Importance of within-lake processes in affecting the dynamics of dissolved organic carbon and dissolved organic and inorganic nitrogen in an Adirondack forested lake/watershed

被引:10
|
作者
Kang, Phil-Goo [1 ,2 ]
Mitchell, Myron J. [1 ]
McHale, Patrick J. [1 ]
Driscoll, Charles T. [3 ]
Inamdar, Shreeram [4 ]
Park, Ji-Hyung [5 ]
机构
[1] SUNY Coll Environm Sci & Forestry, Syracuse, NY 13210 USA
[2] Natl Inst Environm Res, Res Strategy & Planning Div, Inchon 22689, South Korea
[3] Syracuse Univ, Dept Civil & Environm Engn, Syracuse, NY 13244 USA
[4] Univ Delaware, Dept Plant & Soil Sci, Newark, DE 19716 USA
[5] Ewha Womans Univ, Dept Environm Sci & Engn, Seoul 03760, South Korea
基金
美国国家科学基金会;
关键词
SURFACE-WATER CHEMISTRY; NEW-YORK; DOC FLUX; ATMOSPHERIC DEPOSITION; CLIMATE-CHANGE; EXPORT; MATTER; MOUNTAINS; REGION; BIOAVAILABILITY;
D O I
10.5194/bg-13-2787-2016
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Lakes nested in forested watersheds play an important role in mediating the concentrations and fluxes of dissolved organic matter. We compared long-term patterns of concentrations and fluxes of dissolved organic carbon (DOC) and dissolved organic (DON) and inorganic nitrogen (DIN) in aquatic ecosystems of the Arbutus Lake watershed to evaluate how a lake nested in a forested watershed affects the sources (e.g., production) and sinks (e.g., retention) of DOC and DON in the Adirondack Mountains of New York, USA. We observed no significant long-term changes of DOC and DON in the lake outlet since 1983 and 1994, respectively. However, the temporal patterns of DOC and DON concentrations in the lake inlet showed significant seasonality such as increases during the vegetation growing season along with notable decreases in the dormant season. A comparison of mass balances between inlet and outlet for the period from 2000 to 2009 suggested that the lake was a sink of DOC (mean of influx minus out flux: +1140 mol C ha(-1) yr(-1)). In contrast, the difference of discharge-weighted DON concentrations (mean of inlet minus outlet: 1.0 mu mol N L-1) between inlet and outlet was much smaller than the discharge-weighted DOC concentrations (average of inlet minus outlet: + 87 mu mol C L-1). DON fluxes showed considerable variation among years (mean of influx minus outflux: +8 mol N ha(-1) yr(-1); range of differences: -15 to 27 mol N ha(-1) yr(-1)). DON exhibited low percent retention ((influx-outflux)/influx) (mean: 6.9 %, range: 34.8 to +31.2) compared to DOC (mean: 30.1 %, range: +9.2 to +44.1). The resultant increase of DON within the lake was closely linked with a net decrease of DIN through monthly Pearson correlation analysis, suggesting the importance of biotic factors in mediating lake DON dynamics Our results show different relative retentions of DOC compared with DON, along with a larger retention of DIN than DON, suggesting that DOC and DON might display substantially different biogeochemical relationships in oligo-mesotrophic lakes nested forested watersheds and therefore different roles for a sink behavior for DOC compared to a producer of DON.
引用
收藏
页码:2787 / 2801
页数:15
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