洞察不同质的河流流量产生过程和森林源流中水的贡献
Jaime Ortega1, Catalina Segura1, J Renée Brooks2,3
1Department of Forest Engineering, Resources, and Management, OSU.
概括
头水流量流动的变化是由各种地下储存驱动的. 地质复杂性表明储存,影响下游的水贡献和河流对降水的反应.
科学领域:
- 水文学的水文学
- 地质形态学 地质形态学
- 环境科学 环境科学
背景情况:
- 在较大的河流系统中精确建模季节性流动力学,需要了解河头水流的贡献.
- 带有多样化的地下储存的头水流域显著影响下游的水流.
研究的目的:
- 调查多样化的头水流域地下储存如何影响Lookout Creek的下游流量,这是俄勒冈州雨雪过渡区62公里的2个流域.
- 分析流域特征对季节性水贡献和溪流流动性的影响.
主要方法:
- 分析了来自十个河流位置的一年的水度和水稳定同位素数据.
- 利用十年的降水同位素数据进行比较.
- 应用终端混合模型来评估水源和贡献.
主要成果:
- 同位素数据证实,大多数流动源自大型秋季和冬季风暴.
- 捕捞区存储差异被发现会影响季节性支流水贡献.
- 储量较高的特定支流 (Cold和Longer Creek) 维持了夏季溪流流量的很大一部分 (高达50%).
结论:
- 头水流域储存的异质性对于理解山区流动动态至关重要.
- 地质变异性和地形复杂性可以作为地下储存的指标.
- 了解头水储存是预测河流对气候变化和干扰反应的关键.
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