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

Journal of Plant Nutrition and Soil Science 2023 28 citations ? Citation count from OpenAlex, updated daily. May differ slightly from the publisher's own count. Score: 45 ? 0–100 AI score estimating relevance to the microplastics field. Papers below 30 are filtered from public browse.
Wulf Amelung, Eva Lehndorff, Vincent J.M.N.L. Felde, Ni Tang, Georg Guggenberger, Wulf Amelung, Eva Lehndorff, Wulf Amelung, Susanne K. Woche, Wulf Amelung, Georg Guggenberger, Nina Siebers, Erwin Klumpp, Wulf Amelung, Susanne K. Woche, Susanne K. Woche, Susanne K. Woche, Michaela Aehnelt, Stephan Peth, Vincent J.M.N.L. Felde, Wulf Amelung, Eva Lehndorff, Eva Lehndorff, Eva Lehndorff, Wulf Amelung, Wulf Amelung, Stephan Peth, Karin Eusterhues, Eva Lehndorff, Wulf Amelung, Vincent J.M.N.L. Felde, Stephan Peth, Wulf Amelung, Wulf Amelung, Stephan Peth, Eva Lehndorff, Georg Guggenberger, Klaus Kaiser, Wulf Amelung, Ingrid Kögel‐Knabner, Georg Guggenberger, Erwin Klumpp, Wulf Amelung, Wulf Amelung, Wulf Amelung, Claudia Knief, Jens Kruse, Eva Lehndorff, Robert Mikutta, Wulf Amelung, Stephan Peth, Wulf Amelung, Nadja Ray, Alexander Prechtel, Thomas Ritschel, Steffen A. Schweizer, Susanne K. Woche, Bei Wu, Kai Uwe Totsche

Summary

This review covers advanced methodologies for exploring the three-dimensional architecture of soil microaggregates (particles smaller than 250 micrometers), including imaging techniques that reveal pore space, mineral-organic interfaces, and microbial habitats. Understanding microaggregate structure is key to linking soil physical properties with carbon cycling and microbial ecology.

Abstract 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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