Wet sieving versus dry crushing: Soil microaggregates reveal different physical structure, bacterial diversity and organic matter composition in a clay gradient

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External Research Organisations

  • University of Kassel
  • Technical University of Munich (TUM)
  • University of Bonn
  • University of Freiburg
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Details

Original languageEnglish
Pages (from-to)810-828
Number of pages19
JournalEuropean Journal of Soil Science
Volume72
Issue number2
Early online date18 Jun 2020
Publication statusPublished - Mar 2021
Externally publishedYes

Abstract

Soil microaggregates contain particles of different sizes, which may affect their potential to store organic carbon (OC). A variety of methods can be used to isolate microaggregates from the larger soil structures, among which wet sieving approaches are widely employed. We developed a novel dry crushing method that isolates microaggregates along failure planes due to mechanical stresses rather than hydraulic pressures and compared the mechanical stability, OC contents and microbial community composition between dry-crushed and wet-sieved samples with contrasting clay contents. Dry-crushed samples exhibited a higher stability and bacterial diversity compared to wet-sieved samples. As a result, the dry-crushed microaggregates had different size distributions when analysed dry and after wetting. In the dry state, dry-crushed microaggregates were larger and contained more sand-sized primary particles within the aggregate structures. The wetting of dry-crushed aggregates caused a disintegration of larger microaggregates and sand-sized primary particles into smaller microaggregates that contained finer particles. In the soils with lower clay contents, the diameter of dry-crushed microaggregates was 40 μm larger due to more sand-sized primary particles remaining within the aggregates. Depending on how much volume in microaggregates is occupied by large primary particles, the OC concentration increased in the soil with higher clay content. Wet-sieved size fractions also showed a similar pattern of OC distribution, whereas more primary particles were observed outside of aggregates. Wet sieving approaches disperse the soil into OC-rich aggregates and might be preferable if OC dynamics are investigated. Differences in bacterial community composition in dependence on clay content were more pronounced in dry-crushed microaggregates. If intact aggregate architectures are of interest for the isolation of soil structural units, the presented dry crushing method might provide an advantageous alternative that also better preserves bacterial diversity.

Keywords

    SOM distribution, aggregate breakdown dynamics, aggregate carbon, aggregate separation, aggregate stability, aggregation, microaggregate, microbial community structure

ASJC Scopus subject areas

Cite this

Wet sieving versus dry crushing: Soil microaggregates reveal different physical structure, bacterial diversity and organic matter composition in a clay gradient. / Felde, Vincent J.M.N.L.; Schweizer, Steffen A.; Biesgen, Danh et al.
In: European Journal of Soil Science, Vol. 72, No. 2, 03.2021, p. 810-828.

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@article{1768662a3a4e4c02a56654d0576c6734,
title = "Wet sieving versus dry crushing: Soil microaggregates reveal different physical structure, bacterial diversity and organic matter composition in a clay gradient",
abstract = "Soil microaggregates contain particles of different sizes, which may affect their potential to store organic carbon (OC). A variety of methods can be used to isolate microaggregates from the larger soil structures, among which wet sieving approaches are widely employed. We developed a novel dry crushing method that isolates microaggregates along failure planes due to mechanical stresses rather than hydraulic pressures and compared the mechanical stability, OC contents and microbial community composition between dry-crushed and wet-sieved samples with contrasting clay contents. Dry-crushed samples exhibited a higher stability and bacterial diversity compared to wet-sieved samples. As a result, the dry-crushed microaggregates had different size distributions when analysed dry and after wetting. In the dry state, dry-crushed microaggregates were larger and contained more sand-sized primary particles within the aggregate structures. The wetting of dry-crushed aggregates caused a disintegration of larger microaggregates and sand-sized primary particles into smaller microaggregates that contained finer particles. In the soils with lower clay contents, the diameter of dry-crushed microaggregates was 40 μm larger due to more sand-sized primary particles remaining within the aggregates. Depending on how much volume in microaggregates is occupied by large primary particles, the OC concentration increased in the soil with higher clay content. Wet-sieved size fractions also showed a similar pattern of OC distribution, whereas more primary particles were observed outside of aggregates. Wet sieving approaches disperse the soil into OC-rich aggregates and might be preferable if OC dynamics are investigated. Differences in bacterial community composition in dependence on clay content were more pronounced in dry-crushed microaggregates. If intact aggregate architectures are of interest for the isolation of soil structural units, the presented dry crushing method might provide an advantageous alternative that also better preserves bacterial diversity.",
keywords = "SOM distribution, aggregate breakdown dynamics, aggregate carbon, aggregate separation, aggregate stability, aggregation, microaggregate, microbial community structure",
author = "Felde, {Vincent J.M.N.L.} and Schweizer, {Steffen A.} and Danh Biesgen and Angela Ulbrich and Daniel Uteau and Claudia Knief and Markus Graf-Rosenfellner and Ingrid K{\"o}gel-Knabner and Stephan Peth",
note = "Funding Information: We thank Franziska Steiner for performing the size distribution and C and N measurements and Andrei Rodionov and Wulf Amelung for providing the wet‐sieved samples. We gratefully acknowledge financial support from the Deutsche Forschungsgemeinschaft (DFG) within the framework of the research unit “MAD Soil ‐ Microaggregates: Formation and turnover of the structural building blocks of soils” (DFG RU 2179). ",
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Download

TY - JOUR

T1 - Wet sieving versus dry crushing

T2 - Soil microaggregates reveal different physical structure, bacterial diversity and organic matter composition in a clay gradient

AU - Felde, Vincent J.M.N.L.

AU - Schweizer, Steffen A.

AU - Biesgen, Danh

AU - Ulbrich, Angela

AU - Uteau, Daniel

AU - Knief, Claudia

AU - Graf-Rosenfellner, Markus

AU - Kögel-Knabner, Ingrid

AU - Peth, Stephan

N1 - Funding Information: We thank Franziska Steiner for performing the size distribution and C and N measurements and Andrei Rodionov and Wulf Amelung for providing the wet‐sieved samples. We gratefully acknowledge financial support from the Deutsche Forschungsgemeinschaft (DFG) within the framework of the research unit “MAD Soil ‐ Microaggregates: Formation and turnover of the structural building blocks of soils” (DFG RU 2179).

PY - 2021/3

Y1 - 2021/3

N2 - Soil microaggregates contain particles of different sizes, which may affect their potential to store organic carbon (OC). A variety of methods can be used to isolate microaggregates from the larger soil structures, among which wet sieving approaches are widely employed. We developed a novel dry crushing method that isolates microaggregates along failure planes due to mechanical stresses rather than hydraulic pressures and compared the mechanical stability, OC contents and microbial community composition between dry-crushed and wet-sieved samples with contrasting clay contents. Dry-crushed samples exhibited a higher stability and bacterial diversity compared to wet-sieved samples. As a result, the dry-crushed microaggregates had different size distributions when analysed dry and after wetting. In the dry state, dry-crushed microaggregates were larger and contained more sand-sized primary particles within the aggregate structures. The wetting of dry-crushed aggregates caused a disintegration of larger microaggregates and sand-sized primary particles into smaller microaggregates that contained finer particles. In the soils with lower clay contents, the diameter of dry-crushed microaggregates was 40 μm larger due to more sand-sized primary particles remaining within the aggregates. Depending on how much volume in microaggregates is occupied by large primary particles, the OC concentration increased in the soil with higher clay content. Wet-sieved size fractions also showed a similar pattern of OC distribution, whereas more primary particles were observed outside of aggregates. Wet sieving approaches disperse the soil into OC-rich aggregates and might be preferable if OC dynamics are investigated. Differences in bacterial community composition in dependence on clay content were more pronounced in dry-crushed microaggregates. If intact aggregate architectures are of interest for the isolation of soil structural units, the presented dry crushing method might provide an advantageous alternative that also better preserves bacterial diversity.

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KW - aggregate breakdown dynamics

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KW - microbial community structure

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