Long-term release of carbon from grassland soil amended with different slurry particle size fractions: a laboratory incubation study.

Application of animal manure to agricultural soils enhances both native soil carbon (C) and overall (native soil C and added C) respiration. CO(2) effluxes were measured in a laboratory incubation study for 1465 days after the application of different slurry fractions (>2000, 425-2000, 250-425, 150-250, 45-150 and <45 µm) to a grassland soil. The slurry-derived C present in the soil was traced using the natural abundance δ(13)C method. We used two kinetic (single and two pool) models to fit the experimental data and to test the model validity with respect to long-term data sets. Mean residence times (MRTs) of the particle size based slurry-C fractions were estimated using these models and a linear (13)C natural abundance based approach. The results showed that slurry-C degradation in soil over time varied between the different particle size based slurry treatments. The two kinetic soil-C models were successful to predict medium- to long-term carbon release from soil amended with animal slurry. The estimated MRTs did vary between the linear (3.8-5.6 years) and non-linear based (0.8-3.8 years) (model) approaches. Slurry-derived C could still be (isotopically) detected in the soil 4 years after slurry application using the natural abundance δ(13)C method. This suggests that it may take a decadal timescale or longer before the entire amount of C introduced through whole slurry amendments to grassland soils is fully dissipated.

[1]  Y. Kuzyakov Priming effects : interactions between living and dead organic matter , 2010 .

[2]  L. Cárdenas,et al.  Nitrogen mineralization and CO2 and N2O emissions in a sandy soil amended with original or acidified pig slurries or with the relative fractions , 2010, Biology and Fertility of Soils.

[3]  J. Coutinho,et al.  Carbon-mineralization kinetics in an organically managed Cambic Arenosol amended with organic fertilizers , 2010 .

[4]  R. Evershed,et al.  Tracking the fate of dung-derived carbohydrates in a temperate grassland soil using compound-specific stable isotope analysis , 2009 .

[5]  R. Bol,et al.  Molecular turnover time of soil organic matter in particle-size fractions of an arable soil. , 2009, Rapid communications in mass spectrometry : RCM.

[6]  Jingyun Fang,et al.  Soil respiration and human effects on global grasslands. , 2009 .

[7]  Stefano Monaco,et al.  Soil organic matter dynamics and losses in manured maize-based forage systems , 2009 .

[8]  J. W. Groenigen,et al.  Pig slurry treatment modifies slurry composition, N2O, and CO2 emissions after soil incorporation , 2008 .

[9]  R. Evershed,et al.  Off-line pyrolysis and compound-specific stable carbon isotope analysis of lignin moieties: a new method for determining the fate of lignin residues in soil. , 2008, Rapid communications in mass spectrometry : RCM.

[10]  Klaus Kaiser,et al.  How relevant is recalcitrance for the stabilization of organic matter in soils , 2008 .

[11]  D. Fangueiro,et al.  Quantification of priming and CO2 emission sources following the application of different slurry particle size fractions to a grassland soil , 2007 .

[12]  P. Rochette,et al.  Use of 13C abundance to study short-term pig slurry decomposition in the field , 2007 .

[13]  J. Balesdent,et al.  Microbial biosyntheses of individual neutral sugars among sets of substrates and soils , 2007 .

[14]  B. Glaser,et al.  Sequestration and turnover of plant‐ and microbially derived sugars in a temperate grassland soil during 7 years exposed to elevated atmospheric pCO2 , 2007 .

[15]  C. Plaza,et al.  Carbon mineralization in an arid soil amended with thermally-dried and composted sewage sludges , 2007 .

[16]  P. Högberg,et al.  Towards a more plant physiological perspective on soil ecology. , 2006, Trends in ecology & evolution.

[17]  J. Balesdent,et al.  The turnover of carbohydrate carbon in a cultivated soil estimated by 13C natural abundances , 2006 .

[18]  B. Glaser,et al.  Sequestration and turnover of bacterial‐ and fungal‐derived carbon in a temperate grassland soil under long‐term elevated atmospheric pCO2 , 2006 .

[19]  Y. Kuzyakov,et al.  Sources and mechanisms of priming effect induced in two grassland soils amended with slurry and sugar , 2006 .

[20]  R. Rees,et al.  Greenhouse gas emissions from a managed grassland , 2005 .

[21]  B. Glaser,et al.  Reconstruction of climate and landscape changes in a high mountain lake catchment in the Gorkha Himal, Nepal during the Late Glacial and Holocene as deduced from radiocarbon and compound-specific stable isotope analysis of terrestrial, aquatic and microbial biomarkers , 2005 .

[22]  B. Glaser,et al.  Short-term dynamics of slurry-derived plant and microbial sugars in a temperate grassland soil as assessed by compound-specific delta13C analyses. , 2005, Rapid communications in mass spectrometry : RCM.

[23]  R. Evershed,et al.  Quantification of dung carbon incorporation in a temperate grassland soil following spring application using bulk stable carbon isotope determinations , 2005, Isotopes in environmental and health studies.

[24]  J. Béraud,et al.  Modeling carbon and nitrogen transformations for adjustment of compost application with nitrogen uptake by wheat. , 2005, Journal of environmental quality.

[25]  Yiqi Luo,et al.  Net ecosystem carbon exchange in two experimental grassland ecosystems , 2004 .

[26]  B. Glaser,et al.  Short-term sequestration of slurry-derived carbon into particle size fractions of a temperate grassland soil , 2004, Isotopes in environmental and health studies.

[27]  Y. Kuzyakov,et al.  Quantification of priming and CO2 respiration sources following slurry-C incorporation into two grassland soils with different C content. , 2003, Rapid communications in mass spectrometry : RCM.

[28]  Stefaan De Neve,et al.  Carbon mineralization from composts and food industry wastes added to soil , 2003, Nutrient Cycling in Agroecosystems.

[29]  S G Sommer,et al.  Separation efficiency and particle size distribution in relation to manure type and storage conditions. , 2002, Bioresource technology.

[30]  B. Glaser,et al.  Short-term sequestration of slurry-derived carbon and nitrogen in temperate grassland soil as assessed by 13C and 15N natural abundance measurements , 2001 .

[31]  R. Bol,et al.  Tracing dung-derived carbon in temperate grassland using 13C natural abundance measurements. , 2000 .

[32]  P. Rochette,et al.  Soil Carbon and Nitrogen Dynamics Following Application of Pig Slurry for the 19th Consecutive Year I. Carbon Dioxide Fluxes and Microbial Biomass Carbon , 2000 .

[33]  S. Archer,et al.  δ13C values of soil organic carbon and their use in documenting vegetation change in a subtropical savanna ecosystem , 1998 .

[34]  D. M. Howard,et al.  Long-term study of litter decomposition on a Pennine peat bog: which regression? , 1997, Oecologia.

[35]  Mogens Henze,et al.  Wastewater Treatment: Biological and Chemical Processes , 1995 .

[36]  C. Clapp,et al.  Potentially Mineralizable Nitrogen in Soil: The Simple Exponential Model Does Not Apply for the First 12 Weeks of Incubation1 , 1980 .

[37]  V. Owens,et al.  Soil carbon dioxide fluxes in established switchgrass land managed for biomass production , 2007 .

[38]  L. M. Risse,et al.  Land Application of Manure for Beneficial Reuse , 2006 .

[39]  R. Alvarez,et al.  Soil Organic Matter Pools and Their Associations with Carbon Mineralization Kinetics , 2000 .

[40]  L. Rustad,et al.  Controls on soil respiration: Implications for climate change , 2000 .

[41]  J. Balesdent,et al.  Measurement of soil organic matter turnover using 13C natural abundance. , 1996 .

[42]  T. Boutton,et al.  Stable carbon isotope ratios of soil organic matter and their use as indicators of vegetation and climate change. , 1996 .