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Tidal effects on variations of fresh-saltwater interface and groundwater flow in a multilayered coastal aquifer on a volcanic island (Jeju Island, Korea)

机译:潮汐对火山岛(韩国济州岛)多层沿海含水层中淡盐水界面和地下水流量变化的影响

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We conducted various field studies at the seawater intrusion monitoring wells located in the eastern part of Jeju Island, Korea, to observe the tidal effect on groundwater-seawater flow in the coastal aquifer. Studies included monitoring the fluctuations of groundwater and tide levels, electrical and temperature logging, and 2-D heat-pulse flowmeter tests. According to time-series analysis, tidal effects on groundwater level reached up to 3 km inland from the coastline. Water-level variation was more sensitive to tidal fluctuations near the coast, and more related to rainfall toward inland areas. Temporal and spatial variations in the shape and location of the freshwater-saltwater interface were analyzed using data from nine monitoring wells. The results indicated that the interface toe is located at a distance of 6-8 km from the coastline and its location was related to geological layers present. Long-term seasonal variations revealed no major changes in the interface; minor variations were due to moving boundary conditions induced by tidal fluctuations. Using the two-dimensional heat-pulse flowmeter, groundwater flow directions and velocities at four tidal stages were measured on three monitoring wells drilled into the multilayered aquifers. This direct measurement enabled us to relate the differences of flow velocities and directions with geology and tidal fluctuations. Combining the results of EC logging and flowmeter tests, we found a zone where freshwater and saltwater moved alternately in opposite directions, as influenced by the tidal fluctuations. Integrating various physical togging and flowmeter data with water-Level fluctuations improved our understanding of the behavior of fresh and seawater flow in the coastal aquifers. (c) 2006 Elsevier B.V. All rights reserved.
机译:我们对位于韩国济州岛东部的海水入侵监测井进行了各种现场研究,以观察潮汐对沿海含水层中地下水-海水流量的影响。研究包括监测地下水和潮汐水平的波动,电气和温度记录以及二维热脉冲流量计测试。根据时间序列分析,潮汐对地下水位的影响从海岸线向内陆延伸达3 km。水位变化对海岸附近的潮汐变化更为敏感,并且与内陆地区的降雨更为相关。利用来自九个监测井的数据分析了淡水-盐水界面的形状和位置的时空变化。结果表明,界面脚趾距海岸线6-8 km,其位置与存在的地质层有关。长期的季节性变化表明界面没有重大变化。微小的变化是由于潮汐波动引起的移动边界条件。使用二维热脉冲流量计,在钻探到多层含水层中的三个监测井上测量了四个潮汐阶段的地下水流向和流速。这种直接测量使我们能够将流速和方向的差异与地质和潮汐波动联系起来。结合EC测井和流量计测试的结果,我们发现了一个受潮汐波动影响的淡水和盐水沿相反方向交替运动的区域。将各种物理触发和流量计数据与水位波动相结合,可以使我们更好地理解沿海含水层中淡水和海水的流动特性。 (c)2006 Elsevier B.V.保留所有权利。

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