Soil surface CO2 efflux measurements in Norway spruce forests: Comparison between four different sites across Europe - from boreal to alpine forest

被引:57
作者
Acosta, Manuel [1 ]
Pavelka, Marian [1 ]
Montagnani, Leonardo [2 ]
Kutsch, Werner [3 ]
Lindroth, Anders [4 ]
Juszczak, Radoslaw [5 ]
Janous, Dalibor [1 ]
机构
[1] Global Change Res Ctr CzechGlobe, ASCR, Brno, Czech Republic
[2] Autonomous Prov Bolzano, Forest Serv, Bolzano, Italy
[3] Johann Heinrich von Thunen Inst, Braunschweig, Germany
[4] Lund Univ, GeoBiosphere Sci Ctr, Lund, Sweden
[5] Poznan Univ Life Sci, Dept Meteorol, Poznan, Poland
关键词
Soil CO2 efflux; Forest; Chamber method; Q(10); Soil temperature; Spatial variability; ECOSYSTEM RESPIRATION; SPATIAL VARIABILITY; TEMPORAL VARIATION; CHAMBER TECHNIQUE; BEECH FOREST; FINE-ROOT; TEMPERATURE; EXCHANGE; NITROGEN; FLUXES;
D O I
10.1016/j.geoderma.2012.08.027
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Extensive measurements of soil surface (including vegetation cover) CO2 efflux were carried out on 80 positions at four different forest sites (Sweden, Germany, Czech Republic and Italy) using a closed dynamic chamber technique. The period of measurement was 4-5 consecutive days per site. Two approaches were used to analyze the measured data, the Q(10) parameter and the Arrhenius relationship. Basic environmental factors such as soil temperature and moisture were measured. All the four investigated sites showed a positive dependence of the soil surface CO2 efflux on soil temperature. The four datasets generally resulted in good agreement (up to 93%) between the approaches and residual analysis showed no significant difference between approaches (less than 8%). The Q(10) ranged between 2.0 and 23 among the sites. The highest spatial variation of the soil surface CO2 efflux at 10 degrees C (expressed by the coefficient of variation CV) ranged from 30 to 65% between sites. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:295 / 303
页数:9
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