在北极和温带森林的长期分解过程中,N-分解关系的一般逆转
Tao Sun1, Lili Dong2, Yunyu Zhang1,3
1Chinese Academy of Sciences Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China.
概括
(N) 限制了垃圾分解,但长期研究显示这种关系是逆向的. 富含的垃圾最初的快速分解会随着时间的推移导致更大的反抗分子分数.
科学领域:
- 陆地生态系统 地球生态系统
- 生物地质化学循环的过程
- 土壤科学 土壤科学
背景情况:
- 死的有机物质的分解对于碳 (C) 和营养循环至关重要.
- (N) 的可用性被广泛认为是垃圾分解的主要限制因素.
- 目前的生态系统模型通常基于短期研究嵌入积极的N-分解关系.
研究的目的:
- 研究气对垃圾分解的长期影响.
- 挑战在分解中的作用的主流范式.
- 评估短期控制是否可以预测长期分解动态.
主要方法:
- 对62种木质物种进行了为期10年的分解实验.
- 在两种树种上进行了为期5年的丰富实验.
- 分析了45个森林遗址的120个物种的437个测量数据库.
主要成果:
- 较高的初始度导致了更快的早期分解,但后来产生了更大的反抗分数.
- 富含的垃圾积累了大量缓慢分解的分数.
- 富含基质中的微生物残留量增加,有助于随着时间的推移减缓分解.
- 一项元分析证实,较高的N度与较大的缓慢分解分数相关.
结论:
- 和分解之间的积极关系在后来的分解阶段是逆转的.
- 长期分解动态与短期观测有很大的不同.
- 当前的生态系统和地球系统模型可能不准确地表示长期的N-分解相互作用.
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