Impact of dolomite lime on the ground vegetation and on potential net N transformations in Norway spruce (Picea abies (L.) Karst.) and sessile oak (Quercus petraea (Matt.) Lieb.) stands in the Belgian Ardenne

被引:17
作者
Dulière, JF
Carnol, M
Dalem, S
Remacle, J
Malaisse, F
机构
[1] Univ Mons, Fac Sci, B-7000 Mons, Belgium
[2] Fac Univ Sci Agron, Ecol Lab, B-5030 Gembloux, Belgium
[3] Univ Liege, Dept Bot B22, B-4000 Liege, Belgium
关键词
dolomite liming; forest; N mineralisation; nitrification; ground vegetation;
D O I
10.1051/forest:19990501
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The impact of dolomite lime (5 T.ha(-1)) on the ground vegetation and on potential net nitrogen (N) transformations was investigated in two Belgian forest ecosystems. Norway spruce (Picea abies (L.) Karst.) and sessile oak (Quercus petraea (Matt.) Lieb.) stands were situated in the Haute Ardenne (east Belgium) on acid-brown soil. The herb-layer floristic richness increased during the 2 years following liming, with the appearance of light and N-demanding species, which are also found in clear-cut areas or on road verges. Mosses reacted rapidly, showing a decrease acidophilous-dominant species and the establishment of some ruderal species. Six months after liming, the pH was significantly increased in the organic horizon of both stands and in the organomineral horizon of the oak stand. Soils originating from the two stands showed distinct responses in net NO3- production to the dolomite lime treatment. In the organic layer of the Quercus soil, net NH4+ production was decreased, NO3- prediction increased, and total N mineralisation remained unchanged. In the organomineral layer. NO3- production was increased. In the Picea soil, NO3- production was decreased in the organomineral soil layer. These results indicate the possibility of differences in the control of the N transformation processes occurring in the two sites. ((C) Inra/Elsevier, Paris.).
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页码:361 / 370
页数:10
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