添加和变暖对土壤矿化和在草原占主导地位的老田中出水的短期和长期影响
Benjamin F A Souriol1, Hugh A L Henry2
1Department of Biology, University of Western Ontario, 1151 Richmond St. N, London, ON, N6A 5B7, Canada.
Oecologia
|April 27, 2024
概括
(N) 添加和变暖影响土壤N动态随着时间的推移而变化. 早期和长期的反应有所不同,突出显示了年度间的变化.
科学领域:
- 生态生态学 生态生态学
- 环境科学 环境科学
- 土壤科学 土壤科学
背景情况:
- 大气中 (N) 沉积和气候变暖是全球变化的主要驱动因素.
- 这些因素预计将在北方温带生态系统中显著改变 (N) 动态.
- 长期实地实验对于了解生态系统对全球变化的反应至关重要.
研究的目的:
- 为了比较 (N) 添加和土壤变暖的短期和长期影响,N动态.
- 调查图片年龄对草原占主导地位的老田地治疗反应的影响.
- 为了将累积处理效应与年际环境变化分开.
主要方法:
- 利用一项已有16年历史的实地实验,添加了新的 (3年历史的) 图片进行比较分析.
- 应用 (N) 添加和加热处理.
- 估计的净N矿化和使用现场土壤内核的N浸.
主要成果:
- 图片年龄和季节性净N矿化上的N增加之间显著的相互作用.
- 在冬季可提取的无机N.的地块年龄和变暖之间的显著相互作用.
- 治疗对N动态的影响在新旧地块之间有所不同,新地块的当前反应与历史观察有所不同.
结论:
- 土地年龄和年间环境变化显著影响观察到的对土壤N循环的处理效应.
- 对添加和变暖的短期反应并不总能预测生态系统的长期动态.
- 仔细考虑时间尺度和环境变化对于解释全球变化实验至关重要.
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