Carbon storage in southern boreal forests following fire

被引:12
|
作者
Slaughter, KW [1 ]
Grigal, DF
Ohmann, LF
机构
[1] Univ Minnesota, Dept Forest Resources, St Paul, MN 55108 USA
[2] Univ Minnesota, Dept Soil Water & Climate, St Paul, MN 55108 USA
[3] US Forest Serv, USDA, Grand Rapids, MN 55744 USA
关键词
carbon balance; carbon dioxide; global warming; taiga;
D O I
10.1080/02827589809382968
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Changes in carbon (C) after fire were measured in seven southern boreal upland forest stands during the five immediate post-fire years and 23 years after the fire. Pre-fire above-ground C mass of the stands was estimated. Combustion losses were 19% of the pre-fire above-ground C mass (8.4 kg m(-2)), and an additional 4% of that C mass was lost in the following 3-4 years. After 23 years, neither C mass of understory (0.1 kg m(-2)) nor standing snags (0.3 kg m(-2)) differed from that estimated before the fire; tree C was less (2.4 vs. 6.0 kg C m(-2)), and forest floor (2.5 vs. 1.4 kg C m(-2)) and coarse woody debris (1.7 vs. 0.7 kg C m(-2)) C were higher. Above-ground C mass was 84% of pre-fire mass. There were no measured changes in surface soil C following the fire (2.9 kg C m(-2)). Total C mass, including surface soil, was 10.2 kg m(-2) at 23 years or 91% of the estimated pre-fire C. Although gross fluxes of C followed the fire, massive net losses of C did not occur either immediately or in the two decades after fire. Dynamics of C differed among the stands. Data from either a single stand or a chronosequence in space can lead to different conclusions than those derived from multiple stands through time.
引用
收藏
页码:119 / 127
页数:9
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