Biology and Fertility of Soils

Papers
(The median citation count of Biology and Fertility of Soils is 5. 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 2020-09-01 to 2024-09-01.)
ArticleCitations
Phospholipid fatty acids in soil—drawbacks and future prospects100
Diversity and co-occurrence network modularization of bacterial communities determine soil fertility and crop yields in arid fertigation agroecosystems55
Long-term manuring increases microbial carbon use efficiency and mitigates priming effect via alleviated soil acidification and resource limitation53
Divergent mineralization of hydrophilic and hydrophobic organic substrates and their priming effect in soils depending on their preferential utilization by bacteria and fungi47
Biological nitrification inhibition in maize—isolation and identification of hydrophobic inhibitors from root exudates44
Hyphosphere microbiome of arbuscular mycorrhizal fungi: a realm of unknowns42
Carbon investment into mobilization of mineral and organic phosphorus by arbuscular mycorrhiza39
Microbial carbon-use efficiency and straw-induced priming effect within soil aggregates are regulated by tillage history and balanced nutrient supply39
Depth distribution of soil organic matter and burrowing activity of earthworms—mesocosm study using X-ray tomography and luminophores38
Soil microbial biomass phosphorus can serve as an index to reflect soil phosphorus fertility34
Biochar co-application mitigated the stimulation of organic amendments on soil respiration by decreasing microbial activities in an infertile soil34
Litter-inhabiting fungi show high level of specialization towards biopolymers composing plant and fungal biomass33
Plant growth–promoting bacteria improve maize growth through reshaping the rhizobacterial community in low-nitrogen and low-phosphorus soil33
Revisiting plant biological nitrification inhibition efficiency using multiple archaeal and bacterial ammonia-oxidising cultures33
The effect of agroecosystem management on the distribution of C functional groups in soil organic matter: A review33
Rare microbial taxa rather than phoD gene abundance determine hotspots of alkaline phosphomonoesterase activity in the karst rhizosphere soil32
Earthworm ecological categories are not functional groups32
Biochar accelerates soil organic carbon mineralization via rhizodeposit-activated Actinobacteria32
C:P stoichiometric imbalance between soil and microorganisms drives microbial phosphorus turnover in the rhizosphere31
Importance of substrate quality and clay content on microbial extracellular polymeric substances production and aggregate stability in soils31
Application of N2-fixing Paenibacillus triticisoli BJ-18 changes the compositions and functions of the bacterial, diazotrophic, and fungal microbiomes in the rhizosphere and root/shoot endosphere of w30
Hydrolyzable microplastics in soil—low biodegradation but formation of a specific microbial habitat?29
A new primer set for Clade I nosZ that recovers genes from a broader range of taxa28
Effects of moisture and temperature on C and N mineralization from surface-applied cover crop residues27
Revealing interactions between root phenolic metabolomes and rhizosphere bacterial communities in Populus euphratica plantations26
Root exudation of contrasting drought-stressed pearl millet genotypes conveys varying biological nitrification inhibition (BNI) activity25
Theory of microbial coexistence in promoting soil–plant ecosystem health25
Higher ammonium-to-nitrate ratio shapes distinct soil nitrifying community and favors the growth of Moso bamboo in contrast to broadleaf tree species25
Biochar significantly reduced nutrient-induced positive priming in a subtropical forest soil25
Effects of rotational and continuous overgrazing on newly assimilated C allocation25
Repeated litter inputs promoted stable soil organic carbon formation by increasing fungal dominance and carbon use efficiency24
Shifts in soil microbial stoichiometry and metabolic quotient provide evidence for a critical tipping point at 1% soil organic carbon in an agricultural post-mining chronosequence22
Fatty acid 16:1ω5 as a proxy for arbuscular mycorrhizal fungal biomass: current challenges and ways forward22
Identification and verification of key functional groups of biochar influencing soil N2O emission22
Long-term elevated CO2 and warming enhance microbial necromass carbon accumulation in a paddy soil22
Mycorrhizal symbiosis balances rootstock-mediated growth-defence tradeoffs22
Biochar decreased rhizodeposits stabilization via opposite effects on bacteria and fungi: diminished fungi-promoted aggregation and enhanced bacterial mineralization21
Phosphorus fertilization rather than nitrogen fertilization, growing season and plant successional stage structures arbuscular mycorrhizal fungal community in a subtropical forest21
Biochar modifies the content of primary metabolites in the rhizosphere of well-watered and drought-stressed Zea mays L. (maize)21
Co-incorporating leguminous green manure and rice straw drives the synergistic release of carbon and nitrogen, increases hydrolase activities, and changes the composition of main microbial groups21
Effect of protists on rhizobacterial community composition and rice plant growth in a biochar amended soil20
Effects of the nitrification inhibitor 3,4-dimethylpyrazole phosphate (DMPP) on the activity and diversity of the soil microbial community under contrasting soil pH20
Heterotrophic nitrification of organic nitrogen in soils: process, regulation, and ecological significance20
Repeated drying and rewetting cycles accelerate bacterial growth recovery after rewetting20
Inhibitory effect of high nitrate on N2O reduction is offset by long moist spells in heavily N loaded arable soils20
Different community compositions between obligate and facultative oomycete plant parasites in a landscape-scale metabarcoding survey19
Organic nitrogen fertilization benefits selected soil fauna in global agroecosystems19
Impact of nitrogen and phosphorus addition on resident soil and root mycobiomes in beech forests19
Recommendations for stronger biochar research in soil biology and fertility18
Field-aged biochar decreased N2O emissions by reducing autotrophic nitrification in a sandy loam soil18
Seed coat treatment by plant-growth-promoting rhizobacteria Lysobacter antibioticus 13–6 enhances maize yield and changes rhizosphere bacterial communities17
Effects of crabs on greenhouse gas emissions, soil nutrients, and stoichiometry in a subtropical estuarine wetland17
Biological activities affect the dynamic of P in dryland soils17
Procyanidin inhibited N2O emissions from paddy soils by affecting nitrate reductase activity and nirS- and nirK-denitrifier populations17
Effects of synthetic nitrification inhibitor (3,4-dimethylpyrazole phosphate; DMPP) and biological nitrification inhibitor (methyl 3-(4-hydroxyphenyl) propionate; MHPP) on the gross N nitrification ra17
Mineralisation of distinct biogas digestate qualities directly after application to soil17
Correlation of the abundance of bacteria catalyzing phosphorus and nitrogen turnover in biological soil crusts of temperate forests of Germany17
3, 4-Dimethylpyrazole phosphate is an effective and specific inhibitor of soil ammonia-oxidizing bacteria17
Soil-root interface influences the assembly of the endophytic bacterial community in rice plants16
BNI-release mechanisms in plant root systems: current status of understanding16
Biotic and abiotic controls on carbon storage in aggregates in calcareous alpine and prealpine grassland soils16
Dissimilatory nitrate reduction to ammonium increased with rising temperature16
High frequency of extreme precipitation increases Stipa grandis biomass by altering plant and microbial nitrogen acquisition15
Temporal dynamics of total and active prokaryotic communities in two Mediterranean orchard soils treated with solid anaerobic digestate or managed under no-tillage15
Resource stoichiometric and fertility in soil15
Biological nitrification inhibition by sorghum root exudates impacts ammonia-oxidizing bacteria but not ammonia-oxidizing archaea15
Carbon fluxes within tree-crop-grass agroforestry system: 13C field labeling and tracing15
Mineral N suppressed priming effect while increasing microbial C use efficiency and N2O production in sandy soils under long-term conservation management15
Soil pH and long-term fertilization affect gross N transformation and N2O production pathways in Chinese and UK croplands15
Chemical properties of agro-waste compost affect greenhouse gas emission from soils through changed C and N mineralisation15
Responses of microbial activity to carbon, nitrogen, and phosphorus additions in forest mineral soils differing in organic carbon content15
Sensitive control of N2O emissions and microbial community dynamics by organic fertilizer and soil interactions15
Effects of two wood-based biochars on the fate of added fertilizer nitrogen—a 15N tracing study14
Dissimilatory nitrate ammonification and N2 fixation helps maintain nitrogen nutrition in resource-limited rice paddies14
Synergism between feremycorrhizal symbiosis and free-living diazotrophs leads to improved growth and nutrition of wheat under nitrogen deficiency conditions14
Steering microbiomes by organic amendments towards climate-smart agricultural soils14
Spatial analysis of the root system coupled to microbial community inoculation shed light on rhizosphere bacterial community assembly14
Proteomic changes of viable but nonculturable (VBNC) Escherichia coli O157:H7 induced by low moisture in an artificial soil13
Greenhouse gas (CO2, CH4, and N2O) emissions after abandonment of agriculture13
Impacts of application of calcium cyanamide and the consequent increase in soil pH on N2O emissions and soil bacterial community compositions13
Newly assimilated carbon allocation in grassland communities under different grazing enclosure times13
Contrasting response of organic carbon mineralisation to iron oxide addition under conditions of low and high microbial biomass in anoxic paddy soil13
Promoting soil microbial-mediated suppressiveness against Fusarium wilt disease by the enrichment of specific fungal taxa via crop rotation13
Soil N2O flux and nitrification and denitrification gene responses to feed-induced differences in the composition of dairy cow faeces13
Effect of soil bacteriomes on mycorrhizal colonization by Rhizophagus irregularis—interactive effects on maize (Zea mays L.) growth under salt stress13
Long-term appropriate N management can continuously enhance gross N mineralization rates and crop yields in a maize-wheat rotation system13
Saltwater incursion regulates N2O emission pathways and potential nitrification and denitrification in intertidal wetland12
Coupling of δ13C and δ15N to understand soil organic matter sources and C and N cycling under different land-uses and management: a review and data analysis12
Substrate and community regulations on microbial necromass accumulation from newly added and native soil carbon12
High nitrogen uptake and utilization contribute to the dominance of invasive Spartina alterniflora over native Phragmites australis12
Crop residue application at low rates could improve soil phosphorus cycling under long-term no-tillage management12
Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability12
Competition for S-containing amino acids between rhizosphere microorganisms and plant roots: the role of cysteine in plant S acquisition12
A shift from nitrification to denitrification-dominated N2O emission in an acidic soil following organic amendment12
Microbial and isotopomer analysis of N2O production pathways in a calcareous film-mulched farmland12
Syringic acid from rice as a biological nitrification and urease inhibitor and its synergism with 1,9-decanediol12
Deepened snow cover alters biotic and abiotic controls on nitrogen loss during non-growing season in temperate grasslands11
Diurnal dynamics can modify plant–microbial competition for N uptake via C allocation11
Pyrogenic organic matter decreases while fresh organic matter increases soil heterotrophic respiration through modifying microbial activity in a subtropical forest11
The mineralosphere—interactive zone of microbial colonization and carbon use in grassland soils11
Divergent mineralization of exogenous organic substrates and their priming effects depending on soil types11
Determining the effect of soil properties on the stability of scopoletin and its toxicity to target plants11
Discrepancy in exchangeable and soluble ammonium-induced effects on aerobic methane oxidation: a microcosm study of a paddy soil11
Nucleic acids are a major pool of hydrolyzable organic phosphorus in arable organic soils of Southern Ontario, Canada11
Evidence of endophytic nitrogen fixation as a potential mechanism supporting colonization of non-nodulating pioneer plants on a glacial foreland11
Cyanobacterium-primed Chrysanthemum nursery improves performance of the plant and soil quality10
Long-term sod-based rotation promotes beneficial root microbiomes and increases crop productivity10
Common mycorrhizal networks benefit to the asymmetric interspecific facilitation via K exchange in an agricultural intercropping system10
Crop root vs. shoot incorporation drives microbial residue carbon accumulation in soil aggregate fractions10
Assessing the impacts of tillage, cover crops, nitrification, and urease inhibitors on nitrous oxide emissions over winter and early spring10
The priming effect dynamics are driven by microbial activation and growth and constrained by the relative availability of input C and soil N10
Freeze-thaw cycles release nitrous oxide produced in frozen agricultural soils10
Gross N transformation rates in soil system with contrasting Urochloa genotypes do not confirm the relevance of BNI as previously assessed in vitro10
Organic fertilization drives shifts in microbiome complexity and keystone taxa increase the resistance of microbial mediated functions to biodiversity loss10
Microbial carbon use efficiency of litter with distinct C/N ratios in soil at different temperatures, including microbial necromass as growth component10
Amendment with biodiesel co-product modifies genes for N cycling (nirK, nirS, nosZ) and greenhouse gas emissions (N2O, CH4, CO2) from an acid soil9
Mechanism of increased soil phosphorus availability in a calcareous soil by ammonium polyphosphate9
Bacterial communities are associated with the tuber size of Tetrastigma hemsleyanum in stony soils9
Altered soil microbial properties and functions after afforestation increase soil carbon and nitrogen but not phosphorus accumulation9
The causes of the selection of biological nitrification inhibition (BNI) in relation to ecosystem functioning and a research agenda to explore them9
Plant residue-derived hydrophilic and hydrophobic fractions contribute to the formation of soil organic matter9
Sources and intensity of CH4 production in paddy soils depend on iron oxides and microbial biomass9
Variations in the composition of tea leaves and soil microbial community9
Amplitude and frequency of wetting and drying cycles drive N2 and N2O emissions from a subtropical pasture9
Accelerating the development of biological nitrification inhibition as a viable nitrous oxide mitigation strategy in grazed livestock systems8
Nonlinear decoupling of autotrophic and heterotrophic soil respiration in response to drought duration and N addition in a meadow steppe8
Topography-driven soil properties modulate effects of nitrogen deposition on soil nitrous oxide sources in a subtropical forest8
Forest thinning alleviates the negative effects of precipitation reduction on soil microbial diversity and multifunctionality8
Climate warming in an alpine meadow: differential responses of soil faunal vs. microbial effects on litter decomposition8
Canola straw biochars produced under different pyrolysis temperatures and nitrapyrin independently affected cropland soil nitrous oxide emissions8
Niche differentiation and higher uptake of available nitrogen maintained the productivity of alpine meadow at early degradation8
Changes in soil pore structure generated by the root systems of maize, sorghum and switchgrass affect in situ N2O emissions and bacterial denitrification8
Restoration of degraded alpine grasslands alters plant–microbial competition for nitrogen7
Modified universal buffer does not necessarily maintain soil enzyme assay pH7
Chimeric plants favor asynchrony of conditionally rare bacterial species facilitating functional complementarity in rhizosphere7
Absolute microbiome profiling highlights the links among microbial stability, soil health, and crop productivity under long-term sod-based rotation7
Effect of biochar and DMPP application alone or in combination on nitrous oxide emissions differed by soil types7
Cover crops in citrus orchards impact soil nutrient cycling and the soil microbiome after three years but effects are site-specific7
Linking soil aggregation to organic matter chemistry in a Calcic Cambisol: evidence from a 33-year field experiment7
Contrasting effects of elevated CO2 on autotrophic prokaryotes with different CO2 fixation strategies in tea plantation soil7
Impact of the chemical composition of applied organic materials on bacterial and archaeal community compositions in paddy soil7
Functional redundant soil fauna and microbial groups and processes were fairly resistant to drought in an agroecosystem7
Inter-microbial competition for N and plant NO3− uptake rather than BNI determines soil net nitrification under intensively managed Brachiaria humidicola7
The effects of soil incorporation depth of Biodiesel Co-Product (BCP) additions on N leaching losses and on genes involved in soil nitrogen cycling in an acidic Chinese tea soil7
Characterization of maize root microbiome in two different soils by minimizing plant DNA contamination in metabarcoding analysis7
A large nitrogen supply from the stable mineral-associated soil organic matter fraction6
Variations in biomass of fungal guilds are primarily driven by factors related to soil conditions in Mediterranean Pinus pinaster forests6
Protists modulate active bacterial community composition in paddy field soils6
Soil water extract and bacteriome determine N2O emission potential in soils6
Litter quality controls the contribution of microbial carbon to main microbial groups and soil organic carbon during its decomposition6
Yak dung pat fragmentation decreases yield-scaled growing-season nitrous oxide emissions in an alpine steppe on the Qinghai-Tibetan Plateau6
Assessing phosphorus availability in paddy soils: the importance of integrating soil tests and plant responses6
Dynamic changes in soil fungal communities and functional groups in response to sugarcane/soybean intercropping with reduced nitrogen fertilizer application6
Recommendations about soil Biological Nitrification Inhibition (BNI) studies6
Bioturbation as a means to circumvent sodium limitation by termites? Suspected processes and ecological consequences5
Shifts in bacterial community in response to conservation management practices within a soybean production system5
Biochar amendment increases the abundance and alters the community composition of diazotrophs in a double rice cropping system5
Co–elevation of CO2 and temperature enhances nitrogen mineralization in the rhizosphere of rice5
Fixation of CO2 by soil fungi: contribution to organic carbon pool and destination of fixed carbon products5
Shifts in understory plant composition induced by nitrogen addition predict soil fungal beta diversity in a boreal forest5
Rethinking discrepancies between difference and 15 N methods for estimating fertilizer nitrogen recovery5
Evidence of differences in nitrous oxide emissions and biological nitrification inhibition among Elymus grass species5
Does liming improve microbial carbon use efficiency after maize litter addition in a tropical acidic soil?5
Spring barley performance benefits from simultaneous shallow straw incorporation and top dressing as revealed by rhizotrons with resealable sampling ports5
Occurrence and diversity of arbuscular mycorrhizal fungi colonising off-season and in-season weeds and their relationship with maize yield under conservation agriculture5
Rice endophytic communities are strongly dependent on microbial communities specific to each soil5
Contrasting effects of rice husk and its biochar on N2O emissions and nitrogen leaching from Lei bamboo soils under subtropical conditions5
Soil nitrification inhibition by urine of sheep consuming plantain (Plantago lanceolata)5
Grassland conversion to cropland decreased microbial assimilation of mineral N into their residues in a Chernozem soil5
Biochar application reduces residual napropamide in the rhizosphere and improves soil microbial diversity5
Root and shoot growth of spring wheat (Triticum aestivum L.) are differently affected by increasing subsoil biopore density when grown under different subsoil moisture5
Estimation of baseline levels of bacterial community tolerance to Cr, Ni, Pb, and Zn in unpolluted soils, a background for PICT (pollution-induced community tolerance) determination5
Linking long-term soil phosphorus management to microbial communities involved in nitrogen reactions5
Impact of high carbon amendments and pre-crops on soil bacterial communities5
Potassium phosphite enhanced the suppressive capacity of the soil microbiome against the tomato pathogen Ralstonia solanacearum5
Litter decomposition and arthropod composition under different ultraviolet levels following prescribed burn in a subtropical pastureland5
Nitrogen acquisition by two U. humidicola genotypes differing in biological nitrification inhibition (BNI) capacity and associated microorganisms5
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