Abstract
Few studies have focused on the effects of long-term forest plantations on the soil profile of carbon (C) and nitrogen (N) stocks. In this study, we selected 78-year-old tree plantations that included three coniferous tree species (i.e., slash pine, hoop pine and kauri pine) and a Eucalyptus species in subtropical Australia. We measured soil extractable organic C (EOC) and N (EON) contents and total C and N stocks under different tree species on the forest floor and along a soil profile to 100 cm depth. The results showed that Eucalyptus had significantly higher soil EOC contents (3.3 Mg ha−1) than the other tree species (EOC of 1.9–2.3 Mg ha−1) and had significantly higher EON (156 kg ha−1) contents than slash pine (107 kg ha−1). Eucalyptus had significantly higher soil C (58.9 Mg ha−1) and N (2.03 Mg ha−1) stocks than the other tree species (22.3–27.6 Mg C ha−1 and 0.71–1.23 Mg N ha−1) at 0–100 cm depth. There were no differences in soil C stocks at the 0–100 cm depth among the coniferous tree species. Forest floor C stocks had stronger effects on mineral soil total N stocks than fine root biomass, whereas fine root biomass exerted stronger effects on soil total C stocks at the 0–100 cm depth than forest floor C and N stocks. Our results addressed large differences in soil C and N stocks under different tree species, which can provide useful information for local forest management practices in this region.
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References
Baritz R, Seufert G, Montanarella L, Van Ranst E (2010) Carbon concentrations and stocks in forest soils of Europe. For Ecol Manag 260:262–277
Berthrong ST, Lobbagy EG, Jackson RB (2009) A global meta-analysis of soil exchangeable cations, pH, carbon, and nitrogen with afforestation. Ecol Appl 19:2228–2241
Callesen I, Liski J, Raulund-rasmussen K, Olsson MT, Tau-Strand L, Vesterdal L, Westman CJ (2003) Soil carbon stores in Nordic well-drained forest soils—relationships with climate and texture class. Glob Chang Biol 9:358–370
Chen CR, Xu ZH (2008) Analysis and behavior of soluble organic nitrogen in forest soils. J Soils Sediments 8:363–378
Cotrufo MF, Wallenstein MD, Boot CM, Denef K, Paul E (2013) The microbial efficiency-matrix stabilization (MEMS) framework integrates plant litter decomposition with soil organic matter stabilization: do labile plant inputs form stable soil organic matter? Glob Chang Biol 19:988–995
Curtin D, Wright CE, Beare MH, McCallum FM (2006) Hot water extractable nitrogen as an indicator of soil nitrogen availability. Soil Sci Soc Am J 70:1512–1152
Dawud SD, Raulund-Rasmussen K, Domisch T, Finér L, Jaroszewicz B, Vesterdal L (2016) Is tree species diversity or species identity the more important driver of soil carbon stocks, C/N ratio, and pH? Ecosystems 19:645–660
Don A, Steinberg B, Schoning I, Pritsch K, Joschko M, Gleixner G, Schulze ED (2008) Organic carbon sequestration in earthworm burrows. Soil Biol Biochem 40:1803–1812
Finzi AC, van Breemen N, Canham CD (1998) Canopy tree-soil interactions within temperate forests: species effects on soil carbon and nitrogen. Ecol Appl 8:440–446
Fuchs R, Herold M, Verburg PH, Clevers JGPW (2013) A high-resolution and harmonized model approach for reconstructing and analysing historic land changes in Europe. Biogeosciences 10:1543–1559
Grüneberg E, Ziche D, Wellbrock N (2014) Organic carbon stocks and sequestration rates of forest soils in Germany. Glob Chang Biol 20:2644–2662
Guo LB, Gifford RM (2002) Soil carbon stocks and land use change: a meta analysis. Glob Chang Biol 8:345–360
Hansson K, Kleja DB, Kalbitz K, Larsson H (2010) Amounts of carbon mineralised and leached as DOC during decomposition of Norway spruce needles and fine roots. Soil Biol Biochem 42:178–185
Laganière J, Angers DA, Pare D (2010) Carbon accumulation in agricultural soils after afforestation: a meta-analysis. Glob Chang Biol 16:439–453
Lal R (2005) Forest soils and carbon sequestration. For Ecol Manag 220:242–258
Lu SB, Chen CR, Zhou XQ, Xu ZH, Bacon G, Rui YC, Guo XM (2012) Responses of soil dissolved organic matter to long-term plantations of three coniferous tree species. Geoderma 170:136–143
Müller M, Alewell C, Hagedorn F (2009) Effective retention of litter-derived dissolved organic carbon in organic layers. Soil Biol Biochem 41:1066–1074
Nave LE, Swanston CW, Mishra U, Nadelhoffer KJ (2013) Afforestation effects on soil carbon storage in the United States: a synthesis. Soil Sci Soc Am J 77:1035–1047
Paul KL, Polglase PJ, Nyakuengama JG, Khanna PK (2002) Change in soil carbon following afforestation. For Ecol Manag 168:241–257
R Core Team (2015) R: a language and environment for statistical computing. R Foundation for Statistical Computing, Vienna URL http://www.R-project.org
Rumpel C, Kögel-Knabner I (2011) Deep soil organic matter—a key but poorly understood component of terrestrial C cycle. Plant Soil 338:143–158
Shi SW, Zhang W, Zhang P, Yu YQ, Ding F (2013) A synthesis of change in deep soil organic carbon stores with afforestation of agricultural soils. For Ecol Manag 296:53–63
Shipley B (2000) A new inferential test for path models based on directed acyclic graphs. Struct Equ Model 7:206–218
Vesterdal L, Clarke N, Sigurdsson BD, Gundersen P (2013) Do tree species influence soil carbon stocks in temperate and boreal forests? For Ecol Manag 309:4–18
Vesterdal L, Schmidt IK, Callesen I, Nilsson LO, Gundersen P (2008) Carbon and nitrogen in forest floor and mineral soil under six common European tree species. For Ecol Manag 255:35–48
Wang Q, Wang S (2011) Response of labile soil organic matter to changes in forest vegetation in subtropical regions. Appl Soil Ecol 47:210–216
Xing SH, Chen CR, Zhou BQ, Zhang H, Nang ZM, Xu ZH (2010) Soil soluble organic nitrogen and microbial processes under adjacent coniferous and broadleaf plantation forests. J Soils Sediments 10:1071–1081
Zhou XQ, Wu HW, Li GD, Chen CR (2016) Short-term contributions of cover crop surface residue return to soil carbon and nitrogen contents in temperate Australia. Environ Sci Pollut Res 23:23175–23183
Zhou XQ, Guo ZY, Chen CR, Jia ZJ (2017) Soil microbial community structure and diversity are largely influenced by soil pH and nutrient quality in 78-year-old tree plantations. Biogeosciences 14:2101–2111
Zhou XQ, Chen CR, Wang YF, Xu ZH, Duan JC, Hao YB, Smaill S (2013) Soil extractable carbon and nitrogen, microbial biomass and microbial metabolic activity in response to warming and increased precipitation in a semiarid Inner Mongolian grassland. Geoderma 206:24–31
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This study was supported by a Griffith University Research Fellowship, a New Research Grant by Griffith University, the Australian Research Council, East China Normal University (No. 40500-20101-222011) and the National Natural Science Foundation of China (No. 31600406).
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Zhou, X., Dong, H., Lan, Z. et al. Vertical distribution of soil extractable organic C and N contents and total C and N stocks in 78-year-old tree plantations in subtropical Australia. Environ Sci Pollut Res 24, 22312–22320 (2017). https://doi.org/10.1007/s11356-017-9900-x
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DOI: https://doi.org/10.1007/s11356-017-9900-x