Abstract
Key message
A Soil Monitoring Law to improve soil health across all land uses has been proposed by the European Commission. As forests soils have different chemical and physical properties as well as biogeochemical dynamics compared to agricultural land, they also face different challenges in maintaining and restoring soil health. Examples are soil acidification, eutrophication by atmospheric deposition, responses to climate change, and loss of biodiversity. Therefore, we propose forest soil specific health descriptors and thresholds based on experience and knowledge from existing long-term monitoring programs.
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1 Introduction
Soil is one of the basic pillars of the environment, human society and the world economy. Currently, 33% of soils worldwide are already degraded and over 90% of soils could be degraded by the middle of the century (FAO and ITPS 2015; IPBES 2018). It is estimated that in the European Union (EU) alone, the costs associated with soil degradation amount to over 50 billion euros per year (Kraamwinkel et al. 2021). To protect soil resources and maintain and improve their quality, the EU Soil Strategy for 2030 sets the long-term vision that by 2050, all EU soil ecosystems are in healthy condition and are thus more resilient. The Soil Strategy for 2030 announced that the Commission would table a legislative proposal on soil health to enable reaching the objectives of the Soil Strategy. In its resolution of 28 April 2021 on soil protection, the European Parliament emphasised the importance of protecting soil and promoting healthy soils in the EU. The European Parliament called on the Commission to design a Union wide common legal framework, with full respect for the subsidiarity principle, for the protection and sustainable use of soil, addressing all major soil threats. We therefore welcome Soil Monitoring Law (SML) proposed by the European Commission (EU COM) as it will promote soil health, create a soil monitoring network for all soils across the EU, make sustainable soil management a standard in the EU, and enhance restoration of contaminated soils. However, to be successful, the specific characteristics of forest soils in terms of properties and management should be taken into account in the SML, as explained below. This would not only improve the implementation of the EU Soil Strategy, but also increase the acceptance of the SML by the Member States and stakeholders.
2 EU activities to improve soil health
In the EU, different strategic actions dealing with soils underlined the interest of an EU-wide assessment of indicators leading to soil health for all land uses. The SML (EU 2024) said that: “As part of the Green Deal, the Biodiversity Strategy for 2030 announced the update of the 2006 Soil Thematic Strategy (STS) to address soil degradation and fulfil EU and international commitments on land-degradation neutrality. The EU Soil Strategy for 2030 set the vision to have all soils in healthy condition by 2050, to make protection, sustainable use and restoration of soils the norm and proposes a combination of voluntary and legislative actions. Addressing soil degradation and ensuring the protection and sustainable use of soil, including by a Soil Monitoring Law (SML), is also included in the 8th Environment Action Programme.” The second draft of the SML (Rev II) has been developed through expert and scientific workshops and a public consultation process. Furthermore: “The SML proposal puts in place a solid and coherent soil monitoring framework for all soils across the EU, which will address the current gap of knowledge on soils. It should be an integrated monitoring system based on EU level, Member State and private data. This data will be based on a common definition of what constitutes a healthy soil and will underpin the sustainable management of soils, to maintain or enhance soil health, and thus to achieve healthy and resilient soils everywhere across the EU by 2050. The soil monitoring framework is crucial to provide the data and information needed to define the right measures. It is therefore appropriate to lay down criteria for sampling points that are representative of the soil condition under different soil types, climatic conditions and land use.” (EU 2024). That means the EU calls for Member States to prepare a system for the monitoring, descriptors and thresholds of soil for all land uses. At the same time, there is already a great deal of expert knowledge and harmonized monitoring systems.
3 Why are forest soils important and what makes them different?
Forests cover approximately 39% of the EU’s total land area. Compared to arable soils, forest soils are often unsuitable for agriculture, as they tend to be stonier, less fertile, affected by waterlogging, and often located on steeper slopes. Forest soils are not disturbed by annual tillage and harvest, and their management usually takes place over decades to centuries. For this reason, soils under forests have different physical and chemical properties and biogeochemical dynamics compared to adjacent agricultural soils. Forests typically develop an organic surface layer (forest floor). Several properties of the forest floor are used as indicators as mentioned in the European indicator report (EEA 2022). According to EEA (2022), one possible indicator for the impact of nitrogen eutrophication in forests is the low C/N ratio for either the highly humified organic layer (H horizon, for moderate to nutrient-poor forest soils) or the top few centimetres of mineral soils (nutrient-rich forest soils without H horizons). The characteristics of forest soils (incl. well-developed organic layer) should be taken into account when developing EU-wide regulation of soil management and soil monitoring network. Forest soils store much more organic matter than agricultural soils, which is why forests play a crucial role in the European soil carbon balance and related climate change mitigation measures in the EU (Grüneberg et al. 2014; Jonard et al. 2017; Leitgeb et al. 2013). Organic soils like peatlands have the highest C content, but in case they get drained, those turn into a carbon source. Moreover, the forest floor organic layer is a biological hotspot, affecting the carbon, water and nutrient dynamics of forest soil and of the whole ecosystem (Dise et al. 1998).
4 Forest soil health is affected by various factors
Forest soil health is affected by various factors, both natural and human-induced, which are different from the threats to soil health under other land uses. Soil health is affected differently depending on the region and the pollution climate. Human-induced nitrogen deposition, heavy metals and acid rain also have long-lasting effects, e.g., extreme pollution from the second half of the twentieth century is still clearly visible in forest soil properties in some European regions (Ulrich 1991; Thimonier et al. 2019).
Furthermore, climate change become more evident in forests and their soils in recent years (Bytnerowicz et al. 2013; Hickler et al. 2012; Filho et al. 2023). In Europe, most forests are semi-natural ecosystems that are usually managed much less intensively compared to agricultural land. In forests, where tree roots grow in many cases much deeper than those of arable, annual crops, the parent material and soil type play a more important role in the nutrient supply than in agroecosystems because, unlike arable soils, forest soils are only fertilized in exceptional cases. Essential macronutrients like nitrogen and phosphorous both of which widely limit primary productivity across forest ecosystems are decreasing (Talkner et al. 2009; Elser et al. 2007; Vitousek et al. 2010). Thus, increased nitrogen deposition often stimulates tree growth and hence ecosystem Carbon sequestration in nitrogen-limited forests (Högberg 2007; De Vries et al. 2009; Thomas et al. 2010), considering that in forests SOC decomposition is often reduced in response to (high) nitrogen deposition (e.g., Janssens and Luyssaert 2009). The nitrogen-induced increase in the growth can be diminished, however, when the accompanying phosphorous supply is deficient (Braun et al. 2010; Lang et al. 2016). Soil phosphorous availability in terrestrial ecosystems is primarily driven by mineral weathering and atmospheric deposition (Vitousek et al. 2010). P input from atmospheric deposition is low, and this also holds for weathering, which is also generally low.
European forests grow on a wide variety of soil conditions. Moreover, due to long rotation periods, soil and forest management practices have long-term impact and require a longer period of monitoring and evaluation. Such a survey can be less frequent (10–15 years) than is proposed by the SML which expect that “Member States shall ensure that new soil measurements are performed at least every 6 years within one sampling campaign or as part of a continuous sampling scheme which expect sampling every 6 year”.
Specific disturbances threaten forest soil health and are of a different nature and magnitude than on arable soils. For instance, forest fires, soil perturbation by wind-throw, invasive species, pest infestation, improper forestry practices, overuse of timber resources, drainage of peatlands and resulting soil compaction have long-lasting impact on soil properties. In many cases, the deterioration in soil quality cannot be directly attributed to forest management, but is due to many different influencing factors (Fig. 1).
5 Harmonized European forest soil monitoring since the 1990s
Member states can build the proposed soil monitoring on existing forest soil monitoring system, which provides long-time data series, expertise and proven methods for soil surveys based on the ICP Forests Manual (Cools and de Vos 2020). For reasons of representativeness on a country scale, the countries should increase the number of plots accordingly. According to the SML, the number and location size of the national sample sampling points shall meet the requirement of representing the variability of the chosen soil descriptors within the soil units with a maximum per cent error (or coefficient of variation) of 5% for the estimation of the area having unhealthy soils.
The International Co-operative Programme on Assessment and Monitoring of Air Pollution Effects on Forests (UN ECE ICP Forests) under the authority of the Air Convention of the United Nations Economic Commission for Europe is a network to assess forest health, including a soil monitoring programme on a European scale. Forest soil monitoring under the ICP Forests is internationally coordinated through a structured governance system, harmonized and standardized protocols, covers the majority of the member states, and is in line with existing reporting systems such as the LULUCF regulation, the EU Nature Restoration Law or the NEC Directive. The ICP Forests activities include optimization of sampling design considering spatio-temporal variation, methodological uncertainties, investigation of systematic errors to improve accuracy, intercalibrations between analytical procedures, and in-depth understanding of the chemical, physical and biological dynamics of forest soils. Since 1990, a systematic 16 × 16-km grid (Fig. 2) provides monitoring on around 5500 plots across Europe for forest health condition (ICP Forest Level I). Several harmonized soil surveys were realized within the network starting from the 1990s. Together with soil sampling, biodiversity data (forest type, tree species, ground vegetation, deadwood, etc.) was collected during the EU co-funded demonstration project (2006–2009) so that forest soil condition can be closely linked to biomass productivity and to forest condition. Some Member States have soil monitoring schemes in place like the French network ReNEcofor, which is linked to the ICP Forests network.
Pan-European distribution of ICP Forests Level I plots with one or more soil surveys since 1990. On 93% of all plots, the forest floor was sampled by areal-mass. The majority of plots with repeated surveys underwent subsoil sampling to a depth of 80 cm, which is required for proper forest soil health assessments. Average time interval between surveys is 15 years
6 Suggested actions
-
a.
SML — Monitoring should use existing forest monitoring and reporting systems that include forest inventory data. This allows to link tree stand structure, forest productivity, forest management and its impact soil health and is therefore in line with existing reporting systems like LULUCF, the proposed Nature Restoration Law or NEC Directive.
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b.
The design of the sample survey should be using the best available information on soil properties distribution, including, but not limited to information resulting from previous national or subnational surveys, relevant measurements from soil managers and measurements under the LUCAS Soil program and the ICP Forests Program. Data obtained from sampling points taken during soil investigations at contaminated sites may be used for the assessment of soil health criteria provided they are not linked to the contaminating activity. The existing pan-European forests monitoring program (ICP Forests) is particularly suitable because it is harmonized across Europe and offers long-term data to identify thresholds for healthy forest soils.
-
c.
Specific indicators and thresholds applicable for the identification of degraded forest soils are needed. Furthermore, the sampling and inventory design should take into account the whole rooting zone of trees, the spatial heterogeneity of forest soils and the sampling of the forest floor.
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d.
If the number of plots will be expanded by LUCAS Soil or national soil monitoring programmes, the sampling scheme for SML should be improved for proper forest soil spatio-temporal monitoring, in line with existing monitoring programs. Careful sampling of the forest floor on all plots where it exists is particularly important for the evaluation of forest soil condition and its changes. In addition, the bulk density and coarse fraction should also be collected at each plot in order to calculate the stocks and stock changes correctly.
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e.
Building on and upgrading the existing EU soil observatory, the Commission should establish a digital soil health data portal that should be compatible with the EU Data Strategy24 and the EU data spaces and which should be a hub providing access to soil data coming from various sources, in the aggregated form. A data interface like those of the ICP Forests should be developed for the provision of data within the framework of the SML, via which (i) all national data can be checked in a standardized manner and (ii) made available in harmonized formats for further analyses and evaluations.
7 Conclusion
Successful implementation of the proposed Soil Monitoring Law will provide important data for evaluation to enhance soil health and bring the European soil monitoring to a new era. By using existing forest soil monitoring networks and national forest inventories as well as harmonized sampling design and developed expertise, the EU Soil Monitoring Law can build a soil monitoring system that supports the Soil Mission targets and serves stakeholders by providing relevant information about changes in the soil properties. A harmonized approach offers the opportunity to assess soil conditions across Europe with coordinated indicators and threshold values. We recommend to use the long-time series of the ICP Forests for this purpose.
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References
Braun S, Thomas VFD, Quiring R, Flückiger W (2010) Does nitrogen deposition increase forest production? The role of phosphorus. Environ Pollut 158:2043–2052
Bytnerowicz A, Fenn M, McNulty S, Yuan F, Pourmokhtarian A, Driscoll C, Meixner T, (2013) Interactive Effects of Air Pollution and Climate Change on Forest Ecosystems in the United States: Current Understanding and Future Scenarios, Editor(s): Matyssek R, Clarke N, Cudlin P, Mikkelsen TN, Tuovinen JP, Wieser G, Paoletti E, Developments in Environmental Science, Elsevier, Amsterdam, Volume 13, Pages 333–369, ISSN 1474–8177, ISBN 9780080983493.
Cools N, De Vos B (2020) Part X: Sampling and Analysis of Soil. Version 2020–1. In: UNECE ICP Forests Programme Co-ordinating Centre (ed.): Manual on methods and criteria for harmonized sampling, assessment, monitoring and analysis of the effects of air pollution on forests. Thünen Institute of Forest Ecosystems, Eberswalde, Germany, 29 p. Annex [http://www.icp-forests.org/manual.htm] ISBN: 978–3–86576–162–0 /
De Vries W, Solberg S, Dobbertin M, Sterba H, Laubhann D, van Oijen M, Evans C, Gundersen P, Kros J, Wamelink JGG, Reinds GJ, Sutton MA (2009) The impact of nitrogen deposition on carbon sequestration by European forests and heathlands. Forest Ecol Manage 258:1814–1823
Dise NB, Matzner E, Forsius C (1998) Evaluation of organic horizon C: N ratio as an indicator of nitrate leaching in conifer forests across Europe’. Environ Pollut 102:453–456
EEA (2022) Soil monitoring in Europe - Indicators and thresholds for soil health assessments. ISBN 978–92–9480–538–6 ISSN 1977–8449 https://doi.org/10.2800/956606
Elser MB, Cleland EE, Gruner D, Harpole S, Hillebrand H, Ngai JT, Seabloom EW, Shurin JB, Smith J (2007) Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems. Ecol Lett 10:1135–1142. https://doi.org/10.1111/j.1461-0248.2007.01113.x
European Commission (2024) Proposal for a directive of the European Parliament and of the Council on a Soil Monitoring and Resilience (Soil Monitoring Law). (https://eur-lex.europa.eu/legal-content/EN/TXT/HTML/?uri=CELEX:52023PC0416)
FAO and ITPS (2015) Status of the World’s Soil Resources (SWSR) – Main Report. Food and Agriculture Organization of the United Nations and Intergovernmental Technical Panel on Soils, Rome, Italy
Filho WL, Nagy G, Setti A, Sharifi A, Donkor F, Batista K, Djekic I (2023) Handling the impacts of climate change on soil biodiversity. Sci Total Environ 869:161671
Grüneberg E, Ziche D, Wellbrock N (2014) Organic carbon stocks and sequestration rates of forest soils in Germany. Glob Change Biol 20:2644–2662
Hickler T, Vohland K, Feehan J, Miller J, Smith B, Costa L, Giesecke T, Fronzek S, Carter TR, Cramer W, Kühn I, Sykes MT (2012) Projecting the future distribution of European potential natural vegetation zones with a generalized, tree species-based dynamic vegetation model. Glob Ecol Biogeogr. https://doi.org/10.1111/j.1466-8238.2010.00613.x
Högberg P (2007) Environmental science: nitrogen impacts on forest carbon. Nature 447(7146):781–2. https://doi.org/10.1038/447781a. PMID: 17568730
IPBES (2018) The IPBES assessment report on land degradation and restoration. Montanarella L, Scholes R, and Brainich A. (eds.). Secretariat of the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services, Bonn, Germany. 744 pages. https://doi.org/10.5281/zenodo.3237392
IUSS Working Group WRB. (2022). World Reference Base for Soil Resources. International soil classification system for naming soils and creating legends for soil maps. 4th edition. International Union of Soil Sciences (IUSS), Vienna
Janssens IA, Luyssaert S (2009) Nitrogen’s carbon bonus. Nature Geosci 2:318–319
Jonard M, Nicolas M, Coomes DA, Caignet I, Saenger A, Ponette Q (2017) Forest soils in France are sequestering substantial amounts of carbon. Sci Total Environ 574:616–628. https://doi.org/10.1016/j.scitotenv.2016.09.028. ISSN 0048-9697
Kraamwinkel CT, Beaulieu A, Dias T (2021) Planetary limits to soil degradation. Commun Earth Environ 2:249. https://doi.org/10.1038/s43247-021-00323-3
Lang F, Bauhus J, Frossard E, George E, Kaiser K, Kaupenjohann M, Krüger J, Matzner E, Polle A, Prietzel J, Rennenberg H, Wellbrock N (2016) Phosphorus in forest ecosystems: New insights from an ecosystem nutrition perspective†. J Plant Nutrient Soil Sci 179:129–135. https://doi.org/10.1002/jpln.201500541
Leitgeb E, Reiter R, Englisch M, Lüscher P, Schad P, Feger KH (2013) (Hrsg.): Waldböden. Ein Bildatlas der wichtigsten Bodentypen aus Österreich, Deutschland und der Schweiz. Wiley-VCH Verlag GmbH, Weinheim 2012, pp. 387, ISBN 978–3–527–32713–3
Talkner U, Jansen M, Beese FO (2009) Soil phosphorus status and turnover in central-European beech forest ecosystems with differing tree species diversity. Soil Sci 60(3):338–342. https://doi.org/10.1111/j.1365-2389.2008.01117.x
Thimonier A, Kosonen Z, Braun S, Rihm B, Schleppi P, Schmitt M (2019) Total deposition of nitrogen in swiss forests: Comparison of assessment methods and evaluation of changes over two decades. Atmos Environ 198:335–350. https://doi.org/10.1016/j.atmosenv.2018.10.051
Thomas QR, Canham CD, Weathers KC, Goodale CL (2010) Increased tree carbon storage in response to nitrogen deposition in the US. Nat Geosci 3:13–17
Ulrich B (1991). An Ecosystem Approach to Soil Acidification. In: Ulrich, B., Sumner, M.E. (eds) Soil Acidity. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-74442-6_3
Vitousek PM, Porder S, Houlton BZ, Chadwick OA (2010) Terrestrial phosphorus limitation: mechanisms, implications, and nitrogen-phosphorus interactions. Ecol Appl 20(1):5–15. https://doi.org/10.1890/08-0127.1
Zanella A, Jabiol B, Ponge JF, Sartori G, de Waal R, Van Delft B, Graefe U, Cools N, Katzensteiner K, Hager H, Englisch M, Brethes A (2009) Toward a European humus forms reference base. Studi Trent Sci Nat 85:145–151 ©Museo Tridentino di Scienze Naturali, Trento, 2009. ISSN 2035-7699
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Conceptualization: Raisa Mäkipää, Nicole Wellbrock; writing—original draft preparation: Nicole Wellbrock; writing—review and editing: Vit Sramek, Pavel Pavlenda, Bruno de Vos, Ernst Leitgeb, Robert Jandl, Natalie Cools, Kai Schwärtzel, Raisa Mäkipää, Aleski Lethonen; Figures: Bruno de Vos, Nicole Wellbrock.
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Wellbrock, N., Cools, N., de Vos, B. et al. There is a need to better take into account forest soils in the planned soil monitoring law of the European Union. Annals of Forest Science 81, 22 (2024). https://doi.org/10.1186/s13595-024-01238-7
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DOI: https://doi.org/10.1186/s13595-024-01238-7