2500 ppm to about 10,000 ppm. The amounts of CO₂ increased at lower depths as well, but by lesser amounts. However, the increase at 0.05 m was enough to reverse the usual soil CO₂ gradient. Although the control area had higher soil moisture at this time than the chip site, it showed no significant change in the amount of CO₂ or the CO₂ gradient.

  Extended Abstract (964K)

  Recorded presentation

Session 2, local micro-climates
Monday, 22 May 2006, 3:30 PM-5:00 PM, Rousseau Suite

Previous paper  Next paper

Browse or search entire meeting

AMS Home Page