A warming climate and expected changes in average and extreme rainfall emphasise the importance of understanding how the land surface routes and stores surface water. The availability and movement of water within an ecosystem is a fundamental control on biological and geophysical activity, and influences many climatic feedbacks. A key phenomenon influencing water infiltration into the land surface is soil hydrophobicity, or water repellency. Despite repellency dictating the speed, volume and pattern of water infiltration, there is still major uncertainty over whether this critical hydrological process is biologically or physicochemically controlled. Here we show that soil water repellency is likely driven by changes in the plant and soil microbial communities in response to environmental stressors. We carried out a field survey in the summers of 2013 to 2016 in a variety of temperate habitats ranging across arable, grassland, forest and bog sites. We found that moderate to extreme repellency occurs in 68% of soils at a national scale in temperate ecosystems, with 92% showing some repellency. Taking a systems approach, we show that a wetter climate and low nutrient availability alter plant, bacterial and fungal community structure, which in turn are associated with increased soil water repellency across a large-scale gradient of soil, vegetation and land-use. The stress tolerance of the plant community and associated changes in soil microbial communities were more closely linked to changes in repellency than soil physicochemical properties. Our results indicate that there are consistent responses to diverse ecosystem stresses that will impact plant and microbial community composition, soil properties, and hydrological behaviour. We suggest that the ability of a biological community to induce such hydrological responses will influence the resilience of the whole ecosystem to environmental stress. This highlights the crucial role of above-belowground interactions in mediating climatic feedbacks and dictating ecosystem health.
Plant and soil communities are associated with the response of soil water repellency to environmental stress.
F. Seaton,Davey L. Jones,S. Creer,P. George,S. Smart,I. Lebron,G. Barrett,B. Emmett,D. Robinson
Published 2019 in Science of the Total Environment
ABSTRACT
PUBLICATION RECORD
- Publication year
2019
- Venue
Science of the Total Environment
- Publication date
2019-10-01
- Fields of study
Biology, Medicine, Environmental Science
- Identifiers
- External record
- Source metadata
Semantic Scholar, PubMed
CITATION MAP
EXTRACTION MAP
CLAIMS
CONCEPTS
- biological community
The combined plant and microbial assemblage whose composition can shape ecosystem processes.
Aliases: biological community composition
- ecosystem resilience
The capacity of an ecosystem to withstand environmental stress while maintaining function and structure.
Aliases: resilience of the whole ecosystem
- hydrological behaviour
The way water moves through, infiltrates, and is stored in the land surface and ecosystem.
Aliases: hydrological response
- low nutrient availability
A resource-poor soil condition in which plant-available nutrients are scarce.
Aliases: nutrient limitation
- plant community stress tolerance
The capacity of the plant assemblage to persist and function under environmental stress.
Aliases: stress tolerance of the plant community
- plant community structure
The composition and organization of plant species within a site or habitat.
Aliases: vegetation structure
- soil microbial communities
The bacterial and fungal populations inhabiting the soil environment.
Aliases: microbial communities, bacterial and fungal communities
- soil physicochemical properties
The chemical and physical characteristics of soil that influence its behavior and interactions with water.
Aliases: physicochemical properties of soil
- soil water repellency
The tendency of soil to resist wetting and slow or alter infiltration of water into the surface layer.
Aliases: soil hydrophobicity, water repellency
- wetter climate
Environmental conditions characterized by higher moisture or rainfall availability across the surveyed gradient.
Aliases: moist climate
REFERENCES
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