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降雨作为一个重要的过程,在自然恢复的初始阶段,在石荒漠化自然恢复的净N增长
Xia Li1,2, Yu Pang1,2, Hengsheng Lao1,2
1Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, and Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation, Nanning Normal University, No. 175, Mingxiu East Road, Nanning, 530001, China.
Scientific reports
|July 2, 2025
概括
降雨为地生态系统提供必需的 (N),大部分无机N被土壤保留. 溶解有机N (DON) 丢失,但整体N增益支持生态系统的恢复.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 生态生态学 生态生态学
背景情况:
- 在沙漠化后的恢复过程中,地生态系统面临 (N) 限制.
- 人们怀疑快速的水文过程会导致N损失,但缺乏现场数据.
- 了解水文N预算对于岩生态系统恢复至关重要.
研究的目的:
- 量化的输入,损失和净收益通过雨量在地草和草生态系统.
- 研究水文过程在循环中的作用.
- 评估降雨对缓解早期相继阶段的限的贡献.
主要方法:
- 在三年内监测降雨量和相关的水文过程.
- 从降雨中量化输入 (总N,无机N,溶解的有机N).
- 测量水文气损失和净气增益在不同的地生态系统.
主要成果:
- 平均降雨N输入量为12.0公斤N ha-1 y-1,其中56.1%为无机N.
- 平均水文N损失为8.5公斤N ha-1y-1,主要是溶解的有机N (DON,74.1%).
- 平均净N增益为3.4公斤N ha-1y-1,无机N被保留,DON丢失,表明土壤-降雨N交换.
结论:
- 降雨是岩生态系统中重要的源,有助于恢复.
- 卡斯特土壤结构限制了水文N损失,保护了土壤无机N.
- 降雨中的气供应有助于缓解气的限制,在早期的岩相继阶段.
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