Episodic acidification of small streams in the northeastern United States: Ionic controls of episodes

被引:104
作者
Wigington, PJ
DeWalle, DR
Murdoch, PS
Kretser, WA
Simonin, HA
VanSickle, J
Baker, JP
机构
[1] PENN STATE UNIV, SCH FOREST RESOURCES, UNIVERSITY PK, PA 16802 USA
[2] PENN STATE UNIV, ENVIRONM RESOURCES RES INST, UNIVERSITY PK, PA 16802 USA
[3] US GEOL SURVEY, ALBANY, NY 12201 USA
[4] NEW YORK STATE DEPT ENVIRONM CONSERVAT, ADIRONDACK LAKES SURVEY CORP, RAY BROOK, NY 12977 USA
[5] NEW YORK STATE DEPT ENVIRONM CONSERVAT, ROME, NY 13440 USA
[6] MANTECH ENVIRONM TECHNOL INC, ENVIRONM RES LAB, CORVALLIS, OR 97333 USA
关键词
Adirondack Mountains; base cations; Catskill Mountains; episodic acidification; hydrologic events; nitrogen; Northern Appalachian Plateau; organic acids; rainstorms; snow melt; streams; sulfate;
D O I
10.2307/2269378
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
As part of the Episodic Response Project (ERP), we intensively monitored discharge and stream chemistry of 13 streams located in the Northern Appalachian region of Pennsylvania and in the Catskill and Adirondack Mountains of New York from fall 1988 to spring 1990. The ERP clearly documented the occurrence of acidic episodes with minimum episodic pH less than or equal to 5 and inorganic monomeric Al (Al-im) concentrations > 150 mu g/L in at least two study streams in each region. Several streams consistently experienced episodes with maximum Al-im concentrations > 350 mu g/L. Acid neutralizing capacity (ANC) depressions resulted from complex interactions of multiple ions. Base cation decreases often made the most important contributions to ANC depressions during episodes. Organic acid pulses were also important contributors to ANC depressions in the Adirondack streams, and to a lesser extent, in the Catskill and Pennsylvania streams. Nitrate concentrations were low in the Pennsylvania streams, whereas the Catskill and Adirondack study streams had high NO3- concentrations and large episodic pulses (less than or equal to 54 mu eq/L). Most of the Pennsylvania study streams also frequently experienced episodic pulses of SO42- (less than or equal to 78 mu eq/L), whereas the Adirondack and Catskill streams did not. High baseline concentrations of SO42- (all three study areas) and NO3- (Adirondacks and Catskills) reduced episodic minimum ANC, even when these ions did not change during episodes. The ion changes that controlled the most severe episodes (lowest minimum episodic ANC) differed from the ion changes most important to smaller, more frequent episodes. Pulses of NO3- (Catskills and Adirondacks), SO42- (Pennsylvania), or organic acids became more important during major episodes. Overall, the behavior of streamwater SO42- and NO3- is an indicator that acidic deposition has contributed to the severity of episodes in the study streams.
引用
收藏
页码:389 / 407
页数:19
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