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Cooperative Forest Ecosystem Research
Nitrogen Dynamics across Gaps in Young, Thinned Forests of the Density Management Study
Primary Researchers: Aaron Thiel and Steven Perakis
Nitrogen (N) availability in soils plays a critical role in forest dynamics and development. Variations in N availability have been shown to affect tree growth and structural development, decay and turnover of leaves and woody detritus, diversity of understory and soil microbial communities, and many other factors. Consequently, understanding the spatial and temporal dynamics of N in forest soils can be crucial to understanding forest ecosystems as a whole.

The impacts of traditional silvicultural practices on N dynamics have historically been the subject of intense study. Clearcut forest harvest, for instance, has been shown to increase the production of nitrate (NO3-), a highly soluble ion, in forest soils. Subsequent N loss through NO3- leaching may lead to decreased site productivity and water quality levels. The potential impacts of modern silvicultural practices on soil N dynamics, as might result during gap creation to restore complex forest structure, remain less well understood.

The following study will investigate the effects of gap creation on N dynamics in young, thinned Douglas-fir forests. It will focus on three main questions::

How do pools and cycling of plant-available N in soils vary across gaps and into the adjacent forest matrix?
  Does gap size affect the magnitude of these differences?
  What factors (e.g., quantity and quality of litter input, soil moisture, etc.) can explain dynamics of plant-available N in silviculturally created gaps?
   

The study will include three initial thinning sites from the BLM Density Management Study. At each site, three large (0.4-ha) gaps and three small (0.1-ha) gaps will be chosen for study. A series of field- and laboratory-based measures will be used to measure N dynamics across gaps.

For additional information about this research study, see the 2005 CFER Annual Report.

Litter inputs and decomposition rates will be assessed on a monthly basis from October 2005 to September 2006. Mineral N, soil moisture, and microbial C and N of forest floor and mineral soil will be measured in January 2005, May 2006, and August 2006 to coincide with the beginning of three 28-day in situ incubation events. Ion exchange resins will incubate in mineral soil in 3-month intervals from October 2005 to September 2006. Lab inclubation of forest floor and mineral soil will occur in March 2006.


  


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