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Journal of Groundwater Hydrology
In the floodplain composed of gravel and/or sand, the groundwater recharge from the river occurs partially and actively. To estimate the active and partial groundwater recharge from the river in the floodplain, this research examined to estimate the groundwater flux through the bypath in Okayama floodplain, using the temperature variation. Water temperature was monitored at the Asahi River and one spring at which such groundwater discharges in the Asahi River floodplain of Okayama Prefecture indoi:10.5917/jagh.57.207 fatcat:s7sh372ym5fp7iydnemqt6ymny