scholarly journals Trends in lake chemistry in response to atmospheric deposition and climate in selected Class I wilderness areas in Colorado, Idaho, Utah, and Wyoming, 1993-2009

Author(s):  
Alisa Mast ◽  
George P. Ingersoll
2010 ◽  
Vol 103 (1-3) ◽  
pp. 27-43 ◽  
Author(s):  
M. Alisa Mast ◽  
John T. Turk ◽  
David W. Clow ◽  
Donald H. Campbell

2016 ◽  
Author(s):  
Alison C. Dibble ◽  
James W. Hinds ◽  
Ralph Perron ◽  
Natalie Cleavitt ◽  
Richard L. Poirot ◽  
...  

1987 ◽  
Vol 22 (3) ◽  
pp. 365-376
Author(s):  
C. H. Chan ◽  
L. H. Perkins

Abstract Wet deposition estimates were computed from monthly wet precipitation samples collected in the Lake Superior Basin. Sulphate and nitrogen loadings from wet precipitation corresponded to 142 and 40 thousand tonnes per year. On a percentage basis, wet deposition of sulphate and nitrogen accounted for 21% and 54%, respectively, of the total load. Atmospheric sources for other major ions ranged from 1 to 10%. Atmospheric deposition at the eastern end of Lake Superior was higher than the western end of the Basin. The relative accuracy of these estimates were examined in relation to the changes in lake chemistry in Lake Superior from 1973 to 1983.


2021 ◽  
Vol 758 ◽  
pp. 143639 ◽  
Author(s):  
Charles Marty ◽  
Louis Duchesne ◽  
Suzanne Couture ◽  
Christian Gagnon ◽  
Daniel Houle

1989 ◽  
Author(s):  
Douglas G. Fox ◽  
Ann M. Bartuska ◽  
James G. Byrne ◽  
Ellis Cowling ◽  
Richard Fisher ◽  
...  

1988 ◽  
Vol 45 (S1) ◽  
pp. s38-s46 ◽  
Author(s):  
R. G. Semkin ◽  
D. S. Jeffries

Bulk and wet-only deposition and the snowpack were monitored at the Turkey Lakes Watershed in northern Ontario over the winter and spring of 1986. Based on a comparison with snowpack and cumulative snowmelt, the bulk sampler overcollected major ions by factors ranging from 6 to 22%. Nitrate appeared to be preferentially collected by the bulk sampler relative to SO42− during snow events. Dry deposition was estimated to be 12 and 5% of total deposition forSO42− and NO3−, respectively. Ion budgets for cumulative bulk deposition and snowmelt supported the hypothesis that ion losses from the snowpack are insignificant during a winter having no melt episodes. Snowmelt was characterized by chemical fractionation of major ions; SO42− and H+ in initial meltwaters were 10 times more concentrated than the premelt snowpack. Preferential elution of ions in the snowmelt followed the sequence: SO42− > NO3− > H+ > Cl−. Snowmelt chemistry was used to predict changes in lake chemistry: H+, NO3−, and NH4+ levels should increase in lake waters; Ca2+ decreases through dilution by snowmelt; SO42− concentrations remain fairly constant.


2001 ◽  
Vol 1 ◽  
pp. 287-293 ◽  
Author(s):  
Mark W. Williams ◽  
Dave Manthorne

Between June 1, 2000 and September 30, 2000, 32 precipitation events were sampled near Telluride, CO at an elevation of 3200 m. The wet deposition site was operated following protocols of the Atmospheric Integrated Research Monitoring Network (AIRMoN), a network of the National Atmospheric Deposition Network (NADP). Inorganic nitrogen deposition at the Telluride site of 1.41 kg ha-1during the study period was 25 to 50% higher than nearby NADP sites. In turn, nitrogen deposition at these NADP sites was similar to high-elevation sites in and near the Colorado Front Range that have been shown to be impacted by atmospheric deposition of inorganic nitrogen in wetfall. Power plant emissions are a likely source of a major portion of this elevated inorganic nitrogen in wetfall to the San Juan Mountains. Principal component analysis (PCA) shows that solutes formed by gases that are emitted from power plants were clustered tightly together, including nitrate, ammonium, sulfate, and chloride. Trajectory analysis, including both backward and forward trajectories, shows that the air masses that contributed to the precipitation events with high amounts of nitrogen deposition at the Telluride site passed directly over or near power plants. Our results suggest that Class I Wilderness Areas in and near the San Juan Mountains are at risk to ecosystem impairment at present rates of atmospheric deposition of inorganic nitrogen in wetfall. Deployment of proposed power plants to this area will likely increase the risk of degradation of resource values in nearby Class I areas. While these data were collected over a short time span, they indicate that establishment of an official AIRMoN site in the southwestern U.S. may be warranted.


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