Nitrogen retention by peatland buffer areas at six forested catchments in southern and central Finland

被引:29
|
作者
Vikman, Anu [1 ]
Sarkkola, Sakari [1 ]
Koivusalo, Harri [2 ]
Sallantaus, Tapani [3 ]
Laine, Jukka [4 ]
Silvan, Niko [4 ]
Nousiainen, Hannu [1 ]
Nieminen, Mika [1 ]
机构
[1] Finnish Forest Res Inst, Vantaa Res Unit, Vantaa 01301, Finland
[2] Helsinki Univ Technol, Dept Civil & Environm Engn, Espoo 02015, Finland
[3] Finnish Environm Inst, Nat Div, Helsinki 00251, Finland
[4] Finnish Forest Res Inst, Parkano Res Unit, Parkano 39700, Finland
关键词
Ammonium; Forested catchments; Peatland buffer area; Nitrate; Nutrient retention; CONSTRUCTED WETLAND BUFFER; NUTRIENT RETENTION; ORGANIC-CARBON; PHOSPHORUS; VEGETATION; ZONES; LAND; FLOW; POLLUTION; REMOVAL;
D O I
10.1007/s10750-009-0079-0
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
We studied the nitrogen retention capacity of six peatland buffer areas constructed in forested catchments in southern and central Finland. The buffers (0.1-4.9% of the total catchment area) were either undrained mires or drained peatlands rewetted 4-7 years before the present study. The N retention capacity was studied by adding ammonium nitrate (NH(4)NO(3)-N) solution into the inflow waters of the buffers once (one area) or twice (five areas) during a period of 4-6 years. Except for the first N addition in one area, the three largest buffer areas (relative size > 1%) retained the added inorganic N almost completely; their retention efficiencies during the year of addition were > 93% for both NO(3)-N and NH(4)-N. Two of the three small buffers (relative size < 0.25%) were also able to reduce inorganic N from the through-flow waters effectively; their retention capacities for inorganic nitrogen varied between 58 and 89%. However, one small buffer area had a retention capacity of only < 20%. The factors contributing to efficient N retention were hydrological load during N addition, relative size of the buffer area, and its length, i.e. the distance between the inflow and outflow points. If there was any release of the added N, it mostly occurred within a relatively short-time period (< 100 days) after the treatment. The buffer areas appeared to be efficient and long-term sinks for inorganic nitrogen because the release of N during the 2-4 years after N addition was minor.
引用
收藏
页码:171 / 183
页数:13
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