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Linking critical thresholds for acidity to forest condition by using element contents in tree rings: consequences for the development of an integrated ecosystem assessment

iForest - Biogeosciences and Forestry, Volume 2, Issue 1, Pages 51-53 (2009)
doi: https://doi.org/10.3832/ifor0473-002
Published: Jan 21, 2009 - Copyright © 2009 SISEF

Short Communications

Collection/Special Issue: Cost Action E29 Meeting 2008 - Istanbul (Turkey)
Future Monitoring and Research Needs for Forest Ecosystems
Guest Editors: Marcus Schaub (WSL, Birmensdorf, CH)

In the frame of the International Co-operative Programme on the Assessment and Monitoring of Air Pollution Effects on Forests, results are given here on the link of element fluxes through forests to Mn contents in tree rings in order to detect incipient soil acidification.

Critical loads, Critical limits, Acidification, Soil chemistry, Tree rings

  Introduction 

Due to the growing public awareness of possible adverse effects of air pollution on forests, in 1985 the International Co-operative Programme on the Assessment and Monitoring of Air Pollution Effects on Forests, the ICP Forests, was launched under the Convention on Long-range Transboundary Air Pollution (LRTAP Convention) of the United Nations Economic Commission for Europe ([16]).

The aim of the two stage forest monitoring on Level I and Level II of the ICP Forests is the scientific support of political decisions by means of the identification and quantification of indicators for forest condition and their change over time. The monitoring on the regularly distributed (16 km x 16 km grid) Level I plots aimed at detection of spatial and temporal patterns of forest condition indicators. The annual assessment of the forest condition on Level I was complemented by the first soil condition survey ([18]) and the assessment of the forest foliar element survey on a subset of the plots ([15]). While on the Level I plots no processes were studied, the monitoring on the 860 intensive monitoring plots of the Level II system helps to detect key processes of ecosystem functioning by means of analysing, e.g., element fluxes and tree growth ([17]). Both systems together provide a good basis for the integrated evaluation of changes in the state of forest ecosystems. In the following, results were given on the link of element fluxes through forests to Mn contents in tree rings in order to detect incipient soil acidification.

In 1988 the International Co-operative Programme on Modelling and Mapping of Critical Loads and Levels and Air Pollution Effects, Risks and Trends (ICP Modelling & Mapping) was established with the aim to develop an effects-based approach for air pollution abatement policies. This was realised with the elaboration of methods to calculate critical loads for ecosystems. The critical load is “the highest deposition of acidifying compounds that will not cause chemical changes leading to long-term harmful effects on ecosystem structure and function” ([10]). Critical loads were used in the negotiations of the Protocol on Further Reduction of Sulphur Emissions (Oslo - 1994), the Protocol on Abate Acidification, Eutrophication and Ground-level Ozone (Gothenburg - 1999) of the LRTAP Convention as well as the National Emission Ceilings directive of the EU ([11]).

  Results and discussion 

Within the framework of the German interdisciplinary case study “concept and feasibility study for the integrated evaluation of environmental monitoring data in forests”, funded by the German Federal Ministry of Education and Research, data of the German Level I and II monitoring were evaluated ([1]). Additionally, data on tree growth and tree ring chemistry were assessed ([2]).

For acid deposition the most commonly used critical limit is about pH 4.2, which is the thermodynamic threshold were aluminium oxides in soil dissolve. Potential toxic Al is released in the soil solution and “acid stress” for trees becomes possible. Between pH 5 to 4.2, manganese oxides are dissolved and taken up by plants. Thus, very high Mn concentration in soils and plants are an indicator of change in soil quality in the rooting zone ([8]) and the reaching of the critical limit. Changes in the availability of elements and effects of pollution can thus be detected in tree rings and assigned to a distinct time in the past ([8], [6], [13]).

The soil chemistry data from a Level I plot in the Thuringian forest were linked to tree chemical data to identify the time span of the attainment of the critical limits (German case study, for details see [2]). The tree rings of 60-year-old Norway spruce (Picea abies) show a distinct decline in the Mn concentration, beginning in the late 1960s and ending in the late 1970s. The dissolution and depletion of Mn oxides in soils precede the onset of an acid-stress situation for trees, which is characterized by a low availability of Mg, low pH and increasing concentrations of Al. First studies on the observed “novel forest damage” for this region in 1984 show very low Mg contents in spruce needles and soils, leading to the deficiency symptoms. Often elevated Mn concentrations in plant organs distinguish damaged from undamaged tree collectives, and indicate the beginning of “novel forest damage” ([3], [7]). The depletion of the base cations in soil for this time was modelled ([2]). The result correspond to the measured data from this plot in the early 1990s (Level I soil condition survey).

The results show that in principle it is possible to link information of the environmental monitoring in forests with indicators from tree ring analysis to reconstruct soil chemical history on the medium time scale. It could be demonstrated, that the thermodynamic and empirical derived value of the critical limit for acids is linked to the onset of damages. The effect based approach of the critical loads calculation is corroborated by the evaluation of ICP Forests data.

  Conclusions 

A critical load is an ecosystem property and the exceedance of a critical load indicates a long-term potential risk for an ecosystem. Damage symptoms do not necessarily show immediately. For instance, soils may buffer acid inputs for a certain time span. This is called “damage delay time” (Fig. 1). In contrast, the exceedance of a critical limit (e.g., Bc/Al ratio in soil solution for acidity) indicates an “acid stress situation”, finally leading to a “destabilizing” of the system with decline symptoms developing. If critical loads are exceeded, additional acids can not be neutralized and base cations will be mobilized and leave the ecosystem with the seepage water at an unsustainable rate. A net loss of bases is the consequence. This is often observed in regions with high deposition loads and can be calculated with dynamic models.

Fig. 1 - “Typical” temporal (past and future) development of the deposition (top), a soil chemical variable and the corresponding biological response. The delay between the (non-)exceedance of the critical load, the (non-)violation of the critical chemical criterion and the crossing of the critical biological response is indicated in grey shades, highlighting the Damage Delay Time (DDT) and the Recovery Delay Time (RDT) of the system. A fourth sub-figure is added indicating the possible trend of depletion of base cations associated with the exceedance of critical loads (acidity). (adapted from [12]).

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If CL for acidity are no longer exceeded we will come to a situation, were the ecosystems state is considerably changed because base capital is lost in times that exceeded critical loads (see also [9]). Many different endpoints for chemical and biological responses are possible, leading to many different remaining risks for the vegetation. The often observed higher sensitivity of tree growth responses to environmental stress, starting in the 1970s, indicate a higher vulnerability to environmental stress ([4], see also [5]) and must be seen in this context.

Today forests grow well ([14]), which is probably a consequence of nitrogen input but also enhanced CO2 concentration in the atmosphere and climate change. At the same time ecosystems are often eutrophied and their water filtering capacity is failing. Ecosystems recover from acidification, but in most cases they will not reach the “baseline” of an undisturbed, pre-industrial status - which we in fact don’t know. Additionally, the climate is changing, which will lead to a new “normal” state, if all depositions are below critical loads.

For the future risk assessment it is essential to define a “good ecological state” as a baseline for the whole forest ecosystem. The “good ecological state” can be defined as a sustainable situation without any risk for the integrity of forest ecosystems.

An appropriate evaluation system, applicable for different reporting obligations and environmental policy makers (LRTAP Convention, EU: Natura 2000, CBD: biodiversity), should be developed in order to come to a sound scientific assessment of the actual state of ecosystems. The existing long-term and large scale forest monitoring of the ICP Forests provide the basis for this. The system is flexible and upgradeable to include also new issues and to answer new questions.

  Acknowledgements 

The results are based on a study conducted within the framework of the combined project “Concept and Feasibility study for the Integrated evaluation of Environmental Monitoring data in Forests” (No. 0339985), funded by the German Ministry for Research and Education. We would like to thank for this financial support. Specially thanks to Dr. R. Loskill, Ms. H. Neumann, and Ms. P. Mahlitz.

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Authors’ Affiliation

(1)
S Augustin
Bundesamt für Umwelt (BAFU), Abteilung Wald, CH-3003 Bern (Switzerland)

Corresponding author

Citation

Augustin S (2009). Linking critical thresholds for acidity to forest condition by using element contents in tree rings: consequences for the development of an integrated ecosystem assessment. iForest 2: 51-53. - doi: 10.3832/ifor0473-002

Academic Editor

Marcus Schaub

Paper history

Received: Apr 25, 2008
Accepted: Dec 09, 2008

First online: Jan 21, 2009
Publication Date: Jan 21, 2009
Publication Time: 1.43 months

© SISEF - The Italian Society of Silviculture and Forest Ecology 2009

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