实证证据和对生态系统碳和循环相互作用的理论理解
Benjamin D Stocker1,2, Ning Dong3, Evan A Perkowski4
1Institute of Geography, University of Bern, Hallerstrasse 12, CH-3012, Bern, Switzerland.
The New phytologist
|October 24, 2024
概括
陆地生态系统碳和循环是复杂的. 结合植被对二氧化碳和肥的反应的新模型改善了土地碳平衡的预测.
科学领域:
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
- 生态系统建模 生态系统建模
背景情况:
- 陆地生态系统模型模拟碳 (C) 和 (N) 循环,但不同的方法导致过去陆地C平衡的不同预测.
- 最近的理论进展和经验数据需要对生态系统过程和植被建模进行重新评估.
研究的目的:
- 审查当前关于植被对CO2和N输入的反应的知识.
- 评估肥和高CO2对植物生理学和生物质分配的影响.
- 提出一种建模方法,以减少全球C周期预测中的不确定性.
主要方法:
- 对实验证据和特征数据汇编的文献综述.
- 对生态系统建模的理论和生态原理的分析.
- 基于功能平衡假设的演示模型的开发和应用.
主要成果:
- 化肥增加了叶子中的含量,但不一致地提高了光合作用能力.
- 增加的CO2和肥增加了叶面积和生物量,对根部分配产生不同的影响.
- 全球叶子特征数据表明,土壤N的可用性是叶子N含量的较强驱动因素,而不是光合作用能力.
结论:
- 植物对和二氧化碳受精的反应是复杂的,影响组织分配,生长和生物质.
- 基于功能平衡假设的模型准确地预测了这些反应.
- 这种方法为减少全球C周期预测中的不确定性提供了一条途径.
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