2015
DOI: 10.1016/j.advwatres.2015.05.018
|View full text |Cite
|
Sign up to set email alerts
|

Semi-analytical solutions for flow to a well in an unconfined-fractured aquifer system

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4
1

Citation Types

1
7
0

Year Published

2016
2016
2022
2022

Publication Types

Select...
5

Relationship

1
4

Authors

Journals

citations
Cited by 13 publications
(8 citation statements)
references
References 36 publications
(95 reference statements)
1
7
0
Order By: Relevance
“…In this section, the time-drawdown responses of the three-layer aquifer system are investigated by generating the dimensionless drawdown-time type curves. The dimensionless drawdown data are obtained via numerical inverse Laplace (De Hoog et al, 1982) and Hankel (Michels, 1963;Press et al, 1992) transforms following the method outlined by Sedghi and Samani (2015). Type curves for conceptual Model I and Model II ( Fig.…”
Section: Resultsmentioning
confidence: 99%
See 4 more Smart Citations
“…In this section, the time-drawdown responses of the three-layer aquifer system are investigated by generating the dimensionless drawdown-time type curves. The dimensionless drawdown data are obtained via numerical inverse Laplace (De Hoog et al, 1982) and Hankel (Michels, 1963;Press et al, 1992) transforms following the method outlined by Sedghi and Samani (2015). Type curves for conceptual Model I and Model II ( Fig.…”
Section: Resultsmentioning
confidence: 99%
“…We consider unconfined aquifers that are hydraulically connected to underlying fractured aquifers, examples of which are found in different parts of the world (Al-Shaibani, 2008;Milanovic and Aghili, 1993;Sedghi and Samani, 2015;Subyani, 2004;Wagner, 2011). Often, an aquitard separates the unconfined aquifer from the underlying fractured aquifer.…”
Section: Introductionmentioning
confidence: 99%
See 3 more Smart Citations