土壤湿度控制着碳库存在被管理的北极森林景观中的划分
Johannes Larson1, Jörgen Wallerman2, Matthias Peichl3
1Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, 901 83, Umeå, Sweden. Johannes.larson@slu.se.
Scientific reports
|September 9, 2023
概括
玻里亚森林在土壤和树木中储存了大量的碳 (C). 土壤湿度是控制碳储存的关键因素,比区域气候变化更重要.
科学领域:
- 生态生态学 生态生态学
- 森林科学 森林科学 森林科学
- 生物地质化学生物地质化学
背景情况:
- 北极森林是关键的碳汇,储存大量的碳 (C) 池.
- 气候变暖可能会对这些C池产生重大影响.
- 了解控制不同北极生态系统中碳储存的因素至关重要.
研究的目的:
- 在有机层,矿物土壤和树木生物质中量化总C储量.
- 调查控制北极水域C池大小的因素.
- 评估当地土壤湿度与区域因素对C积累的影响.
主要方法:
- 在68平方公里的北极流域内,在430个地块进行了现场测量.
- 有机层,矿物土壤和树木生物质中的量化C储量.
- 利用模拟的土壤湿度数据进行分析.
主要成果:
- 有机层占最大的C池 (39%),其次是树木生物质 (38%) 和矿物土壤 (23%).
- 土壤C池的大小与模拟的土壤湿度正相关,特别是在有机层 (R2 = 0.50).
- 树C池表现出与湿度的单模关系,在中间条件下达到峰值.
结论:
- 当地的土壤湿度条件是北极景观中碳积累的主要驱动因素.
- 极地碳积累似乎比区域气候或沉积更敏感于当地土壤水分的变化.
- 这些发现强调了理解微尺度水文变异对于预测森林C动态的重要性.
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