ISSN:
1573-2932
Keywords:
nitrogen
;
wet deposition
Source:
Springer Online Journal Archives 1860-2000
Topics:
Energy, Environment Protection, Nuclear Power Engineering
Notes:
Abstract We measured concentrations and fluxesof major ions in wet deposition, throughfall andstream water in a forested watershed on the AlleghenyPlateau of western Maryland to investigatecanopy-atmosphere interactions and to calculate input–output budgets. Wet deposition was dominated byH+, SO 4 2− , NO 3 − andNH 4 + ions. Hydrogen and SO 4 2− accounted for 70 and 58% of the total cation andanion equivalents, respectively. Annual wet depositionrates of SO 4 2− (0.56 keq ha−1 yr−1), NO 3 − (0.31 keq ha−1 yr −1)and NH 4 + (0.17 keq ha−1 yr −1)were at the high end of the range in wet depositionrates reported for other sites in the eastern UnitedStates. On an annual basis, the forest canopy consumed20% of the free acidity in incident precipitation,had no net effect on Na+ and NH 4 + deposition, and was a net source of K+,Ca2+, Mg2+, SO 4 2− andNO 3 − ; 1.5 to 22 times greater than the wetdeposition rates. On an annual basis, the watershed ofthe unnamed tributary to Herrington Creek (HCWS)retained essentially all of the throughfall H+ andNH 4 + inputs, 35% of the throughfall K+input and 62% of the throughfall NO 3 − input. In contrast, HCWS was a net source ofSO 4 2− , Cl−, Ca2+, Mg2+ andNa+; export rates were 2 to 5 times greater thanthroughfall inputs. Sulfate was the dominant anionassociated with cation leaching, accounting for 78%of the total anion export of 1.8 keq ha−1 yr −1 in 1996–1997.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1023/A:1005113426448
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