In North America, anthropogenic activities such as fossil fuel combustion and high-intensity agriculture have increased the inputs of nitrogen oxides in the atmosphere far above natural, biogenic inputs. The effect of this excess N depends on how it is distributed through the environment. If fixed N is deposited as nitrate in forests, it may act as a "fertilizer", stimulating growth and thus enhancing carbon sequestration. But when accumulated deposition exceeds the nutritional needs of the ecosystem, nitrogen saturation may result. Soil fertility declines due to leaching of cations and thus, carbon uptake diminishes. The balance between fertilization and saturation depends on the spatial and temporal extent of nitrogen deposition.
NO, NO2, NO3
* rapid interconversion:
minutes to hours
= NOx, N2O5
|Measurements of nitrogen oxide concentrations and fluxes made at Harvard Forest are intended to quantify the deposition of nitrogen oxides and to examine the rates for oxidation and deposition of reactive nitrogen that are critical in controlling how far the influence of nitrogen oxide emission sources extends. Measurements made to date indicate that dry deposition of NOy to the Harvard Forest canopy is controlled by advection from source regions, vertical mixing, and chemical reaction. The input is about equally divided between wet and dry deposition depending on the amount of precipitation.Southwesterly winds bring air from the major urban areas along the mid-Atlantic coast, whereas northwesterly wind bring air from less populated regions of northern New England and Canada. As a result, southwesterly winds transport higher concentrations and fluxes of NOx and NOy than northwesterly winds. In the summer, aerodynamically rough forests intercept NOx and emit reactive hydrocarbons that accelerate the oxidation of NOx to rapidly depositing species. As a result, much of the NOx emitted by North America is retained by the region in the summer. This deposition leads to a summertime decrease in reactive nitrogen concentrations and fluxes relative to spring levels. Such results have been reported in Munger et al. 1996, and Munger et al. 1998.|
In addition to their role as a plant nutrient, nitrogen oxides are a major precursor for photochemical production of tropospheric ozone, a pollutant and greenhouse gas. Measurements at Harvard Forest are used to examine the interannual variability and trends in ozone production and background ozone concentrations.
The family of nitrogen oxide species is partitioned between active radicals (NOx, NO3), reservoir species (e.g., peroxyacetylnitrate PAN) which can convert back into NO2 and terminal species (HNO3, organic nitrates), which no longer contribute to photochemistry and are efficiently deposited. At low wintertime temperatures, PAN is stable and can be transported to the upper troposphere and remote regions. In the summer, however, the lifetime of PAN is short (few hours) so concentrations may remain low despite abundant photochemical radicals that promote PAN formation. Thus, temperature directly affects the partitioning of nitrogen oxides, which will in turn affect deposition.
Further measurements resolving key species are needed to distinguish the contributions due to direct NO2 deposition, HNO3 deposition and organic nitrate deposition. A dual Tunable Diode Laser Absorption Spectrometer (TDLAS) for eddy covariance flux measurements of NO2 and concentrations of HNO3 and NO2 has been operational since 1999 and a new CG/ECD for continuous measurement of PAN was installed in the spring of 2000. The combination of HNO3 and NO2 concentrations with existing measurements of O3, NOy, NO, PAN, hydrocarbons, tracers of anthropogenic emissions, and meteorological parameters at the site, will provide important new data on the speciation and removal mechanisms for reactive nitrogen in the troposphere and subsequently the photochemistry of ozone in both urban and rural air masses. Simultaneous NOy, NOx, PAN and CO data will allow us to distinguish PAN deposition (loss on NOy) from PAN decomposition (leads to NOx increase, no change in NOy). Because seasonal cycles of PAN loss and formation remain a major uncertainty in understanding atmospheric transport and N deposition, we plan to continue measurements of NOy speciation over several seasonal cycles and climactic variation. The addition of PAN and HNO3 measurements provides a comprehensive analysis of the reactive nitrogen at this site, allowing us to examine the diel and seasonal trends in concentrations to determine their production, deposition, and loss rates.
Data are available through our data exchange.
For more information, contact Bill Munger or Cassandra Volpe Horii.