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

ORCID
0000-0002-4920-4667
Affiliation
Institute of Crop Science and Resource Conservation (INRES), Soil Science and Soil Ecology University of Bonn Bonn Germany
Amelung, Wulf;
ORCID
0000-0002-6726-2481
Affiliation
Institute of Crop Science and Resource Conservation (INRES), Soil Science and Soil Ecology University of Bonn Bonn Germany
Tang, Ni;
ORCID
0000-0002-6431-0046
Affiliation
Institute of Bio‐ and Geosciences Agrosphere (IBG‐3) Forschungszentrum Jülich GmbH Jülich Germany
Siebers, Nina;
GND
135893356
Affiliation
Department of Hydrogeology, Institute for Geosciences Friedrich Schiller University Jena Jena Germany
Aehnelt, Michaela;
GND
122480066
Affiliation
Department of Hydrogeology, Institute for Geosciences Friedrich Schiller University Jena Jena Germany
Eusterhues, Karin;
ORCID
0000-0002-1018-2376
Affiliation
Institute of Soil Science Soil Biophysics Leibniz University Hannover Hannover Germany
Felde, Vincent J. M. N. L.;
Affiliation
Institute of Soil Science Soil Chemistry Leibniz University Hannover Hannover Germany
Guggenberger, Georg;
ORCID
0000-0001-7376-443X
Affiliation
Department of Soil Science and Protection, Institute of Agricultural and Nutrition Science Martin Luther University Halle‐Wittenberg Halle (Saale) Germany
Kaiser, Klaus;
ORCID
0000-0002-7216-8326
Affiliation
School of Life Sciences, Chair of Soil Science Technical University Munich Freising Germany
Kögel‐Knabner, Ingrid;
ORCID
0000-0002-4810-9414
Affiliation
Institute of Bio‐ and Geosciences Agrosphere (IBG‐3) Forschungszentrum Jülich GmbH Jülich Germany
Klumpp, Erwin;
ORCID
0000-0001-5259-2675
Affiliation
Institute of Crop Science and Resource Conservation (INRES), Molecular Biology of the Rhizosphere University of Bonn Bonn Germany
Knief, Claudia;
Affiliation
Institute of Bio‐ and Geosciences Agrosphere (IBG‐3) Forschungszentrum Jülich GmbH Jülich Germany
Kruse, Jens;
Affiliation
Department of Soil Ecology, Faculty for Biology, Chemistry, and Earth Science Bayreuth University Bayreuth Germany
Lehndorff, Eva;
ORCID
0000-0002-7186-6528
Affiliation
Department of Soil Science and Protection, Institute of Agricultural and Nutrition Science Martin Luther University Halle‐Wittenberg Halle (Saale) Germany
Mikutta, Robert;
ORCID
0000-0001-9799-212X
Affiliation
Institute of Soil Science Soil Biophysics Leibniz University Hannover Hannover Germany
Peth, Stephan;
Affiliation
Department of Mathematics, Mathematical Institute for Machine Learning and Data Science, Chair of Geomatics and Geomathematics Catholic University of Eichstätt‐Ingolstadt Ingolstadt Germany
Ray, Nadja;
Affiliation
Department of Mathematics–Modelling and Numerics Friedrich‐Alexander University Erlangen‐Nürnberg Erlangen Germany
Prechtel, Alexander;
GND
111566784X
ORCID
0000-0002-9922-1107
Affiliation
Department of Hydrogeology, Institute for Geosciences Friedrich Schiller University Jena Jena Germany
Ritschel, Thomas;
ORCID
0000-0002-9489-1005
Affiliation
School of Life Sciences, Chair of Soil Science Technical University Munich Freising Germany
Schweizer, Steffen A.;
Affiliation
Institute of Soil Science Soil Chemistry Leibniz University Hannover Hannover Germany
Woche, Susanne K.;
Affiliation
Institute of Bio‐ and Geosciences Agrosphere (IBG‐3) Forschungszentrum Jülich GmbH Jülich Germany
Wu, Bei;
GND
113227426
ORCID
0000-0002-2692-213X
Affiliation
Department of Hydrogeology, Institute for Geosciences Friedrich Schiller University Jena Jena Germany
Totsche, Kai U.

The 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.

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