阿尔卑斯山沼泽草原的气动态对气候变暖的反应不如阿尔卑斯山草原
Xiaopeng Chen1, Genxu Wang2, Na Li3
1College of Grassland Science, Shanxi Agricultural University, Taigu 030801, China.
The Science of the total environment
|April 15, 2024
概括
气候变暖增加了植物在生长季节吸收的. 在冬季,变暖加剧了阿尔卑斯山草原根的气损失,但不是沼泽草原.
科学领域:
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
- 永久土科学 永久土科学
背景情况:
- 结冰解周期极大地影响永久土的水热条件, (N) 循环和植物群体组成.
- 气候变暖影响N动态和损失,特别是在不同的湿度条件下,但详细的季节性反应仍然不清楚.
研究的目的:
- 研究气候变暖对青海-西藏高原永久土区域内高山草原和沼泽草原中气动态和损失的影响.
- 为了区分季节性N命运和损失对不同湿度制度下的变暖反应.
主要方法:
- 使用稳定同位素标记物 (15N) 来追踪温暖和环境高山草原和高山沼泽草原中的命运.
- 在整个生长和非生长季节的植物组织 (芽,根) 和土壤层中监测的回收和分布.
主要成果:
- 变暖显著增加了在阿尔卑斯山草原生长季节的植物芽,子和根的N恢复.
- 在非生长季节的高山草原中,变暖减少了根的储量,但在更深层的土壤中增加了,表明了潜在的损失.
- 阿尔卑斯山沼泽草地对变暖的反应较弱,在非生长季节的N损失不受影响.
结论:
- 变暖提高了植物N的利用率,并在生长季节增加了植物N池.
- 在非生长季节的高山草原中,由变暖引起的冷解周期促进了根N的损失和向下迁移.
- 与高山草原相比,高山沼泽草原在N动态方面对气候变暖具有更强的弹性.
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