| A multi-scale approach to determine accurate elemental and isotopic ratios by nano-scale secondary ion mass spectrometry imaging. |
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| A novel method for the study of the biophysical interface in soils using nano-scale secondary ion mass spectrometry. |
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| Advancements in the application of NanoSIMS and Raman microspectroscopy to investigate the activity of microbial cells in soils. |
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| Advances in the Analysis of Biogeochemical Interfaces: NanoSIMS to Investigate Soil Microenvironments. |
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| Aging shapes the distribution of copper in soil aggregate size fractions. |
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| Alteration of rocks by endolithic organisms is one of the pathways for the beginning of soils on Earth. |
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| Biodegradation of synthetic polymers in soils: Tracking carbon into CO2 and microbial biomass. |
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| Biogeochemical cycling of phosphorus in subsoils of temperate forest ecosystems. |
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| Calcareous organic matter coatings sequester siderophores in alkaline soils. |
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| Carbon Mineralizability Determines Interactive Effects on Mineralization of Pyrogenic Organic Matter and Soil Organic Carbon. |
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| Characterization of Biogeochemical Processes at the Microscale: Challenges and Opportunities (pp. 193–212). |
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| Characterization of Cu distribution in clay-sized soil aggregates by NanoSIMS and micro-XRF. |
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| Correlative Imaging Reveals Holistic View of Soil Microenvironments. |
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| Deciphering the Incipient Phases of Ice–Mineral Interactions as a Precursor of Physical Weathering. |
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| Dynamics of PAHs and derived organic compounds in a soil-plant mesocosm spiked with 13C-phenanthrene. |
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| Earthworm Cast Formation and Development: A Shift From Plant Litter to Mineral Associated Organic Matter. |
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| Enhanced loss but limited mobility of pyrogenic and organic matter in continuous permafrost-affected forest soils. |
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| Enrichment of Lignin-Derived Carbon in Mineral-Associated Soil Organic Matter. |
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| Evidence of organic matter control on As oxidation by iron oxides in riparian wetlands. |
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| Fungal Nanophase Particles Catalyze Iron Transformation for Oxidative Stress Removal and Iron Acquisition. |
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| Identification of Distinct Functional Microstructural Domains Controlling C Storage in Soil. |
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| Imaging of Al/Fe ratios in synthetic Al-goethite revealed by nanoscale secondary ion mass spectrometry. |
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| In Situ Mapping of Nutrient Uptake in the Rhizosphere Using Nanoscale Secondary Ion Mass Spectrometry. |
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| Incorporation of 13C labelled shoot residues in Lumbricus terrestris casts: A combination of transmission electron microscopy and nanoscale secondary ion mass spectrometry. |
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| Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw. |
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| Legacy of Rice Roots as Encoded in Distinctive Microsites of Oxides, Silicates, and Organic Matter. |
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| Linking 3D Soil Structure and Plant-Microbe-Soil Carbon Transfer in the Rhizosphere. |
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| Micro-scale heterogeneity of soil phosphorus depends on soil substrate and depth. |
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| Microscale spatial distribution and soil organic matter persistence in top and subsoil. |
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| Microscale soil structures foster organic matter stabilization in permafrost soils. |
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| Mineral protection of soil carbon counteracted by root exudates. |
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| Multiple element isotope probes, NanoSIMS, and the functional genomics of microbial carbon cycling in soils in response to chronic climatic change. |
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| Multiple exchange processes on mineral surfaces control the transport of dissolved organic matter through soil profiles. |
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| Mycelium-mediated transfer of water and nutrients stimulates bacterial activity in dry and oligotrophic environments. |
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| Nano-scale investigation of the association of microbial nitrogen residues with iron (hydr)oxides in a forest soil O-horizon. |
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| Nano-scale secondary ion mass spectrometry — A new analytical tool in biogeochemistry and soil ecology: A review article. |
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| Nanoscale evidence of contrasted processes for root-derived organic matter stabilization by mineral interactions depending on soil depth. |
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| NanoSIMS investigation of glycine-derived C and N retention with soil organo-mineral associations. |
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| NanoSIMS Study of Organic Matter Associated with Soil Aggregates: Advantages, Limitations, and Combination with STXM. |
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| New strategies for submicron characterization the carbon binding of reactive minerals in long-term contrasting fertilized soils: Implications for soil carbon storage. |
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| Nitrogen-rich microbial products provide new organo-mineral associations for the stabilization of soil organic matter. |
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| Novel Sample Preparation Technique To Improve Spectromicroscopic Analyses of Micrometer-Sized Particles. |
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| Organic Matter Amendment and Plant Colonization Drive Mineral Weathering, Organic Carbon Sequestration, and Water-Stable Aggregation in Magnetite Fe Ore Tailings. |
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| Organo-mineral interactions and soil carbon mineralizability with variable saturation cycle frequency. |
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| Phosphorus nutrition of Populus × canescens reflects adaptation to high P-availability in the soil. |
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| Porosity and organic matter distribution in jarositic phyto tubules of sulfuric soils assessed by combined µCT and NanoSIMS analysis. |
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| Priming mechanisms with additions of pyrogenic organic matter to soil. |
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| Promoting plant growth and carbon transfer to soil with organic amendments produced with mineral additives. |
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| Rapid soil formation after glacial retreat shaped by spatial patterns of organic matter accrual in microaggregates. |
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| Sequential Ammonia and Carbon Dioxide Adsorption on Pyrolyzed Biomass to Recover Waste Stream Nutrients. |
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| Small but mighty: Microorganisms offer inspiration for mine remediation and waste stabilisation. |
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| Small-scale distribution of copper in a Technosol horizon studied by nano-scale secondary ion mass spectrometry. |
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| Soil carbon storage informed by particulate and mineral-associated organic matter |
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| Soil Organic Matter and Phosphate Sorption on Natural and Synthetic Fe Oxides under in Situ Conditions. |
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| Soil organic matter is stabilized by organo-mineral associations through two key processes: The role of the carbon to nitrogen ratio. |
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| Sorption of Cu(II) by Al hydroxide organo–mineral coprecipitates: Microcalorimetry and NanoSIMS observations. |
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| STXM and NanoSIMS Investigations on EPS Fractions before and after Adsorption to Goethite. |
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| Submicron structures provide preferential spots for carbon and nitrogen sequestration in soils. |
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| Subsoil organo-mineral associations under contrasting climate conditions. |
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| Synergies between mycorrhizal fungi and soil microbial communities increase plant nitrogen acquisition. |
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| The role of soil redox conditions in microbial phosphorus cycling in humid tropical forests. |
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| Understanding the fate and linkage of N and S in earthworm-engineered peat soil by coupling stable isotopes and nano-scale secondary ion mass spectrometry. |
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| Unexpected bulk density and microstructures response to long-term pig manure application in a Ferralic Cambisol Soil: Implications for rebuilding a healthy soil. |
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| Unveiling of active diazotrophs in a flooded rice soil by combination of NanoSIMS and 15N2-DNA-stable isotope probing. |
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| Using stable isotopes to explore root-microbe-mineral interactions in soil. |
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| Visualizing the transfer of organic matter from decaying plant residues to soil mineral surfaces controlled by microorganisms. |
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