Please wait a minute...
干旱区科学  2012, Vol. 4 Issue (4): 411-419    DOI: 10.3724/SP.J.1227.2012.00411
  学术论文 本期目录 | 过刊浏览 | 高级检索 |
Carbon sequestration in the total and light fraction soil organic matter along a chronosequence in grazing exclosures in a semiarid degraded sandy site in China
YinPing CHEN1, YuQiang LI2, Tala AWADA3, JuanJuan HAN2, YongQing LUO2
1 School of Environmental and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou 730070, China;
2 Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
3 School of Natural Resources, University of Nebraska, Lincoln, NE 68583, USA
Carbon sequestration in the total and light fraction soil organic matter along a chronosequence in grazing exclosures in a semiarid degraded sandy site in China
YinPing CHEN1, YuQiang LI2, Tala AWADA3, JuanJuan HAN2, YongQing LUO2
1 School of Environmental and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou 730070, China;
2 Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
3 School of Natural Resources, University of Nebraska, Lincoln, NE 68583, USA
下载:  PDF (524KB) 
输出:  BibTeX | EndNote (RIS)      
摘要 Horqin Sandy Land is a fragile, seriously desertified region located in Inner Mongolia of China. Over-grazing is one of the primary drivers of desertification in this region. We investigated whether the establishment of grazing exclosures in areas with active sand dunes enhances soil carbon (C) sequestration and benefits soil re-covery. The results showed that soil organic C storage was 1.4, 1.9, and 3.5 times, and light fraction C storage was 2.3, 3.2, and 4.4 times in the 100-cm topsoil after 7, 12, and 25 years of grazing exclusion, respectively, compared to the case in active sand dunes. The light fraction of soil played an important role in soil C sequestration, although it might not change rapidly to provide an early indication of how soil C is increasing in response to grazing exclusion. The results indicated that soils could potentially sequester up to 13.8 Mt C in 25 years if active sand dunes in the study area were to be protected by exclosures. This corresponds to 12.8% of the estimated carbon loss (107.53 Mt) that has been associated with desertification over the past century in the Horqin Sandy Land. Our results suggested that exclosures have the capacity to increase soil C sequestration; however, decades will be required for soil C to recover to historical grassland levels observed prior to desertification.
服务
把本文推荐给朋友
加入引用管理器
E-mail Alert
RSS
作者相关文章
YinPing CHEN
YuQiang LI
Tala AWADA
JuanJuan HAN
YongQing LUO
关键词:  Feflow  time series analysis  groundwater table dynamics  simulation  prediction    
Abstract: Horqin Sandy Land is a fragile, seriously desertified region located in Inner Mongolia of China. Over-grazing is one of the primary drivers of desertification in this region. We investigated whether the establishment of grazing exclosures in areas with active sand dunes enhances soil carbon (C) sequestration and benefits soil re-covery. The results showed that soil organic C storage was 1.4, 1.9, and 3.5 times, and light fraction C storage was 2.3, 3.2, and 4.4 times in the 100-cm topsoil after 7, 12, and 25 years of grazing exclusion, respectively, compared to the case in active sand dunes. The light fraction of soil played an important role in soil C sequestration, although it might not change rapidly to provide an early indication of how soil C is increasing in response to grazing exclusion. The results indicated that soils could potentially sequester up to 13.8 Mt C in 25 years if active sand dunes in the study area were to be protected by exclosures. This corresponds to 12.8% of the estimated carbon loss (107.53 Mt) that has been associated with desertification over the past century in the Horqin Sandy Land. Our results suggested that exclosures have the capacity to increase soil C sequestration; however, decades will be required for soil C to recover to historical grassland levels observed prior to desertification.
Key words:  Feflow    time series analysis    groundwater table dynamics    simulation    prediction
收稿日期:  2012-02-27      修回日期:  2012-05-24           出版日期:  2012-12-15      发布日期:  2012-09-21      期的出版日期:  2012-12-15
基金资助: 

The National Natural Science Foundation of China (40901049; 31060060), the Major State Basic Research Development Program of China (2009CB 421303), and the ‘Qing Lan’ Talent Engineering Funds of Lanzhou Jiaotong University (QL-08-14A).

通讯作者:  YuQiang LI    E-mail:  yqli1975@yahoo.com.cn
引用本文:    
YinPing CHEN, YuQiang LI, Tala AWADA, JuanJuan HAN, YongQing LUO. Carbon sequestration in the total and light fraction soil organic matter along a chronosequence in grazing exclosures in a semiarid degraded sandy site in China[J]. 干旱区科学, 2012, 4(4): 411-419.
YinPing CHEN, YuQiang LI, Tala AWADA, JuanJuan HAN, YongQing LUO. Carbon sequestration in the total and light fraction soil organic matter along a chronosequence in grazing exclosures in a semiarid degraded sandy site in China. Journal of Arid Land, 2012, 4(4): 411-419.
链接本文:  
http://jal.xjegi.com/CN/10.3724/SP.J.1227.2012.00411  或          http://jal.xjegi.com/CN/Y2012/V4/I4/411
Bending G D, Turner M K. 2009. Incorporation of nitrogen from crop residues into light-fraction organic matter in soils with con-trasting management histories. Biology and Fertility of Soils, 45: 281–287.

Conant R T, Paustian K, Del Grosso S J, et al. 2005. Nitrogen pools and fluxes in grassland soils sequestering carbon. Nutrient Cy-cling in Agroecosystems, 71: 239–248.

Cooper A, McCann T, Ballard E. 2005. The effects of livestock grazing and recreation on Irish machair grassland vegetation. Plant Ecology, 181: 255–267.

Dregne H E. 1986. Desertification of arid lands. In: El-Baz F, Has-san M H A. Physics of Desertification. Dordrecht, The Nether-lands: Martinus, Nijhoff.

FAO. 2006. FAO/IUSS Working Group WRB, World Reference Base for Soil Resources 2006. World Soil Resources Reports 103. FAO, Rome.

Gong W, Yan X Y, Wang J Y, et al. 2009. Long-term manure and fertilizer effects on soil organic matter fractions and microbes under a wheat–maize cropping system in northern China. Ge-oderma, 149: 318–324.

Grandy A S, Robertson G P. 2007. Land use intensity effects on soil C accumulation rates and mechanisms. Ecosystems, 10: 59–74.

Gregorich E G, Ellert B H, Drury C F, et al. 1996. Fertilization effects on soil organic matter turnover and corn residue C stor-age. Soil Science Society of America Journal, 60: 472–476.

Hassink J, Whitmore A P, Kubat J. 1997. Size and density frac-tionation of soil organic matter and the physical capacity of soils to protect organic matter. European Journal of Agronomy, 7: 189–199.

Ibáñez J, Martínez J, Schnabel S. 2007. Desertification due to over-grazing in a dynamic commercial livestock–grass–soil system. Ecological Modelling, 205: 277–288.

ISO. 1998. Soil Quality—Determination of Particle Size Distribu-tion in Mineral Soil Material—Method by Sieving and Sedi-mentation. Geneva: International Organization for Standardiza-tion.

Laycock W A. 1991. Stable states and thresholds of range condition on North American rangelands: a viewpoint. Journal of Range Management, 44: 427–433.

McIntosh P D, Allen R B, Scott N. 1997. Effects of exclosure and management on biomass and soil nutrient pools in seasonally dry high country, New Zealand. Journal of Environmental Management, 51: 169–186.

Murage E W, Voroney P, Beyaert R P. 2007. Turnover of carbon in the free light fraction with and without charcoal as determined using the 13C natural abundance method. Geoderma, 138: 133–143.

Nelson D W, Sommers L E. 1982. Total carbon, organic carbon and organic matter. In: Page A L, Miller R H, Keeney D R. Methods of Soil Analysis, Part 2, 2nd ed. Madison: American Society of Agronomy, 539–577.

Pei S F, Fu H, Wan C G. 2008. Changes in soil properties and vegetation following exclosure and grazing in degraded Alxa desert steppe of Inner Mongolia, China. Agriculture, Ecosys-tems & Environment, 124: 33–39.

Reeder J D, Schuman G E. 2002. Influence of livestock grazing on C sequestration in semi-arid mixed-grass and short-grass range-lands. Environmental Pollution, 116: 457–463.

Shrestha G, Stahl P D. 2008. Carbon accumulation and storage in semi-arid sagebrush steppe: effects of long-term grazing exclu-sion. Agriculture, Ecosystems & Environment, 125: 173–181.

Six J, Callewaert P, Lenders S, et al. 2002. Measuring and under-standing carbon storage in afforested soils by physical frac-tionation. Soil Science Society of America Journal, 66: 1981–1987.

Soderstrom B, Part T, Linnarsson E. 2001. Grazing effects on be-tween-year variations of farmland bird communities. Ecological Applications, 11: 1141–1150.

Soon Y K, Arshad M A, Haq A, et al. 2007. The influence of 12 years of tillage and crop rotation on total and labile organic carbon in a sandy loam soil. Soil & Tillage Research, 95: 38–46.

Steffens M, Kölbl A, Totsche K U, et al. 2008. Grazing effects on soil chemical and physical properties in a semiarid steppe of Inner Mongolia (P.R. China). Geoderma, 143: 63–72.

Su Y Z, Li Y L, Cui J Y, et al. 2005. Influences of continuous grazing and livestock exclusion on soil properties in a degraded sandy grassland, Inner Mongolia, northern China. Catena, 59: 267–278.

Tan Z, Lal R, Owens L, et al. 2007. Distribution of light and heavy fractions of soil organic carbon as related to land use and tillage practice. Soil & Tillage Research, 92: 53–59.

Wang X L, Jia Y, Li X G, et al. 2009. Effects of land use on soil total and light fraction organic, and microbial biomass C and N in a semi-arid ecosystem of northwest China. Geoderma, 153: 285–290.

Weinhold B J, Hendrickson J R, Karn J F. 2001. Pasture management influences on soil properties in the Northern Great Plains. Journal of Soil and Water Conservation, 56: 27–31.

Westoby M B, Walker B, Noy-Meir I. 1989. Opportunistic management for rangelands not at equilibrium. Journal of Range Management, 42: 2–13.

Wu W. 2005. Study on Dynamic Evolvement of Modern Sandy Deser-tification Land in Horqin Sandy Land. Beijing: Ocean Press, 189–226.

Zhou R L, Li Y Q, Zhao H L, et al. 2008. Desertification effects on C and N content of sandy soils under grassland in Horqin, northern China. Geoderma, 145: 370–375.

 
 
[1] LIU Feng, GENG Xiaoyuan, ZHU A-xing, Walter FRASER, SONG Xiaodong, ZHANG Ganlin. Soil polygon disaggregation through similarity-based prediction with legacy pedons[J]. 干旱区科学, 2016, 8(5): 760-772.
[2] Ibrahim YAHIAOUI, AbdelKader DOUAOUI, ZHANG Qiang, Ahmed ZIANE. Soil salinity prediction in the Lower Cheliff plain (Algeria) based on remote sensing and topographic feature analysis[J]. 干旱区科学, 2015, 7(6): 794-805.
[3] SongHao SHANG. A general multi-objective programming model for minimum ecological flow or water level of inland water bodies[J]. 干旱区科学, 2015, 7(2): 166-176.
[4] WenZhi ZENG, Chi XU, JingWei WU, JieSheng HUANG. Soil salt leaching under different irrigation regimes: HYDRUS-1D modelling and analysis[J]. 干旱区科学, 2014, 6(1): 44-58.
[5] Lan MA, XiaoMei WEI, AnMing BAO, ShiFei WANG. Simulation of groundwater table dynamics based on Feflow in the Minqin Basin, China[J]. 干旱区科学, 2012, 4(2): 123-131.
[6] ChengYi ZHAO, Yu SHENG, Yilihm·Yimam. Quantifying the impacts of soil water stress on the winter wheat growth in an arid region, Xinjiang[J]. 干旱区科学, 2009, 1(1): 34-42.
No Suggested Reading articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed