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Different response of CO2 and N2O fluxes to N deposition with seasons in a temperate forest in northeastern China

Abstract

Purpose

Elevated nitrogen (N) deposition had changed terrestrial carbon (C) and N cycling during the last several decades. Greenhouse gas (GHG) emission, serving as an important process of global C and N cyclings, was susceptible to elevated N deposition. However, the lack of GHG measurements in the spring freezing-thawing cycles (FTC) period and inconstant results of GHG emissions in growing season result in the uncertainties of GHG emission responding to elevated N deposition.

Materials and methods

Static chambers were used to monitor CO2 and N2O fluxes in growing season and spring FTC period in a simulated N deposition forest in northeastern China, which had been fertilized with different N amounts for 6 years.

Results and discussion

The temperate forest soil that subjected to N fertilizer was a net source of CO2 and N2O. The intensely fluctuant fluxes during the spring FTC period were due to stimulation of microbial activities induced by sharply changed soil temperature and moisture. The physical release of trapped gases beneath ice layer during the whole winter also contributed to the drastic increase of fluxes. No effect of N addition on the CO2 efflux was detected in the growing season or spring FTC period, indicating that N was not limited for microbial respiration. In contrast, N addition decreased the N2O flux by 72.8~85.7% in the growing season whereas increased by 11.2~17.8 times in the spring FTC period, which could be explained by the shift in structure of microbial community. Over the entire dataset, soil temperature and moisture could explain about 60 and 30% of seasonal variations of CO2 or N2O flux, respectively. By fitting the RST5W5 model to separate season, poorer fit was achieved in the spring FTC period compared with growing season, suggesting a weakening effect of soil microclimates on CO2 efflux.

Conclusions

These results indicate that long-term elevated N deposition affected CO2 and N2O fluxes differently with seasons in a temperate forest soil, which will help to predict soil GHG flux under the conditions of global climate change.

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References

  1. van ochove E, Prévost D, Pelletier F (2000) Effects of freeze–thaw and soil structure on nitrous oxide produced in a clay soil. Soil Sci Soc Am J 64:1638–1643

  2. Boberg JB, Finlay RD, Stenlid J, Ekblad A, Lindahl BD (2014) Nitrogen and carbon reallocation in fungal mycelia during decomposition of boreal forest litter. PLoS One 9(3):e92897. https://doi.org/10.1371/journal.pone.0092897

  3. Bowden R, Rullo G, Stevens G, Steudler P (2000) Soil fluxes of carbon dioxide, nitrous oxide, and methane at a productive temperate deciduous forest. J Environ Qual 29(1):268–276. https://doi.org/10.2134/jeq2000.00472425002900010034x

  4. Boyle SA, Yarwood RR, Bottomley PJ, Myrold DD (2008) Bacterial and fungal contributions to soil nitrogen cycling under Douglas fir and red alder at two sites in Oregon. Soil Biol Biochem 40(2):443–451. https://doi.org/10.1016/j.soilbio.2007.09.007

  5. Chapuis-Lardy L, Wrage N, Metay A, Chotte JL, Bernoux M (2007) Soils, a sink for N2O? A review. Glob Chang Biol 13(1):1–17. https://doi.org/10.1111/j.1365-2486.2006.01280.x

  6. Cheng Y, Wang J, Wang SQ, Zhang JB, Cai ZC (2014) Effects of soil moisture on gross N transformations and N2O emission in acid subtropical forest soils. Biol Fert Soils 50(7):1099–1108. https://doi.org/10.1007/s00374-014-0930-y

  7. Elberling B, Brandt KK (2003) Uncoupling of microbial CO2 production and release in frozen soil and its implications for field studies of arctic C cycling. Soil Biol Biochem 35(2):263–272. https://doi.org/10.1016/S0038-0717(02)00258-4

  8. Enrique AG, Bruno EC, Christopher A, Virgile C, Stéven C (2008) Effects of nitrogen availability on microbial activities, densities and functional diversities involved in the degradation of a Mediterranean evergreen oak litter (Quercus ilex L.) Soil Biol Biochem 40(7):1654–1661. https://doi.org/10.1016/j.soilbio.2008.01.020

  9. Fontaine S, Henault C, Aamor A, Bdioui N, JMG B, Maire V, Mary B, Revaillot S, Maron PA (2011) Fungi mediate long term sequestration of carbon and nitrogen in soil through their priming effect. Soil Biol Biochem 43:86–96

  10. Goldberg SD, Gebauer G (2009) Drought turns a Central European Norway spruce forest soil from an N2O source to a transient N2O sink. Glob Chang Biol 15(4):850–860. https://doi.org/10.1111/j.1365-2486.2008.01752.x

  11. Hashida S-N, Johkan M, Kitazaki K, Shoji K, Goto F, Yoshihara T (2013) Management of nitrogen fertilizer application, rather than functional gene abundance, governs nitrous oxide fluxes in hydroponics with rockwool. Plant Soil 374:715–725

  12. Högberg P, Nordgren A, Buchmann N, Taylor AF, Ekblad A, Högberg MN, Nyberg G, Ottosson-Löfvenius M, Read DJ (2001) Large-scale forest girdling shows that current photosynthesis drives soil respiration. Nature 411(6839):789–792. https://doi.org/10.1038/35081058

  13. Holst J, Liu C, Yao Z, Brüggemann N, Zheng X, Giese M, Butterbach-Bahl K (2008) Fluxes of nitrous oxide, methane and carbon dioxide during freezing–thawing cycles in an Inner Mongolian steppe. Plant Soil 308:105–117

  14. Hwang S, Hanaki K (2000) Effects of oxygen concentration and moisture content of refuse on nitrification, denitrification and nitrous oxide production. Bioresour Technol 71(2):159–165. https://doi.org/10.1016/S0960-8524(99)90068-8

  15. Inselsbacher E, Wanek W, Ripka K, Hackl E, Sessitsch A, Strauss J, Zechmeister-Boltenstern S (2010) Greenhouse gas fluxes respond to different N fertilizer types due to altered plant-soil-microbe interactions. Plant Soil 343:17–35

  16. IPCC (2013) Climate change 2013: the physical science basis. Contribution of working group I to the fifth assessment report of the intergovernmental panel on climate change. Cambridge University Press, 2013

  17. Janssens IA, Dieleman W, Luyssaert S, Subke JA, Reichstein M, Ceulemans R, Ciais P, Dolman AJ, Grace J, Matteucci G, Papale D, Piao SL, Schulze ED, Tang J, Law BE (2010) Reduction of forest soil respiration in response to nitrogen deposition. Nat Geosci 3(5):315–322. https://doi.org/10.1038/ngeo844

  18. Kang S, Doh S, Lee D, Lee D, Jin VL, Kimball JS (2003) Topographic and climatic controls on soil respiration in six temperate mixed-hardwood forest slopes, Korea. Glob Chang Biol 9(10):1427–1437. https://doi.org/10.1046/j.1365-2486.2003.00668.x

  19. Koehler B, Corre MD, Veldkamp E, Wullaert H, Wright SJ (2009) Immediate and long-term nitrogen oxide emissions from tropical forest soils exposed to elevated nitrogen input. Glob Chang Biol 15(8):2049–2066. https://doi.org/10.1111/j.1365-2486.2008.01826.x

  20. Krause K, Niklaus PA, Schleppi P (2013) Soil-atmosphere fluxes of the greenhouse gases CO2, CH4 and N2O in a mountain spruce forest subjected to long-term N addition and to tree girdling. Agric For Meteorol 181:61–68. https://doi.org/10.1016/j.agrformet.2013.07.007

  21. Lashof DA, Ahuja DR (1990) Relative contributions of greenhouse gas emissions to global warming. Nature 344(6266):529–531. https://doi.org/10.1038/344529a0

  22. Law B (2013) Biogeochemistry: nitrogen deposition and forest carbon. Nature 496(7445):307–308. https://doi.org/10.1038/496307a

  23. Liu L, Greaver TL (2009) A review of nitrogen enrichment effects on three biogenic GHGs: the CO2 sink may be largely offset by stimulated N2O and CH4 emission. Ecol Lett 12(10):1103–1117. https://doi.org/10.1111/j.1461-0248.2009.01351.x

  24. Liu YY, Li FR, Jin GZ (2014) Spatial patterns and associations of four species in an old-growth temperate forest. J Plant Interact 9(1):745–753. https://doi.org/10.1080/17429145.2014.925146

  25. Lu RK (2000) Soil agro-chemical analyses. Agricultural Technical Press of China, Beijing

  26. Maljanen M, Jokinen H, Saari A, Strommer R, Martikainen PJ (2006) Methane and nitrous oxide fluxes, and carbon dioxide production in boreal forest soil fertilized with wood ash and nitrogen. Soil Use Manage 22(2):151–157. https://doi.org/10.1111/j.1475-2743.2006.00029.x

  27. Meunier CL, Gundale MJ, Sánchez IS, Liess A (2016) Impact of nitrogen deposition on forest and lake food webs in nitrogen-limited environments. Glob Chang Biol 22(1):164–179. https://doi.org/10.1111/gcb.12967

  28. Mo W, Lee MS, Uchida M, Inatomi M, Saigusa N, Mariko S, Koizumi H (2005) Seasonal and annual variations in soil respiration in a cool-temperate deciduous broad-leaved forest in Japan. Agric For Meteorol 134(1-4):81–94. https://doi.org/10.1016/j.agrformet.2005.08.015

  29. Panikov N, Flanagan P, Oechel W, Mastepanov M, Christensen T (2006) Microbial activity in soils frozen to below −39°C. Soil Biol Biochem 38:785–794

  30. Qi YJ, Li FR, Liu ZL, Jin GZ (2014) Impact of understorey on overstorey leaf area index estimation from optical remote sensing in five forest types in northeastern China. Agric For Meteorol 198-199:72–80. https://doi.org/10.1016/j.agrformet.2014.08.001

  31. Sakata R, Shimada S, Arai H, Yoshioka N, Yoshioka R, Aoki H, Kimoto N, Sakamoto A, Melling L, Inubushi K (2015) Effect of soil types and nitrogen fertilizer on nitrous oxide and carbon dioxide emissions in oil palm plantations. Soil Sci Plant Nutr 61(1):48–60. https://doi.org/10.1080/00380768.2014.960355

  32. Schlesinger WH (2013) An estimate of the global sink for nitrous oxide in soils. Glob Chang Biol 19(10):2929–2931. https://doi.org/10.1111/gcb.12239

  33. Shaaban M, Peng Q, Hu R, Lin S, Zhao J (2016) Soil nitrous oxide and carbon dioxide emissions following incorporation of above- and below-ground biomass of green bean. Int J Environ Sci Te 13(1):179–186. https://doi.org/10.1007/s13762-015-0843-9

  34. Shvaleva A, Costa E Silva F, Costa JM, Correia A, Anderson M, Lobo-do-Vale R, Fangueiro D, Bicho C, Pereira JS, Chaves MM, Skiba U, Cruz C (2013) Comparison of methane, nitrous oxide fluxes and CO2 respiration rates from a Mediterranean cork oak ecosystem and improved pasture. Plant Soil 374:883–898

  35. Soil Survey Staff (1999) Soil taxonomy: a basic system of soil classification for making and interpreting soil surveys. USDA-NRCS, US Gov Print Office Washington, DC

  36. Song L, Tian P, Zhang JB, Jin GZ (2017) Effects of three years of simulated nitrogen deposition on soil nitrogen dynamics and greenhouse gas emissions in a Korean pine plantation of northeast China. Sci Total Environ 609:1303–1311. https://doi.org/10.1016/j.scitotenv.2017.08.017

  37. Sun LY, Li L, Chen ZZ, Wang JY, Xiong ZQ (2014) Combined effects of nitrogen deposition and biochar application on emissions of N2O, CO2 and NH3 from agricultural and forest soils. Soil Sci Plant Nutr 60(2):254–265. https://doi.org/10.1080/00380768.2014.885386

  38. Tian P, Zhang JB, Müller C, Cai ZC, Jin GZ (2017) Effects of six years of simulated N deposition on gross soil N transformation rates in an old-growth temperate forest. J Forestry Res doi:https://doi.org/10.1007/s11676-017-0484-6

  39. Wang W, Peng SS, Wang T, Fang JY (2010) Winter soil CO2 efflux and its contribution to annual soil respiration in different ecosystems of a forest-steppe ecotone, north China. Soil Biol Biochem 42(3):451–458. https://doi.org/10.1016/j.soilbio.2009.11.028

  40. Wang CK, Han Y, Chen JQ, Wang XC, Zhang QZ, Bond-Lamberty B (2013) Seasonality of soil CO2 efflux in a temperate forest: biophysical effects of snowpack and spring freeze–thaw cycles. Agric For Meteorol 177:83–92. https://doi.org/10.1016/j.agrformet.2013.04.008

  41. Wang YS, Cheng SL, Fang HJ, Yu GR, Xu MJ, Dang XS, Li LS, Wang L (2014) Simulated nitrogen deposition reduces CH4 uptake and increases N2O emission from a subtropical plantation forest soil in southern China. PLoS One 9(4):e93571. https://doi.org/10.1371/journal.pone.0093571

  42. Wang H, Yu L, Zhang Z, Liu W, Chen L, Cao G, Yue H, Zhou J, Yang Y, Tang Y, He JS (2016) Molecular mechanisms of water table lowering and nitrogen deposition in affecting greenhouse gas emissions from a Tibetan alpine wetland. Glob Chang Biol 23:815–829

  43. Warneke S, Macdonald BCT, Macdonald LM, Sanderman J, Farrell M (2015) Abiotic dissolution and biological uptake of nitrous oxide in Mediterranean woodland and pasture soil. Soil Biol Biochem 82:62–64. https://doi.org/10.1016/j.soilbio.2014.12.014

  44. World Meteorological Organization (WMO) (2006) The state of greenhouse gases in the atmosphere using global observations up to December 2004. WMO Greenhouse Gas Bulletin 1, Geneva, Switzerland

  45. Wu DM, Dong WX, Oenema O, Wang YY, Trebs I, Hu CS (2013) N2O consumption by low-nitrogen soil and its regulation by water and oxygen. Soil Biol Biochem 60:165–172. https://doi.org/10.1016/j.soilbio.2013.01.028

  46. Zhang JB, Song CC, Yang WY (2005) Cold season CH4, CO2 and N2O fluxes from freshwater marshes in northeast China. Chemosphere 59(11):1703–1705. https://doi.org/10.1016/j.chemosphere.2004.11.051

  47. Zhang W, Mo JM, Yu GR, Fang YT, Li DJ, Lu XK, Wang H (2008) Emissions of nitrous oxide from three tropical forests in Southern China in response to simulated nitrogen deposition. Plant Soil 306(1-2):221–236. https://doi.org/10.1007/s11104-008-9575-7

  48. Zhang JB, Zhu TB, Cai ZC, Müller C (2011) Nitrogen cycling in forest soils across climate gradients in Eastern China. Plant Soil 342(1-2):419–432. https://doi.org/10.1007/s11104-010-0706-6

  49. Zhang CP, Niu DC, Hall SJ, Wen HY, Li XD, Fu H, Wan CG, Elser JJ (2014) Effects of simulated nitrogen deposition on soil respiration components and their temperature sensitivities in a semiarid grassland. Soil Biol Biochem 75:113–123. https://doi.org/10.1016/j.soilbio.2014.04.013

  50. Zhou M, Butterbach-Bahl K (2013) Assessment of nitrate leaching loss on a yield-scaled basis from maize and wheat cropping systems. Plant Soil 374:977–991

  51. Zifcakova L, Vetrovsky T, Lombard V, Henrissat B, Howe A, Baldrian P (2017) Feed in summer, rest in winter: microbial carbon utilization in forest topsoil. Microbiome 5(122):122. https://doi.org/10.1186/s40168-017-0340-0

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Acknowledgements

This work was supported by grants from the “973” Project (2014CB953803) and the Fundamental Research Funds for the Central Universities (2572017EA02).

Author information

Correspondence to Guangze Jin.

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Responsible editor: Woo-Jung Choi

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Tian, P., Zhang, J., Cai, Z. et al. Different response of CO2 and N2O fluxes to N deposition with seasons in a temperate forest in northeastern China. J Soils Sediments 18, 1821–1831 (2018). https://doi.org/10.1007/s11368-018-1919-1

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Keywords

  • GHG flux
  • N addition
  • R ST 5W 5 model
  • Growing season
  • Spring FTC period