Growth reactions of Pinus sylvestris L. and Quercus pubescens Willd. to drought years at a xeric site in Valais, Switzerland

2006 ◽  
Vol 23 (3) ◽  
pp. 121-132 ◽  
Author(s):  
Britta Eilmann ◽  
Pascale Weber ◽  
Andreas Rigling ◽  
Dieter Eckstein
2010 ◽  
Vol 161 (11) ◽  
pp. 450-459 ◽  
Author(s):  
Thomas Wohlgemuth ◽  
Christoph Hester ◽  
Anna-Regula Jost ◽  
Ulrich Wasem ◽  
Barbara Moser

After the intensive forest fire near Leuk, in 2003 the question arose whether and how fast the forest would regenerate. To answer this question, we observed the recolonisation by plants in the 300 ha of burned area annually from 2004 to 2008, using a set of permanently installed and systematically arranged sample plots of 200 m2 (n = 151). Five years after the fire, natural regeneration of the trees at altitudes above 1,700 m attains a density of 1,760 stems/ha, wich is comparable with results found after the forest fire in Val Müstair (Graubünden) in 1983, or after windthrow “Vivian” in 1990 in the Northern Prealps. The most frequent tree species are the pioneers, namely the European aspen (Populus tremula), large-leaved willow and goat willow (Salix appendiculata and S. caprea). Norway spruce (Picea abies) and European larch (Larix decidua) are present in small numbers. Natural regeneration is smaller at middle and lower altitudes, with roughly 1,160 stems/ha at altitudes between 1,300 and 1,700 m, and 700 stems/ha below 1,300 m. Here in many places pubescent oak (Quercus pubescens) regenerates itself with coppice shoots. Scots pine (Pinus sylvestris) regenerates only sparsely. By applying Ripley's K-function to triangle plots, we found that regeneration is significantly clumped in 79% of the plots having more than ten trees of at least 25 cm of height. Spatial aggregation often starts at very short distances between trees, and is observable both within and between species. Five years after the forest fire, we can confirm that forest will regenerate at all altitudes. The first forest phase will be bush forest.


2005 ◽  
Vol 9 (5) ◽  
pp. 493-505 ◽  
Author(s):  
R. Poyatos ◽  
P. Llorens ◽  
F. Gallart

Abstract. Stand transpiration was measured during the 2003 and 2004 growing seasons using heat dissipation sap flow sensors in a Scots pine (Pinus sylvestris L.) and a pubescent oak (Quercus pubescens Willd.) forests located in a montane area of the Eastern Pyrenees (NE Spain). The first aim of the study was to assess the differences in quantitative estimates of transpiration (Ec) and the response to evaporative demand of the two stands. Over the studied period of 2003, characterised by a severe drought episode during the summer, the oak stand (Ec was only 110 mm compared to the 239 mm transpired by the Scots pine stand, although the ratio of transpiration to reference evapotranspiration (Ec/ET0) in the oak stand compares well with the expected values predicted for low leaf area index (LAI) oak forests in southern Europe. Scots pine showed a strong reduction in (Ec/ET0 as the drought developed, whereas pubescent oak was less affected by soil moisture deficits in the upper soil. As a second objective, and given the contrasting meteorological conditions between 2003 and 2004 summer periods, the interannual variability of transpiration was studied in the Scots pine plot. Rainfall during the summer months (June-September) in 2003 was almost 40% less than in the same interval in 2004. Accordingly, transpiration was also reduced about 25% in 2003. Finally, Scots pine data from 2003 and 2004 was used to calibrate a simple transpiration model using ET0 and soil moisture deficit (SMD) as input variables, and implicitly including stomatal responses to high vapour pressure deficits (Dd) and soil water status.


2005 ◽  
Vol 2 (3) ◽  
pp. 1011-1046 ◽  
Author(s):  
R. Poyatos ◽  
P. Llorens ◽  
F. Gallart

Abstract. Stand transpiration was measured during the 2003 and 2004 growing seasons using heat dissipation sap flow sensors in a Scots pine (Pinus sylvestris L.) and a pubescent oak (Quercus pubescens Willd.) forest located in a montane area of the Eastern Pyrenees (NE Spain). The first aim of the study was to assess the differences in quantitative estimates of transpiration (Ec) and the response to evaporative demand of the two stands. Over the studied period of 2003, characterised by a severe drought episode during the summer, the oak stand Ec was only 110mm compared to the 239 mm transpired by the Scots pine stand, although the ratio of transpiration to reference evapotranspiration (Ec/ET0) in the oak stand compares well with the expected values predicted for low leaf area index (LAI) oak forests in southern Europe. Scots pine showed a strong reduction in Ec/ET0 as the drought developed, whereas pubescent oak was less affected by soil moisture deficits in the upper soil. As a second objective, and given the contrasting meteorological conditions between 2003 and 2004 summer periods, the interanual variability of transpiration was studied in the Scots pine plot. Rainfall during the summer months (June-September) in 2003 was almost 40% less than in the same interval in 2004. Accordingly, transpiration was also reduced about 25% in 2003. Finally, Scots pine data from 2003 and 2004 was used to calibrate a simple transpiration model using ET0 and soil moisture deficit (SMD) as input variables, and implicitly including stomatal responses to high vapour pressure deficits (Dδ) and soil water status.


2003 ◽  
Vol 18 (1) ◽  
pp. 29-38 ◽  
Author(s):  
Reza Yazdani ◽  
Jan-erik Nilsson ◽  
Christophe Plomion ◽  
Gaurov Mathur

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