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Biogeochemistry

, Volume 123, Issue 1–2, pp 27–47 | Cite as

Optimization of method to quantify soil organic matter dynamics and carbon sequestration potential in volcanic ash soils

  • Susan E. Crow
  • Mataia Reeves
  • Olivia S. Schubert
  • Carlos A. Sierra
Article

Abstract

Volcanic ash-derived soils are important globally for their C sequestration potential and because they are at risk of compaction and degradation due to land use change. Poorly or non-crystalline minerals impart enormous capacity for soils to store and stabilize C, but also unusual chemical and physical properties that make quantifying meaningful soil C pools challenging. Here, we optimize a soil physical fractionation method to effectively assess soil organic matter dynamics in volcanic ash soils by first comparing three common methods for Andisols of the same soil series under three land uses. Components of those methods that (1) effectively isolated C pools of different size and turnover and (2) demonstrated potential sensitivity to land use change were then modified for a final, combined method. The isolation of C pools corresponding to fundamental mechanisms of protection within aggregates and organo-mineral control on the stabilization of C, which often function to the extreme in volcanic ash soils, underlie these modifications. Combined application of ultrasonic energy to disrupt aggregates and the removal of light fractions with sequential high density fractionation successfully isolated multiple C pools that ranged in radiocarbon-based turnover time from 7 to 1,011 year in the surface 0–15 cm of mineral soil in an undisturbed, native forest. Soil C accumulates as a result of high, continuous input that cycles through a transitional (century-scale) organo-mineral pool and then either becomes occluded and protected within aggregates (multiple centuries) or enters a continuum of organo-mineral and non-crystalline mineral-dominated pools (from centuries to millennium-scale). Comparison of relative C pool sizes and C isotope signature among soils from native forest, grazed pasture, and managed Eucalyptus plantation revealed the potential for making accurate, direct measurements of soil C change over time with land use and management change or disturbance regime.

Keywords

Andisol Carbon cycle Carbon sequestration Land use change Physical fractionation Volcanic ash soil 

Notes

Acknowledgments

Support for this work was provided by National Science Foundation Industry & University Cooperative Research Program (NSF I/UCRC) funding the Center for Bioenergy Research and Development (CBeRD), award No. IIP-0832554 to Scott Turn, P. I. Additional radiocarbon funds were provided through Christopher Swanston and Kate Heckman of the Northern Research Station, USDA Forest Service for preparation and radiocarbon analysis of soil samples at Lawrence Livermore National Lab. We thank Creighton Litton, Christian Giardina, Nicholas Koch (Forest Solutions, Inc.), and Parker Ranch for access to study locations and advice. Appreciation is expressed for Goro Uehara, Jonathan Deenik, Amy Koch, Alisa Davis, Mariko Panzella, Maxim Irion, Jon Wells, and Heather Kikkawa for mentoring, field, and lab work assistance. Troy Baisden provided valuable input and advice on the dataset. We appreciate the thoughtful reviews and comments made by the associate editor and three anonymous reviewers.

Supplementary material

10533_2014_51_MOESM1_ESM.jpg (301 kb)
Supplemental Fig. 1 Relative C balance among soil physical fractions isolated by various methods at the pasture site, bars are mean values ± one standard error for the laboratory replicates. Supplementary material 1 (JPEG 301 kb)
10533_2014_51_MOESM2_ESM.jpg (320 kb)
Supplemental Fig. 2 Relative C balance among soil physical fractions isolated by various methods at the managed Eucalyptus plantation site, bars are mean values ± one standard error for the laboratory replicates. Supplementary material 2 (JPEG 320 kb)
10533_2014_51_MOESM3_ESM.docx (28 kb)
Supplementary material 3 (DOCX 28 kb)

References

  1. Amundson R (2001) The carbon budget in soils. Annu Rev Earth Planet Sci 29:535–562CrossRefGoogle Scholar
  2. Asano M, Wagai R (2014) Evidence of aggregate hierarchy at micro- to submicron scales in an allophanic Andisol. Geoderma 216:62–74CrossRefGoogle Scholar
  3. Baldock J, Oades J, Waters A, Peng X, Vassalo A, Wilson M (1992) Aspects of the chemical structure of soil organic materials as revealed by solid-state 13C NMR spectroscopy. Biogeochemistry 16:1–42CrossRefGoogle Scholar
  4. Basile-Doelsch I, Amundson R, Stone W, Massiello C, Bottero J, Colin F, Masin F, Borschneck D, Meunier J (2005) Mineralogical control of organic carbon dynamics in a volcanic ash soil on La Reunion. Eur J Soil Sci 56:689–703Google Scholar
  5. Basile-Doelsch I, Amundson R, Stone W, Borschneck D, Bottero J, Moustier S, Masin F, Colin F (2007) Mineral control of carbon pools in a volcanic soil horizon. Geoderma 137:477–489CrossRefGoogle Scholar
  6. Buytaert W, Deckers J, Dercon G, de Bièvre B, Poesen J, Govers G (2002) Impact of land use changes on the hydrological properties of volcanic ash soils in South Ecuador. Soil Use Manag 18:94–100. doi: 10.1111/j.1475-2743.2002.tb00226.x CrossRefGoogle Scholar
  7. Cheng W, Parton WJ, Gonzalez-Meler MA, Phillips R, Asao S, McNickle GG, Brzostek E, Jastrow JD (2013) Synthesis and modeling perspectives of rhizosphere priming. New Phytol 201:31–44CrossRefGoogle Scholar
  8. Chevallier T, Woignier T, Toucet J, Blanchart E, Dieudonne P (2008) Fractal structure in natural gels: effect on carbon sequestration in volcanic soils. J Sol-Gel Sci Technol 48:231–238CrossRefGoogle Scholar
  9. Chevallier T, Woignier T, Toucet J, Blanchart E (2010) Organic carbon stabilization in the fractal pore structure of Andosols. Geoderma 159:182–188CrossRefGoogle Scholar
  10. Cole RJ, Litton CM, Koontz MJ, Loh RK (2012) Vegetation recovery 16 years after feral pig removal from a wet Hawaiian forest. Biotropica 44(4):463–471CrossRefGoogle Scholar
  11. Courchesne F, Turmel MC (2008) Extractable Al, Fe, Mn and Si. In: Carter MR, Gregorich EG (eds) Soil sampling and methods of analysis, 2nd edn. Canadian Society of Soil Science, CRC Press, Boca Raton, pp 307–315Google Scholar
  12. Crow SE, Swanston C, Lajtha K, Brooks R, Keirstead H (2007) Density fractionation of forest soils: methodological question and interpretation of incubation results and turnover time in an ecosystem context. Biogeochemistry 85:69–90CrossRefGoogle Scholar
  13. Dahlgren R, Saigusa M, Ugolini F (2004) The nature, properties and management of volcanic soils. Adv Agron 82:113–182CrossRefGoogle Scholar
  14. Dorel M, Roger-Estrade J, Manicho H, Delvaux B (2000) Porosity and soil water properties of Caribbean volcanic ash soils. Soil Use Manag 16:133–140CrossRefGoogle Scholar
  15. Giardina CP, Litton CM, Crow SE, Asner GP (2014) Warming-related increases in soil CO2 efflux are explained by increased below-ground carbon flux. Nat Clim Change. doi: 10.1038/NCLIMATE2322 Google Scholar
  16. Golchin A, Oades J, Skjemstad J, Clarke P (1994) Study of free and occluded particulate organic matter in soils by solid state 13C CP/MAS NMR spectroscopy and scanning electron microscopy. Aust J Soil Res 32:285–309CrossRefGoogle Scholar
  17. Hua Q, Barbetti M, Rakowski A (2013) Atmospheric radiocarbon for the period 1950–2010. Radiocarbon 55:2059–2072CrossRefGoogle Scholar
  18. Huygens D, Boeckx P, Van Cleemput O, Oyarzun C, Godoy R (2005) Aggregate and soil organic carbon dynamics in South Chilean Andisols. Biogeosciences 2:159–174CrossRefGoogle Scholar
  19. Ikawa H, Sato H, Chang A, Nakamura S, Robello E, Periaswamy S (1985) Soils of the Hawaii Agricultural Experiment Station, University of Hawaii: soil survey, laboratory data, and soil descriptions. Research Extension Series 022. BSP Tech. Rep. 4. Research extension series, ISSN 0271-9916Google Scholar
  20. Jenkinson DS (1990) The turnover of organic carbon and nitrogen in soil. Philos Trans R Soc B 329:361–368CrossRefGoogle Scholar
  21. Kaiser K, Guggenberger G (2007) Sorptive stabilization of organic matter by microporous goethite: sorption into small pores vs. surface complexation. Eur J Soil Sci 58:45–59CrossRefGoogle Scholar
  22. Kaiser M, Berhe A, Sommer M, Kleber M (2012) Application of ultrasound to disperse soil aggregates of high mechanical stability. J Plant Nutr Soil Sci 000:1–6Google Scholar
  23. Kimble J, Ping C, Sumner M, Wilding L (2000) Andisols. In: Sumner ME (ed) Handbook of soil science. CRC Press, Boca Raton, pp 209–224Google Scholar
  24. Kramer M, Sanderman J, Chadwick O, Chorover J, Vitousek P (2012) Long-term carbon storage through retention of dissolved aromatic acids by reactive particles in soil. Glob Change Biol 18:2594–2605CrossRefGoogle Scholar
  25. Kubota T (1972) Aggregate-formation of allophanic soils: effects of drying on the dispersion of the soils. Coil Sci Plant Nutr 18:79–87CrossRefGoogle Scholar
  26. Kuzyakov Y (2010) Priming effects: interactions between living and dead organic matter. Soil Biol Biochem 42:1363–1371CrossRefGoogle Scholar
  27. Lal R (2008) Carbon Sequestration. Philos Trans R Soc B Biol Sci 363:815–830CrossRefGoogle Scholar
  28. Lal R (2013) Soil carbon management and climate change. Carbon Manag 4(4):439–462CrossRefGoogle Scholar
  29. Levin I (2012) Earth science: the balance of the carbon budget. Nature 488:35–36CrossRefGoogle Scholar
  30. Manzoni S, Porporato A (2009) Soil carbon and nitrogen mineralization: theory and models across scales. Soil Biol Biochem 41:1355–1379CrossRefGoogle Scholar
  31. Mikutta R, Schaumann GE, Gildemeister D, Bonneville S, Kramer MG, Chadwick OA, Guggenberger G (2009) Biogeochemistry of mineral–organic associations across a long-term mineralogical soil gradient (0.3–4100 kyr), Hawaiian Islands. Geochim Cosmochim Acta 73:234–260Google Scholar
  32. Moni C, Derrien D, Hatton PJ, Zeller B, Kleber M (2012) Density fractions versus size separates: does physical fractionation isolate functional soil compartments? Biogeosciences 9:5181–5197CrossRefGoogle Scholar
  33. Neris J, Tejedor M, Fuentes J, Jiménez C (2013) Infiltration, runoff and soil loss in Andisols affected by forest fire (Canary Islands, Spain). Hydrol Process 27(19):2814–2824CrossRefGoogle Scholar
  34. North PF (1976) Towards an absolute measurement of soil structural stability using ultrasound. J Soil Sci 27:451–459CrossRefGoogle Scholar
  35. Parfitt R (1980) Chemical properties of variably charged soils. In: Theng BKG (ed) Soils with variable charge. Soil Bureau D.S.I.R., Lower Hutt, pp 167–194Google Scholar
  36. Parfitt RL, Churchman GJ (1988) Clay minerals and humus complexes in five Kenyan soils derived from volcanic ash—a discussion. Geoderma 42:365–367CrossRefGoogle Scholar
  37. Parton WJ, Schimel DS, Cole CV, Ojima DS (1987) Analysis of factors controlling soil organic matter levels in Great Plains Grasslands. Soil Sci Soc Am J 51:1173–1179CrossRefGoogle Scholar
  38. Paul S, Martinson G, Veldkamp E (2008) Sample pretreatment affects the distribution of organic carbon in aggregates of tropical grassland soils. Soil Sci Soc Am J 72:500–506CrossRefGoogle Scholar
  39. Perdrial N, Perdrial J, Delphin J, Elsass F, Liewig N (2010) Temporal and spatial monitoring of mobile nanoparticles in a vineyard soil: evidence of nanoaggregate formation. Eur J Soil Sci 61:456–468CrossRefGoogle Scholar
  40. Poulenard J, Podwojewski P, Janeau JL, Collinet J (2001) Runoff and soil erosion under rainfall simulation of Andisols from the Ecuadorian Páramo: effect of tillage and burning. Catena 45(3):185–207CrossRefGoogle Scholar
  41. Reimer PJ, Brown TA, Reimer RW (2004) Discussion: reporting and calibration of post-bomb C-14 data. Radiocarbon 46:1299–1304Google Scholar
  42. Roscoe R, Buurman P, Velthorst EJ (2000) Disruption of soil aggregates by varied amounts of ultrasonic energy in fractionation of organic matter of a clay Latosol: carbon, nitrogen and delta13C distribution in particle-size fractions. Eur J Soil Sci 51:445–454CrossRefGoogle Scholar
  43. Ross GJ, Wang C, Schuppli PA (1985) Hydroxylamine and ammonium oxalate solutions as extractants for iron and aluminum from soils. Soil Sci Soc Am J 49:783–785CrossRefGoogle Scholar
  44. Schmidt MW, Torn MS, Abiven S, Dittmar T, Guggenberger G, Janssen IA, Kleber M, Kogel-Knabner I, Lehmann J, Manning DAC, Nannipieri P, Rasse DP, Weiner S, Trumbore SE (2011) Persistence of soil organic matter as an ecosystem property. Nature 478:49–56CrossRefGoogle Scholar
  45. Selmants PC, Litton CM, Giardina CP, Asner GP (2014) Ecosystem carbon storage does not vary with mean annual temperature in Hawaiian tropical montane wet forests. Glob Change Biol 20:2927–2937CrossRefGoogle Scholar
  46. Shoji S, Nanzyo M, Shirato Y, Ito T (1993) Chemical kinetics of weathering in young Andisols from northeastern Japan using soil age normalized to 10C. Soil Sci 155:53–60CrossRefGoogle Scholar
  47. Sierra CA, Müller M, Trumbore SE (2012) Models of soil organic matter decomposition: the SoilR package, version 1.0. Geosci Model Dev 5:1045–1060CrossRefGoogle Scholar
  48. Sierra CA, Müller M, Trumbore SE (2014) Modeling radiocarbon dynamics in soils: soilR version 1.1. Geosci Model Dev 7:3161–3192CrossRefGoogle Scholar
  49. Silva JHS, Deenik JL, Yost RS, Bruland GL, Crow SE (2015)  Improving clay measurement in oxidic and volcanic ash soil of Hawaii by increasing dispersant concentration and ultrasonic energy levels. Geoderma 237-238:211-223Google Scholar
  50. Six J, Paustian K, Elliott ET, Combrink C (2000) Soil structure and organic matter I. Distribution of aggregate-size classes and aggregate-associated carbon. Soil Sci Soc Am J 64(2):681–689CrossRefGoogle Scholar
  51. Six J, Callewaert P, Lenders S, De Gryze S, Morris SJ, Gregorich EG, Paul EA, Paustian K (2002) Measuring and understanding carbon storage in afforested soils by physical fractionation. Soil Sci Soc Am J 66:1981–1987CrossRefGoogle Scholar
  52. Soetaert K, Petzoldt T, Setzer R (2010) Solving differential equations in R: package deSolve. J Stat Softw 33:1–25Google Scholar
  53. Soil Survey Staff, Natural Resources Conservation Service, United States Department of Agriculture. Web Soil Survey. http://www.websoilsurvey.nrcs.usda.gov/. Accessed 09/01/2014
  54. Sollins P, Swanston C, Kleber M, Filley T, Kramer M, Crow S, Caldwell B, Lajtha K, Bowden R (2006) Organic C and N stabilization in a forest soil: evidence from sequential density fractionation. Soil Biol Biochem 38:3313–3324CrossRefGoogle Scholar
  55. Sollins P, Swanston C, Kramer M (2007) Stabilization and destabilization of soil organic matter—a new focus. Biogeochemistry 85:1–7CrossRefGoogle Scholar
  56. Sollins P, Kramer M, Swanston C, Lajtha K, Filley T, Aufdenkampe A, Wagai R, Bowden R (2009) Sequential density fractionation across soils of contrasting mineralogy: evidence for both microbial- and mineral-controlled soil organic matter stabilization. Biogeochemistry 96:209–231CrossRefGoogle Scholar
  57. Stockmann U, Adams MA, Crawford JW, Field DJ, Henakaarchchi N, Jenkins M, Minasny B, McBratney AB, de Remy de Courcelles V, Singh K, Wheeler I, Abbott L, Angers DA, Baldock J, Bird M, Brookes PC, Chenu C, Jastrow JD, Lal R, Lehmann J, O’Donnell AG, Parton WJ, Whitehead D, Zimmermann M (2013) The knowns, known unknowns and unknowns of sequestration of soil organic carbon. Agric Ecosyst Environ 164:80–99Google Scholar
  58. Swanston CW, Caldwell BA, Homann PS, Ganio L, Sollins P (2002) C dynamics during a long-term incubation of separate and recombined density fractions from seven forest soils. Soil Biol Biochem 34:1121–1130CrossRefGoogle Scholar
  59. Swanston C, Homann PS, Caldwell BA, Myrold DD, Ganio L, Sollins P (2004) Long-term effects of elevated nitrogen on forest soil organic matter stability. Biogeochemistry 70:227–250CrossRefGoogle Scholar
  60. Torn M, Trumbore S, Chadwick O, Vitousek P, Hendricks D (1997) Mineral control of soil organic carbon storage and turnover. Nature 389:170–173CrossRefGoogle Scholar
  61. Trumbore SE (1993) Comparison of carbon dynamics in tropical and temperate soils using radiocarbon measurements. Global Biogeochem Cycles 7(2):275–290Google Scholar
  62. Virto I, Barre P, Chenu C (2008) Microaggregation and organic matter storage at the silt-size scale. Geoderma 146:326–335Google Scholar
  63. Vitousek PM (1990) Biological invasions and ecosystem processes: towards an integration of population biology and ecosystem studies. Oikos 57:7–13CrossRefGoogle Scholar
  64. Vogel JS, Southon JR, Nelson DE, Brown TA (1984) Performance of catalytically condensed carbon for use in accelerator mass-spectrometry. Nucl Instrum Methods Phys Res Sect B 233:289–293CrossRefGoogle Scholar
  65. von Lützow M, Kögel-Knabner I, Ludwig B, Matzner E, Flessa H, Ekschmitt K, Guggenberger G, Marschner B, Kalbitz K (2008) Stabilization mechanisms of organic matter in four temperate soils: development and application of a conceptual model. J Plant Nutr Soil Sci 171:111–124CrossRefGoogle Scholar
  66. Wada K (1985) Distinctive properties of andosols. In: Stewart BS (ed) Advances in soil science, vol 2. Springer, New York, pp 173–229CrossRefGoogle Scholar
  67. Wada K (1989) Allophane and imogolite. In: Dixson JB, Weed SB (eds) Minerals in soil environments, 2nd edn. Soil Science Society of America, Madison, pp 1051–1087Google Scholar
  68. Walker AL (1983) The effects of magnetite on oxalate- and dithionite-extractable iron. Soil Sci Soc Am J 47:1022–1025CrossRefGoogle Scholar
  69. Woignier T, Primera J, Hashmy A (2006) Application of DLCA model to “natural” gels: the allophanic soils. J Sol-Gel Sci Technol 40:201–207CrossRefGoogle Scholar

Copyright information

© Springer International Publishing Switzerland 2014

Authors and Affiliations

  • Susan E. Crow
    • 1
  • Mataia Reeves
    • 1
  • Olivia S. Schubert
    • 1
  • Carlos A. Sierra
    • 2
  1. 1.Natural Resources and Environmental Management Department (NREM Department)University of Hawaii ManoaHonoluluUSA
  2. 2.Max Planck Institute for BiogeochemistryJenaGermany

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