http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-2.xsd
Atmospheric input of nitrogen to the coastal region of southeastern Texas
xii, 96 leaves : illustrations, maps ; 28 cm.
(Galveston), concentrations of DIN and DON were
2 day-', respectively. These values were similar for DIN and
32.16︢3.4 limol I- I and II 81︢13 @Mol M-2 day- 1,
atmospheric nitrogen with sea-salt aerosol particles. Mean
came from the southern direction. In the coastal region
College Station were 35.31︢04.7 gmol 1-1 and 1312︢47 IIMOI M-
concentration and flux of DIN in College Station were
concentrations of DIN and DON from southern wind sectors (SE,
concentrations of most major ions in wet deposition
correlated with winds from the northwest. In contrast,
DIN, and DON in wet deposition samples collected in College
DON. The isotopic data of rain nitrate and ammonium showed
Houston and this enhanced nitrogen affected the concentration
inorganic nitrogen (DIN; NH4+, N03-), and dissolved organic
measured in College Station. Concentrations of major ions,
nitrogen (DON) were measured in rainwater collected at three
of nitrogen species in College Station rain when the air mass
respectively. The mean concentration and flux of DON in
S, SW, and W) were higher than those from northern wind
sampling sites (College Station, Houston, and Galveston,
sectors (NW, N, NE, and E). Anthropogenic sources
significantly affected by marine sources, which diluted
significantly contributed to atmospheric nitrogen over
Station depended on surface wind direction. High
Texas). Dry deposition rate of nitrogen species was also
that the surface wind direction was a significant factor