Soil respiration response to prescribed burning and thinning in mixed-conifer and hardwood forests

被引:49
作者
Concilio, A
Ma, SY
Li, QL
LeMoine, J
Chen, JQ
North, M
Moorhead, D
Jensen, R
机构
[1] Univ Toledo, Dept Earth Ecol & Environm Sci, Toledo, OH 43606 USA
[2] Univ Calif Berkeley, Dept Environm Sci Policy & Management, Berkeley, CA 94720 USA
[3] Univ Michigan, Dept Ecol & Evolut Biol, Ann Arbor, MI 48109 USA
[4] USDA, Forest Serv Pacific SW Res Stn, Sierra Nevada Res Ctr, Davis, CA 95616 USA
[5] Missouri Dept Conservat, Ellington, MO 63638 USA
关键词
D O I
10.1139/X05-091
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The effects of management on soil carbon efflux in different ecosystems are still largely unknown yet crucial to both our understanding and management of global carbon flux. To compare the effects of common forest management practices on soil carbon cycling, we measured soil respiration rate (SRR) in a mixed-conifer and hardwood forest that had undergone various treatments from June to August 2003. The mixed-conifer forest, located in the Sierra Nevada Mountains of California, had been treated with thinning and burning manipulations in 2001, and the hardwood forest, located in the southeastern Missouri Ozarks, had been treated with harvesting manipulations in 1996 and 1997. Litter depth, soil temperature, and soil moisture were also measured. We found that selective thinning produced a similar effect on both forests by elevating SRR, soil moisture, and soil temperature, although the magnitude of response was greater in the mixed-conifer forest. Selective harvest increased SRR by 43% (from 3.38 to 4.82 mu mol center dot m(-2 center dot)s(-1)) in the mixed-conifer forest and by 14% (from 4.25 to 4.84 mu mol center dot m(-2 center dot)s(-1)) in the hardwood forest. Burning at the conifer site and even-aged harvesting at the mixed-hardwood site did not produce significantly different SRR from controls. Mean SRR were 3.24, 3.42, and 4.52 mu mol center dot m(-2 center dot)s(-1), respectively. At both sites, manipulations did significantly alter SRR by changing litter depth, soil structure, and forest microclimate. SRR response varied by vegetation patch type, the scale at which treatments altered these biotic factors. Our findings provide forest managers first-hand information on the response of soil carbon efflux to various management strategies in different forests.
引用
收藏
页码:1581 / 1591
页数:11
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