实验性沉积对沙漠草原土壤化学的累积影响:一项为期12年的实地研究
Jieqiong Su1, Ying Ma2, Zhihao Xu3
1Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands and Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China.
The Science of the total environment
|August 9, 2024
概括
在沙漠草原中长期沉积增加了土壤有机碳,但加剧了限制. 这项研究揭示了的含量.
科学领域:
- 土壤科学 土壤科学
- 生态生态学 生态生态学
- 环境科学 环境科学
背景情况:
- 人类增强的大气 (N) 沉积对生态系统产生影响.
- 由于水文和土壤异质性,干旱土地土壤对沉积的反应尚不清楚.
- 沙漠草原是对环境变化的敏感生态系统.
研究的目的:
- 调查模拟沉积对沙漠草原土壤性质的长期影响.
- 了解输入对土壤碳,,和pH的影响.
- 探索土壤特性与营养循环之间的关系.
主要方法:
- 在中国的沙漠草原中,模拟了12年的沉积 (0,3.5,7,14 g N m-2 yr-1).
- 对土壤总N,可用的N (NH4+,NO3−),pH,CaCO3,总 (P) 和土壤有机碳 (SOC) 的分析.
- 皮尔森的相关性分析,以确定土壤特性和植物营养含量之间的关系.
主要成果:
- 在上层土壤层增加了总N和可用的N;在下层土壤层减少了可用的N和NO3−-N,这表明N漏.
- 降低了土壤pH值,增加了土壤上层和下层的CaCO3含量.
- 两层土壤有机碳 (SOC) 增加,但总 (P) 随着肥的增加而减少.
- 可用的土壤P与植物Mn含量负相关;SOC和CaCO3正相关,表明Ca循环参与P循环和SOC封存.
结论:
- 长期的沉积加剧了沙漠草原土壤中的限制.
- 的输入增强了这些干旱生态系统中的土壤有机碳封存.
- 了解这些营养动态对于管理沙漠草原生态系统在增加的沉积下至关重要.
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