DIRECT MEASUREMENT OF 3D-GROUNDWATER FLOW IN SANDY BEACH ADGACENT TO TIDAL FLAT

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  • 干潟に隣接する砂浜における3次元地下水流向の直接計測

Abstract

<p> The purpose of this study was to develop a simple 3-D groundwater flowmeter to directly measure seawater inflow to the beach, and to clarify the occurrence of vertical seepage during the rising tide and seawater upwelling during the falling tide. A new paper-cylinder type groundwater flow directional anemometer was devised, tested in a laboratory experiment, and used to observe coastal groundwater infiltration in Yamaguchi Bay. As a result, it was possible to measure the three-dimensional groundwater flow directional velocity of groundwater infiltrating into the beach in 15 minutes, and the groundwater recharge and discharge of the beach at the site were clarified.</p>

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