Articles | Volume 20, issue 3
https://doi.org/10.5194/hess-20-1225-2016
https://doi.org/10.5194/hess-20-1225-2016
Technical note
 | 
22 Mar 2016
Technical note |  | 22 Mar 2016

Technical Note: Three-dimensional transient groundwater flow due to localized recharge with an arbitrary transient rate in unconfined aquifers

Chia-Hao Chang, Ching-Sheng Huang, and Hund-Der Yeh

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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (02 Feb 2016) by Alberto Guadagnini
AR by Hund-Der Yeh on behalf of the Authors (03 Feb 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (10 Feb 2016) by Alberto Guadagnini
RR by Anonymous Referee #1 (04 Mar 2016)
ED: Publish as is (08 Mar 2016) by Alberto Guadagnini
AR by Hund-Der Yeh on behalf of the Authors (09 Mar 2016)
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Short summary
Most previous solutions for groundwater flow due to localized recharge assumed either aquifer incompressibility or 2-D flow without vertical flow. This paper develops a 3-D flow model for hydraulic head change induced by the recharge with random transient rates in a compressible unconfined aquifer. The analytical solution of the model for the head is derived. The quantitative criteria for the validity of those two assumptions are presented by the developed solution.