亚酸盐的菌根气候变化是贫森林生态系统中重要的源
Joel D Blum1, Andrea Klaue, Carmen A Nezat
1Department of Geological Sciences, University of Michigan, 425 East University Avenue, Ann Arbor, Michigan 48109, USA. jdblum@umich.edu
Nature
|June 18, 2002
概括
由于酸性沉积,美国东北部的森林正在失去. 无地气候提供了重要的源,被树木利用,可能有助于生态系统恢复.
科学领域:
- 森林生态森林生态学
- 地质化学 地质化学
- 环境科学环境科学
背景情况:
- 美国东北部森林的耗与酸性沉积有关,阻碍了生态系统的恢复.
- 现有的来源 (大气沉积,酸盐气候变化) 不能平衡森林河流中观察到的产量.
- 怀疑损失来自可交换和有机结合的土壤池.
研究的目的:
- 在Hubbard Brook实验森林中调查的来源.
- 量化阿帕溶解对森林预算的贡献.
- 确定菌根在从阿帕蒂特中吸收中的作用.
主要方法:
- 对和丰度的分析.
- 测量同位素的比率.
- 检查土壤,植被和水文样本.
主要成果:
- 酸盐溶解被确定为可与大气沉积和酸盐气候变化相比较的源.
- 来自阿帕的主要由生菌类树种利用.
- 菌根的吸收可能会绕过可交换的土壤池.
结论:
- 无气候的气候变化可以显著促进森林生态系统中的.
- 菌根结合体在获取阿帕酸中起着关键作用.
- 在评估土壤酸化和循环影响时,应考虑无气候变化.
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