Tree roots in a changing world

被引:177
作者
Brunner, Ivano
Godbold, Douglas L.
机构
[1] Swiss Fed Inst Forest Snow & Landscape Res, CH-8903 Birmensdorf, Switzerland
[2] Univ Wales, Sch Agr & Forest Sci, Bangor, Gwynedd, Wales
关键词
fine root turnover; global change; root carbon; root morphology and physiology; soil carbon;
D O I
10.1007/s10310-006-0261-4
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Globally, forests cover 4 billion hectares or 30% of the Earth's land surface, and 20%-40% of the forest biomass is made up of roots. Roots play a key role for trees: they take up water and nutrients from the soil, store carbon (C) compounds, and provide physical stabilization. Estimations from temperate forests of Central Europe reveal that C storage in trees accounts for about 110 t Cha(-1), of which 26 t C ha(-1) is in coarse roots and 1.2 t C ha(-1) is in fine roots. Compared with soil C, which is about 65 t C ha(-1) (without roots), the contribution of the root C to the total below-ground C pool is about 42%. Flux of C into soils by plant litter (stemwood excluded) compared with the total soil C pool, however, is relatively small (4.4 t C ha(-1) year(-1)) with the coarse and fine roots each contributing about 20%. Elevated CO2 concentrations and N depositions lead to increased plant biomass, including that of roots. Recent analysis in experiments with elevated CO2 concentrations have shown increases of the forest net primary productivity by about 23%, and, in the case of poplars, an increase of the standing root biomass by about 62%. The turnover of fine roots is also positively influenced by elevated CO2 concentrations and can be increased in poplars by 25%-45%. A recently established international platform for scientists working on woody root processes, COST action E38, allows the exchange of information, ideas, and personnel, and it has the aim to identify knowledge gaps and initiate future collaborations and research activities.
引用
收藏
页码:78 / 82
页数:5
相关论文
共 45 条
[1]   Detection of tree roots and determination of root diameters by ground penetrating radar under optimal conditions [J].
Barton, CVM ;
Montagu, KD .
TREE PHYSIOLOGY, 2004, 24 (12) :1323-1331
[2]   Soil acidification in southern Switzerland between 1987 and 1997: A case study based on the critical load concept [J].
Blaser, P ;
Zysset, M ;
Zimmermann, S ;
Luster, J .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1999, 33 (14) :2383-2389
[3]   Wood-ash recycling affects forest soil and tree fine-root chemistry and reverses soil acidification [J].
Brunner, I ;
Zimmermann, S ;
Zingg, A ;
Blaser, P .
PLANT AND SOIL, 2004, 267 (1-2) :61-71
[4]   Molecular markers reveal extensive intraspecific below-ground overlap of silver fir fine roots [J].
Brunner, I ;
Ruf, M ;
Lüscher, P ;
Sperisen, C .
MOLECULAR ECOLOGY, 2004, 13 (11) :3595-3600
[5]   Utility of ground-penetrating radar as a root biomass survey tool in forest systems [J].
Butnor, JR ;
Doolittle, JA ;
Johnsen, KH ;
Samuelson, L ;
Stokes, T ;
Kress, L .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2003, 67 (05) :1607-1615
[6]   Linking fine root traits to maximum potential growth rate among 11 mature temperate tree species [J].
Comas, LH ;
Eissenstat, DM .
FUNCTIONAL ECOLOGY, 2004, 18 (03) :388-397
[7]   Linking root traits to potential growth rate in six temperate tree species [J].
Comas, LH ;
Bouma, TJ ;
Eissenstat, DM .
OECOLOGIA, 2002, 132 (01) :34-43
[8]   USE OF CALCIUM ALUMINUM RATIOS AS INDICATORS OF STRESS IN FOREST ECOSYSTEMS [J].
CRONAN, CS ;
GRIGAL, DF .
JOURNAL OF ENVIRONMENTAL QUALITY, 1995, 24 (02) :209-226
[9]   Root architecture and wind-firmness of mature Pinus pinaster [J].
Danjon, F ;
Fourcaud, T ;
Bert, D .
NEW PHYTOLOGIST, 2005, 168 (02) :387-400
[10]   CARBON POOLS AND FLUX OF GLOBAL FOREST ECOSYSTEMS [J].
DIXON, RK ;
BROWN, S ;
HOUGHTON, RA ;
SOLOMON, AM ;
TREXLER, MC ;
WISNIEWSKI, J .
SCIENCE, 1994, 263 (5144) :185-190