Spatially-integrated estimates of net ecosystem exchange and methane fluxes from Canadian peatlands.

BACKGROUND: Peatlands are an important component of Canada's landscape, however there is little information on their national-scale net emissions of carbon dioxide [Net Ecosystem Exchange (NEE)] and methane (CH4). This study compiled results for peatland NEE and CH4 emissions from chamber and eddy covariance studies across Canada. The data were summarized by bog, poor fen and rich-intermediate fen categories for the seven major peatland containing terrestrial ecozones (Atlantic Maritime, Mixedwood Plains, Boreal Shield, Boreal Plains, Hudson Plains, Taiga Shield, Taiga Plains) that comprise > 96% of all peatlands nationally. Reports of multiple years of data from a single site were averaged and different microforms (e.g., hummock or hollow) within these peatland types were kept separate. A new peatlands map was created from forest composition and structure information that distinguishes bog from rich and poor fen. National Forest Inventory k-NN forest structure maps, bioclimatic variables (mean diurnal range and seasonality of temperatures) and ground surface slope were used to construct the new map. The Earth Observation for Sustainable Development map of wetlands was used to identify open peatlands with minor tree cover. RESULTS: The new map was combined with averages of observed NEE and CH4 emissions to estimate a growing season integrated NEE (± SE) at - 108.8 (± 41.3) Mt CO2 season-1 and CH4 emission at 4.1 (± 1.5) Mt CH4 season-1 for the seven ecozones. Converting CH4 to CO2 equivalent (CO2e; Global Warming Potential of 25 over 100 years) resulted in a total net sink of - 7.0 (± 77.6) Mt CO2e season-1 for Canada. Boreal Plains peatlands contributed most to the NEE sink due to high CO2 uptake rates and large peatland areas, while Boreal Shield peatlands contributed most to CH4 emissions due to moderate emission rates and large peatland areas. Assuming a winter CO2 emission of 0.9 g CO2 m-2 day-1 creates an annual CO2 source (24.2 Mt CO2 year-1) and assuming a winter CH4 emission of 7 mg CH4 m-2 day-1 inflates the total net source to 151.8 Mt CO2e year-1. CONCLUSIONS: This analysis improves upon previous basic, aspatial estimates and discusses the potential sources of the high uncertainty in spatially integrated fluxes, indicating a need for continued monitoring and refined maps of peatland distribution for national carbon and greenhouse gas flux estimation.

Is there synchronicity in nitrogen input and output fluxes at the Noland Divide Watershed, a small N-saturated forested catchment in the Great Smoky Mountains National Park?

High-elevation red spruce [Picea rubens Sarg.]-Fraser fir [Abies fraseri (Pursh.) Poir] forests in the Southern Appalachians currently receive large nitrogen (N) inputs via atmospheric deposition (30 kg N ha(-1) year(-1)) but have limited N retention capacity due to a combination of stand age, heavy fir mortality caused by exotic insect infestations, and numerous gaps caused by windfalls and ice storms. This study examined the magnitude and timing of the N fluxes into, through, and out of a small, first-order catchment in the Great Smoky Mountains National Park. It also examined the role of climatic conditions in causing interannual variations in the N output signal. About half of the atmospheric N input was exported annually in the streamwater, primarily as nitrate (NO3-N). While most incoming ammonium (NH4-N) was retained in the canopy and the forest floor, the NO3-N fluxes were very dynamic in space as well as in time. There was a clear decoupling between NO3-N input and output fluxes. Atmospheric N input was greatest in the growing season while largest NO3-N losses typically occurred in the dormant season. Also, as water passed through the various catchment compartments, the NO3-N flux declined below the canopy, increased in the upper soil due to internal N mineralization and nitrification, and declined again deeper in the mineral soil due to plant uptake and microbial processing. Temperature control on N production and hydrologic control on NO3-N leaching during the growing season likely caused the observed inter-annual variation in fall peak NO3-N concentrations and N discharge rates in the stream.

Mode-medium instability and its correction with a Gaussian-reflectivity mirror.

A high-power CO(2) laser beam is known to deteriorate after a few microseconds because of a mode-medium instability (MMI) that results from an intensity-dependent heating rate that is related to the vibrationalto-translational decay of the upper and lower CO(2) lasing levels. An iterative numerical technique has been developed to model the time evolution of the beam as it is affected by the MMI. The technique is used to study the MMI in an unstable CO(2) resonator with a hard-edge output mirror for different parameters, e.g., the Fresnel number and the gas density. The results show that the mode of the hard-edge unstable resonator deteriorates because of the diffraction ripples in the mode. We use a Gaussian-reflectivity mirror to correct the MMI. This mirror produces a smoother intensity profile, which significantly reduces the effects of the MMI. Quantitative results on the peak density variation and beam quality are presented.

Complications of muscle-flap transposition for traumatic defects of the leg.

A careful study of 95 consecutive muscle-flap procedures performed on 71 patients with traumatic soft-tissue defects of the leg was carried out. Although there were only 5 cases of total muscle-flap necrosis, major and minor complications were found in 31 patients, requiring additional surgery for coverage. Technical errors resulted in partial split-thickness skin-graft loss or hematoma and were responsible for the 10 minor complications. Inadequate debridement of necrotic soft tissue and bone, the use of diseased or traumatized muscle, and unrealistic objectives for the muscle-flap coverage were the source of 21 major complications. We feel fewer complications would result with more careful preoperative evaluation and surgical planning, adequate debridement of bone and soft tissue, and the transfer of healthy, nontraumatized muscle.