Skip to main content

Advertisement

Log in

Fallow associated with autumn-plough favors structure stability and storage of soil organic carbon compared to continuous maize cropping in Mollisols

  • Regular Article
  • Published:
Plant and Soil Aims and scope Submit manuscript

Abstract

Background and aims

Aggregate formation and stability of soil organic carbon (SOC) differ in different farming systems, probably due to differences in effects of tillage and residue management. This study used a 24-year field experiment to compare the effects of continuous maize cropping and natural fallow on aggregate formation and SOC storage in various aggregate-size classes and density fractions of a Chinese Mollisol.

Methods

Soils collected from the upper 0.2-m layer were wet-sieved into four aggregate-size classes (>2, 0.25–2, 0.053–0.25 and <0.053 mm) which were then fractionated into light, occluded and mineral C fractions. The concentrations of SOC and natural 13C abundance of each fraction in bulk soil and the aggregate classes were determined.

Results

Continuous maize cropping decreased the proportion of macro-aggregates (>0.25 mm) and increased that of micro-aggregates (<0.25 mm) compared to the initial value while the opposite was observed in the natural fallow system. The fallow system generally had greater SOC concentration in the occluded fraction, higher proportion of newly-derived C as % total SOC in the light fraction and greater contribution of total residue C to new C in macro-aggregates and light fractions compared to the continuous maize system. Furthermore, the fallow system resulted in shorter turnover time of SOC than the continuous maize system.

Conclusions

Natural fallow associated with autumn-plough improved soil structural stability and SOC storage while continuous maize cropping with residue removal decreased SOC sequestration and soil aggregate stability.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6

Similar content being viewed by others

References

  • Álvaro-Fuentes J, Arrúe JL, Cantero-Martínez C, López MV (2008) Aggregate breakdown during tillage in a Mediterranean loamy soil. Soil Tillage Res 101:62–68

    Article  Google Scholar 

  • Ando K, Shinjo H, Kuramitsu H, Miura R, Sokotela S, Funakawa S (2014) Effects of cropping and short-natural fallow rotation on soil organic carbon in the Eastern Province of Zambia. Agric Ecosyst Environ 196:34–41

    Article  Google Scholar 

  • Barley KP (1970) The configuration of the root system in relation to nutrient uptake. Adv Agron 22:159–201

    Article  Google Scholar 

  • Breulmann M, Boettger T, Buscot F, Gruendling R, Schulz E (2016) Carbon storage potential in size–density fractions from semi-natural grassland ecosystems with different productivities over varying soil depths. Sci Total Environ 545:30–39

    Article  PubMed  Google Scholar 

  • Burrows RL, Pfleger FL (2002) Arbuscular mycorrhizal fungi respond to increasing plant diversity. Can J Bot 80:120–130

    Article  Google Scholar 

  • Buyanovsky GA, Wagner GH (1998) Carbon cycling in cultivated land and its global significance. Glob Chang Biol 4:131–141

    Article  Google Scholar 

  • Carter MR (2002) Soil quality for sustainable land management: organic matter and aggregation interactions that maintain soil functions. Agron J 94:38–47

    Article  Google Scholar 

  • Cerli C, Celi L, Kalbitz K, Guggenberger G, Kaiser K (2012) Separation of light and heavy organic matter fractions in soil-testing for proper density cut-off and dispersion level. Geoderma 170:403–416

    Article  CAS  Google Scholar 

  • Cotrufo MF, Soong JL, Horton AJ, Campbell EE, Haddix ML, Wall DH, Parton WJ (2015) Formation of soil organic matter via biochemical and physical pathways of litter mass loss. Nat Geosci 8:776–779

    Article  CAS  Google Scholar 

  • Dorodnikov M, Kuzyakov Y, Fangmeier A, Wiesenberg GLB (2011) C and N in soil organic matter density fractions under elevated atmospheric CO2: turnover vs. stabilization. Soil Biol Biochem 43:579–589

    Article  CAS  Google Scholar 

  • 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 100:118–124

    Article  CAS  Google Scholar 

  • Fu S, Cheng W (2002) Rhizosphere priming effects on the decomposition of soil organic matter in C4 and C3 grassland soils. Plant Soil 238:289–294

    Article  CAS  Google Scholar 

  • Fuentes M, Govaerts B, Hidalgo C, Etchevers J, González-Martín I, Hernández-Hierro JM, Sayre KD, Dendooven L (2010) Organic carbon and stable 13C isotope in conservation agriculture and conventional systems. Soil Biol Biochem 42:551–557

    Article  CAS  Google Scholar 

  • Golchin A, Oades JM, Skjemstad JO, 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 32:285–309

    Article  CAS  Google Scholar 

  • Golchin A, Baldock JA, Oades JM (1997) A model linking organic matter decomposition, chemistry, and aggregate dynamics. CRC Press, Boca Raton

    Google Scholar 

  • Gunina A, Kuzyakov Y (2014) Pathways of litter C by formation of aggregates and SOM density fractions: implications from 13C natural abundance. Soil Biol Biochem 71:95–104

    Article  CAS  Google Scholar 

  • Haynes RJ, Naidu R (1998) Influence of lime, fertilizer and manure applications on soil organic matter content and soil physical conditions: a review. Nutr Cycl Agroecosyst 51:123–137

    Article  Google Scholar 

  • He SX, Liang ZS, Han RL, Wang Y, Liu GB (2016) Soil carbon dynamics during grass restoration on abandoned sloping cropland in the hilly area of the loess plateau, China. Catena 137:679–685

    Article  Google Scholar 

  • Jastrow JD (1996) Soil aggregate formation and the accrual of particulate and mineral-associated organic matter. Soil Biol Biochem 28:665–676

    Article  CAS  Google Scholar 

  • John B, Yamashita T, Ludwig B, Flessa H (2005) Storage of organic carbon in aggregate and density fractions of silty soils under different types of land use. Geoderma 128:63–79

    Article  CAS  Google Scholar 

  • Johnston AE, Poulton PR, Coleman K (2009) Soil organic matter: its importance in sustainable agriculture and carbon dioxide fluxes. Adv Agron 101:1–57

    Article  Google Scholar 

  • Kasper M, Buchan GD, Mentler A, Blum WEH (2009) Influence of soil tillage systems on aggregate stability and the distribution of C and N in different aggregate fractions. Soil Tillage Res 105:192–199

    Article  Google Scholar 

  • Kou TJ, Zhu P, Huang S, Peng XX, Song ZW, Deng AX, Gao HJ, Peng C, Zhang WJ (2012) Effects of long-term cropping regimes on soil carbon sequestration and aggregate composition in rainfed farmland of Northeast China. Soil Tillage Res 118:132–138

    Article  Google Scholar 

  • Kuzyakov Y (2010) Priming effects: interactions between living and dead organic matter. Soil Biol Biochem 42:1363–1371

    Article  CAS  Google Scholar 

  • Liao JD, Boutton TW, Jastrow JD (2006) Organic matter turnover in soil physical fractions following woody plant invasion of grassland: evidence from natural 13C and 15N. Soil Biol Biochem 38:3197–3210

    Article  CAS  Google Scholar 

  • Lichter K, Govaerts B, Six J, Sayre KD, Deckers J, Dendooven L (2008) Aggregation and C and N contents of soil organic matter fractions in a permanent raised-bed planting system in the highlands of Central Mexico. Plant Soil 305:237–252

    Article  CAS  Google Scholar 

  • Majumder B, Kuzyakov Y (2010) Effect of fertilization on decomposition of 14C labelled plant residues and their incorporation into soil aggregates. Soil Tillage Res 109:94–102

    Article  Google Scholar 

  • Mandiola M, Studdert GA, Domínguez GF, Videla CC (2011) Organic matter distribution in aggregate sizes of a mollisol under contrasting managements. J Soil Sci Plant Nutr 11:41–57

    Article  Google Scholar 

  • McCarthy JF, Ilavsky J, Jastrow JD, Mayer LM, Perfect E, Zhuang J (2008) Protection of organic carbon in soil microaggregates via restructuring of aggregate porosity and filling of pores with accumulating organic matter. Geochim Cosmochim Acta 72:4725–4744

    Article  CAS  Google Scholar 

  • McLauchland KK, Hobbie SE, Post WM (2006) Conversion from agriculture to grassland builds soil organic matter on decadal timescales. Ecol Appl 16:143–153

    Article  Google Scholar 

  • Millard P, Midwood AJ, Hunt JE, Barbour MM, Whitehead D (2010) Quantifying the contribution of soil organic matter turnover to forest soil respiration, using natural abundance δ13C. Soil Biol Biochem 42:935–943

    Article  CAS  Google Scholar 

  • Monreal CM, Schulten HR, Kodama H (1997) Age, turnover and molecular diversity of soil organic matter in aggregates of a Gleysol. Can J Soil Sci 77:379–388

    Article  Google Scholar 

  • Nyamadzawo G, Nyamangara J, Nyamugafata P, Muzulu A (2009) Soil microbial biomass and mineralization of aggregate protected carbon in fallow-maize systems under conventional and no-tillage in Central Zimbabwe. Soil Tillage Res 102:151–157

    Article  Google Scholar 

  • Oehl F, Laczko E, Bogenrieder A, Stahr K, Bosch R, van der Heijden M, Sieverding E (2010) Soil type and land use intensity determine the composition of arbuscular mycorrhizal fungal communities. Soil Biol Biochem 42:724–738

    Article  CAS  Google Scholar 

  • Paustian K, Andren O, Janzen HH, Lal R, Smith P et al (1997) Agricultural soils as a sink to mitigate CO2 emissions. Soil Use Manag 13:230–244

    Article  Google Scholar 

  • Puget P, Chenu C, Balesdent J (2000) Dynamics of soil organic matter associated with particle-size fractions of water-stable aggregates. Eur J Soil Sci 51:595–605

    Article  Google Scholar 

  • Qiao YF, Miao SJ, Silva LCR, Horwath WR (2014) Understory species regulate litter decomposition and accumulation of C and N in forest soils: a long-term dual-isotope experiment. Forest Eco Manag 329:318–327

    Article  Google Scholar 

  • Qiao YF, Miao SJ, Li N, Xu YL, Han XZ, Zhang B (2015) Crop species affect soil organic carbon turnover in soil profile and among aggregate sizes in a mollisol as estimated from natural 13C abundance. Plant Soil 392:163–174

    Article  CAS  Google Scholar 

  • Quenea K, Lamy I, Winterton P, Bermond A, Dumat C (2009) Interactions between metals and soil organic matter in various particle size fractions of soil contaminated with waste water. Geoderma 149:217–223

    Article  CAS  Google Scholar 

  • Rasmussen C, Torn MS, Southard RJ (2005) Mineral assemblage and aggregates control carbon dynamics in a California conifer forest. Soil Sci Soc Am J 69:1711–1721

    Article  CAS  Google Scholar 

  • Schrumpf M, Kaiser K, Guggenberger G, Persson T, Kogel-Knabner I, Schulze ED (2013) Storage and stability of organic carbon in soils as related to depth, occlusion within aggregates, and attachment to minerals. Biogeosciences 10:1675–1691

    Article  CAS  Google Scholar 

  • Shang SY, Jiang PK, Chang SX, Song ZL, Liu J, Sun L (2014) Soil organic carbon in particle size and density fractionations under four forest vegetation-land use types in subtropical China. Forests 5:1391–1408

    Article  Google Scholar 

  • Six J, Jastrow JD (2002) Organic matter turnover. Marcel Dekker, New York

    Google Scholar 

  • Six J, Elliott ET, Paustian K, Doran JW (1998) Aggregation and soil organic matter accumulation in cultivated and native grassland soils. Soil Sci Soc Am J 62:1367–1377

    Article  CAS  Google Scholar 

  • Six J, Paustian K, Elliott ET, Combrink C (2000) Soil structure and soil organic matter: I. Distribution of aggregate size classes and aggregate associated carbon. Soil Sci Soc Am J 64:681–689

    Article  CAS  Google Scholar 

  • Six J, Conant RT, Paul EA, Paustian K (2002) Stabilization mechanisms of soil organic matter: implications for C-saturation of soils. Plant Soil 241:155–176

    Article  CAS  Google Scholar 

  • Sohi SP, Mahieu N, Arah JRM, Powlson DS, Madari B, Gaunt JL (2001) A procedure for isolating soil organic matter fractions suitable for modeling. Soil Sci Soc Am J 65:1121–1128

    Article  CAS  Google Scholar 

  • Soka GS, Ritchie ME, Mayemba EP (2015) Influence of current land use and edaphic factors on arbuscular mycorrhizal (AM) hyphal abundance and soil organic matter in and near Serengeti National Park. J Ecol Nat Environ 7:158–169

    Article  Google Scholar 

  • Song ZW, Zhu P, Gao HJ, Peng C, Deng AX, Zheng CY, Mannaf MA, Islam MN, Zhang WJ (2015) Effects of long-term fertilization on soil organic carbon content and aggregate composition under continuous maize cropping in Northeast China. J Agric Sci 153:236–244

    Article  CAS  Google Scholar 

  • Tisdall JM, Oades JM (1982) Organic matter and water-stable aggregates in soils. J Soil Sci 33:141–163

    Article  CAS  Google Scholar 

  • Tivet F, de Moraes Sá JC, Lal R, Briedis C, Borszowskei PR, dos Santos JB, Farias A, Eurich G, da Cruz Hartman D, Nadolny Junior M, Bouzinac S, Séguy L (2013) Aggregate C depletion by plowing and its restoration by diverse biomass-C inputs under no-till in sub-tropical and tropical regions of Brazil. Soil Tillage Res 126:203–218

    Article  Google Scholar 

  • Urbanek E, Smucker AJM, Horn R (2011) Total and fresh organic carbon distribution in aggregate size classes and single aggregate regions using natural 13C/12C tracer. Geoderma 164:164–171

    Article  CAS  Google Scholar 

  • Van Bravel C (1950) Mean weight-diameter of soil aggregates as a statistical index of aggregation. Soil Sci Soc Am J 14:20–23

    Article  Google Scholar 

  • von Lützow M, Kögel-Knabner I, Ekschmitt K, Flessa H, Guggenberger G, Matzner E (2007) SOM fractionation methods: relevance to functional pools and to stabilization mechanisms. Soil Biol Biochem 39:2183–2207

    Article  Google Scholar 

  • Wagai R, Mayer LM, Kitayama K, Knicker H (2008) Climate and parent material controls on organic matter storage in surface soils: a three-pool, density-separation approach. Geoderma 147:23–33

    Article  CAS  Google Scholar 

  • Werth M, Kuzyakov Y (2010) 13C fractionation at the root-microorganisms-soil interface: a review and outlook for partitioning studies. Soil Biol Biochem 42:1372–1384

    Article  CAS  Google Scholar 

  • Xie JY, Xu MG, Ciren Q, Yang Y, Zhang SL, Sun BH, Yang XY (2015) Soil aggregation and aggregate associated organic carbon and total nitrogen under long-term contrasting soil management regimes in loess soil. J Integr Agric 14:2405–2416

    Article  CAS  Google Scholar 

  • Yamashita T, Flessa H, John B, Helfrich M, Ludwig B (2006) Organic matter in density fractions of water-stable aggregates in silty soils: effect of land use. Soil Biol Biochem 38:3222–3234

    Article  CAS  Google Scholar 

  • Yang XM (2000) Carbon sequestration in farming land soils: an approach to buffer the global warming and to improve soil productivity. Soil Environ Sci 9:311–315

    Google Scholar 

  • Yu G, Fang H, Gao L, Zhang W (2006) Soil organic carbon budget and fertility variation of black soils in Northeast China. Ecol Res 21:855–867

    Article  CAS  Google Scholar 

  • Zimmermann M, Leifeld J, Schmidt MWI, Smith P, Fuhrer J (2007) Measured soil organic matter fractions can be related to pools in the Roth C model. Eur J Soil Sci 58:658–667

    Article  Google Scholar 

Download references

Acknowledgements

We thank Nang Seng Aye for valuable comments on the manuscript. This project was supported by National Natural Science Foundation of China (41371297, 41471240), Special Fund for Agro-Scientific Research in the Public Interest (201503116), and Nanjing University of Information Science and Technology talent start. The δ13C abundance was analyzed at the Stable Isotope Facility in University of California Davis.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Caixian Tang.

Additional information

Responsible Editor: Johan Six.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Miao, S., Qiao, Y., Li, P. et al. Fallow associated with autumn-plough favors structure stability and storage of soil organic carbon compared to continuous maize cropping in Mollisols. Plant Soil 416, 27–38 (2017). https://doi.org/10.1007/s11104-017-3187-z

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11104-017-3187-z

Keywords

Navigation