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Effects of wildfire on structure and function of boreal forest ecosystems.

机译:野火对北方森林生态系统结构和功能的影响。

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The effect of wildfire on the structure and function of boreal forests is a key issue for understanding the boreal forest role in the climate system and global carbon (C) cycle. The objectives of this dissertation were to (1) quantify the effects of wildfire on C distribution and net primary production (NPP) for the Dahurian larch (Larix gmelinii Rupr.) forest ecosystems in northeastern China; (2) quantify sources and magnitude of error for biomass estimates from allometry models for boreal forests in central Canada; (3) measure and model CO2 fluxes from coarse woody debris (RCWD) and soil surface (RS) in a black spruce ( Picea mariana (Mill.) BSP) fire chronosequence in northern Manitoba, Canada; and (4) examine changes in structure and C distribution in the fire chronsequence. I used field measurements, laboratory experiments, and statistical modeling to address these objectives during the period of 1998–2002.; Wildfire strongly affected C cycling in boreal forest ecosystems by direct C release from biomass combustion and indirect effects on thermal and hydrological regimes, ecosystem structure and function during post-fire succession. The direct C emission from the 1987 wildfire in northeastern China was estimated to comprise 0.6–1.3% of that year's global C emission from biomass burning. Wildfire removed vegetation, produced a large amount of coarse woody debris (CWD), increased soil temperature and resource availability, and hence increased microbial activity (RCWD and RS), accelerated vegetation reestablishment and C accumulation. The RCWD varied from 6.3 to 22.7 kg Ct−1 CWD year−1 depending upon temperature, water content, and decay status of the black spruce CWD; RS ranged from 146 to 413 g C m−2 year−1 across the black spruce fire chronosequences on contrasting soil drainages; the mean annual aboveground C accumulation rates varied from 10 to 75 g C m−2 year−1 . Species diversity was greatest in the younger stands, but by 71 years after wildfire black spruce comprised more than 83% of the overstory C content.; I also demonstrated that forest types, fire regime, biotic and abiotic interactions, stand age, and soil drainage must be considered when developing C budgets for boreal forest ecosystems.
机译:野火对北方森林结构和功能的影响是了解北方森林在气候系统和全球碳(C)循环中的作用的关键问题。本文的目的是(1)量化野火对东北地区达胡尔落叶松( Larix gmelinii Rupr。)森林生态系统碳分布和净初级生产(NPP)的影响; (2)量化加拿大中部北方森林的异速生长模型的生物量估计值的误差来源和误差大小; (3)测量和模拟黑云杉中粗木屑(R CWD )和土壤表面(R S )的CO 2 通量加拿大马尼托巴北部的 Picea mariana (密歇根州BSP)点火时序。 (4)检查火灾时序中的结构和碳分布的变化。在1998年至2002年期间,我使用现场测量,实验室实验和统计模型来解决这些目标。野火强烈影响了北方森林生态系统中的碳循环,其原因是生物量燃烧过程中直接释放了碳,并间接影响了火后演替过程中的热力和水文状况,生态系统结构和功能。估计1987年中国东北山火造成的直接C排放量占当年生物质燃烧全球C排放量的0.6–1.3%。野火清除了植被,产生了大量的粗木屑(CWD),增加了土壤温度和资源利用率,并因此增加了微生物活性(R CWD 和R S ),加快了植被重建和碳积累。 R CWD 的变化范围为6.3至22.7 kg Ct −1 CWD年 −1 ,具体取决于温度,含水量和黑色的衰减状态云杉CWD;在黑云杉火成因时序上,在不同的土壤排水条件下,R S 的范围为146至413 g C m −2 year −1 。地上碳的年平均积累速率在10至75 g C m −2 −1 之间。在较年轻的林分中,物种多样性最大,但是到野火黑云杉在71年后,其碳含量就超过了83%。我还证明,在为北方森林生态系统制定C预算时,必须考虑森林类型,火灾,生物和非生物相互作用,林分年龄和土壤排水。

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