2013
DOI: 10.1007/s11104-013-1791-0
|View full text |Cite
|
Sign up to set email alerts
|

Mechanisms linking plant community properties to soil aggregate stability in an experimental grassland plant diversity gradient

Abstract: Background and aims Soil aggregate stability depends on plant community properties, such as functional group composition, diversity and biomass production. However, little is known about the relative importance of these drivers and the role of soil organisms in mediating plant community effects. Methods We studied soil aggregate stability in an experimental grassland plant diversity gradient and considered several explanatory variables to mechanistically explain effects of plant diversity and plant functional … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

3
83
5

Year Published

2014
2014
2023
2023

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 131 publications
(91 citation statements)
references
References 70 publications
3
83
5
Order By: Relevance
“…After the cropland was converted to grassland, the soil structure, originally destroyed by ploughing, redeveloped via the formation of aggregates and continuous pores with the potential to connect top‐ and subsoil quickly. Both soil aggregate and pore formation are closely related to several biotic factors within the soil compartment, which are affected by plant diversity, for example, soil microbial biomass and activity (Eisenhauer et al, ) and soil fauna (Eisenhauer et al, ), SOC concentration (Lange, Eisenhauer, et al, ; Steinbeiss et al, ), and root biomass (Ravenek et al, ) and accordingly previous research has showed diversity effects on aggregate stability (Gould et al, ; Pérès et al, ). Our results suggest that soil structure formation progresses faster in plots with more plant species.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…After the cropland was converted to grassland, the soil structure, originally destroyed by ploughing, redeveloped via the formation of aggregates and continuous pores with the potential to connect top‐ and subsoil quickly. Both soil aggregate and pore formation are closely related to several biotic factors within the soil compartment, which are affected by plant diversity, for example, soil microbial biomass and activity (Eisenhauer et al, ) and soil fauna (Eisenhauer et al, ), SOC concentration (Lange, Eisenhauer, et al, ; Steinbeiss et al, ), and root biomass (Ravenek et al, ) and accordingly previous research has showed diversity effects on aggregate stability (Gould et al, ; Pérès et al, ). Our results suggest that soil structure formation progresses faster in plots with more plant species.…”
Section: Discussionmentioning
confidence: 99%
“…Besides direct effects on water fluxes (evaporation and transpiration), plant community composition, including species richness and functional group assembly, influences soil functions such as soil microbial biomass and activity (Drenovsky, Vo, Graham, & Scow, ; Eisenhauer et al, ; Lange et al, ; Zak, Holmes, White, Peacock, & Tilman, ), soil fauna (Eisenhauer et al, ), and soil organic matter dynamics (Lange, Eisenhauer, et al, ; Steinbeiss et al, ), all of which affect soil properties related to soil water percolation, such as soil aggregation (Gould et al, ; Pérès et al, ), soil pore volume, and water infiltration capacity (Fischer et al, ). The close relationship between the biogeochemical and water cycles can incur further indirect effects of biodiversity on the availability of other resources that are mediated by soil water (Allan et al, ; Loreau & Hector, ; Tilman et al, ).…”
Section: Introductionmentioning
confidence: 99%
“…Meanwhile, water-stable aggregates (WSAs) in macroaggregates, which are stable to the action of repeated soil wetting and drying cycles, are widely used to evaluate aggregate stability by means of the wet-sieving analysis6. As an indicator of soil structure related to soil water regime, erodibility, and nutrient availability, aggregate stability is affected by soil physical, chemical, and/or microbial community properties, root systems, plant species and/or communities78910.…”
mentioning
confidence: 99%
“…Soil aggregate stability increased signifi cantly from monocultures to plant species mixtures ( Pérès et al 2013 ). Root-derived carbon (C) is preferentially retained in soil compared to aboveground C inputs, and microbial communities assimilating rhizodeposit-C are sensitive to their microenvironment.…”
Section: Soil Sustainabilitymentioning
confidence: 99%