Altered Belowground Carbon Cycling Following Land-Use Change to Perennial Bioenergy Crops

被引:135
作者
Anderson-Teixeira K.J. [1 ,2 ,5 ]
Masters M.D. [1 ,2 ]
Black C.K. [1 ,2 ,3 ]
Zeri M. [1 ,2 ,6 ]
Hussain M.Z. [1 ]
Bernacchi C.J. [1 ,2 ,3 ,4 ]
DeLucia E.H. [1 ,2 ,3 ]
机构
[1] Institute of Genomic Biology, University of Illinois, Urbana, IL
[2] Energy Bioscience Institute, University of Illinois, Urbana, IL
[3] Department of Plant Biology, University of Illinois, Urbana, IL
[4] Photosynthesis Research Unit, US Department of Agriculture, University of Illinois, Urbana, IL
[5] Smithsonian Institution, Center for Tropical Forest Science-Smithsonian Institution Global Earth Observatory, Smithsonian Conservation Biology Institute, Front Royal, VA, 22630
[6] Centro de Ciência do Sistema Terrestre, Instituto Nacional de Pesquisas Espaciais, Cachoeira Paulista, SP
关键词
belowground carbon allocation; bioenergy/biofuels; carbon cycle; establishment phase; perennial grasses; root allocation; soil organic carbon; soil respiration;
D O I
10.1007/s10021-012-9628-x
中图分类号
学科分类号
摘要
Belowground carbon (C) dynamics of terrestrial ecosystems play an important role in the global C cycle and thereby in climate regulation. Globally, land-use change is a major driver of changes in belowground C storage. The emerging bioenergy industry is likely to drive widespread land-use changes, including the replacement of annually tilled croplands with perennial bioenergy crops, and thereby to impact the climate system through alteration of belowground C dynamics. Mechanistic understanding of how land-use changes impact belowground C storage requires elucidation of changes in belowground C flows; however, altered belowground C dynamics following land-use change have yet to be thoroughly quantified through field measurements. Here, we show that belowground C cycling pathways of establishing perennial bioenergy crops (0- to 3. 5-year-old miscanthus, switchgrass, and a native prairie mix) were substantially altered relative to row crop agriculture (corn-soy rotation); specifically, there were substantial increases in belowground C allocation (>400%), belowground biomass (400-750%), root-associated respiration (up to 2,500%), moderate reductions in litter inputs (20-40%), and respiration in root-free soil (up to 50%). This more active root-associated C cycling of perennial vegetation provides a mechanism for observed net C sequestration by these perennial ecosystems, as well as commonly observed increases in soil C under perennial bioenergy crops throughout the world. The more active root-associated belowground C cycle of perennial vegetation implies a climate benefit of grassland maintenance or restoration, even if biomass is harvested annually for bioenergy production. © 2013 Springer Science+Business Media New York.
引用
收藏
页码:508 / 520
页数:12
相关论文
共 58 条
[1]  
Al-Kaisi M.M., Grote J.B., Cropping systems effects on improving soil carbon stocks of exposed subsoil, Soil Sci Soc Am J, 71, (2007)
[2]  
Anderson-Teixeira K.J., DeLucia E.H., The greenhouse gas value of ecosystems, Glob Change Biol, 17, 1, pp. 425-438, (2011)
[3]  
Anderson-Teixeira K.J., Davis S.C., Masters M.D., DeLucia E.H., Changes in soil organic carbon under biofuel crops, GCB Bioenergy, 1, 1, pp. 75-96, (2009)
[4]  
Anderson-Teixeira K.J., Snyder P.K., DeLucia E.H., Do biofuels life cycle analyses accurately quantify the climate impacts of biofuels-related land use change?, Ill Law Rev, 2, pp. 589-622, (2011)
[5]  
Anderson-Teixeira K.J., Snyder P.K., Twine T.E., Cuadra S.V., Costa M.H., DeLucia E.H., Climate-regulation services of natural and agricultural ecoregions of the Americas, Nat Climate Change, 2, 3, pp. 177-181, (2012)
[6]  
Bernacchi C.J., Hollinger S.E., Meyers T.P., The conversion of the corn/soybean ecosystem to no-till agriculture may result in a carbon sink, Glob Change Biol, 11, 11, (2005)
[7]  
Blanco-Canqui H., Energy crops and their implications on soil and environment, Agron J, 102, (2010)
[8]  
Blanco-Canqui H., Lal R., Soil and crop response to harvesting corn residues for biofuel production, Geoderma, 141, 3-4, pp. 355-362, (2007)
[9]  
Chapin F., Woodwell G., Randerson J., Rastetter E., Lovett G., Baldocchi D., Clark D., Harmon M., Schimel D., Valentini R., Et al., Reconciling carbon-cycle concepts, terminology, and methods, Ecosystems, 9, 7, pp. 1041-1050, (2006)
[10]  
Crutzen P.J., Mosier A.R., Smith K.A., Winiwarter W., N<sub>2</sub>O release from agro-biofuel production negates global warming reduction by replacing fossil fuels, Atmos Chem Phys, 8, pp. 389-395, (2008)