首页> 外文学位 >Assessing the long-term impact of acid deposition and the risk of soil acidification in boreal forests in the Athabasca oil sands region in Alberta, Canada.
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Assessing the long-term impact of acid deposition and the risk of soil acidification in boreal forests in the Athabasca oil sands region in Alberta, Canada.

机译:评估加拿大艾伯塔省阿萨巴斯卡油砂地区的北方森林中酸沉降的长期影响和土壤酸化的风险。

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摘要

Significant amounts of SO2 and NOx have been emitted from the Athabasca oil sands region (AOSR) in Alberta, Canada, in the past several decades. The impact of acid deposition on forest ecosystems and the risk of soil acidification were assessed in jack pine (Pinus banksiana) and trembling aspen (aspen) (Populus tremuloides ) stands in acid-sensitive watersheds (NE7 and SM8) in the AOSR. NE7 has been exposed to greater rates of deposition. A simulated N and S deposition experiment was also conducted. Nitrogen deposition increased N availability in NE7, indicated by increasing Diff_N (Diff_x: the difference of parameter x in tree rings between NE7 and SM8) and decreasing Diff_δ15 N over time in aspen stands. Sulfur deposition increased in stemflow due to interception deposition, which decreased pH and base cations in soil towards jack pine but not towards aspen releasing enough base cations through canopy leaching. The Ca/Al ratio did not reach the critical limits of 1.0 for soil solution (range: 1.0 to 4.1) or 0.5 for fine roots (range: 0.7 to 7.9) while Al concentrations in soil solutions (range: 0.1 to 8.5 mg L -1) achieved the level inhibiting seedling growth of aspen and Picea glauca (a common species succeeding aspen). Critical loads of S deposition ranged from 223 to 711 molc ha-1 yr-1, and S deposition did not exceed critical loads; N deposition was not considered due to N limitation in boreal forests. Exceedances were underestimated when only bulk deposition was considered as compared to those that use total deposition because intercepted SO42- deposition made up approximately 60% of total deposition. The H+ budgets of soils were negative in NE7 and SM8, implying that soils were recovering from previous acidification, reflecting the reducing trends of S emission. Simulated N deposition provided beneficial effects on tree growth but not for understory. Simulated S deposition increased leaching loss of base cations and reduced exchangeable base cations in the surface soil. I concluded that acid deposition has changed soil and tree chemistry, and tree growth in the AOSR, which could give adverse effects on understory plants sensitive to Al toxicity and cationic nutrient deficiency.
机译:在过去的几十年中,加拿大艾伯塔省的阿萨巴斯卡油砂地区(AOSR)排放了大量的SO2和NOx。在AOSR的酸敏感流域(NE7和SM8)中,评估了杰克松(Pinus bankiana)和颤抖的白杨(aspen)(杨木)的酸沉降对森林生态系统的影响和土壤酸化的风险。 NE7暴露于更高的沉积速率。还进行了模拟的N和S沉积实验。氮沉降增加了NE7中的氮素利用率,这通过增加Diff_N(Diff_x:NE7和SM8之间树环中参数x的差)和在白杨林中随时间降低Diff_δ15N来表明。由于截留沉积物,茎流中的硫沉积物增加,这使土壤中的pH值和碱性阳离子向顶松降低,但没有降低白杨通过冠层浸出释放足够的碱性阳离子。 Ca / Al比未达到土壤溶液的1.0(范围:1.0至4.1)或细根0.5(范围:0.7至7.9)的临界极限,而土壤溶液中的Al浓度(范围:0.1至8.5 mg L- 1)达到了抑制白杨和青云杉(接替白杨的常见物种)的幼苗生长的水平。 S沉积的临界负荷范围为223至711 molc ha-1 yr-1,S沉积未超过临界负荷。由于北方森林中的氮限制,未考虑氮的沉积。与仅使用整体沉积的情况相比,仅考虑整体沉积的情况会低估过剩的数量,因为拦截的SO42-沉积约占全部沉积的60%。 NE7和SM8中土壤的H +预算为负,表明土壤已从先前的酸化中恢复,这反映了S排放量的减少趋势。模拟的氮沉降对树木生长提供了有益的影响,但对林下植被没有帮助。模拟的S沉积增加了表层土壤中碱性阳离子的淋失,并减少了可交换的碱性阳离子。我得出的结论是,酸沉积改变了土壤和树木的化学性质以及AOSR中树木的生长,这可能会对对铝毒性和阳离子养分缺乏敏感的林下植物产生不利影响。

著录项

  • 作者

    Jung, Kangho.;

  • 作者单位

    University of Alberta (Canada).;

  • 授予单位 University of Alberta (Canada).;
  • 学科 Agriculture Forestry and Wildlife.;Environmental Sciences.;Natural Resource Management.;Agriculture Soil Science.
  • 学位 Ph.D.
  • 年度 2012
  • 页码 219 p.
  • 总页数 219
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 老年病学;
  • 关键词

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