首页> 外文会议>International Commission on Irrigation and Drainage;International congress on irrigation and drainage >STREAM WATER - GROUNDWATER INTERACTION CHANGES IN LOWER NAKDONG RIVER BASIN BY USING THE TIME SERIES ANALYSIS AND GROUNDWATER QUALITY
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STREAM WATER - GROUNDWATER INTERACTION CHANGES IN LOWER NAKDONG RIVER BASIN BY USING THE TIME SERIES ANALYSIS AND GROUNDWATER QUALITY

机译:基于时间序列分析和地下水水质的下游纳东河流域地下水-地下水相互作用变化。

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Total of sixteen river dams has been constructed in four major rivers in South Korea(eight at the Nakdong River, three each at the Han River and Geum River, and two at theYeongsan River) for the purpose of fl ood control and effective water resource vis-a-vis climatechange. However, the river dam construction induced groundwater level rise and streamwater-groundwater interaction at the upstream regions of the river dams. In this study, weexamined stream water-groundwater interaction properties by using the time series analysisof groundwater level and river water level with groundwater quality at the Changreong-Hamanriver dam in lower Nakdong River. Total of 34 manually monitored wells and 5 automaticallymonitored wells in the riparian zone of the Gwangryeo Stream and Iryeong Stream tributariesof the Nakdong River were observed during Mayl 2011–September 2013 with river level(Ducknam observatory station) and rainfall (Jindong rainfall station). As a result of this study,the groundwater level was found to rise by an average of 1.62 m for the observed period. Thecross-correlation function of groundwater level and Nakdong river level has changed from0.04-0.68 (before river dam) to 0.05-0.71(after river dam) and response time ranged 3-229hours(before river dam) to 1-251 hours(after river dam). Also, groundwater quality displayeda lower Ca2+, HCO3-, and CO32- concentration and higher NO3- concentration near theNakdong River after river dam construction. These are indicating a greater interaction betweengroundwater and river water due to the river dam.
机译:在韩国的四个主要河流中建造了十六座河坝的总数 (八龙河八,每河河河河,两岸,两者在 云山河)为氟于控制和有效的水资源VIS-Vis气候 改变。但是,河流施工诱导地下水位上升和流 河流上游地区的水土地区互动。在这项研究中,我们 通过使用时间序列分析检查流水地互动性能 Changreong-Haman地下水位与地下水位水位的地下水位 河坝在下部的Nakdong河。总共34个手动监控井和5 在Gwangryeo流和Iryeong溪流支流的河岸区监测井 在2011年5月2011年5月期间观察到了Nakdong River,2013年9月与河流 (Ducknam Daniveratoration Station)和降雨(金东降雨站)。由于这项研究, 在观察期内,发现地下水位平均增长1.62米。这 地下水位和内东河水位的互相关功能发生了变化 0.04-0.68(河坝前)至0.05-0.71(河流后)和响应时间范围3-229 几小时(河流坝前)至1-251小时(河坝之后)。此外,显示地下水质量 靠近的CA2 +,HCO3和CO32浓度较低,NO3-浓度 河坝建设后的河东河。这些表明之间的相互作用更大 地下水和河流由于河流。

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