基流
过程线
水文学(农业)
地下水
地下水排放
水流
水文地质学
环境科学
出院手续
地表径流
地下水流
回流
银行
地表水
地质学
含水层
流量(数学)
流域
地貌学
地理
环境工程
生态学
地图学
岩土工程
生物
几何学
数学
出处
期刊:Water
[MDPI AG]
日期:2023-02-21
卷期号:15 (5): 844-844
被引量:1
摘要
This study investigated the role of bank return flow to two medium size rivers in southeast Queensland using a combination of hydrograph separation techniques and geochemical baseflow separations. The main aims were to provide a case study to demonstrate spatial and temporal variability in groundwater contributions to two river systems in Southeast Victoria; the Avon River and the Mitchell River. The two rivers show large spatial and temporal variations in groundwater contributions with higher percentages during low flow periods and more surface runoff during wet years. At the end of the Australian millennium drought, groundwater discharge accounted for 60% of the total flow for the Avon River and 42% for the Michell River, whereas groundwater discharge only had a minor component to the total discharge in wetter years, ∼15% for the Avon River and only 3% for the Mitchell River. Radon and chloride were used for the geochemical baseflow separation and provide a means to separate regional groundwater discharge to the rivers from bank return flow. Bank return flow accounts for 2 to 5 times higher fluxes in certain areas. Geochemistry in combination with physical hydrogeology enhances the overall understanding of groundwater connected river systems over the river length.
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