Structure–function co‐evolution during pedogenesis—Microaggregate development and turnover in soils DOI Open Access
Kai Uwe Totsche, Nadja Ray, Ingrid Kögel‐Knabner

и другие.

Journal of Plant Nutrition and Soil Science, Год журнала: 2024, Номер 187(1), С. 5 - 16

Опубликована: Фев. 1, 2024

The development of soil structure and its linkage to functions have become a major research theme boosted by the increasing threat health fertility due climate land-use changes. Water retention, flow fluids, matter dispersal, habitat provision, nutrient supply, organic element storage are fundamental life-sustaining ecosystem services. It is well accepted that soil's intimately linked architecture state aggregation, void network, composition properties solid–fluid biogeochemical interfaces therein (Figure 1). Broad consensus exists develops synergistic action physical, chemical, biological processes. Inspired these insights, we see growing number activities focus on unraveling intricate interplay interdependence in search theoretical framework allows for understanding function. Substantial progress has been achieved experimental pedogenesis joint application advanced spectroscopic, microscopic, tomographic techniques, which enabled studying structure, composition, interface already at submicron scale. In line with this, modeling endeavors give feedback designs testing various scenarios serve explore factors govern co-evolution function, or challenge concepts silico, considerably improved over last decade. This special issue responds awareness importance functioning soils other natural permeable media. We compile recent achievements shed light between "from pedon" scale delineate future directions. insights obtained from fields assembled here employ combinations experimental, observational, instrumental, computational methods will certainly allow deeper pathways fascinating function during pedogenesis. There broad functions, properties, traits is, spatial arrangement organic, inorganic, biotic components build fabric soil. At what point time this establishes, including as role variety materials diversity organisms play stability intrigued science decades. desire also inspired MADSoil consortium subject team combines empirical, theoretical, numerical expertise (Totsche et al., 2018). coordinated program was streamlined along two themes understand: Within explore, aimed characterize intact artificial microaggregates suite tomographic, spectroscopic instrumental techniques employed fashion. endeavor, however, required novel sophisticated (e.g., Amelung 2023; Bucka 2019; Dultz 2018; Guhra Krause Rodionov Ritschel 2023) approaches 2021; Felde 2019). understand link functions—habitat microorganisms, retention water, carbon, cycling elements—by rigorous mechanistic approach that, again, appropriate, comprehensive, operative codes explanatory power (Guhra Ray 2017; & Totsche, Rupp Zech, Ritschel, 2022; Schweizer, 2022). built premise quality depends physicochemical heterogeneity solid-void interfaces, so-called 2010), network morphology (cf. Rabot 2018) formation originate molecular interactions compounds act aggregate-forming composite building units Based suppositions, set hypotheses formation, stability, microscale were devised: Formation microaggregates. Aggregate follows deterministic patterns, reflected microaggregate-forming materials. Minerals like iron oxyhydroxides, phyllosilicate clay minerals, plant microbial residues nuclei Stability accumulation type increases amount pedogenic oxides fine Loss causes destabilization disintegration aggregates, release microaggregates, units, materials, then prone transport reaggregation. Functions Soil develop mineral controls turnover rate associated minerals. complexity microaggregate provides different ecological niches support diversity. community differ composition. These approached effort combined competences scientific disciplines, chemistry, mineralogy, physical microbiology, physics, data sciences, modeling. Recent outcomes be presented response three-dimensional build-up, called architecture, media microscale. MADSoil's comprised observational studies. closely investigations based simulations our observations aiming numerically 2). To separation investigation collected topsoil well-studied field sites Scheyern, Bavaria, Rotthalmünster. For studies, chose provided gradients contents minerals matter. included an optimization harmonization step optimize protocol analysis. With toposequence study, targeted (Biesgen 2020; 2018, Schweizer 2021). studies accompanied dedicated multi-stable-isotope labeling experiment, full consortium, able follow aggregation processes gluing agents inorganic cementing without presence roots (Amelung 2023). experiment 57Fe-labeled iron-oxihydroxide, 29Si-labeled 13C-labeled extracellular polymeric substances, 15N-labeled bacterial strain. depletion trial, their (composite) loss explored. Dedicated experiments focused (SOM) mechanical (Roosch 2024, issue; Siebers issue) impacts carbon (SOC) across rock fragment gradient (Schweizer issue). A series aggregate under conditions diverse typical temperate 2019, 2019) conducted. complemented Lehmann Pronk 2012; 2023): dynamic relocation explored against stress conditions, nuclei-framing examined disturbance 2024 [this issue]). Realizing advancement designs, analytical methods, sample preparation harmonized protocols multidisciplinary analysis Microaggregates commonly found part linings, crusts, embedded macroaggregates even larger aggregated structures frequently hierarchical organization. Thus, separating challenging delicate effort. comparative reasons published results, established wet fractions (Krause 2018), common isolate However, sieving known producing fractions, particular when sonication. example, cells removed surfaces uncontrolled manner, thereby precluding exploration original biogeography, thus relation (Bach mind, alternative dry developed, crushing load frame followed (Felde spectro-microscopic issue), becomes visible evolves complex bound aggregates Organo–mineral associations, small blocks studied. Aggregation up size rather rapid process (hours–weeks), mechanisms chronological order 2023), interrelated pedogenetic depending (Kögel-Knabner Amelung, arranged heterogeneous, random systematic organized pattern (Lehndorff Meyer Organic seems accumulate eventually patchy piled-up (Schweizer, Steffens 2017). variability involved build-up increased exhibiting hierarchy organo–mineral associations smallest compound 3). Various homo- und heteronucleation suspensions (Dultz identified (Bucka origin initiate accelerate resulted mineral, no nucleus. content clay-sized influences distribution stored occluded particulate (POM; Tang water related Fe-speciation (Siebers contrasting texture, al. (2024, studied using They dissolved caused water-stable shifted toward sizes. very low depended mainly but did not show strong correlation type. corresponds findings dry-separated soil, where higher SOC went difference strength samples compared cropped site, showed decrease post-modern 14C, Roosch pore connectivity contributed observed more concentrated effect decreasing both mineral-associated POM coarse fragments. further investigated laser ablation-isotope ratio mass spectrometry (Rodionov Sosa 2021), analyze decadal scales. could C reduced 58 years bulk 105 mean residence free agricultural (Rotthalmünster, Germany). only <5% micro-size fraction aggregated. abundance prokaryotic communities inhabiting responded differences matter, indicating strategists (Yao populations degraded POM, biomass contributes necromass promoting first step, while necromass-degrading bacteria role, likewise produce contribute aggregation. mixture decomposed fresh substances origin. includes exudates, lysis products, metabolites litter faunal tissues, biopolymers excreted from, roots, earthworms. numerous ways 2022), forming favoring inhibiting (Freitas 2015; Sheng 2016). might screening surfaces, agent, mediating particle (im-)mobilization (Flynn Pen 2015). Despite earthworms transfer into bioturbation mucus excretion (Brown 2000; Frelich Lavelle Stolze Szlavecz control earthworm constituents recently illuminated mucus–mineral narrow carbon/phosphorus carbon/nitrogen ratios, underpinning nutrients. activity results (re-)arrangement incorporation permeation intestinal cutaneous mucus. casts, linings burrow walls form consequence bioturbation. Considering high translocation nutrients down subsoils, attention should paid contribution biogenic polymer mixtures matterproperties. Over beyond, empirical relationship earthworms, dynamics predict structural compositional pedon impressive shapes initial stages host weathering maturation distinct horizons. dissolution neoformation, OM decomposition, metabolization stabilization, structuring, dispersion, colonization spread, unexplored many areas still awaits understanding. promising way illuminate nontrivial interdependencies empirically offered pedogenesis, representation tailored controlled boundary Hemkemeyer 2014; Münch 2002; 2012). (2023) time-lapse irrigating columns cumulative precipitation represented rainfall multiple conditions. way, authors spread total mobile inventory (Lehmann 2021) induced choosing limestone substrate weathering. features secondary released texture OC incubation soils. all variants. most pronounced clay-rich soils, having activity, independent texture. observation fosters how develop. Collaborative comprising scientists varying experience data-model integration struggle efficient quantitative framework, model. models, essential tools test silico derive causal dependencies settings, large big datasets variables mutually coupled multitude nonlinear, time-dependent relations. environmental sciences science, such models ideally integrate levels conceptual realized within approaches. guarantee make use theories farthest extent, devised supervised model collaborative interdisciplinary groups 4). aims comprehensible theories. model-data integration, web-based database binary objects (big data) needs comprise completeness produced data, (observational lab trials studies) (model runs, scenario simulation, sensitivity analysis, projections). ensures parametrization simulation parameters directly core moderated directed group involving whole consortium. formulation processes, interactions, rates, manners, mirror, anneal, confront individual researchers "semantic level." must seen crucial ongoing task. Confronting iterative refinement ("level evidence"). appropriate physics collecting developing laws reproduce reactions interactions. Hence, substantiation rates "natural laws," principles. Casting principles mathematical (Ray coding algorithms programs final steps bits bytes"). Successful presented, (2019), (2021), Zech (2020) entangled particularly expresses aggregates. necessitates assessment habitats (Van Leeuwen 2019), determines elements, retains channels fluids. combination regarding transport, attachment, re-arrangement reveal shaped emerge transition scales (Pot Roose Early (Crawford 1997, 2012) introduced self-organization cellular automaton setting binding key drivers (representing chemical bonds bindings products fungi). approaches, (2017) (2018) developed comprehensive toolbox simulate spatially temporally explicit complement discrete method rearrangement continuous partial differential equation fluids solutes. By specific it possible identify evolution establishment stationary structure. Complementarily, Totsche (2019) prototypical quartz, illite, goethite) diffusively displaced walk until they merge upon contact once Derjaguin-Landau-Verwey-Overbeek (DLVO)-type energy barrier overcome. physically allowed reconstructing milieu geometry 5). (2021) extended include gravity decisive mechanism settling particles and, therefore, fractionation accumulation. can decelerate among others relative velocity aqueous density size. Adopting prototypes approach, size, shape, formed. degree shielded oppositely charged main governs if favored hindered. Later, impact aspect ratio, surface charge, mixing heteroaggregation edge-to-edge edge-to-face card-house resemble those experiments. Building (2022) hydrolysis unsaturated, heterogeneous CO2 output. Finally, combining previous attempts simultaneous formation/disaggregation (Zech, revealed primed decomposition native addition 6). Last, exemplified continuum-scale pore-scale limitations diffusive oxygen availability, texture-dependent occlusion, determined production storage. Throughout applied tool subtle synergism inherent E-science, capital E referring "enhanced," describes paradigm forcefully consistently utilizes digital infrastructure aspects. E-science integrates resources concepts, tools. means questions organize capacities generating, analyzing, curating FAIR (i.e., findable, accessible, interoperable, reusable) publication results. observation, correlative increasingly finer spatiotemporal detail spectro-microscopy tomography multi-omics), disciplines generate operate Big Data, enormous rapidly state, development, acquisition, collection, storage, processing, curation information meta-analysis. operating Data unearthing hidden information, uncovering correlations, or, generally, analyzing relations patterns. objectives realm data-driven intelligence (AI), neural networks, machine learning, deep learning. If research, targeting generation structure–function relationships scenario-based projections ("digital twins"), drawing inferences management, rigorously biological, laws. Such intrinsically explanatory, logic reproducible, generated intelligible, decisions made traceable. Of course, informed populated wealth harbored available science. hand, answer "why" "how": Why result? How reached? Future efforts AI-based invest comprehensible-explanatory big-data inform algorithms. Soils vulnerable thin subsurface ecosystems. alter exchange energy, controlling phreatic zone groundwater. Assessing transformative metabolic ecosystems services provide sustain life. An unprecedented forward generating respect processing multi-omics, metagenomics, proteomics, metabolomics. aligning omics in-depth fingerprinting immobile insight hand. characterization actual activities, connected cycles identified. fluid fluxes domains life viruses, communities, interplay, proximate Climate changes affecting renewable manner. fertility, groundwater recharge quality, biodiversity, sequestration, cycling, production, mature increase temperature altered seasonal share, type, intensity precipitation, five governing constantly change. addition, alien floral species, wanted unwanted, migrate invade consequence, competition, ecology shifts, species extrusion, extinction. Effects microbiome degradative consequences greenhouse gas emission, retention. systems, micro-structured store retain extreme habitats, harbor Functional redundancy external finally Management strategies service protection restoration, change attenuation adaptation, aim conservation, amelioration Linchpin thorough effects land micron landscape So far, discussion relate confronted perspectives Vogel Yudina Kuzyakov, 2019): solid-phase perspective pore-phase perspective. one alleged conceive solids, primary ("solid phase perspective"). conceives voids pores, framed solid particles. Both "hierarchy" constitutive feature conceived complementary aspects Indeed, review, refer "soil solids considering (surface)." Ignoring topography, ignore exposed space particles, (micro-)aggregates, phases hyphae. habitat, so forth, governed variable topography emerging interface. anneal extent basis PIs Wulf Georg Guggenberger, Klaus Kaiser, Claudia Knief, Erwin Klumpp, Ingrid Kögel-Knabner, Eva Lehndorff, Robert Mikutta, Stephan Peth, Alexander Prechtl, Nadja Ray, Nina Siebers, Daniel Uteau, Bei Wu, Kai Totsche; postdoctoral Michaela Aehnelt, Stefan Dultz, Vincent Felde, Nele Meyer, Andrey Rodionov, Steffen Susanne Woche; PhDs Franziska Bucka, Danh Biesgen, Fechner, Tom Guhra, Jacqueline Kaldun, Lars Krause, Svenja Roosch, Andreas Rupp, Ni Tang, Tongyan Yao, Simon deeply acknowledged fruitful inspiring cooperation than 7 Research Unit MAD Soil—Microaggregates: (DFG RU 2179). highly appreciate financial Deutsche Forschungsgemeinschaft (Contract No 251268514) thankful continued Patricia Schmitz-Möller her DFG. Very thanks go Aehnelt least constructive engagement coordination unit. Thomas his constant endorsement Ina Voigt enthusiastic assistance sharing applicable article, analyzed current study.

Язык: Английский

Initial soil formation by biocrusts: Nitrogen demand and clay protection control microbial necromass accrual and recycling DOI
Baorong Wang, Yimei Huang, Na Li

и другие.

Soil Biology and Biochemistry, Год журнала: 2022, Номер 167, С. 108607 - 108607

Опубликована: Фев. 15, 2022

Язык: Английский

Процитировано

114

Nitrogen fertilizer builds soil organic carbon under straw return mainly via microbial necromass formation DOI
Xiangtian Meng, Xuechen Zhang,

Yunuo Li

и другие.

Soil Biology and Biochemistry, Год журнала: 2023, Номер 188, С. 109223 - 109223

Опубликована: Окт. 22, 2023

Язык: Английский

Процитировано

77

Will fungi solve the carbon dilemma? DOI Creative Commons
S. Emilia Hannula, Elly Morriën

Geoderma, Год журнала: 2022, Номер 413, С. 115767 - 115767

Опубликована: Фев. 12, 2022

Soils are hotspots of diversity and sustain many globally important functions. Here we focus on the most burning issue: how to keep soils as carbon sinks while maintaining their productivity. Evidence shows that life in plays a crucial role improving soil health yet ecological processes often ignored sciences. In this review, highlight potential fungi increase sequestration crop yield, functions needed human population Earth at same time livable. We propose management strategies steer towards more fungal activity but also high functional which will lead stable sources affects structure food web up ecosystem level. list knowledge gaps limit our ability communities such stabilising top becomes effective. Using natural capacity biodiverse community sequester delivers double benefit: reduction atmospheric dioxide by storing photosynthesized increasing agricultural yields restoring organic matter content degraded soils.

Язык: Английский

Процитировано

76

From rhizosphere to detritusphere – Soil structure formation driven by plant roots and the interactions with soil biota DOI Creative Commons
Carsten W. Mueller, Vera Baumert, Andrea Carminati

и другие.

Soil Biology and Biochemistry, Год журнала: 2024, Номер 193, С. 109396 - 109396

Опубликована: Март 9, 2024

Roots and the associated soil directly affected by root activity, termed rhizosphere, have both been extensively studied recognized for their crucial role in functioning. The formation of rhizosphere is primarily driven effect roots on shaping physical structure soil, which turn has direct feedbacks interactions between physical, biological chemical processes. As a result, hot spot microbial cycling nutrients turnover organic matter. Despite pivotal controlling processes, we still lack quantitative description understanding interrelationships root-systems creation stabilization structure. We provide comprehensive review current knowledge novel insights into processes that drive rhizosphere. These are regulated multiple indirect pathways, involving growth, production rhizodeposits hairs, as well activity microorganisms fauna. Further, highlight may persist evolve after death to an extent currently largely unknown. Finally, identify five pertinent challenges should be addressed fully apprehend thus harness potential resilience plant-soil interactions. include refining structural assessment sampling rhizosheaths, examining in-situ bridging gap solid phase pore scale research. In our view, overcoming these obstacles can accomplished combining power imaging isotopic approaches, especially at field scale, encompassing diverse soils plant species. ultimate objective future research upscale conducting more experiments concert with modeling efforts, under umbrella collaborative interdisciplinary

Язык: Английский

Процитировано

36

Evaluation of aggregate stability methods for soil health DOI Creative Commons
Elizabeth L. Rieke, Dianna K. Bagnall, Cristine L.S. Morgan

и другие.

Geoderma, Год журнала: 2022, Номер 428, С. 116156 - 116156

Опубликована: Сен. 18, 2022

Aggregate stability is a commonly used indicator of soil health because improvements in aggregate are related to reduced erodibility and improved soil–water dynamics. During the past 80 90 years, numerous methods have been developed assess stability. Limited comparisons among resulted varied magnitudes response management practices influences inherent properties climate. It not clear whether selection specific method creates any advantage investigator. This study assessed four measuring using data collected as part North American Project Evaluate Soil Health Measurements. The included water stable aggregates Cornell Rainfall Simulator (WSACASH), wet sieved (WSAARS), slaking captured adapted from SLAKES smart-phone image recognition software (STAB10), mean weight diameter (MWD). Influence climate at continental scale were analyzed addition responses rotation diversity, cash crop count, residue management, organic nutrient amendments, cover crops, tillage. moderately correlated with each other. All sensitive differences between sites, although different degrees. None measured significant effects diversity or but all detected increases resulting Significant positive trends observed for relation cropping, increased retention, except STAB10, which expressed slightly negative amendments. Considering these results, no single was clearly superior viable options Therefore, secondary considerations (e.g., cost, availability, sensitivity practice, minimal within-treatment variability) driven by needs investigator, should determine most suitable method.

Язык: Английский

Процитировано

65

Environmental implications of interaction between humic substances and iron oxide nanoparticles: A review DOI
Erika Di Iorio, Luana Circelli, Ruggero Angelico

и другие.

Chemosphere, Год журнала: 2022, Номер 303, С. 135172 - 135172

Опубликована: Май 29, 2022

Язык: Английский

Процитировано

57

Carbon allocation to root exudates is maintained in mature temperate tree species under drought DOI Creative Commons
Melanie Brunn, Benjamin Häfner, Marie J. Zwetsloot

и другие.

New Phytologist, Год журнала: 2022, Номер 235(3), С. 965 - 977

Опубликована: Апрель 11, 2022

Summary Carbon (C) exuded via roots is proposed to increase under drought and facilitate important ecosystem functions. However, it unknown how exudate quantities relate the total C budget of a drought‐stressed tree, that is, much net‐C assimilation allocated exudation at tree level. We calculated proportion daily root during early summer by collecting exudates from mature Fagus sylvatica Picea abies exposed experimental drought, combining above‐ belowground fluxes with leaf, stem fine‐root surface area. Exudation individual increased exponentially decreasing soil moisture, highest wilting point. Despite c . 50% reduced systems was maintained trees 1.0% ( F. ) 2.5% P. net into rhizosphere, increasing allocation two‐ three‐fold. Water‐limited released two‐thirds its soil, whereas in droughted only one‐third. Across entire system, similar controls, suggesting drought‐imposed investment, which could be beneficial for resilience.

Язык: Английский

Процитировано

55

Responses of soil aggregate stability and soil erosion resistance to different bedrock strata dip and land use types in the karst trough valley of Southwest China DOI Creative Commons

Fengling Gan,

Hailong Shi,

Junfei Gou

и другие.

International Soil and Water Conservation Research, Год журнала: 2023, Номер 12(3), С. 684 - 696

Опубликована: Сен. 7, 2023

Soil aggregate stability is an important index that reflects soil quality and anti-erosion ability strongly affects processes functions. Bedrock strata dips (dip anti-dip slopes) land use types primarily influence stability, whereas the detailed mechanisms are unclear in karst trough valley. Therefore, to explore effects of bedrock dip type on valleys, soils were collected from five major (abandoned land, grassland, pepper fields, corn fields forest) slopes. The was fractionated into macroaggregates microaggrates using dry wet sieving analysis. particle size distributions microaggregates measured conventional laboratories. results showed significant differences among different dips, slope positions, (P < 0.05). variation ranges higher than those slope. Comparing all types, forest had >0.25 mm water-stable aggregates (85.31%) mean weight diameter (2.67 mm) upper compared other positions In addition, a percentage destruction (35.57%) (29.81%), erodibility factor value natural dip/anti-dip significantly lower When content large larger, macroaggregate greater. failure rate lower, structure better. Overall, these suggest forests can improve aggregates, thereby improving erosion resistance. recovery measures should be implemented slopes valleys.

Язык: Английский

Процитировано

27

Changes in soil aggregate stability and aggregate-associated carbon under different slope positions in a karst region of Southwest China DOI

Shiwei Liu,

Rutong Wang,

Yang Yan

и другие.

The Science of The Total Environment, Год журнала: 2024, Номер 928, С. 172534 - 172534

Опубликована: Апрель 16, 2024

Язык: Английский

Процитировано

14

Synergistic impacts of Landscape, Soil, and environmental factors on the spatial distribution of soil aggregates stability in the Danjiangkou reservoir area DOI

Zhiguo Li,

Yusi Fan, Runhua Zhang

и другие.

CATENA, Год журнала: 2024, Номер 237, С. 107840 - 107840

Опубликована: Янв. 22, 2024

Язык: Английский

Процитировано

12