Regional patterns and local variability of dry and occult deposition strongly influence sulfate concentrations in Maine lakes
There is great uncertainty and large cost in making dry deposition measurements. The authors present evidence based on wet deposition, evapotranspiration, S storage in lake sediments, and sulfate concentrations in lakes and streams in Maine that the dry deposition flux of sulfur to drainage basins of lakes in Maine ranges from nearly 0% to more than 100% of wet deposition, even in small areas. The regional pattern of sulfate concentrations in Maine lakes is due to gradients in both wet and dry deposition and variation in evapotranspiration. Patterns are modified locally by lakes hydrologic type, elevation, vegetation, and terrestrial drainage basin aspect. (Copyright (c) 1988 Elsevier Science Publishers B.V.)
- Research Organization:
- Environmental Protection Agency, Corvallis, OR (United States). Environmental Research Lab.
- OSTI ID:
- 5624123
- Report Number(s):
- PB-92-136951/XAB
- Resource Relation:
- Other Information: Pub. in Science of the Total Environment 72, p183-196 1988. See also PB87-110409. Prepared in cooperation with Maine Univ. at Orono, and Western Washington Univ., Bellingham. Inst. for Watershed Studies. EPA/--600/J-92/013
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
01 COAL, LIGNITE, AND PEAT
LAKES
ACIDIFICATION
MAINE
WATER POLLUTION
STREAMS
SULFATES
ECOLOGICAL CONCENTRATION
ACID RAIN
AIR POLLUTION
AIR-WATER INTERACTIONS
EVAPORATION
HYDROLOGY
REGIONAL ANALYSIS
SEDIMENTS
TRANSPIRATION
ATMOSPHERIC PRECIPITATIONS
DEVELOPED COUNTRIES
NORTH AMERICA
OXYGEN COMPOUNDS
PHASE TRANSFORMATIONS
POLLUTION
RAIN
SULFUR COMPOUNDS
SURFACE WATERS
USA
540320* - Environment
Aquatic- Chemicals Monitoring & Transport- (1990-)
010900 - Coal
Lignite
& Peat- Environmental Aspects