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Plant and Soil

, Volume 430, Issue 1–2, pp 329–348 | Cite as

Demonstration of the rapid incorporation of carbon into protective, mineral-associated organic carbon fractions in an eroded soil from the CarboZALF experimental site

  • Rainer Remus
  • Michael Kaiser
  • Markus Kleber
  • Jürgen Augustin
  • Michael Sommer
Regular Article

Abstract

Aims

The goal of this work was to quantitatively describe the influence of soil erosion on the distribution of recently assimilated carbon (C) within the plant-soil system and different soil fractions.

Methods

Surface soil was manipulated in the field to simulate a strong erosion event, and maize plants were cultivated in a growth chamber using soil material from the manipulated (eroded) and non-eroded sites. The maize plants were pulse labeled with 14C-labeled carbon dioxide (CO2) at the start of flowering, and C partitioning within the plants and the distribution of recently assimilated C into organo-mineral soil fractions of different particle size were assessed after 25 days.

Results

The distribution of C differed significantly between the particle size fractions separated from the soil material of the eroded and non-eroded sites. For example, a much higher percentage of 14C was found in macro-aggregate-occluded organic particles of the eroded soil than in the same fraction of soil from the non-eroded site. Furthermore, a significantly higher absolute amount of recently assimilated C was found in the < 20-μ m mineral particles and aggregates of the eroded soil than in the same particle fraction of the non-eroded soil. We show that this C is most likely derived from rhizodeposition or metabolites originating from the microbial decomposition of rhizodeposits.

Conclusions

The findings provide experimental evidence of the concept of the “dynamic replacement” of organic C (OC) losses due to erosion by C derived from crops growing on eroded soils. The rapid and enhanced sorption of recently assimilated C on the surfaces of mineral particles and occlusion in aggregates < 20 μ m confirms the role of erosion processes in creating an immediate terrestrial C sink with the potential to enhance long-term soil C storage.

Keywords

Soil erosion Rhizodeposition Dynamic C replacement 

Notes

Acknowledgements

We are grateful to the employees of the ZALF Agricultural Landscape Data Centre (DZA) for their support of the CarboZALF-D field trial. We also thank Andrea Neumann and Chandan C. Kemparaju from the Leibniz Center for Agricultural Landscape Research (ZALF) in Müncheberg (Germany) for preparing the soil, root and shoot samples.

References

  1. Amundson R, Berhe AA, Hopmans JW, Olson C, Sztein AE, Sparks DL (2015) Soil and human security in the 21st century. Science 348(6235):1261071.  https://doi.org/10.1126/science.1261071 CrossRefPubMedGoogle Scholar
  2. Berhe AA, Kleber M (2013) Erosion, deposition, and the persistence of soil organic matter: mechanistic considerations and problems with terminology. Earth Surf Proc Land 38:908–912.  https://doi.org/10.1002/esp.3408 CrossRefGoogle Scholar
  3. Berhe AA, Harte J, Harden JW, Torn MS (2007) The significance of the erosion-induced terrestrial carbon sink. Bioscience 57:337–346.  https://doi.org/10.1641/B570408 CrossRefGoogle Scholar
  4. Berhe AA, Harden JW, Torn MS, Harte J (2008) Linking soil organic matter dynamics and erosion-induced terrestrial carbon sequestration at different landform positions. J Geophys Res Biogeosci 113:G4039.  https://doi.org/10.1029/2008JG000751 CrossRefGoogle Scholar
  5. Berhe AA, Harden JW, Torn MS, Kleber M, Burton SD, Harte J (2012) Persistence of soil organic matter in eroding versus depositional landform positions. J Geophys Res Biogeosci 117:G02019.  https://doi.org/10.1029/2011JG001790 CrossRefGoogle Scholar
  6. Berhe AA, Barnes RT, Six J, Marín-Spiotta E (2018) Role of soil erosion in biogeochemical cycling of essential elements: carbon, nitrogen, and phosphorus. Annu Rev Earth Planet Sci 46:521–548CrossRefGoogle Scholar
  7. Deumlich D, Rogasik H, Hierold W, Onasch I, Völker L, Sommer M (2017) The carboZALF-d manipulation experiment – experimental design and SOC patterns. Int J Environ Agric Res 3:40–50Google Scholar
  8. DINISO 10390 (1997) Bodenbeschaffenheit: Bestimmung des pH Wertes. Tech. rep., Deutsche Normen (ed., fachnormenausschuß Wasserwesen im DIN Deutsches Institut für Normung e.V.) 3.5.1a. Beuth Verlag, BerlinGoogle Scholar
  9. DINISO 11277 (1998) Bodenbeschaffenheit: Bestimmung der Partikelgrößenverteilung in Mineralböden – Verfahren mittels Siebung und Sedimentation. Tech. rep. Deutsches Institut für Normung. Beuth, BerlinGoogle Scholar
  10. Doetterl S, Nadeu E, Berhe A, Wang Z, Sommer M, Fiener P (2016) Erosion, deposition and soil carbon: a review of processlevel controls, experimental tools and models to address C cycling in dynamic landscapes. Earth-Sci Rev 154:102–122CrossRefGoogle Scholar
  11. Feng W, Shi Z, Jiang J, Xia J, Liang J, Zhou J, Luo Y (2016) Methodological uncertainty in estimating carbon turnover times of soil fractions. Soil Biol Biochem 100:118–124CrossRefGoogle Scholar
  12. Harden J, Sharpe J, Parton W, Ojima D, Fries T, Huntington T, Dabney S (1999) Dynamic replacement and loss of soil carbon on eroding cropland. Glob Biogeochem Cycles 13:885–901.  https://doi.org/10.1029/1999GB900061 CrossRefGoogle Scholar
  13. IUSS Working Group WRB (2015) World reference base for soil resources 2014. international soil classification system for naming soils and creating legends for soil maps. Update 2015. Technical report, World Soil Resources Reports No 106. FAO, RomeGoogle Scholar
  14. Kaiser M, Berhe A (2014) How does sonication affect the mineral and organic constituents of soil aggregates? - a review. J Plant Nutr Soil Sci 177:479–495CrossRefGoogle Scholar
  15. Kaiser M, Wirth S, Ellerbrock R, Sommer M (2010) Microbial respiration activities related to sequentially separated, particulate and water-soluble organic matter fractions from arable and forest topsoils. Soil Biol Biochem 42:418–428CrossRefGoogle Scholar
  16. Keith H, Oades JM, Martin JK (1986) Input of carbon to soil from wheat plants. Soil Biol Biochem 18:445–449CrossRefGoogle Scholar
  17. Kirkels FMSA, Cammeraat LH, Kuhn NJ (2014) The fate of soil organic carbon upon erosion, transport and deposition in agricultural landscapes - A review of different concepts. Geomorphology 226:94–105.  https://doi.org/10.1016/j.geomorph.2014.07.023 CrossRefGoogle Scholar
  18. Lynch J, Whipps J (1990) Substrate flow in the rhizosphere. Plant Soil 129:1–10CrossRefGoogle Scholar
  19. Majzik A, Tombácz E (2007) Interaction between humic acid and montmorillonite in the presence of calcium ions ii. colloidal interactions: Charge state, dispersing and/or aggregation of particles in suspension. Org Geochem 38:1330–1340CrossRefGoogle Scholar
  20. Marx M, Buegger F, Gattinger A, Marschner B, Zsolnay A, Munch JC (2007) Determination of the fate of C-13 labelled maize and wheat rhizodeposit-C in two agricultural soils in a greenhouse experiment under C-13-CO2-enriched atmosphere. Soil Biol Biochem 39:3043–3055.  https://doi.org/10.1016/j.soilbio.2007.06.016 CrossRefGoogle Scholar
  21. Meng F, Dungait JAJ, Zhang X, He M, Guo Y, Wu W (2013) Investigation of photosynthate-C allocation 27 days after 13C-pulse labeling of Zea mays L. at different growth stages. Plant Soil 373:755–764CrossRefGoogle Scholar
  22. Moni C, Rumpel C, Virto I, Chabbi A, Chenu C (2010) Relative importance of sorption versus aggregation for organic matter storage in subsoil horizons of two contrasting soils. Eur J Soil Sci 61:958–969CrossRefGoogle Scholar
  23. Montgomery D (2007) Soil erosion and agricultural sustainability. PNAS 104:13,268–13,272CrossRefGoogle Scholar
  24. Nadeu E, Berhe AA, de Vente J, Boix-Fayos C (2012) Erosion, deposition and replacement of soil organic carbon in Mediterranean catchments: a geomorphological, isotopic and land use change approach. Biogeosciences 9:1099–1111.  https://doi.org/10.5194/bg-9-1099-2012 CrossRefGoogle Scholar
  25. Nguyen C, Todorovic C, Robin C, Christophe A, Guckert A (1999) Continuous monitoring of rhizosphere respiration after labelling of plant shoots with (CO2)-C-14. Plant Soil 212:191–201CrossRefGoogle Scholar
  26. North P (1976) Towards an absolute measurement of soil structural stability using ultrasound. J Soil Sci 27:451–459CrossRefGoogle Scholar
  27. Pausch J, Tian J, Riederer M, Kuzyakov Y (2013) Estimation of rhizodeposition at field scale: upscaling of a C-14 labeling study. Plant Soil 364:273–285CrossRefGoogle Scholar
  28. Powlson D, Gregory P, Whalley J, Quinton WR, Hopkins D, Whitmore A, Hirsch P, Goulding K (2011) Soil management in relation to sustainable agriculture and ecosystem services. Food Policy 36:72–87CrossRefGoogle Scholar
  29. Pritchard SG, Rogers HH (2000) Spatial and temporal deployment of crop roots in CO2-enriched environments. New Phytol 147:55–71CrossRefGoogle Scholar
  30. Qureshi RM, Fritz P, Drimmie RJ (1985) The use of CO2 absorbers for the determination of specific C-14 activities. Int J Appl Radiat Isot 36:165–170.  https://doi.org/10.1016/0020-708X(85)90239-X CrossRefGoogle Scholar
  31. Rasse D, Rumpel C, Dignac MF (2005) Is soil carbon mostly root carbon? Mechanisms for a specific stabilisation. Plant Soil 269:341–356CrossRefGoogle Scholar
  32. Remus R, Augustin J (2016) Dynamic linking of 14C partitioning with shoot growth allows a precise determination of plant-derived C input to soil. Plant Soil 408:493–513.  https://doi.org/10.1007/s11104-016-3006-y CrossRefGoogle Scholar
  33. Remus R, Hüve K, Pörschmann J, Augustin J (2016) Determining the timepoint when 14C tracer accurately reflect photosynthate use in the plant-soil system. Plant Soil 408:457–474.  https://doi.org/10.1007/s11104-016-3002-2 CrossRefGoogle Scholar
  34. Schlichting E, Blume HP, Stahr K (1995) Soils Practical (in German). Blackwell, BerlinGoogle Scholar
  35. Sey BK, Manceur AM, Whalen JK, Gregorich EG, Rochette P (2010) Root-derived respiration and nitrous oxide production as affected by crop phenology and nitrogen fertilization. Plant Soil 326:369–379CrossRefGoogle Scholar
  36. Sommer M, Augustin J, Kleber M (2016) Feedbacks of soil erosion on soc patterns and carbon dynamics in agricultural landscapes - the carbozalf experiment. Soil Tillage Res 156:182–184CrossRefGoogle Scholar
  37. Stallard R (1998) Terrestrial sedimentation and the carbon cycle: Coupling weathering and erosion to carbon burial. Glob Biogeochem Cycles 12(2):231–257.  https://doi.org/10.1029/98GB00741 CrossRefGoogle Scholar
  38. Stewart CE, Paustian K, Conant RT, Plante AF, Six J (2008) Soil carbon saturation: Evaluation and corroboration by long-term incubations. Soil Boil Biochem 40(7):1741–1750.  https://doi.org/10.1016/j.soilbio.2008.02.014 CrossRefGoogle Scholar
  39. Swinnen J, Van Veen JA, Merckx R (1994) Rhizosphere carbon fluxes in field-grown spring wheat - model calculation based on C-14 partitioning after pulse-labeling. Soil Biol Biochem 26:171–182CrossRefGoogle Scholar
  40. Van Oost K, Quine TA, Govers G, De Gryze S, Six J, Harden JW, Ritchie JC, McCarty GW, Heckrath G, Kosmas C, Giraldez JV, da Silva JRM, Merckx R (2007) The impact of agricultural soil erosion on the global carbon cycle. Science 318:626–629.  https://doi.org/10.1126/science.1145724 CrossRefPubMedGoogle Scholar
  41. VandenBygaart AJ, Gregorich EG, Helgason BL (2015) Cropland C erosion and burial: Is buried soil organic matter biodegradable?. Geoderma 239:240–249.  https://doi.org/10.1016/j.geoderma.2014.10.011 CrossRefGoogle Scholar
  42. Virto I, Moni C, Swanston C, Chenu C (2010) Turnover of intra- and extra-aggregate organic matter at the silt-size scale. Geoderma 156:1–10CrossRefGoogle Scholar
  43. Wilkinson B, McElroy B (2007) The impact of humans on continental erosion and sedimentation. GSA Bull 119:140–156CrossRefGoogle Scholar
  44. Wuddivira M, Camps-Roach G (2007) Effects of organic matter and calcium on soil structural stability. Eur J Soil Sci 58:722–727CrossRefGoogle Scholar
  45. Xiao H, Li Z, Chang X, Huang B, Nie X, Liu C, Liu L, Wang D, Jiang J (2018) The mineralization and sequestration of organic carbon in relation to agricultural soil erosion. Geoderma 329:73–81CrossRefGoogle Scholar
  46. Xu JG, Juma NG (1993) Aboveground and belowground transformation of photosynthetically fixed carbon by 2 barley (Hordeum vulgare L.) cultivars in a typic cryoboroll. Soil Biol Biochem 25:1263–1272CrossRefGoogle Scholar
  47. Zhao Q, Poulson S, Obrist D, Sumaila S, Dynes J, McBeth J, Yang Y (2016) Iron-bound organic carbon in forest soils: quantification and characterization. Biogeosciences 13:4777–4788CrossRefGoogle Scholar

Copyright information

© Springer International Publishing AG, part of Springer Nature 2018

Authors and Affiliations

  • Rainer Remus
    • 1
  • Michael Kaiser
    • 2
  • Markus Kleber
    • 3
  • Jürgen Augustin
    • 1
  • Michael Sommer
    • 1
  1. 1.Leibniz Centre for Agricultural Landscape Research (ZALF)MünchebergGermany
  2. 2.Department of Agronomy and HorticultureUniversity of Nebraska - LincolnLincolnUSA
  3. 3.Department of Crop and Soil ScienceOregon State UniversityCorvallisUSA

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