The long-term effects of catchment liming and reduced sulphur deposition on forest soils and runoff chemistry in southwest Sweden

被引:43
|
作者
Lofgren, Stefan [1 ]
Cory, Neil [2 ]
Zetterberg, Therese [3 ]
Larsson, Per-Erik [4 ]
Kronnas, Veronika [3 ]
机构
[1] Swedish Univ Agr Sci, SLU, Dept Aquat Sci & Assessment, S-75007 Uppsala, Sweden
[2] Swedish Univ Agr Sci, Dept Forest Resource Management, SLU, S-90183 Umea, Sweden
[3] IVL, Swedish Environm Res Inst, S-40014 Gothenburg, Sweden
[4] Swedish Univ Agr Sci, SLU, Asa Expt Forest & Res Stn, S-36030 Lammhult, Sweden
关键词
Forest liming; Whole catchment liming; Acidification; Soil; Water; Liming; WATER CHEMISTRY; EPISODIC ACIDIFICATION; HUMIC SUBSTANCES; ALUMINUM; RECOVERY; DOLOMITE; GERMANY; STREAMS; BOREAL; NORWAY;
D O I
10.1016/j.foreco.2009.04.030
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Whole catchment liming or forest liming has been proposed and implemented as a countermeasure to the effects of elevated sulphur deposition. Since the end of the 1980s the Swedish Forest Agency has undertaken experimental forest liming experiments in selected catchments in southern Sweden. These studies were with low doses (3 tonnes ha(-1)) of lime (CaCO(3)) and dolomite (CaMg(CO(3))(2)). Data from both soil samples and stream water samples have been collected for the 16 years following treatment. The stream data has been complemented with data from untreated catchments, from the Swedish monitoring stream network. Significant differences due to treatment were seen for Ca, cation exchange capacity (CEC) and base saturation (BS) in the humus layer, none of these variables showed a statistically significant change in the mineral soil due to treatment alone. Soil samples from both the treated and untreated sites showed temporal changes in both the humus layer and the mineral soils with increases in pH, Ca and CEC and decreases in BS and AI which were independent of treatment. A combination of treatment and time, gave significant changes in BS and TA down to 10 cm in the mineral soil. In the stream water samples no statistically significant differences were observed between treated and untreated sites. Regardless of treatment, the streams exhibited a general pattern of declining concentrations of SO(4), Ca, sum of base cations (BC) and increasing acid neutralizing capacity (ANC). In summary, the application of a low dose of lime (3 tonnes ha(-1)) did not result in significant changes in surface water chemistry in the study catchments and changes in soil chemistry were mainly restricted to the humus layer during the 16 years following treatment. The natural recovery, as a result of reductions in sulphur deposition, dominated the effects and was clearly seen in both the treated and untreated study sites. MAGIC simulations indicate that this recovery will continue in the coming decades. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:567 / 578
页数:12
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