Ganzlin Peter W, Gundale Michael J, Becknell Rachel E, Cleveland Cory C
Department of Ecosystem and Conservation Sciences, College of Forestry and Conservation, University of Montana, Missoula, Montana, 59812, USA.
Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå, 901 83, Sweden.
Ecol Appl. 2016 Jul;26(5):1503-1516. doi: 10.1002/15-1100.
Decades of fire suppression following extensive timber harvesting have left much of the forest in the intermountain western United States exceedingly dense, and forest restoration techniques (i.e., thinning and prescribed fire) are increasingly being used in an attempt to mitigate the effects of severe wildfire, to enhance tree growth and regeneration, and to stimulate soil nutrient cycling. While many of the short-term effects of forest restoration have been established, the long-term effects on soil biogeochemical and ecosystem processes are largely unknown. We assessed the effects of commonly used forest restoration treatments (thinning, burning, and thinning + burning) on nutrient cycling and other ecosystem processes 11 yr after restoration treatments were implemented in a ponderosa pine (Pinus ponderosa var. scopulorum)/Douglas fir (Pseudotsuga menziesii var. glauca) forest at the Lubrecht Fire and Fire Surrogates Study (FFS) site in western Montana, USA. Despite short-term (<3 yr) increases in soil inorganic nitrogen (N) pools and N cycling rates following prescribed fire, long-term soil N pools and N mineralization rates showed only subtle differences from untreated control plots. Similarly, despite a persistent positive correlation between fuels consumed in prescribed burns and several metrics of N cycling, variability in inorganic N pools decreased significantly since treatments were implemented, indicating a decline in N spatial heterogeneity through time. However, rates of net nitrification remain significantly higher in a thin + burn treatment relative to other treatments. Short-term declines in forest floor carbon (C) pools have persisted in the thin + burn treatment, but there were no significant long-term differences among treatments in extractable soil phosphorus (P). Finally, despite some short-term differences, long-term foliar nutrient concentrations, litter decomposition rates, and rates of free-living N fixation in the experimental plots were not different from control plots, suggesting nutrient cycles and ecosystem processes in temperate coniferous forests are resilient to disturbance following long periods of fire suppression. Overall, this study provides forest managers and policymakers valuable information showing that the effects of these commonly used restoration prescriptions on soil nutrient cycling are ephemeral and that use of repeated treatments (i.e., frequent fire) will be necessary to ensure continued restoration success.
在美国西部山间地区,大量木材采伐后数十年的火灾抑制使得许多森林变得极其茂密,如今森林恢复技术(即间伐和规定火烧)正越来越多地被用于减轻严重野火的影响、促进树木生长和更新以及刺激土壤养分循环。虽然森林恢复的许多短期影响已经明确,但对土壤生物地球化学和生态系统过程的长期影响在很大程度上仍不清楚。在美国蒙大拿州西部的卢布雷希特火灾与火灾替代研究(FFS)站点的黄松(西黄松变种)/花旗松(北美黄杉变种)森林中,我们评估了常用森林恢复处理措施(间伐、火烧以及间伐 + 火烧)在实施恢复处理11年后对养分循环和其他生态系统过程的影响。尽管规定火烧后土壤无机氮(N)库和氮循环速率在短期内(<3年)有所增加,但长期来看,土壤氮库和氮矿化速率与未处理的对照地块相比仅显示出细微差异。同样,尽管规定火烧消耗的燃料与氮循环的几个指标之间存在持续的正相关关系,但自实施处理以来,无机氮库的变异性显著降低,这表明氮的空间异质性随时间下降。然而,相对于其他处理,间伐 + 火烧处理的净硝化速率仍然显著更高。间伐 + 火烧处理中,林地碳(C)库的短期下降一直持续,但各处理间可提取土壤磷(P)没有显著的长期差异。最后,尽管存在一些短期差异,但实验地块的长期叶片养分浓度、凋落物分解速率和自由生活固氮速率与对照地块没有差异,这表明温带针叶林的养分循环和生态系统过程在长期火灾抑制后的干扰下具有恢复力。总体而言,本研究为森林管理者和政策制定者提供了有价值的信息,表明这些常用恢复措施对土壤养分循环的影响是短暂的,并且需要使用重复处理(即频繁火烧)来确保恢复的持续成功。