溶解通过干湿干的过渡在一个小的水河流盆地:运输模式,出口控制和命运的综合理解
H K M Mihiranga1,2,3, Yan Jiang1,2, M G S Sathsarani1,4
1State Key Laboratory for Ecological Security of Regions and Cities, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China. yanjiang@rcees.ac.cn.
Environmental science. Processes & impacts
|January 27, 2025
概括
了解在被堵塞的河流中溶解 (DP) 的出口是恢复的关键. 溶解有机 (DOP) 的出口在雨季显著增加,受水文连接和土壤来源的影响.
科学领域:
- 环境科学 环境科学
- 水文学的水文学
- 生态生态学 生态生态学
背景情况:
- 溶解 (DP) 出口对于水盆地的河流生态恢复至关重要,因为它具有生物可用性和保留性.
- 了解干旱和潮湿期间的DP出口机制和控制对于管理这些生态系统至关重要.
研究的目的:
- 为了调查河流DP运输模式,出口管制,以及在半干旱,小水域的命运.
- 为了理解陆地DP源与水域DP下沉之间在不同水文条件下的联系.
主要方法:
- 在潮湿和干旱季节进行和总悬浮固体 (TSSs) 的时空监测.
- 使用歇斯底里,层次分区和变化系数分析.
- 量化总DP (TDP),溶解有机P (DOP) 和酸P (PO4-P) 的组成和流量.
主要成果:
- DP形式与排放有很强的相关性,在干湿过渡期间有显著的转变.
- 在干燥基础流中,TDP的DOP分量从4%增加到雨季结束时的64%.
- 污水处理厂 (WWTP) 的废水是主要的PO4-P来源,而DOP源自土壤来源,通过地表和土壤水流量运输.
结论:
- 水文连接和土壤湿度动态控制着季节性DOP趋势.
- 小水系统和内流过程对河流PO4-P流量产生了重大影响,但对DOP流量的影响较小.
- 对DP出口机制的综合理解对于水系统中有效的河流生态恢复至关重要.
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