Deterioration of Norway spruce vitality despite a sharp decline in acid deposition: a long-term integrated perspective

Since the late 1970s, several long‐term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands in the Ardennes as these nutrient‐poor ecosystems were subject to high levels of acid deposition and exhibited symptoms of tree health decline. Betwee...

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Published inGlobal change biology Vol. 18; no. 2; pp. 711 - 725
Main Authors Jonard, Mathieu, Legout, Arnaud, Nicolas, Manuel, Dambrine, Etienne, Nys, Claude, Ulrich, Erwin, van der Perre, Raphaele, Ponette, Quentin
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LanguageEnglish
Published Oxford Blackwell Publishing Ltd 01.02.2012
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Abstract Since the late 1970s, several long‐term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands in the Ardennes as these nutrient‐poor ecosystems were subject to high levels of acid deposition and exhibited symptoms of tree health decline. Between 1978 and 2009, acid deposition declined sharply, especially sulfur and to a lesser extent nitrogen deposition. The aim of this study was (i) to determine if the Norway spruce stands recovered after the reduction of acid deposition and (ii) to explain why such a recovery occurred or not. Therefore, we collected data from different projects carried out in the Ardennes to characterize the long‐term temporal trends in soil solution chemistry, foliar nutrition, and crown condition. In parallel, a model describing the nutrient cycling in forests (NuCM) was calibrated and used to check the consistency of the observed temporal trends and to explain them. The soil solution concentration of most of the elements decreased between 1978 and 2002, which was ascribed to a decrease in atmospheric deposition. For potassium, a decline in the exchangeable pool was also showed based on the simulation carried out with NuCM. As nitrogen (N) deposition remained at an elevated level, Norway spruce stands were progressively saturated in N and mineral nutrition became more and more unbalanced. Except the foliar N and Al concentration that remained constant and increased respectively, the foliar concentration of all other nutrients decreased between 1993 and 2009, which can be explained by the decrease in ion concentration in solution. These nutritional disorders weakened trees and were probably exacerbated during the 2003 summer drought, after which symptoms of vitality loss progressively appeared. In these N‐saturated ecosystems, the N cycle was disrupted by this health decline, which increased NO3− leaching reinforcing soil acidification and risk of aluminum (Al) toxicity.
AbstractList Since the late 1970s, several long‐term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands in the Ardennes as these nutrient‐poor ecosystems were subject to high levels of acid deposition and exhibited symptoms of tree health decline. Between 1978 and 2009, acid deposition declined sharply, especially sulfur and to a lesser extent nitrogen deposition. The aim of this study was (i) to determine if the Norway spruce stands recovered after the reduction of acid deposition and (ii) to explain why such a recovery occurred or not. Therefore, we collected data from different projects carried out in the Ardennes to characterize the long‐term temporal trends in soil solution chemistry, foliar nutrition, and crown condition. In parallel, a model describing the nutrient cycling in forests (NuCM) was calibrated and used to check the consistency of the observed temporal trends and to explain them. The soil solution concentration of most of the elements decreased between 1978 and 2002, which was ascribed to a decrease in atmospheric deposition. For potassium, a decline in the exchangeable pool was also showed based on the simulation carried out with NuCM. As nitrogen (N) deposition remained at an elevated level, Norway spruce stands were progressively saturated in N and mineral nutrition became more and more unbalanced. Except the foliar N and Al concentration that remained constant and increased respectively, the foliar concentration of all other nutrients decreased between 1993 and 2009, which can be explained by the decrease in ion concentration in solution. These nutritional disorders weakened trees and were probably exacerbated during the 2003 summer drought, after which symptoms of vitality loss progressively appeared. In these N‐saturated ecosystems, the N cycle was disrupted by this health decline, which increased NO3− leaching reinforcing soil acidification and risk of aluminum (Al) toxicity.
Since the late 1970s, several long-term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands in the Ardennes as these nutrient-poor ecosystems were subject to high levels of acid deposition and exhibited symptoms of tree health decline. Between 1978 and 2009, acid deposition declined sharply, especially sulfur and to a lesser extent nitrogen deposition. The aim of this study was (i) to determine if the Norway spruce stands recovered after the reduction of acid deposition and (ii) to explain why such a recovery occurred or not. Therefore, we collected data from different projects carried out in the Ardennes to characterize the long-term temporal trends in soil solution chemistry, foliar nutrition, and crown condition. In parallel, a model describing the nutrient cycling in forests (NuCM) was calibrated and used to check the consistency of the observed temporal trends and to explain them. The soil solution concentration of most of the elements decreased between 1978 and 2002, which was ascribed to a decrease in atmospheric deposition. For potassium, a decline in the exchangeable pool was also showed based on the simulation carried out with NuCM. As nitrogen (N) deposition remained at an elevated level, Norway spruce stands were progressively saturated in N and mineral nutrition became more and more unbalanced. Except the foliar N and Al concentration that remained constant and increased respectively, the foliar concentration of all other nutrients decreased between 1993 and 2009, which can be explained by the decrease in ion concentration in solution. These nutritional disorders weakened trees and were probably exacerbated during the 2003 summer drought, after which symptoms of vitality loss progressively appeared. In these N-saturated ecosystems, the N cycle was disrupted by this health decline, which increased NO3- leaching reinforcing soil acidification and risk of aluminum (Al) toxicity.
Abstract Since the late 1970s, several long-term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands in the Ardennes as these nutrient-poor ecosystems were subject to high levels of acid deposition and exhibited symptoms of tree health decline. Between 1978 and 2009, acid deposition declined sharply, especially sulfur and to a lesser extent nitrogen deposition. The aim of this study was (i) to determine if the Norway spruce stands recovered after the reduction of acid deposition and (ii) to explain why such a recovery occurred or not. Therefore, we collected data from different projects carried out in the Ardennes to characterize the long-term temporal trends in soil solution chemistry, foliar nutrition, and crown condition. In parallel, a model describing the nutrient cycling in forests (NuCM) was calibrated and used to check the consistency of the observed temporal trends and to explain them. The soil solution concentration of most of the elements decreased between 1978 and 2002, which was ascribed to a decrease in atmospheric deposition. For potassium, a decline in the exchangeable pool was also showed based on the simulation carried out with NuCM. As nitrogen (N) deposition remained at an elevated level, Norway spruce stands were progressively saturated in N and mineral nutrition became more and more unbalanced. Except the foliar N and Al concentration that remained constant and increased respectively, the foliar concentration of all other nutrients decreased between 1993 and 2009, which can be explained by the decrease in ion concentration in solution. These nutritional disorders weakened trees and were probably exacerbated during the 2003 summer drought, after which symptoms of vitality loss progressively appeared. In these N-saturated ecosystems, the N cycle was disrupted by this health decline, which increased NO3- leaching reinforcing soil acidification and risk of aluminum (Al) toxicity. [PUBLICATION ABSTRACT]
Author Nicolas, Manuel
Ulrich, Erwin
Ponette, Quentin
van der Perre, Raphaele
Legout, Arnaud
Nys, Claude
Dambrine, Etienne
Jonard, Mathieu
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Issue 2
Keywords Acidification
Atmospheric deposition
Vitality
Acid precipitation
tree vitality
Gymnospermae
Tree crown
Tree
Soil solution
Nutrition
Norway spruce
Biogeochemical cycle
Long term
nutrient cycling
crown condition
Soils
soil solution chemistry
Deterioration
Trend analysis
soil acidification
Nutrient
Coniferales
Spermatophyta
Picea abies
foliar nutrition
FOLIAR NUTRIENT STATUS
FRENCH PRIMARY ARDENNES
FOREST ECOSYSTEMS
EUROPEAN BEECH STANDS
SOIL CHEMISTRY
atmospheric deposition
AIR-POLLUTION
BELGIAN ARDENNES
PICEA-ABIES
trend analysis
LEAF-AREA INDEX
Language English
License CC BY 4.0
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2004; 200
2004; 123
1998; 48
1989; 41
2010; 16
2009; 41
2010; 13
1991; 12
2010; 106
2005; 137
2006; 36
2007; 141
2004; 68
1994; 23
2004; 4
2009; 157
2009; 151
2006; 370
1996; 186
2008; 72
2004; 128
2003; 54
1992; 51
1974; 17
2009; 55
2009; 14
1986; 1
1927; 49
1990
2000
1997; 98
1995; 24
2003; 7
1987
2003; 3
1988; 45
1981; 38
1985
2008; 65
1992; 49
1995; 29
2005; 39
2007; 22
2001; 58
1998; 55
1998; 99
1988
2010; 408
2009b; 66
1986; 50
1986; 95
1996; 48B
2006; 12
2009a; 66
2010; 129
1977; 83
2008
1997
2007
1995
2008; 127
1999; 224
1992
1998; 138
1995; 3
2003; 177
2010; 40
2009; 258
1999
1995; 85
1995; 83
2009; 73
1989; 244
1996; 272
1983; 40
1994; 58
1981; 18
1985; 315
1996; 47
1999; 116
1989; 19
2006; 144
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Snippet Since the late 1970s, several long‐term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands in the...
Abstract Since the late 1970s, several long-term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands...
Since the late 1970s, several long-term ecological studies were conducted to better understand the biogeochemical functioning of Norway spruce stands in the...
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SubjectTerms Acid deposition
Acidification
Aluminum
Animal and plant ecology
Animal, plant and microbial ecology
atmospheric deposition
Biogeochemistry
Biological and medical sciences
crown condition
Drought
Ecological studies
Evergreen trees
foliar nutrition
Forests
Fundamental and applied biological sciences. Psychology
General aspects
Leaching
Life Sciences
Nitrogen
Norway spruce
Nutrient cycles
nutrient cycling
Picea abies
Pine trees
Pollutant deposition
Sedimentation & deposition
Soil acidification
Soil chemistry
Soil solution
soil solution chemistry
Sulfur
Synecology
Terrestrial ecosystems
tree vitality
Trees
trend analysis
Title Deterioration of Norway spruce vitality despite a sharp decline in acid deposition: a long-term integrated perspective
URI https://api.istex.fr/ark:/67375/WNG-7K0Q9R1L-T/fulltext.pdf
https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fj.1365-2486.2011.02550.x
https://www.proquest.com/docview/915498773
https://www.proquest.com/docview/920803887
https://hal.inrae.fr/hal-02647511
Volume 18
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