Trends in hydrometeorological conditions and stream water organic carbon in boreal forested catchments

被引:108
|
作者
Sarkkola, Sakari [1 ]
Koivusalo, Harri [2 ]
Lauren, Ari [2 ]
Kortelainen, Pirkko [3 ]
Mattsson, Tuija [3 ]
Palviainen, Marjo [4 ]
Piirainen, Sirpa [2 ]
Starr, Mike [4 ]
Finer, Leena [2 ]
机构
[1] Finnish Forest Res Inst, Vantaa Res Unit, FI-01301 Vantaa, Finland
[2] Finnish Forest Res Inst, Joensuu Res Unit, FI-80101 Joensuu, Finland
[3] Finnish Environm Inst, FI-00251 Helsinki, Finland
[4] Univ Helsinki, Dept Forest Ecol, FI-00014 Helsinki, Finland
关键词
Catchment; Climate change; Dissolved organic carbon; Export; Forest; Runoff; Peatland; CLIMATE-CHANGE; ACID DEPOSITION; NORWAY SPRUCE; PEAT SOILS; EXPORT; PEATLANDS; LAKES; DOC; PHOSPHORUS; NITROGEN;
D O I
10.1016/j.scitotenv.2009.09.008
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Temporal trends in stream water total organic carbon (TOC) concentration and export were studied in 8 forested headwater catchments situated in eastern Finland. The Seasonal Kendall test was conducted to identify the trends and a mixed model regression analysis was used to describe how catchment characteristics and hydrometeorological variables (e.g. precipitation, air and stream water temperatures, and atmospheric deposition) related to the variation in the concentration and export of stream water TOC. The 8 catchments varied in size from 29 to 494 ha and in the proportion of peatland they contained, from 8 to 70%. Runoff and TOC concentration were monitored for 15-29 years (1979-2006). Trends and variation in TOC levels were analysed from annual and seasonal time series. Mean annual TOC concentration increased significantly in seven of the eight catchments. The trends were the strongest in spring and most apparent during the last decade of the study period. The slopes of the trends were generally smaller than the variation in TOC concentration between years and seasons and between catchments. The annual TOC export showed no clear trends and values were largely determined by the temporal variability in runoff. Annual runoff showed a decreasing trend in two of the eight catchments. Mean annual air and stream water temperatures showed increasing trends, most clearly seen in the summer and autumn series. According to our modeling results. stream water temperature, precipitation and peatland percentage were the most important variables explaining annual and most seasonal TOC concentrations. The atmospheric deposition of SO(4), NH(4), and NO(3) decreased significantly over the study period, but no significant link with TOC concentration was found. Precipitation was the main hydrometeorological driver of the TOC export. We concluded that stream water TOC concentrations and exports are mainly driven by catchment characteristics and hydrometeorological factors rather than trends in atmospheric acid deposition. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:92 / 101
页数:10
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