Architecture of soil microaggregates: Advanced methodologies to explore properties and functions

Author:

Amelung Wulf12ORCID,Tang Ni1ORCID,Siebers Nina2ORCID,Aehnelt Michaela3,Eusterhues Karin3,Felde Vincent J. M. N. L.4ORCID,Guggenberger Georg5,Kaiser Klaus6ORCID,Kögel‐Knabner Ingrid78ORCID,Klumpp Erwin2ORCID,Knief Claudia9ORCID,Kruse Jens2,Lehndorff Eva10,Mikutta Robert6ORCID,Peth Stephan4ORCID,Ray Nadja11,Prechtel Alexander12,Ritschel Thomas3ORCID,Schweizer Steffen A.7ORCID,Woche Susanne K.5,Wu Bei2,Totsche Kai U.3ORCID

Affiliation:

1. Institute of Crop Science and Resource Conservation (INRES), Soil Science and Soil Ecology University of Bonn Bonn Germany

2. Institute of Bio‐ and Geosciences Agrosphere (IBG‐3) Forschungszentrum Jülich GmbH Jülich Germany

3. Department of Hydrogeology, Institute for Geosciences Friedrich Schiller University Jena Jena Germany

4. Institute of Soil Science Soil Biophysics Leibniz University Hannover Hannover Germany

5. Institute of Soil Science Soil Chemistry Leibniz University Hannover Hannover Germany

6. Department of Soil Science and Protection, Institute of Agricultural and Nutrition Science Martin Luther University Halle‐Wittenberg Halle (Saale) Germany

7. School of Life Sciences, Chair of Soil Science Technical University Munich Freising Germany

8. Institute for Advanced Study Technical University of Munich Garching Germany

9. Institute of Crop Science and Resource Conservation (INRES), Molecular Biology of the Rhizosphere University of Bonn Bonn Germany

10. Department of Soil Ecology, Faculty for Biology, Chemistry, and Earth Science Bayreuth University Bayreuth Germany

11. Department of Mathematics, Mathematical Institute for Machine Learning and Data Science, Chair of Geomatics and Geomathematics Catholic University of Eichstätt‐Ingolstadt Ingolstadt Germany

12. Department of Mathematics–Modelling and Numerics Friedrich‐Alexander University Erlangen‐Nürnberg Erlangen Germany

Abstract

AbstractThe functions of soils are intimately linked to their three‐dimensional pore space and the associated biogeochemical interfaces, mirrored in the complex structure that developed during pedogenesis. Under stress overload, soil disintegrates into smaller compound structures, conventionally named aggregates. Microaggregates (<250 µm) are recognized as the most stable soil structural units. They are built of mineral, organic, and biotic materials, provide habitats for a vast diversity of microorganisms, and are closely involved in the cycling of matter and energy. However, exploring the architecture of soil microaggregates and their linkage to soil functions remains a challenging but demanding scientific endeavor. With the advent of complementary spectromicroscopic and tomographic techniques, we can now assess and visualize the size, composition, and porosity of microaggregates and the spatial arrangement of their interior building units. Their combinations with advanced experimental pedology, multi‐isotope labeling experiments, and computational approaches pave the way to investigate microaggregate turnover and stability, explore their role in element cycling, and unravel the intricate linkage between structure and function. However, spectromicroscopic techniques operate at different scales and resolutions, and have specific requirements for sample preparation and microaggregate isolation; hence, special attention must be paid to both the separation of microaggregates in a reproducible manner and the synopsis of the geography of information that originates from the diverse complementary instrumental techniques. The latter calls for further development of strategies for synlocation and synscaling beyond the present state of correlative analysis. Here, we present examples of recent scientific progress and review both options and challenges of the joint application of cutting‐edge techniques to achieve a sophisticated picture of the properties and functions of soil microaggregates.

Funder

Deutsche Forschungsgemeinschaft

Publisher

Wiley

Subject

Plant Science,Soil Science

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