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Soil nitrous oxide dynamics associated with forest harvesting in a transitional temperate-boreal forest ecosystem.

机译:过渡性温带-北方森林生态系统中与森林采伐相关的土壤一氧化二氮动力学。

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摘要

The role of forest harvesting on nitrous oxide (N2O) production in and emission from soils is still poorly understood in northern environments. In this study N2O surface fluxes, coupled with subsurface soil air N2O concentrations, were measured at 2 forest and post-harvest pairs of contrasting soil texture in Nova Scotia, Canada between March and November, 2005. No significant difference in the magnitude of N2O surface fluxes between treatments was observed in this study. All sites acted as both sources and sinks of N2O over the sampling period. Surface fluxes observed at the forested sites ranged from -811ugN 2O-N/m2/day to 1367ugN2O-N/m 2/day with a median of 9ugN2O-N/m 2/day, while fluxes observed at the 4 year post-harvest sites ranged from -629ugN2O-N/m2/day to 583 ugN2O-N/m2/day, with a median of 9 ugN2O-N/m2/day. Fluxes from all sites were highly variable and showed no significant temporal patterns. On the other hand, subsurface soil air N2O concentrations were significantly higher at harvested than forested sites, with high variability observed at both sites. Subsurface soil air N2O concentrations at the forested sites ranged from 85ppb to 50667ppb, with a median concentration of 361ppb, and the harvested sites ranged from 80 to 27323ppb, with a median concentration of 413ppb. The magnitude of N2O surface fluxes and subsurface soil air N2O concentrations were examined to determine whether a positive relationship existed between the two variables. Relationships were observed more often during the drier, warmer months at these sites, however this relationship was not always predictable. This points to the presence of a sink of N 2O during transport through the soil profile in these soils. Both N 2O surface fluxes and subsurface soil air N2O concentrations were spatially and temporally transient, with some minor evidence of persisting microsites of both elevated N2O surface fluxes and subsurface soil air N2O concentrations over the sampling period.
机译:在北方环境中,森林砍伐对土壤中一氧化二氮(N2O)产生和排放的作用仍然知之甚少。在这项研究中,在2005年3月至11月之间,在加拿大新斯科舍省的2个森林和收获后的对比土壤质地对中,测量了N2O表面通量以及地下土壤空气N2O浓度。N2O表面大小没有显着差异在这项研究中观察到治疗之间的通量。在采样期间,所有站点都是N2O的源和汇。在森林地带观察到的表面通量范围为-811ugN 2O-N / m2 /天至1367ugN2O-N / m 2 /天,中位数为9ugN2O-N / m 2 /天,而收获后4年观察到的通量站点范围从-629ugN2O-N / m2 /天到583ugN2O-N / m2 /天,中位数为9ugN2O-N / m2 /天。所有部位的通量变化很大,没有明显的时间分布。另一方面,收获时地下土壤空气中的N2O浓度显着高于森林地点,在这两个地点均观察到高变异性。森林站点地下土壤空气中的N2O浓度范围为85ppb至50667ppb,中位数浓度为361ppb,收获站点范围为80至27323ppb,中值浓度为413ppb。检查N2O表面通量的大小和地下土壤空气中N2O的浓度,以确定两个变量之间是否存在正相关关系。在较干燥,较暖和的月份中,这些地点经常观察到这种关系,但是这种关系并非总是可预测的。这表明在通过这些土壤中的土壤剖面传输过程中存在N 2O汇。 N 2O表面通量和地下土壤空气N2O浓度在空间和时间上都是瞬态的,一些较小的证据表明,在采样期间,N2O表面通量和地下土壤空气N2O浓度都持续存在着微场所。

著录项

  • 作者

    Kavanaugh, Krista.;

  • 作者单位

    St. Francis Xavier University (Canada).;

  • 授予单位 St. Francis Xavier University (Canada).;
  • 学科 Agriculture Forestry and Wildlife.; Geochemistry.
  • 学位 M.Sc.
  • 年度 2007
  • 页码 145 p.
  • 总页数 145
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 森林生物学;地质学;
  • 关键词

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