Related Experiment Video
Updated: Sep 10, 2025

09:04
Assessment of Labile Organic Carbon in Soil Using Sequential Fumigation Incubation Procedures
Published on: October 29, 2016
11.6K
Forest Topsoil Organic Carbon Declines Under Ash Dieback
Fiona M Seaton1, David A Robinson2, Claire M Wood1
1UK Centre for Ecology & Hydrology, Lancaster, UK.
Global Change Biology
|August 19, 2025
Summary
Ash dieback disease is reducing soil organic matter (SOM) in Great Britain
Area of Science:
- Ecology
- Forestry
- Soil Science
Background:
- Tree diseases pose a growing threat to global woodland ecosystems.
- The impact of these diseases on soil carbon dynamics remains poorly understood.
- Ash dieback (Hymenoscyphus fraxineus) is a significant disease affecting ash trees.
Purpose of the Study:
- To evaluate the fifty-year trend in topsoil carbon.
- To assess the impact of ash dieback on soil organic matter (SOM).
- To quantify potential soil carbon loss due to ash dieback in Great Britain.
Main Methods:
- Field survey of ~100 woodlands across Great Britain in 1971, 2001, and 2022.
- Measurement of topsoil (0-15 cm) organic matter (SOM).
- Application of Beta mixture modelling within a Bayesian framework to analyze SOM distribution.
Main Results:
- Average SOM remained constant across all woodlands over fifty years.
- Woodlands with ash dieback showed lower SOM compared to those without.
- A modelled mean SOM difference of 1.23 percentage points was observed between plots with and without ash dieback.
- Estimated total topsoil carbon loss due to ash dieback in Great Britain is 6 MtCO2.
Conclusions:
- Ash dieback disease leads to a decline in topsoil organic matter.
- Understanding tree disease impacts is crucial for woodland carbon dynamics.
- The study highlights significant potential carbon loss from ash dieback in British woodlands.
Keywords:
Fraxinus excelsiorHymenoscyphus fraxineusloss on ignitionsoil organic mattersoil pHtree diseasewoodlandMore Related Videos
Related Concept Videos
The Carbon Cycle
39.7K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
39.7K
The Soil Ecosystem
21.7K
Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
21.7K
Threats to Biodiversity
22.9K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
22.9K

