Geoderma

Papers
(The TQCC of Geoderma is 16. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-04-01 to 2025-04-01.)
ArticleCitations
The contribution of microbial activity to soil–water interactions and soil microstructural stability of a silty loam soil under moisture dynamics282
Modelling of soil mechanical stability and hydraulic permeability of the interface between coated biopore and matrix pore regions271
Thermogravimetric data suggest synergy between different organic fractions and clay in soil structure formation124
Preferential flow in soils is key to the development of nebkhas in water limited regions118
Variations and controlling factors of soil CO2 release at daytime and nighttime scales in the loess hilly regions of China116
Creating soil districts for Australia based on pedogenon mapping113
Impacts of groundwater storage variability on soil salinization in a semi-arid agricultural plain107
How will permafrost carbon respond to future climate change? A new assessment for future thaw trends of permafrost carbon on the Tibetan Plateau105
Soil physicochemical properties explain land use/cover histories in the last sixty years in China101
Soil dissolved organic matter quality and bacterial community composition regulate the substrate-binding affinity of hydrolytic enzymes under short-term nitrogen addition97
Chemical and hydrological controls on salt accumulation in irrigated soils of southwestern U.S97
Stronger link of nosZI than nosZII to the higher total N2O consumption in anoxic paddy surface soils90
Timber plantations do not homogenize soil arthropod diversity but do alter species composition85
Can application of liquid dairy manure onto no-tillage oxisols reduce runoff, sediment, phosphorus, and nitrogen losses over 9 years of natural rainfall?81
Nematodes require space: The relationship between nematode community assemblage and soil carbon across varying aggregate fractions80
Biochar amendment benefits 15N fertilizer retention and rhizosphere N enrichment in a maize-soil system79
Plant responses to nitrate and ammonium availability in Australian soils as measured by diffusive gradients in thin-films (DGT) and KCl extraction76
Diverse regulations on the accumulation of fungal and bacterial necromass in cropland soils75
Factors limiting microbial N2O and CO2 production in a cultivated peatland overlying an acid sulphate subsoil derived from black schist70
Litterfall quality modulates soil ammonium and nitrate supply through altering microbial function in bamboo encroachment of broadleaf forests67
Non-typical degraded and regraded humus forms in metal-contaminated areas, or there and back again66
Spatial distribution of urea induced ammonia loss potentials of German cropland soils65
Interaction of fulvic acid with soil organo-mineral nano-aggregates and corresponding phosphate release64
National-scale mapping of soil-thickness probability in hilly and mountainous areas of Japan using legacy and modern soil survey64
Soil organic carbon stocks maintained despite intensification of shifting cultivation63
Effect of smart phone cameras on color-based prediction of soil organic matter content63
Land-use- and climate-mediated variations in soil bacterial and fungal biomass across Europe and their driving factors61
Geochemical evidence of illuvial processes in clay-rich soils on limestones in a humid temperate climate61
Lithology-driven soil properties control of N2O production by ammonia oxidizers in subtropical forest soils61
Deep soil moisture limits the sustainable vegetation restoration in arid and semi-arid Loess Plateau60
Soil carbon change in intensive agriculture after 25 years of conservation management59
Geochemical factors controlling the mobilization of geogenic cadmium in soils developed on carbonate bedrocks in Southwest China59
Crop rotational diversity enhances soil microbiome network complexity and multifunctionality59
Molecular diversity and the fate of biochemical fractions of eucalypt tissues in soil58
Nitrogen immobilization caused by chemical formation of black- and amide-N in soil57
Field-ready methods for casting soil biopores56
Visual assessment of soil structural quality across soil textures and compaction levels – Part II: Examination of profile walls vs Intact soil cores56
Deforestation alters protease regulation by amino acids55
Editorial Board54
Editorial Board54
Linkages between soil organic matter and magnetic mineral formation in agricultural fields in southeastern Minnesota, USA53
Editorial Board52
Editorial Board52
Soil organic matter changes under experimental pedoclimatic modifications in mountain grasslands of the French Alps52
Editorial Board52
Dual effects of carbon in Red Ferralitic soils in the San José de Las Lajas Polje, Cuba51
Microbial mechanisms for methane source-to-sink transition after wetland conversion to cropland51
Influences of plant traits on the retention and redistribution of bioavailable nitrogen within the plant-soil system51
Soil burrow characterization by 3D image analysis: Prediction of macroinvertebrate groups from biopore size distribution parameters50
Weathering of Viamão granodiorite, South Brazil: Part 1 – Clay minerals formation and increase in total porosity50
Spectral soil analysis for fertilizer recommendations by coupling with QUEFTS for maize in East Africa: A sensitivity analysis50
Editorial Board50
Comment on “Characterizing detachment and transport processes of interrill soil erosion, Geoderma 376 (2020) 114549”50
A Bayesian approach to understand controls on total and labile soil carbon in cultivated soils of Central and Southern Malawi49
An improved estimate of soil carbon pool and carbon fluxes in the Qinghai-Tibetan grasslands using data assimilation with an ecosystem biogeochemical model49
Soil chemical extractions can alter potassium coordination in agricultural soils: A combined wet chemical and X-ray absorption spectroscopic approach49
Soil spectroscopy with the Gaussian pyramid scale space49
Editorial Board49
Sustained increases in soil respiration accompany increased carbon input under long-term warming across global grasslands48
Validation of uncertainty predictions in digital soil mapping48
Can fusion of vis-NIR and MIR spectra at three levels improve the prediction accuracy of soil nutrients?48
Microplastics effects on wettability, pore sizes and saturated hydraulic conductivity of a loess topsoil48
Integrating multi-year crop inventories as a proxy for soil management within a digital soil mapping framework for predicting nitrogen indices47
Factors controlling peat soil thickness and carbon storage in temperate peatlands based on UAV high-resolution remote sensing47
Integration of multimodal data for large-scale rapid agricultural land evaluation using machine learning and deep learning approaches47
Aggregate stability and size distribution regulate rainsplash erosion: Evidence from a humid tropical soil under different land-use regimes47
Responses of soil nitrogen cycling to changes in aboveground plant litter inputs: A meta-analysis47
Impacts of 21-year field warming on soil erodibility in the Qinghai-Tibetan Plateau, China46
Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland46
The organic layer reduces water repellency of surface mineral soil under a humid-temperate forest46
Nitrogen-fixing tree species rather than tree species diversity shape soil nematode communities in subtropical plantations46
Paired resampling to detect field-level soil organic carbon stock change. Comment on “Testing the feasibility of quantifying change in agricultural soil carbon stocks through empirical sampling” by Br45
Simulation of soil water content through the combination of meteorological and satellite data44
Phosphorus limitation reduces microbial nitrogen use efficiency by increasing extracellular enzyme investments44
Editorial Board44
Long-term drainage induces divergent changes of soil organic carbon contents but enhances microbial carbon accumulation in fen and bog44
Metal cation concentrations improve understanding of controls on soil organic carbon across a precipitation by vegetation gradient in the Patagonian Andes44
Contribution of root decay process on soil infiltration capacity and soil water replenishment of planted forestland in semi-arid regions43
Biochar-based urea increases soil methane uptake in a subtropical forest43
Allocation of foliar-P fractions of Alhagi sparsifolia and its relationship with soil-P fractions and soil properties in a hyperarid desert ecosystem43
Artificial light at night triggers negative impacts on nutrients cycling and plant health regulated by soil microbiome in urban ecosystems43
Modelling changes in soil structure caused by livestock treading43
Carbon dynamics as a function of soil moisture following repeated wet-dry cycles in irrigated soils43
Improved geochemical baseline establishment based on diffuse sources contribution of potential toxic elements in agricultural alluvial soils43
Litter quality, mycorrhizal association, and soil properties regulate effects of tree species on the soil fauna community43
The role of Nyctelia circumundata (Coleoptera: Tenebrionidae) on litter fragmentation processes and soil fertility in northeastern arid patagonia42
Relationships of priming effects with organic amendment composition and soil microbial properties42
Comparison of three quantification methods used to detect biochar carbon migration in a tropical soil: A 4.5-year field experiment in Zambia42
Estimating lime requirements for tropical soils: Model comparison and development42
Spatial distributions and the main driving factors of soil total nitrogen in Zhejiang Province, China42
Vertical distribution and variability of soil organic carbon and CaCO3 in deep Colluvisols modeled by hyperspectral imaging41
Soil analysis is pivotal for fertilizer recommendations: Comment on “Soil based, field specific fertilizer recommendations are a pipe-dream” by A.G.T. Schut and K.E. Giller. Geoderma (https:/doi.org/141
Spatial predictions of maize yields using QUEFTS – A comparison of methods41
Uncertainty assessment of soil available water capacity using error propagation: A test in Languedoc-Roussillon41
Evaluating soil water and salt transport in response to varied rainfall events and hydrological years under brackish water irrigation in the North China Plain40
Long-term effects of crop rotation and nitrogen fertilization on phosphorus cycling and balances in loess-derived Mollisols40
Assessing the accumulation efficiency of various microbial carbon components in soils of different minerals40
Soil inorganic carbon distribution, stocks and environmental thresholds along a major climatic gradient40
Applications and challenges of digital soil mapping in Africa40
Manure application decreases soil organic carbon priming by increasing mineral protection and nitrogen availability39
Linking fungal community structure with soil nitrogen dynamics following forest conversion in a subalpine forest in China39
Low-grade silicate minerals as value-added natural potash fertilizer in deeply weathered tropical soil39
Soil pH does not interfere with nitrification inhibitor efficiency for reducing N2O emissions from soils treated with concentrated vinasse and urea39
Urban soil properties distinguished by parent material, land use, time since urbanization, and pre-urban geomorphology39
Evidence for preservation of organic carbon interacting with iron in material displaced from retrogressive thaw slumps: Case study in Peel Plateau, western Canadian Arctic39
Legacy of plaggen agriculture: High soil organic carbon stocks as result from high carbon input and volume increase38
Arsenic-triggered bacterial minorities correlate with arsenic accumulation in cabbage38
Ammonia-oxidizing bacteria-driven autotrophic nitrification dominated nitrous oxide production in calcareous soil under long term plastic film mulching38
The time it takes to reduce soil legacy phosphorus to a tolerable level for surface waters: What we learn from a case study in the catchment of Lake Baldegg, Switzerland38
Enhanced plant growth in the presence of earthworms correlates with changes in soil microbiota but not nutrient availability38
Microbes with high–abundance attributes dominate the prokaryote communities of saline–alkali soil and construct more complex networks in the plant rhizosphere38
Genesis of lamellae in sandy soils: A case study in a semi-arid region in NE-Brazil37
Pre-conversion soil organic carbon level did not affect accumulation rate following conversion from arable land to semi-natural grassland37
Fragmentation alters the soil water conservation capacity of hillside alpine meadows on the Qinghai-Tibetan Plateau37
Comammox bacteria and ammonia oxidizing archaea are major drivers of nitrification in glacier forelands37
Effect of Nostoc commune cover on shallow soil moisture, runoff and erosion in the subtropics37
The Dutch soil physical units map: BOFEK37
Characterizing erosion processes on a convex slope based on 3D reconstruction method37
Effectiveness of mixed cultivated grasslands to reduce sediment concentration in runoff on hillslopes in the Qinghai-Tibetan Plateau37
Immediate and prolonged effects of snow coverage alteration on soil carbon dynamics and microbial activity: A meta-analysis36
Food security in a changing climate starts with managing soil water repellency36
On the parsimony, interpretability and predictive capability of a physically−based model in the optical domain for estimating soil moisture content36
Improving Soil Quality Index Prediction by Fusion of Vis-NIR and pXRF spectral data36
Forest gap regulates soil nematode community through understory plant diversity and soil pH35
Global meta-analysis reveals differential effects of climate and litter quality on soil fauna-mediated litter decomposition across size classes35
Mineral-organic interactions drive the aging and stabilization of exogenous Pb in soils35
Fractionation of stable boron isotopes in alfisols: Application of a novel tool for tracing boron behavior in two soil profiles35
Heat pulse probe design optimization using numerical simulation35
Exploring spatiotemporal dynamics in temporal stability of soil carbon, nitrogen, phosphorus, and pH in Tibetan grasslands35
Experimental drought increased the belowground sink strength towards higher topsoil organic carbon stocks in a temperate mature forest35
Estimating soil bacterial abundance and diversity in the Southeast Qinghai-Tibet Plateau35
Local parallel free generation and dynamic affine transformation method for soil three-dimensional pore structure information model35
No-tillage does not on average reduce soil carbon storage compared to conventional tillage. Comment on “Declines in soil carbon storage under no tillage can be alleviated in the long run” by Cai et al35
Digging deeper to find the effect of long-term greenhouse cultivation with excessive fertilization and irrigation on the structure and assemblage of soil bacterial community35
Decadal warming-induced changes in abiotic factors and multitrophic diversity drive soil multifunctionality in an alpine meadow35
Response time of soil moisture to rain in a vineyard with permanent cover35
Seasonal change of tensile crack morphology and its spatial distribution along gully bank and gully slope in the Mollisols region of Northeast China35
New insights into the swelling of black soil aggregates35
Environmental memory of microbes regulates the response of soil enzyme kinetics to extreme water events: Drought-rewetting-flooding34
Use of composite samples and NIR spectroscopy to detect changes in SOC contents34
Effects of carbon input quality and timing on soil microbe mediated processes34
Differences in the flow of spruce-derived needle leachates and root exudates through a temperate coniferous forest mineral topsoil34
Rediscovering the edaphic knowledge of smallholder farmers in southern Ecuador34
Effect of snow cover on water content, carbon and nutrient availability, and microbial biomass in complexes of biological soil crusts and subcrust soil in the desert34
Evaluation of 14 frozen soil thermal conductivity models with observations and SHAW model simulations34
Nematode community structure and functional guilds differ in tea fields and tropical forest33
Phosphorus solubility changes following additions of bioenergy wastes to an agricultural soil: Implications for crop availability and environmental mobility33
Phosphorus abundance and speciation in acid forest Podzols – Effect of postglacial weathering33
Global patterns and influencing factors of Mn accumulation in litter at different decomposition stages—A synthesis33
The high content of mineral-free organic matter in soils increases their vulnerability to wildfire in humid-temperate zones33
Cumulative effects of salvage logging and slash removal on erosion, soil functioning indicators and vegetation in a severely burned area in NW Spain33
Anthropogenic and climatic shaping of soil nitrogen properties across urban-rural-natural forests in the Beijing metropolitan region33
Monitoring soil organic matter on grassland farms: An exploratory analysis33
Drainage estimation across mountainous regions from large-scale soil moisture observations33
Enhanced topsoil P leaching in a short term flooded calcareous soil with combined straw and ammonium nitrogen incorporation33
Changes in the activity of soil enzymes after fire33
25-years of stewardship programs enhance regenerative outcomes in river delta soils of southwestern British Columbia, Canada33
Berken plow and intercropping with pigeon pea ameliorate degraded soils with a hardpan in the Ethiopian highlands33
Rangeland application of biochar and rotational grazing interact to influence soil and plant nutrient dynamics33
Effects of nitrogen addition and precipitation alteration on soil respiration and its components in a saline-alkaline grassland33
Effects of shell sand content on soil physical properties and salt ions under simulated rainfall leaching33
Arsenic sorption and oxidation by natural manganese-oxide-enriched soils: Reaction kinetics respond to varying environmental conditions33
Equations for soil freezing characteristics curves based on the thermodynamics principles33
Slash-and-burn in karst regions lowers soil gross nitrogen (N) transformation rates and N-turnover32
Macroaggregate persistence: Definition and applications to describe soil surface dynamics32
Early-Mid Holocene climatic changes inferred from colors of eolian deposits in the Mu Us Desert32
Impact of invasive alien tree species on symbiotic soil fungal communities in pine-dominated forest ecosystems in central Europe32
Changes in pools of organic matter and major elements in the soil following prescribed pastoral burning in the central Pyrenees32
Soil aminopeptidase activities under 145-year crop rotation and fertility practices in the North Central US32
Geographic variations of aggregate mechanical stability controlled by inorganic cementing agents across the East Asian monsoon region32
Substrate quality effects on stabilized soil carbon reverse with depth31
Estimating soil organic carbon stock change at multiple scales using machine learning and multivariate geostatistics31
Negative priming effect from tree leaf and root residues with contrasting chemical composition31
Comparing laser-induced breakdown spectroscopy and visible near-infrared spectroscopy for predicting soil properties: A pan-European study31
Temperature and moisture alter organic matter composition across soil fractions31
Mapping and describing natural terroir units in Denmark31
Quantifying sediment source contributions in an agricultural catchment with ephemeral and classic gullies using 137Cs technique31
Organic matter governs weathering rates and microstructure evolution during early pedogenesis31
Arbuscular mycorrhizal hyphal networks and glomalin-related soil protein jointly promote soil aggregation and alter aggregate hierarchy in Calcaric Regosol31
Effects of biochar amendment on tomato rhizosphere bacterial communities and their utilization of plant-derived carbon in a calcareous soil31
Stimulating effects of snow cover on gaseous nitrogen emissions are intensified by biological soil crusts31
Additive effects of organic and inorganic amendments can significantly improve structural stability of a sodic dispersive subsoil31
Estimation of soil organic matter content based on spectral indices constructed by improved Hapke model31
Weathering of calcareous bedrocks is strongly affected by the activity of soil microorganisms30
Sensitivity of soil dust emissions to driving factor variability in earth's main drylands30
Enhancing farmers’ soil conservation behavior: Beyond soil science knowledge30
The impact of biochar on the activities of soil nutrients acquisition enzymes is potentially controlled by the pyrolysis temperature: A meta-analysis30
Iron isotope fractionation during the formation of ferromanganese nodules under different conditions of hydromorphism30
A global numerical classification of the soil surface layer30
Dissolved organic matter as a confounding factor in the determination of pollution-induced community tolerance (PICT) of bacterial communities to heavy metals using the leucine incorporation method30
A systematic approach to predicting and mapping soil particle size distribution from unknown samples using large mid-infrared spectral libraries covering large-scale heterogeneous areas30
N, P and straw return influence the accrual of organic carbon fractions and microbial traits in a Mollisol30
A novel retrieval model for soil salinity from CYGNSS: Algorithm and test in the Yellow River Delta30
Using soil classification to improve interpretation of biological soil health indicators30
Rare earth elements associated with pedogenic iron oxides in humid and tropical soils from different parent materials30
Aluminum speciation in forest soils and forest floor density fractions using synchrotron-based XANES spectroscopy29
The role of inherited characteristics from parent materials in shaping bacterial communities in agricultural soils29
Mechanisms underlying the responses of soil N2O production by ammonia oxidizers to nitrogen addition are mediated by topography in a subtropical forest29
Testing the feasibility of quantifying change in agricultural soil carbon stocks through empirical sampling29
Developing spectrotransfer functions (STFs) to predict basic physical and chemical properties of calcareous soils29
A novel local-global dependency deep learning model for soil mapping29
Pedogenic pathways and deep weathering controls on soil organic carbon in Pacific Northwest forest soils29
Impact of calcareous concretions on soil shrinkage of a Vertisol and their relation model development29
Changes in physicochemical properties on a chronosequence of gold mine tailings29
Measuring sand content using sedimentation, spectroscopy, and laser diffraction29
Evidence of prehistoric and early medieval agriculture and its impact on soil and land relief transformation in the Białowieża natural forest (NE Poland)29
Modeling dust emission in alpine regions with low air temperature and low air pressure – A case study on the Qinghai-Tibetan Plateau (QTP)29
Impact of burning on soil organic carbon of maize-upland rice system in Mae Chaem Basin of Northern Thailand29
Global meta-analysis reveals positive effects of biochar on soil microbial diversity29
Intensity and duration of exposure determine prokaryotic community response to salinization in freshwater wetland soils28
Variation in matric potential at field capacity in stony soils of fluvial and alluvial fans28
Digital soil mapping of peatland using airborne radiometric data and supervised machine learning – Implication for the assessment of carbon stock28
Using remote sensors to predict soil properties: Radiometry and peat depth in Dartmoor, UK28
Green more than brown food resources drive the effect of simulated climate change on Collembola: A soil transplantation experiment in Northeast China28
Identifying plant cell wall remnants in detritus of a subtropical wetland with fluorescence labeling28
Storage of persistent organic matter in temperate gypsum soils –Relevance of the parent material and vegetation cover28
Does calculation method affect the nutrient-addition effect on priming?28
Climate and intertidal zonation drive variability in the carbon stocks of Sri Lankan mangrove forests28
Effects of forest fires on soil lead elemental contents and isotopic ratios28
Differentiation of fine-textured podzolic soils controlled by climate and landscape in Taiwan28
Role of compaction and drying-wetting cycles on the capability of precompression stress to indicate load history of heavily disturbed soils27
Redox-driven changes in organic C stabilization and Fe mineral transformations in temperate hydromorphic soils27
New insights into organic carbon stabilization in soil macroaggregates: An in situ study by optical microscopy and SEM-EDS technique27
Seeing the forest for the fractions – Comparing soil organic matter fractionation methods using molecular features after forest stand conversion27
Arbuscular mycorrhizal symbiosis enhances water stable aggregate formation and organic matter stabilization in Fe ore tailings27
Estimating root zone soil moisture using the SMAR model and regression method at a headwater catchment with complex terrain27
Arbuscular mycorrhizal traits are good indicators of soil multifunctionality in drylands27
Changes in soil microbial communities and priming effects induced by rice straw pyrogenic organic matter produced at two temperatures27
Multi-objective optimization sampling based on Pareto optimality for soil mapping27
Heat-induced changes in soil water-extractable organic matter characterized using fluorescence and FTIR spectroscopies coupled with dimensionality reduction methods27
Seasonal cryogenic processes control supra-permafrost pore water chemistry in two contrasting Cryosols27
Evaluating the impact of using digital soil mapping products as input for spatializing a crop model: The case of drainage and maize yield simulated by STICS in the Berambadi catchment (India)27
Estimating and modelling the risk of redox-sensitive phosphorus loss from saturated soils using different soil tests27
Cover crop root-derived organic carbon influences aggregate stability through soil internal forces in a clayey red soil27
Corrigendum to “Organic carbon in Mollisols of the world − A review” [Geoderma 447 (2024) 116937]27
Sample design optimization for soil mapping using improved artificial neural networks and simulated annealing27
Livestock trampling regulates the soil carbon exchange by mediating surface roughness and biocrust cover26
Land use conversion and soil moisture affect the magnitude and pattern of soil-borne N2, NO, and N2O emissions26
Combining UAV remote sensing and pedological analyses to better understand soil piping erosion26
Potential of soil minerals to sequester soil organic carbon26
Carbon sequestration potential and fractionation in soils after conversion of cultivated land to hedgerows26
Do soil names matter in scientific publications?26
The effectiveness of digital soil mapping with temporal variables in modeling soil organic carbon changes26
Multivariate random forest for digital soil mapping26
Relationships between soil biodiversity and multifunctionality in croplands depend on salinity and organic matter26
Reducing location error of legacy soil profiles leads to improvement in digital soil mapping26
Response of soil erosion to vegetation and terrace changes in a small watershed on the Loess Plateau over the past 85 years26
Corrigendum to “Borehole nuclear magnetic resonance as a promising 3D mapping tool in peatland studies” [Geoderma 443 (2024) 116814]26
Applying biochar under topsoil facilitates soil carbon sequestration: A case study in a dryland agricultural system on the Loess Plateau26
Decreased CH4 emissions associated with methanogenic and methanotrophic communities and their interactions following Fe(III) fertiliser application in rice paddies26
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