Abstract
Dry deposition of S was estimated for watershed-ecosystems of the Hubbard Brook Experimental Forest from 1964-65 through 1986-87. Two approaches, a regression analysis of bulk precipitation inputs and stream outputs and a mass-balance method, gave similar average values for Watershed 6 430 and 410 eq SO{sub 4}{sup =}/ha-yr, respectively, for this 23-year period. Dry deposition contributed about 37% of total S deposition, varying from 12% in 1964-65 to 61% in 1983-84. Long-term data from 'replicated' watershed-ecosystems showed that temporal variability in estimates of dry deposition was considerably greater than spatial (between watersheds) variability.
Likens, G E;
Eaton, J S;
[1]
Bormann, F H;
[2]
Hedin, L O;
[3]
Driscoll, C T
[4]
- Inst. of Ecosystem Studies, The New York Botanical Garden, NY (US)
- School of Forestry and Environmental Studies Yale Univ., New Haven, CT (US)
- Dept. of Biology, Yale Univ., New Haven, CT (US)
- Dept. of Civil and Environmental Engineering, Syracuse, NY (US)
Citation Formats
Likens, G E, Eaton, J S, Bormann, F H, Hedin, L O, and Driscoll, C T.
Dry deposition of sulfur: a 23-year record for the Hubbard Brook Forest ecosystem.
Sweden: N. p.,
1990.
Web.
doi:10.1034/j.1600-0889.1990.t01-3-00002.x.
Likens, G E, Eaton, J S, Bormann, F H, Hedin, L O, & Driscoll, C T.
Dry deposition of sulfur: a 23-year record for the Hubbard Brook Forest ecosystem.
Sweden.
https://doi.org/10.1034/j.1600-0889.1990.t01-3-00002.x
Likens, G E, Eaton, J S, Bormann, F H, Hedin, L O, and Driscoll, C T.
1990.
"Dry deposition of sulfur: a 23-year record for the Hubbard Brook Forest ecosystem."
Sweden.
https://doi.org/10.1034/j.1600-0889.1990.t01-3-00002.x.
@misc{etde_6799738,
title = {Dry deposition of sulfur: a 23-year record for the Hubbard Brook Forest ecosystem}
author = {Likens, G E, Eaton, J S, Bormann, F H, Hedin, L O, and Driscoll, C T}
abstractNote = {Dry deposition of S was estimated for watershed-ecosystems of the Hubbard Brook Experimental Forest from 1964-65 through 1986-87. Two approaches, a regression analysis of bulk precipitation inputs and stream outputs and a mass-balance method, gave similar average values for Watershed 6 430 and 410 eq SO{sub 4}{sup =}/ha-yr, respectively, for this 23-year period. Dry deposition contributed about 37% of total S deposition, varying from 12% in 1964-65 to 61% in 1983-84. Long-term data from 'replicated' watershed-ecosystems showed that temporal variability in estimates of dry deposition was considerably greater than spatial (between watersheds) variability.}
doi = {10.1034/j.1600-0889.1990.t01-3-00002.x}
journal = []
volume = {42B:4}
journal type = {AC}
place = {Sweden}
year = {1990}
month = {Jan}
}
title = {Dry deposition of sulfur: a 23-year record for the Hubbard Brook Forest ecosystem}
author = {Likens, G E, Eaton, J S, Bormann, F H, Hedin, L O, and Driscoll, C T}
abstractNote = {Dry deposition of S was estimated for watershed-ecosystems of the Hubbard Brook Experimental Forest from 1964-65 through 1986-87. Two approaches, a regression analysis of bulk precipitation inputs and stream outputs and a mass-balance method, gave similar average values for Watershed 6 430 and 410 eq SO{sub 4}{sup =}/ha-yr, respectively, for this 23-year period. Dry deposition contributed about 37% of total S deposition, varying from 12% in 1964-65 to 61% in 1983-84. Long-term data from 'replicated' watershed-ecosystems showed that temporal variability in estimates of dry deposition was considerably greater than spatial (between watersheds) variability.}
doi = {10.1034/j.1600-0889.1990.t01-3-00002.x}
journal = []
volume = {42B:4}
journal type = {AC}
place = {Sweden}
year = {1990}
month = {Jan}
}