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首页> 外文期刊>Forest Ecology and Management >The effects of wildfire, salvage logging, and post-fire N-fixation on the nutrient budgets of a Sierran forest.
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The effects of wildfire, salvage logging, and post-fire N-fixation on the nutrient budgets of a Sierran forest.

机译:野火,打捞伐木和大火后固氮对Sierran森林养分收支的影响。

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The effects of fire, post-fire salvage logging and revegetation on nutrient budgets were estimated for a site in the eastern Sierra Nevada Mountains, California, USA, that burned in a wildfire in 1981. Approximately two decades after the fire, the shrub (former fire) ecosystem contained less C and more N than the adjacent forest ecosystem. Reconstruction of pre-fire nutrient budgets suggested that most C was exported in biomass during salvage logging and will not be recovered until forest vegetation occupies the site again. Salvage logging may have resulted in longer-term C sequestration in wood products than would have occurred had the logs been left in the field to decay, however. Reconstructed budgets suggested that most N was lost via volatilization during the fire rather than in post-fire salvage logging (assuming that foliage and O horizons were combusted). Comparisons of the pre-fire and present day N budgets also suggested that the lost N was rapidly replenished in O horizons and mineral soils, probably due to N-fixation by snowbush (Ceanothus velutinus), the dominant shrub on the former fire site. There were no significant differences in ecosystem P, K, or S contents and no consistent, significant differences in soil extractable P or S between the shrub and forested plots. Exchangeable K+, Ca2+ and Mg2+ were consistently and significantly higher in shrub than in adjacent forested soils, however, and the differences were much larger than could be accounted for by estimated ash inputs. In the case of Ca, even the combustion of all aboveground organic matter could not account for more than a fraction of the difference in exchangeable pools. We speculate that the apparent large increased in soil and ecosystem Ca content resulted from either the release of Ca from non-exchangeable forms in the soil or the rapid uptake and recycling of Ca by post-fire vegetation..
机译:据估计,美国加利福尼亚州内华达山脉东部的一块火在1981年一场野火中燃烧,火灾,火灾后的打捞记录和植被恢复对养分收支的影响。火灾后大约二十年,灌木丛(以前火灾)生态系统所含碳和氮比邻近森林生态系统少。火灾前营养物预算的重建表明,大部分碳在救助伐木期间以生物量的形式出口,直到森林植被再次占据该地点后才被回收。但是,与将原木留在田地里腐烂相比,打捞伐木可能导致木制品中的长期C螯合。重建的预算表明,大部分N都是在火灾期间通过挥发损失的,而不是在火灾后的打捞伐木中损失的(假设树叶和O层被燃烧了)。对大火前和当前氮素预算的比较还表明,损失的氮素在O层和矿质土壤中得到了迅速补充,这很可能是由于雪丛(Ceanothus velutinus)对氮的固定作用,雪丛是前火场上的主要灌木丛。在灌木林地和森林地之间,生态系统中磷,钾或硫的含量没有显着差异,土壤可提取磷或硫也没有一致的显着差异。灌木中可交换的K +,Ca2 +和Mg2 +始终如一且显着高于邻近的林地,但差异远大于估计的灰分输入所能解释的。就钙而言,即使所有地上有机物的燃烧也不能解释可交换池差异的一小部分。我们推测土壤和生态系统中Ca含量的明显增加是由于土壤中不可交换形式的Ca释放或火后植被对Ca的快速吸收和再循环造成的。

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