在森林土壤中,的沉积导致植物衍生的有机碳的增加高于微生物衍生的有机碳
Xuechao Zhao1, Peng Tian2, Wei Zhang3
1Anhui Province Key Laboratory of Forest Resources and Silviculture, Anhui Agricultural University, Hefei 230036, China; Huitong Experimental Station of Forest Ecology, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Shenyang 110016, China.
The Science of the total environment
|March 17, 2024
概括
增加的沉积增加了植物衍生的土壤有机碳 (SOC) 超过微生物衍生的 SOC 在森林中. 来自植物的SOC在碳封存中起着关键作用,特别是在温带地区.
科学领域:
- 土壤科学 土壤科学
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
背景情况:
- 土壤有机碳 (SOC) 对陆地生态系统至关重要.
- 大气中 (N) 沉积影响植物和微生物衍生的SOC.
- 了解SOC对沉积的反应对于预测碳封存至关重要.
研究的目的:
- 研究植物和微生物衍生的SOC的空间模式.
- 为了确定N添加如何影响森林土壤中的SOC成分.
- 阐明驱动SOC对N沉积反应的机制.
主要方法:
- 量化植物衍生SOC使用素.
- 使用氨基糖的微生物衍生SOC量化.
- 分析了四个不同条件的森林场所的N添加效应.
主要成果:
- 在温带,但不是热带森林中,N添加增加了微生物残留物 (平均20.5%),主要来自真菌.
- 在温带 (63.8%) 森林中,红热带 (15.7%) 森林中,素的增加显著多.
- 在温带森林中,氨基糖与红素的比例随N添加而下降.
- N添加通过pH,SOC,Ca2+,细菌和C:N比率影响了微生物残留物.
- 此外,N通过SOC,C:N比率和细菌间接影响着类.
结论:
- 沉积增强了植物性SOC,而不是微生物性SOC.
- 来自植物的SOC在N沉积下对SOC的封存至关重要,特别是在温带森林中.
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