土壤源对陆地植物的相对贡献的全球分布和驱动因素
Chao-Chen Hu1, Xue-Yan Liu2, Avery W Driscoll3
1School of Earth System Science, Tianjin University, Tianjin, China.
Nature communications
|July 30, 2024
概括
全球植物 (N) 吸收主要由年平均温度 (MAT) 调节. 较高的温度有利于酸盐和的使用,而有机的使用随着变暖而减少,影响陆地生态系统.
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
- 植物生理学 植物生理学
背景情况:
- 土壤 (N) 对植物生产力和社区结构至关重要.
- 了解植物如何使用不同的土壤N形式 (酸盐,,有机N) 和环境法规是有限的.
研究的目的:
- 量化土壤酸盐,和有机对全球植物吸收的贡献.
- 确定调节工厂N利用的关键环境因素.
主要方法:
- 全球植物和土壤中天然 (N) 同位素的分析.
- 量化土壤酸盐 (fNO3-), (fNH4+) 和有机N (fEON) 的部分贡献,以种植N.
主要成果:
- 年平均温度 (MAT) 是全球植物N来源利用的主要调节者.
- 酸盐和的贡献随着MAT的增加而增加,而有机N的贡献则减少.
- 为植物N来源偏好的转移确定了特定的温度值.
结论:
- 工厂N的使用模式在全球范围内是由温度调节的,而不是降水或N沉积.
- 在控制植物在陆地生态系统中的利用方面,温度比人类的负荷更为重要.
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