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|Title:||Reply to comment by Kong et al. on “Appropriate Boundary Condition for Dupuit-Boussinesq Theory on the Steady Groundwater Flow in an Unconfined Sloping Aquifer With Uniform Recharge”|
|Author's alias:||吳, 映昕|
|Publisher:||American Geophysical Union (AGU)|
|Journal title:||Water Resources Research|
|Abstract:||The article aims to respond a comment made on our paper about appropriate boundary condition for the original Dupuit‐Boussinesq theory for two‐dimensional steady groundwater flow in an unconfined sloping aquifer with uniform rainfall recharge. To respond to the comments arguing the existence of lateral groundwater flows and negative groundwater table, clarifications are made for our analysis focusing on two‐dimensional groundwater flow without considering lateral effects by using the original and classical approximate theory.|
|Rights:||An edited version of this paper was published by AGU. Copyright 2019 American Geophysical Union.|
The full-text file will be made open to the public on 22 November 2019 in accordance with publisher's 'Terms and Conditions for Self-Archiving'.
|Appears in Collections:||Journal Articles|
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