More new carbon in the mineral soil of a poplar plantation under Free Air Carbon Enrichment (POPFACE): Cause of increased priming effect?

被引:134
作者
Hoosbeek, MR
Lukac, M
van Dam, D
Godbold, DL
Velthorst, EJ
Biondi, FA
Peressotti, A
Cotrufo, MF
de Angelis, P
Scarascia-Mugnozza, G
机构
[1] Univ Wageningen & Res Ctr, Lab Soil Sci & Geol, NL-6700 AA Wageningen, Netherlands
[2] Univ Wales, Sch Agr & Forest Sci, Bangor LL57 2UW, Gwynedd, Wales
[3] Geol Agr, Geol Tecn & Ambientale, Orvieto, Italy
[4] Univ Udine, Dipartimento Prod Vegetale & Technol Ambientali, I-33100 Udine, Italy
[5] Seconda Univ Studi Napoli, Dipartimento Sci Ambientali, I-80110 Caserta, Italy
[6] Univ Tuscia, Dipartimento Sci Ambiente Forestale & Risorse, I-01100 Viterbo, Italy
关键词
C sequestration; FACE; soil carbon;
D O I
10.1029/2003GB002127
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
[1] In order to establish suitability of forest ecosystems for long-term storage of C, it is necessary to characterize the effects of predicted increased atmospheric CO2 levels on the pools and fluxes of C within these systems. Since most C held in terrestrial ecosystems is in the soil, we assessed the influence of Free Air Carbon Enrichment (FACE) treatment on the total soil C content (C-total) and incorporation of litter derived C (C-new) into soil organic matter (SOM) in a fast growing poplar plantation. C-new was estimated by the C3/C4 stable isotope method. C-total contents increased under control and FACE respectively by 12 and 3%, i.e., 484 and 107 gC/m(2), while 704 and 926 gC/m(2) of new carbon was sequestered under control and FACE during the experiment. We conclude that FACE suppressed the increase of C-total and simultaneously increased C-new. We hypothesize that these opposite effects may be caused by a priming effect of the newly incorporated litter, where priming effect is defined as the stimulation of SOM decomposition caused by the addition of labile substrates.
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页数:7
相关论文
共 44 条
[1]  
[Anonymous], 1993, SOIL SURV MAN, V3rd
[2]  
[Anonymous], 2002, SOIL FORMATION
[3]   SOIL ORGANIC-MATTER TURNOVER IN LONG-TERM FIELD EXPERIMENTS AS REVEALED BY C-13 NATURAL ABUNDANCE [J].
BALESDENT, J ;
WAGNER, GH ;
MARIOTTI, A .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1988, 52 (01) :118-124
[4]   Free-air CO2 enrichment (FACE) enhances biomass production in a short-rotation poplar plantation [J].
Calfapietra, C ;
Gielen, B ;
Galema, ANJ ;
Lukac, M ;
De Angelis, P ;
Moscatelli, MC ;
Ceulemans, R ;
Scarascia-Mugnozza, G .
TREE PHYSIOLOGY, 2003, 23 (12) :805-814
[5]   The effective stagnant thermal conductivity of porous media with periodic structures [J].
Cheng, P ;
Hsu, CT .
JOURNAL OF POROUS MEDIA, 1999, 2 (01) :19-38
[6]   Elevated CO2, rhizosphere processes, and soil organic matter decomposition [J].
Cheng, WX ;
Johnson, DW .
PLANT AND SOIL, 1998, 202 (02) :167-174
[7]   Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model [J].
Cox, PM ;
Betts, RA ;
Jones, CD ;
Spall, SA ;
Totterdell, IJ .
NATURE, 2000, 408 (6809) :184-187
[8]   PRIMING EFFECT OF SOME ORGANIC ADDITIONS TO C-14-LABELED SOIL [J].
DALENBERG, JW ;
JAGER, G .
SOIL BIOLOGY & BIOCHEMISTRY, 1989, 21 (03) :443-448
[9]   Mechanisms of phosphorus acquisition for ponderosa pine seedlings under high CO2 and temperature [J].
Delucia, EH ;
Callaway, RM ;
Thomas, EM ;
Schlesinger, WH .
ANNALS OF BOTANY, 1997, 79 (02) :111-120
[10]   LOW-MOLECULAR-WEIGHT ORGANIC-ACIDS IN SELECTED FOREST SOILS OF THE SOUTHEASTERN USA [J].
FOX, TR ;
COMERFORD, NB .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1990, 54 (04) :1139-1144