Abstract
Purpose
The impacts of land-use change on dynamics of soil organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP) in the subsoil (> 30 cm) are poorly understood. This study aims to investigate whether the effects of land-use change on stocks and stoichiometric ratios (RCN, RCP, and RNP) of SOC, TN, and TP can be different between topsoil (0–30 cm) and subsoil (30–60 cm) in the Ili River Valley, northwest China.
Materials and methods
Soil samples (0–10, 10–20, 20–30, 30–40, 40–50, and 50–60 cm) were collected from a pasture (PT), a 27-year-old cropland (CL) converted from PT, and a 13-year-old poplar (Populus tomentosa Carr.) plantation (PP) converted from CL. SOC, TN, and TP concentrations and soil bulk density were determined to calculate stocks and stoichiometric ratios (molar ratios) of SOC, TN, and TP.
Results and discussion
Conversion from PT to CL led to substantial losses in SOC, TN, and TP pools in both topsoil and subsoil, and the reduction rates in subsoil (13.8–24.7%) were higher than those in topsoil (8.5–17.3%), indicating that C, N, and P pools in subsoil could also be depleted by cultivation. Similar to topsoil, significant increases in SOC, TN, and TP stocks were detected after afforestation on CL in subsoil, although the increase rates (31.2–56.2%) were lower than those in topsoil (47.8–69.1%). Soil pH and electrical conductivity (EC), which generally increased after conversion from PT to CL while decreased after CL afforestation, showed significant negative correlations with SOC, TN, and TP, suggesting that cultivation might lead to soil degradation, whereas afforestation contributed to soil restoration in this area. Significant changes in C:N:P ratios in topsoil were only detected for RNP after conversion from CL to PP. By contrast, land-use change significantly altered both RCN and RNP in the subsoil, demonstrating that the impacts of land-use change on RCN and RNP were different between topsoil and subsoil. The significant relationship between soil EC and RNP suggested that RNP might be a useful indicator of soil salinization.
Conclusions
Stocks of SOC, TN, and TP as well as RCN and RNP in subsoil showed different responses to land-use change compared to those in topsoil in this typical agro-pastoral region. Therefore, it is suggested that the effects of land-use change on dynamics of SOC, TN, and TP in subsoil should also be evaluated to better understand the role of land-use change in global biogeochemical cycles.
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References
Aitkenhead JA, McDowell WH (2000) Soil C:N ratio as a predictor of annual riverine DOC flux at local and global scales. Glob Biogeochem Cycles 14(1):127–138
Al-Kaisi MM, Grote JB (2007) Cropping systems effects on improving soil carbon stocks of exposed subsoil. Soil Sci Soc Am J 71(4):1381–1388
Angers DA, Chantigny MH, MacDonald JD, Rochette P, Côté D (2010) Differential retention of carbon, nitrogen and phosphorus in grassland soil profiles with long-term manure application. Nutr Cycl Agroecosyst 86(2):225–229
Baddeley JA, Edwards AC, Watson CA (2017) Changes in soil C and N stocks and C:N stoichiometry 21 years after land use change on an arable mineral topsoil. Geoderma 303:19–26
Batjes NH (1996) Total carbon and nitrogen in the soils of the world. Eur J Soil Sci 47:151–163
Bauska TK, Joos F, Mix AC, Roth R, Ahn J, Brook EJ (2015) Links between atmospheric carbon dioxide, the land carbon reservoir and climate over the past millennium. Nat Geosci 8:383–387
Bouwman AF, Beusen AHW, Billen G (2009) Human alteration of the global nitrogen and phosphorus soil balances for the period 1970–2050. Glob Biogeochem Cycles 23:GB0A04
Bui EN, Henderson BL (2013) C:N:P stoichiometry in Australian soils with respect to vegetation and environmental factors. Plant Soil 373(1–2):553–568
Chen ZS, Chen YN, Li WH, Chen YP (2010) Evaluating effect of land use change on environment in Ili Valley based on ecosystem service value analysis. J Desert Res 30:870–877 (in Chinese)
Cherubin MR, Franco ALC, Cerri CEP, Karlen DL, Pavinato PS, Rodrigues M, Davies CA, Cerri CC (2016) Phosphorus pools responses to land-use change for sugarcane expansion in weathered Brazilian soils. Geoderma 265:27–38
Cleveland CC, Liptzin D (2007) C: N: P stoichiometry in soil: is there a “Redfield ratio” for the microbial biomass? Biogeochemistry 85(3):235–252
DuPont ST, Culman SW, Ferris H, Buckley DH, Glover JD (2010) No-tillage conversion of harvested perennial grassland to annual cropland reduces root biomass, decreases active carbon stocks, and impacts soil biota. Agric Ecosyst Environ 137:25–32
Fan J, Zhong H, Harris W, Yu G, Wang S, Hu Z, Yue Y (2008) Carbon storage in the grasslands of China based on field measurements of above-and below-ground biomass. Clim Chang 86:375–396
Fanelli G, Lestini M, Sauli AS (2008) Floristic gradients of herbaceous vegetation and P/N ratio in soil in a Mediterranean area. Plant Ecol 194(2):231–242
Fontaine S, Barot S, Barré P, Bdioui N, Mary B, Rumpel C (2007) Stability of organic carbon in deep soil layers controlled by fresh carbon supply. Nature 450(7167):277–280
Fröberg M, Jardine PM, Hanson PJ, Swanston CW, Todd DE, Tarver JR, Garten CT (2007) Low dissolved organic carbon input from fresh litter to deep mineral soils. Soil Sci Soc Am J 71:347–354
Gahoonia TS, Nielsen NE (1992) The effects of root-induced pH changes on the depletion of inorganic and organic phosphorus in the rhizosphere. Plant Soil 143:185–191
Gao Y, He N, Yu G, Chen W, Wang Q (2014) Long-term effects of different land use types on C, N, and P stoichiometry and storage in subtropical ecosystems: a case study in China. Ecol Eng 67:171–181
Hu C, Li F, Xie YH, Deng ZM, Chen XS (2017) Soil carbon, nitrogen, and phosphorus stoichiometry of three dominant plant communities distributed along a small-scale elevation gradient in the East Dongting Lake. Phys Chem Earth 103:28–34
Jiao F, Wen ZM, An SS, Yuan Z (2013) Successional changes in soil stoichiometry after land abandonment in Loess Plateau, China. Ecol Eng 58:249–254
Kemmitt SJ, Wright D, Goulding KWT, Jones DL (2006) pH regulation of carbon and nitrogen dynamics in two agricultural soils. Soil Biol Biochem 38:898–911
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 (2003) Soil erosion and the global carbon budget. Environ Int 29:437–450
Lal R (2004) Soil carbon sequestration impacts on global climate change and food security. Science 304:1623–1627
Lal R (2011) Sequestering carbon in soils of agro-ecosystems. Food Policy 36:S33–S39
Li D, Niu S, Luo Y (2012) Global patterns of the dynamics of soil carbon and nitrogen stocks following afforestation: a meta-analysis. New Phytol 195:172–181
Li YF, Zhang JJ, Chang SX, Jiang PK, Zhou GM, Fu SL, Yan ER, Wu JS, Lin L (2013) Long-term management effects on soil organic carbon pools and chemical composition in Moso bamboo (Phyllostachys pubescens) forests in subtropical China. For Ecol Manag 303:121–130
Li C, Zhao L, Sun P, Zhao F, Kang D, Yang G, Han X, Feng Y, Ren G (2016) Deep soil C, N, and P stocks and stoichiometry in response to land use patterns in the Loess Hilly Region of China. PLoS One 11:e0159075
Liu Z, Shao M, Wang Y (2011) Effect of environmental factors on regional soil organic carbon stocks across the Loess Plateau region, China. Agric Ecosyst Environ 142:184–194
Liu J, Kuang W, Zhang Z, Xu X, Qin Y, Ning J, Zhou W, Zhang S, Li R, Yan C, Wu S, Shi X, Jiang N, Yu D, Pan X, Chi W (2014) Spatiotemporal characteristics, patterns, and causes of land-use changes in China since the late 1980s. J Geogr Sci 24:195–210
Liu X, Li L, Qi Z, Han J, Zhu Y (2017a) Land-use impacts on profile distribution of labile and recalcitrant carbon in the Ili River Valley, northwest China. Sci Total Environ 586:1038–1045
Liu X, Ma J, Ma ZW, Li LH (2017b) Soil nutrient contents and stoichiometry as affected by land-use in an agro-pastoral region of northwest China. Catena 150:146–153
McLauchlan K (2006) The nature and longevity of agricultural impacts on soil carbon and nutrients: a review. Ecosystems 9:1364–1382
Mobley ML, Lajtha K, Kramer MG, Bacon AR, Heine PR, Richter DD (2015) Surficial gains and subsoil losses of soil carbon and nitrogen during secondary forest development. Glob Change Biol 21(2):986–996
Paul EA (ed) (2007) Soil microbiology, ecology, and biochemistry, 3rd edn. Academic, Amsterdam
Poeplau C, Don A (2013) Sensitivity of soil organic carbon stocks and fractions to different land-use changes across Europe. Geoderma 192:189–201
Rawls WJ, Pachepsky YA, Ritchie JC, Sobecki TM, Bloodworth H (2003) Effect of soil organic carbon on soil water retention. Geoderma 116:61–76
Redfield A (1958) The biological control of chemical factors in the environment. Am Sci 46:205–221
Ross DJ, Tate KR, Scott NA, Feltham CW (1999) Land-use change: effects on soil carbon, nitrogen and phosphorus pools and fluxes in three adjacent ecosystems. Soil Biol Biochem 31(6):803–813
Rousk J, Brookes PC, Bååth E (2009) Contrasting soil pH effects on fungal and bacterial growth suggest functional redundancy in carbon mineralization. Appl Environ Microbiol 75:1589–1596
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
Scurlock JMO, Hall DO (1998) The global carbon sink: a grassland perspective. Glob Chang Biol 4:229–233
Setia R, Marschner P, Baldock J, Chittleborough D, Smith P, Smith J (2011) Salinity effects on carbon mineralization in soils of varying texture. Soil Biol Biochem 43:1908–1916
Sheng H, Zhou P, Zhang Y, Kuzyakov Y, Zhou Q, Ge T, Wang C (2015) Loss of labile organic carbon from subsoil due to land-use changes in subtropical China. Soil Biol Biochem 88:148–157
Shi S, Zhang W, Zhang P, Yu Y, Ding F (2013) A synthesis of change in deep soil organic carbon stores with afforestation of agricultural soils. For Ecol Manag 296:53–63
Smith P (2008) Land use change and soil organic carbon dynamics. Nutr Cycl Agroecosyst 81:169–178
Soil Survey Staff (1994) Keys to soil taxonomy, 6th edn. US Department of Agriculture, Soil Conservation Service, Lincoln
Spohn M, Novák TJ, Incze J, Giani L (2016) Dynamics of soil carbon, nitrogen, and phosphorus in calcareous soils after land-use abandonment—a chronosequence study. Plant Soil 401:185–196
Stockmann U, Adams MA, Crawford JW, Field DJ, Henakaarchchi N, Jenkins M, Minasny B, McBratney AB, de Remy de Courcells 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 164:80–99
Sun G, Li W, Zhu C, Chen Y (2017) Spatial variability of soil carbon to nitrogen ratio and its driving factors in Ili River valley, Xinjiang, northwest China. Chin Geogr Sci 27:529–538
Tian H, Chen G, Zhang C, Melillo JM, Hall CAS (2010) Pattern and variation of C: N: P ratios in China’s soils: a synthesis of observational data. Biogeochemistry 98:139–151
Wang Y, Zhang X, Huang C (2009) Spatial variability of soil total nitrogen and soil total phosphorus under different land uses in a small watershed on the Loess Plateau, China. Geoderma 150(1–2):141–149
Wong VNL, Greene RSB, Dalal RC, Murphy BW (2010) Soil carbon dynamics in saline and sodic soils: a review. Soil Use Manag 26(1):2–11
Xu X, Zhou Y, Ruan H, Luo Y, Wang J (2010) Temperature sensitivity increases with soil organic carbon recalcitrance along an elevational gradient in the Wuyi Mountains, China. Soil Biol Biochem 42(10):1811–1815
Xu X, Thornton PE, Post WM (2013) A global analysis of soil microbial biomass carbon, nitrogen and phosphorus in terrestrial ecosystems. Glob Ecol Biogeogr 22(6):737–749
Zhang Z, Lu X, Song X, Guo Y, Xue Z (2012) Soil C, N and P stoichiometry of Deyeuxia angustifolia and Carex lasiocarpa wetlands in Sanjiang Plain, Northeast China. J Soils Sediments 12(9):1309–1315
Zhang J, Wang X, Wang J (2014) Impact of land use change on profile distributions of soil organic carbon fractions in the Yanqi Basin. Catena 115:79–84
Zhao F, Kang D, Han X, Yang G, Feng Y, Ren G (2015a) Soil stoichiometry and carbon storage in long-term afforestation soil affected by understory vegetation diversity. Ecol Eng 74:415–422
Zhao FZ, Sun J, Ren CJ, Kang D, Deng J, Han XH, Yang GH, Feng YZ, Ren GX (2015b) Land use change influences soil C, N, and P stoichiometry under ‘Grain-to-Green Program’ in China. Sci Rep 5:10195
Funding
This study was supported by the Project under the auspices of West Light Foundation of the Chinese Academy of Sciences (Grant No.: 2016-QNXZ-B-13) and the Project of Science and Technology Plan of Xinjiang (Grant No.: 201531116). The first author appreciates the financial support from the China Scholarship Council for his joint Ph.D. Scholarship (Grant No.: 201504910637).
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Liu, X., Li, L., Wang, Q. et al. Land-use change affects stocks and stoichiometric ratios of soil carbon, nitrogen, and phosphorus in a typical agro-pastoral region of northwest China. J Soils Sediments 18, 3167–3176 (2018). https://doi.org/10.1007/s11368-018-1984-5
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DOI: https://doi.org/10.1007/s11368-018-1984-5