Ecosystem carbon and nitrogen storage following farmland afforestation with black locust (Robinia pseudoacacia) on the Loess Plateau, China

Guangqi Zhang , Ping Zhang , Yang Cao

Journal of Forestry Research ›› 2017, Vol. 29 ›› Issue (3) : 761 -771.

PDF
Journal of Forestry Research ›› 2017, Vol. 29 ›› Issue (3) : 761 -771. DOI: 10.1007/s11676-017-0479-3
Original Paper

Ecosystem carbon and nitrogen storage following farmland afforestation with black locust (Robinia pseudoacacia) on the Loess Plateau, China

Author information +
History +
PDF

Abstract

Although afforestation of farmlands has been proposed as an effective method of carbon (C) sequestration, there remain uncertainties that deter us from developing a clear picture of C stocks in plantation ecosystems. This study investigated the dynamics of stand structure and plant diversity, and C and nitrogen (N) pools in trees, herbs, litter, and soil (0–100 cm depth) in black locust plantations aged 9, 17, 30, and 37 years, and in newly abandoned farmlands as pre-afforestation sites, on the Loess Plateau, China. Stand density decreased significantly, while tree diameter at breast height and height increased during stand development. The dominant species of the herb layer differed with age. Afforestation resulted in slight increases in tree C and N storage in plantations from 9 to 30 years of age, and then significantly increased from 30 to 37 years. Compared to pre-afforestation, C and N storage in soil decreased to minimum values in stands aged 17 and 9 years, respectively. The soil re-accumulated C and N during stand development, attaining equilibrium levels similar to those in pre-afforestation when stands reached about 30 years of age. Soil C and N storage in 37-year stands were 29 and 16% higher, respectively, than in pre-afforestation levels. However, C and N concentrations in the subsoil (20–40 cm) were still less than the pre-afforestation levels for stands of all ages (from 9 to 37 years). The relative contribution to the total ecosystem C and N pools increased in trees and decreased in soil during the observed period. Our results indicate that afforestation reduced soil C and N storage during the early stages of stand development. We conclude that the growing phase of an afforested stand over its initial 30 years is important for C and N sequestration by black locust due to the C and N storage that result from recovered soil quality and an increase in tree biomass.

Keywords

Afforestation / Biomass / Carbon content / Plantation ecosystem / Nitrogen sequestration

Cite this article

Download citation ▾
Guangqi Zhang, Ping Zhang, Yang Cao. Ecosystem carbon and nitrogen storage following farmland afforestation with black locust (Robinia pseudoacacia) on the Loess Plateau, China. Journal of Forestry Research, 2017, 29(3): 761-771 DOI:10.1007/s11676-017-0479-3

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

Arevalo CBM, Bhatti JS, Chang SX, Sidders D. Ecosystem carbon stocks and distribution under different land-uses in north central Alberta, Canada. For Ecol Manag, 2009, 257: 1776-1785.

[2]

Aryal DR, De Jong BHJ, Ochoa-Gaona S, Esparza-Olguin L, Mendoza-Vega J. Carbon stocks and changes in tropical secondary forests of southern Mexico. Agric Ecosyst Environ, 2014, 195: 220-230.

[3]

Berthrong ST, Jobbagy EG, Jackson RB. A global meta-analysis of soil exchangeable cations, pH, carbon, and nitrogen with afforestation. Ecol Appl, 2009, 19: 2228-2241.

[4]

Bradford JB, Kastendick DN. Age-related patterns of forest complexity and carbon storage in pine and aspen-birch ecosystems of northern Minnesota, USA. Can J For, 2010, 40: 401-409.

[5]

Bremner JM, Mulvaney CS. Page AL, Miller RH, Keeney DR. Nitrogen-total. Methods of soil analysis. Part 2. Chemical and microbiological properties, 1982, Madison: American Society of Agronomy 595 624

[6]

Chang RY, Fu BJ, Liu GH, Liu SG. Soil carbon sequestration potential for “Grain for Green” project in Loess Plateau, China. Environ Manag, 2011, 48: 1158-1172.

[7]

Chen Y, Cao Y. Response of tree regeneration and understory plant species diversity to stand density in mature Pinus tabulaeformis plantations in the hilly area of the Loess Plateau, China. Ecol Eng, 2014, 73: 238-245.

[8]

Chen GS, Yang ZJ, Gao R, Xie JS, Guo JF, Huang ZQ, Yang YS. Carbon storage in a chronosequence of Chinese fir plantations in southern China. For Ecol Manag, 2013, 300: 68-76.

[9]

Cheng XQ, Han HR, Kang FF, Song YL, Liu K. Variation in biomass and carbon storage by stand age in pine (Pinus tabulaeformis) planted ecosystem in Mt. Taiyue, Shanxi, China. J Plant Interact, 2014, 9: 521-528.

[10]

Cote L, Brown S, Pare D, Fyles J, Bauhus J. Dynamics of carbon acid nitrogen mineralization in relation to stand type, stand age and soil texture in the boreal mixedwood. Soil Biol Biochem, 2000, 32: 1079-1090.

[11]

Davidson EA, Janssens IA. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change. Nature, 2006, 440: 165-173.

[12]

Deng L, Shangguan ZP, Sweeney S. Changes in soil carbon and nitrogen following land abandonment of farmland on the Loess Plateau, China. PLoS ONE, 2013, 8: e71923.

[13]

Deng L, Liu GB, Shangguan ZP. Land-use conversion and changing soil carbon stocks in China’s ‘Grain-for-Green’ Program: a synthesis. Glob Change Biol, 2014, 20: 3544-3556.

[14]

Deng L, Shangguan ZP, Sweeney S. “Grain for Green” driven land use change and carbon sequestration on the Loess Plateau, China. Sci Rep, 2014, 4: 7039.

[15]

Deng L, Wang KB, Li JP, Shangguan ZP, Sweeney S. Carbon Storage Dynamics in Alfalfa (Medicago sativa) Fields in the Hilly-Gully Region of the Loess Plateau, China. Clean Soil Air Water, 2014, 42: 1253-1262.

[16]

Dixon RK, Brown S, Houghton RA, Solomon AM, Trexler MC, Wisniewski J. Carbon pools and flux of global forest ecosystems. Science, 1994, 263: 185-190.

[17]

Drake JE, Davis SC, Raetz LM, DeLucia EH. Mechanisms of age-related changes in forest production: the influence of physiological and successional changes. Glob Change Biol, 2011, 17: 1522-1535.

[18]

Fang JY, Chen AP, Peng CH, Zhao SQ, Ci L. Changes in forest biomass carbon storage in China between 1949 and 1998. Science, 2001, 292: 2320-2322.

[19]

FAO–UNESCO. Soil map of the world (1:5,000,000), 1974, Paris: Food and Agricultural Organisation of the United Nations, UNECO.

[20]

Feng X, Fu B, Lu N, Zeng Y, Wu B. How ecological restoration alters ecosystem services: an analysis of carbon sequestration in China’s Loess Plateau. Sci Rep, 2013, 3: 2846.

[21]

Forrester DI, Pares A, O’Hara C, Khanna PK, Bauhus J. Soil organic carbon is increased in mixed-species plantations of eucalyptus and nitrogen-fixing. Acacia Ecosyst, 2013, 16: 123-132.

[22]

Guo LB, Gifford RM. Soil carbon stocks and land use change: a meta analysis. Glob Change Biol, 2002, 8: 345-360.

[23]

Hu Y, Zeng D, Jiang T. Effects of afforested poplar plantations on the stock and distribution of C, N, P at Keerqin Sandy Lands. Acta Ecol Sin, 2009, 29: 4206-4214.

[24]

Jackson RB, Schlesinger WH. Curbing the U.S. carbon deficit. Proc Natl Acad Sci USA, 2004, 101: 15827-15829.

[25]

Jiao JY, Zhang ZG, Bai WJ, Jia YF, Wang N. Assessing the ecological success of restoration by afforestation on the Chinese Loess Plateau. Restor Ecol, 2012, 20: 240-249.

[26]

Jobbágy E, Jackson R. The distribution of soil nutrients with depth: global patterns and the imprint of plants. Biogeochemistry, 2001, 53: 51-77.

[27]

Józefowska A, Pietrzykowski M, Woś B, Cajthaml T, Frouz J. The effects of tree species and substrate on carbon sequestration and chemical and biological properties in reforested post-mining soils. Geoderma, 2017, 292: 9-16.

[28]

Khanna PK. Comparison of growth and nutrition of young monocultures and mixed stands of Eucalyptus globulus and Acacia mearnsii. For Ecol Manag, 1997, 94: 105-113.

[29]

Laganiere J, Angers DA, Pare D. Carbon accumulation in agricultural soils after afforestation: a meta-analysis. Glob Change Biol, 2010, 16: 439-453.

[30]

Lal R. Soil carbon sequestration to mitigate climate change. Geoderma, 2004, 123: 1-22.

[31]

Lee YC, Nam JM, Kim JG. The influence of black locust (Robinia pseudoacacia) flower and leaf fall on soil phosphate. Plant Soil, 2011, 341: 269-277.

[32]

Li T, Liu G. Age-related changes in carbon accumulation and allocation in plants and soil of a black locust forest on the Loess Plateau. Chin Geogr Sci, 2014, 24: 414-422.

[33]

Li X, Yi MJ, Son Y, Park PS, Lee KH, Son YM, Kim RH, Jeong MJ. Biomass and carbon storage in an age-sequence of Korean Pine (Pinus koraiensis) plantation forests in Central Korea. J Plant Biol, 2011, 54: 33-42.

[34]

Li D, Niu S, Luo Y. Global patterns of the dynamics of soil carbon and nitrogen stocks following afforestation: a meta-analysis. New Phytol, 2012, 195: 172-181.

[35]

Li H, Li J, He YL, Li SJ, Liang ZS, Peng CH, Polle A, Luo Zh. Changes in carbon, nutrients and stoichiometric relations under different soil depths, plant tissues and ages in black locust plantations. Acta Physiol Plant, 2013, 35: 2951-2964.

[36]

Li YQ, Brandle J, Awada T, Chen YP, Han JJ, Zhang FX, Luo YQ. Accumulation of carbon and nitrogen in the plant-soil system after afforestation of active sand dunes in China’s Horqin Sandy Land. Agric Ecosyst Environ, 2013, 177: 75-84.

[37]

Liao CZ, Luo YQ, Fang CM, Li B. Ecosystem carbon stock influenced by plantation practice: implications for planting forests as a measure of climate change mitigation. PLoS ONE, 2010, 5: e10867.

[38]

Liu ZP, Shao MA, Wang YQ. Effect of environmental factors on regional soil organic carbon stocks across the Loess Plateau region, China. Agric Ecosyst Environ, 2011, 142: 184-194.

[39]

Liu ZP, Shao MA, Wang YQ (2014) The contribution of China’s Grain to Green Program to carbon sequestration. Landsc Ecol 29:1675–1688

[40]

Lu N, Liski J, Chang RY, Akujarvi A, Wu X, Jin TT, Wang YF, Fu BJ. Soil organic carbon dynamics of black locust plantations in the middle Loess Plateau area of China. Biogeosciences, 2013, 10: 7053-7063.

[41]

Luo Y, Bo S, William SC, Jeffery SD. Progressive nitrogen limitation of ecosystem responses to rising atmospheric carbon dioxide. Bioscience, 2004, 54: 731-739.

[42]

Mao R, Zeng DH, Hu YL, Li LJ, Yang D. Soil organic carbon and nitrogen stocks in an age-sequence of poplar stands planted on marginal agricultural land in Northeast China. Plant Soil, 2010, 332: 277-287.

[43]

Mazurek R, Bejger R. The role of black locust (Robinia pseudoacacia L.) shelterbelts in the stabilization of carbon pools and humic substances in chernozem. Pol J Environ Stud, 2014, 23: 1263-1271.

[44]

Mei L, Zhang Z, Gu J, Quan X, Yang L, Huang D. Carbon and nitrogen storages and allocation in tree layers of Fraxinus mandshurica and Larix gmelinii plantations. Chin J Appl Ecol, 2009, 20: 1791-1796.

[45]

Metz B, Davidson OR, Bosch PR, Dave R, Meyer LA (2007) Contribution of Working Group III to the fourth assessment report of the Intergovernmental Panel on Climate Change

[46]

Oades JM. The retention of organic matter in soils. Biogeochemistry, 1988, 5: 35-70.

[47]

Paul KI, Polglase PJ, Nyakuengama JG, Khanna PK. Change in soil carbon following afforestation. For Ecol Manag, 2002, 168: 241-257.

[48]

Peichl M, Arain MA. Allometry and partitioning of above- and belowground tree biomass in an age-sequence of white pine forests. For Ecol Manag, 2007, 253: 68-80.

[49]

Persson M, Moberg J, Ostwald M, Xu JT. The Chinese Grain for Green Programme: assessing the carbon sequestered via land reform. J Environ Manag, 2013, 126: 142-146.

[50]

Pielou EC. An introduction to mathematical ecology, 1969, New York: Wiley.

[51]

Pietrzykowski M, Daniels WL. Estimation of carbon sequestration by pine (Pinus sylvestris L.) ecosystems developed on reforested post-mining sites in Poland on differing mine soil substrates. Ecol Eng, 2014, 73: 209-218.

[52]

Pietrzykowski M, Krzaklewski W. Soil organic matter, C and N accumulation during natural succession and reclamation in an opencast sand quarry (southern Poland). Arch Agron Soil Sci, 2007, 53: 473-483.

[53]

Post WM, Kwon KC. Soil carbon sequestration and land-use change: processes and potential. Glob Change Biol, 2000, 6: 317-327.

[54]

Pregitzer KS, Euskirchen ES. Carbon cycling and storage in world forests: biome patterns related to forest age. Glob Change Biol, 2004, 10: 2052-2077.

[55]

Qiu LP, Zhang XC, Cheng JM, Yin XQ. Effects of black locust (Robinia pseudoacacia) on soil properties in the loessial gully region of the Loess Platea, Chinau. Plant Soil, 2010, 332: 207-217.

[56]

Rastetter EB, Agren GI, Shaver GR. Responses of N-limited ecosystems to increased CO2: a balanced-nutrition, coupled-element-cycles model. Ecol Appl, 1997, 7: 444-460.

[57]

Ritter E. Carbon, nitrogen and phosphorus in volcanic soils following afforestation with native birch (Betula pubescens) and introduced larch (Larix sibirica) in Iceland. Plant Soil, 2007, 295: 239-251.

[58]

Sang PM, Lamb D, Bonner M, Schimdt S. Carbon sequestration and soil fertility of tropical tree plantations and secondary forest established on degraded land. Plant Soil, 2013, 362: 187-200.

[59]

Sartori F, Lal R, Ebinger MH, Eaton JA. Changes in soil carbon and nutrient pools along a chronosequence of poplar plantations in the Columbia Plateau, Oregon, USA. Agric Ecosyst Environ, 2007, 122: 325-339.

[60]

Shannon CE, Weaver W. The mathematical theory of communication, 1949, Urbana: University of Illinois Press.

[61]

Shen JP, Zhang WH. Characteristics of carbon storage and sequestration of Robinia pseudoacacia forest land converted by farmland in the Hilly Loess Plateau Region. Acta Ecol Sin, 2014, 34: 2746-2754.

[62]

Shi H, Shao MA. Soil and water loss from the Loess Plateau in China. J Arid Environ, 2000, 45: 9-20.

[63]

Simpson EH. Measurement of diversity. Nature, 1949, 163: 688.

[64]

Song X, Peng C, Zhou G, Jiang H, Wang W. Chinese Grain for Green Program led to highly increased soil organic carbon levels: a meta-analysis. Sci Rep, 2014, 4: 4460.

[65]

Walkley A, Black IA. An examination of the Degtjareff method for determining soil organic matter, and a proposed modification of the chromic acid titration method. Soil Sci, 1934, 34: 29-38.

[66]

Wang H, Huang Y, Feng Z, Wang S. C and N stocks under three plantation forest ecosystems of Chinese fir, Michelia macclurei and their mixture. Front For Chin, 2007, 2: 251-259.

[67]

Wang B, Liu GB, Xue S. Effect of black locust (Robinia pseudoacacia) on soil chemical and microbiological properties in the eroded hilly area of China’s Loess Plateau. Environ Earth Sci, 2012, 65: 597-607.

[68]

Yang YH, Luo YQ, Finzi AC. Carbon and nitrogen dynamics during forest stand development: a global synthesis. New Phytol, 2011, 190: 977-989.

[69]

Yang Y, Wang GX, Shen HH, Yang Y, Cui HJ, Liu Q. Dynamics of carbon and nitrogen accumulation and C:N stoichiometry in a deciduous broadleaf forest of deglaciated terrain in the eastern Tibetan Plateau. For Ecol Manag, 2014, 312: 10-18.

[70]

Zhang QJ, Fu BJ, Chen LD, Zhao WW, Yang QK, Liu GB, Gulinck H (2004) Dynamics and driving factors of agricultural landscape in the semiarid hilly area of the Loess Plateau, China. Agric Ecosyst Environ 103:535–543

[71]

Zhang F, Zhang SL, Cheng ZJ, Zhao HY. Time structure and dynamics of the insect communities in bush vegetation restoration areas of Zhifanggou watershed in Loess hilly region. Acta Ecol Sin, 2007, 27: 4555-4562.

[72]

Zhang H, Song TQ, Wang KL, Du H, Yue YM, Wang GX, Zeng FP. Biomass and carbon storage in an age-sequence of Cyclobalanopsis glauca plantations in southwest China. Ecol Eng, 2014, 73: 184-191.

[73]

Zhou GY, Liu SG, Li Z, Zhang DQ, Tang XL, Zhou CY, Yan JH, Mo JM. Old-growth forests can accumulate carbon in soils. Science, 2006, 314: 1417.

AI Summary AI Mindmap
PDF

124

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/