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Persistence of soil organic matter as an ecosystem property

Nature (London), 2011-10, Vol.478 (7367), p.49-56

2011

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Transformation and stabilization of pyrogenic organic matter in a temperate forest field experiment

Global change biology, 2014-05, Vol.20 (5), p.1629-1642

2014

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Nitrogen deposition promotes the production of new fungal residues but retards the decomposition of old residues in forest soil fractions

Global change biology, 2014-01, Vol.20 (1), p.327-340

2014

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Climate warming and elevated CO2 alter peatland soil carbon sources and stability

Nature communications, 2023-11, Vol.14 (1), p.7533-7533, Article 7533

2023

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What on Earth Have We Been Burning? Deciphering Sedimentary Records of Pyrogenic Carbon

Environmental science & technology, 2017-11, Vol.51 (21), p.12972-12980

2017

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Black carbon in soils and sediments: Analysis, distribution, implications, and current challenges

Global biogeochemical cycles, 2000-09, Vol.14 (3), p.777-793

2000

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Lignin content and chemical characteristics in maize and wheat vary between plant organs and growth stages: consequences for assessing lignin dynamics in soil

Plant and soil, 2011-06, Vol.343 (1/2), p.369-378

2011

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Marked isotopic variability within and between the Amazon River and marine dissolved black carbon pools

Nature communications, 2019-09, Vol.10 (1), p.4018-8, Article 4018

2019

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Nine years of warming and nitrogen addition in the Tibetan grassland promoted loss of soil organic carbon but did not alter the bulk change in chemical structure

Biogeosciences, 2024-01, Vol.21 (2), p.575-589

2024

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Pyrogenic carbon soluble fraction is larger and more aromatic in aged charcoal than in fresh charcoal

Soil biology & biochemistry, 2011-07, Vol.43 (7), p.1615-1617

2011

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Improved assessment of pyrogenic carbon quantity and quality in environmental samples by high-performance liquid chromatography

Journal of Chromatography A, 2013-08, Vol.1304, p.246-250

2013

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C 1s K-edge near edge X-ray absorption fine structure (NEXAFS) spectroscopy for characterizing functional group chemistry of black carbon

Organic geochemistry, 2011-10, Vol.42 (9), p.1055-1064

2011

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Nitrogen addition alters mineralization dynamics of 13C-depleted leaf and twig litter and reduces leaching of older DOC from mineral soil

Global change biology, 2012-04, Vol.18 (4), p.1412-1427

2012

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Interactive effects of elevated CO2 and nitrogen deposition on fatty acid molecular and isotope composition of above‐ and belowground tree biomass and forest soil fractions

Global change biology, 2015-01, Vol.21 (1), p.473-486

2015

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Rapid molecular screening of black carbon (biochar) thermosequences obtained from chestnut wood and rice straw: A pyrolysis-GC/MS study

Biomass & bioenergy, 2012-10, Vol.45, p.115-129

2012

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Toward a “Molecular Thermometer” to Estimate the Charring Temperature of Wildland Charcoals Derived from Different Biomass Sources

Environmental science & technology, 2013-10, Vol.47 (20), p.11490-11495

2013

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How far do experimentally elevated CO₂ levels reach into the surrounding? - An example using the ¹³C label of soil organic matter as an archive

Global change biology, 2009-06, Vol.15 (6), p.1598-1602

2009

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Sodium hypochlorite separates an older soil organic matter fraction than acid hydrolysis

Geoderma, 2007-04, Vol.139 (1), p.171-179

2007

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Comparison of gas with liquid chromatography for the determination of benzenepolycarboxylic acids as molecular tracers of black carbon

Organic geochemistry, 2011-03, Vol.42 (3), p.275-282

2011

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Decoupled sedimentary records of combustion: Causes and implications

Geophysical research letters, 2016-05, Vol.43 (10), p.5098-5108

2016

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Discrepancies in utilization of density fractionation along with ultrasonic dispersion to obtain distinct pools of soil organic matter

Journal of plant nutrition and soil science, 2013-08, Vol.176 (4), p.500-504

2013

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Charcoal quality does not change over a century in a tropical agro-ecosystem

Soil biology & biochemistry, 2011-09, Vol.43 (9), p.1992-1994

2011

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Ryegrass-derived pyrogenic organic matter changes organic carbon and nitrogen mineralization in a temperate forest soil

Soil biology & biochemistry, 2014-02, Vol.69, p.291-301

2014

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Persistence of soil organic matter as an ecosystem property

Transformation and stabilization of pyrogenic organic matter in a temperate forest field experiment

Nitrogen deposition promotes the production of new fungal residues but retards the decomposition of old residues in forest soil fractions

Climate warming and elevated CO2 alter peatland soil carbon sources and stability

What on Earth Have We Been Burning? Deciphering Sedimentary Records of Pyrogenic Carbon

Black carbon in soils and sediments: Analysis, distribution, implications, and current challenges

Lignin content and chemical characteristics in maize and wheat vary between plant organs and growth stages: consequences for assessing lignin dynamics in soil

Marked isotopic variability within and between the Amazon River and marine dissolved black carbon pools

Dissolved carbon leaching from soil is a crucial component of the net ecosystem carbon balance

Nine years of warming and nitrogen addition in the Tibetan grassland promoted loss of soil organic carbon but did not alter the bulk change in chemical structure

Pyrogenic carbon soluble fraction is larger and more aromatic in aged charcoal than in fresh charcoal

Improved assessment of pyrogenic carbon quantity and quality in environmental samples by high-performance liquid chromatography

C 1s K-edge near edge X-ray absorption fine structure (NEXAFS) spectroscopy for characterizing functional group chemistry of black carbon

Nitrogen addition alters mineralization dynamics of 13C-depleted leaf and twig litter and reduces leaching of older DOC from mineral soil

Interactive effects of elevated CO2 and nitrogen deposition on fatty acid molecular and isotope composition of above‐ and belowground tree biomass and forest soil fractions

Rapid molecular screening of black carbon (biochar) thermosequences obtained from chestnut wood and rice straw: A pyrolysis-GC/MS study

Toward a “Molecular Thermometer” to Estimate the Charring Temperature of Wildland Charcoals Derived from Different Biomass Sources

How far do experimentally elevated CO₂ levels reach into the surrounding? - An example using the ¹³C label of soil organic matter as an archive

Sodium hypochlorite separates an older soil organic matter fraction than acid hydrolysis

Comparison of gas with liquid chromatography for the determination of benzenepolycarboxylic acids as molecular tracers of black carbon

Decoupled sedimentary records of combustion: Causes and implications

Discrepancies in utilization of density fractionation along with ultrasonic dispersion to obtain distinct pools of soil organic matter

Charcoal quality does not change over a century in a tropical agro-ecosystem

Ryegrass-derived pyrogenic organic matter changes organic carbon and nitrogen mineralization in a temperate forest soil

Microbial carbon use efficiency promotes global soil carbon storage

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