土壤有机碳储量及其物理分量的变化,沿着亚热带山林中的一个高度
Guopeng Wu1, Gang Huang1, Sinuo Lin1
1School of Geographical Sciences, School of Carbon Neutrality Future Technology, Fujian Normal University, 1 Science and Technology Road, Qishan District, Fuzhou, Fujian, 350117, China.
Journal of environmental management
|December 18, 2023
概括
土壤有机碳 (SOC) 库存随着海拔的提高而增加,由有机碳颗粒 (POC) 而不是矿物相关有机碳 (MAOC) 驱动. 微生物生长率随着海拔的提高而增加,这与POC动态有关.
科学领域:
- 土壤科学 土壤科学
- 生态生态学 生态生态学
- 微生物学 微生物学
背景情况:
- 土壤微生物驱动土壤有机碳 (SOC) 矿化和动态.
- 了解微生物碳代谢与SOC库存之间的联系,特别是不同的分数,如颗粒有机碳 (POC) 和矿物相关有机碳 (MAOC),至关重要,但研究不足.
研究的目的:
- 为了研究SOC库存,POC库存,MAOC库存以及微生物碳代谢在亚热带山林中沿着海拔梯度的变化.
- 确定微生物生长,碳使用效率,生物质循环时间和不同土壤碳池之间的关系.
主要方法:
- 量化SOC,POC和MAOC库存在0-20厘米深处沿着一个海拔梯度.
- 评估微生物碳代谢指标,包括微生物生长,碳使用效率和生物质周转时间.
- 采用结构方程建模来分析土壤碳分数和微生物活动之间的关系.
主要成果:
- SOC和POC库存随着海拔的上升而增加,而MAOC库存保持稳定.
- 土壤微生物的生长增加,生物质的循环时间随着海拔的增加而减少.
- 增加的微生物生长与高的POC库存有关;MAOC库存与微生物生长有正相关,但与POC库存和土壤pH负相关.
结论:
- 沿着海拔梯度的SOC总库存增加主要归因于POC库存的变化.
- 土壤碳分量的升高变化受到微生物生长和活动的显著影响.
- 考虑不同的土壤碳分数和微生物过程对于预测SOC对环境变化的反应至关重要,例如与气候变化相关的变化.
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