A mathematical model of water table fluctuation in a semi‐infinite aquifer induced by localized transient recharge | Zendy

Rai Shivendra Nath | Zendy; Singh Rishi Narain | Zendy

AI Assistant Blog Pricing

Home ZAIA Blog

Premium

A mathematical model of water table fluctuation in a semi‐infinite aquifer induced by localized transient recharge

Author(s) -

Rai Shivendra Nath,

Singh Rishi Narain

Publication year - 1981

Publication title -

water resources research

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 1.863

H-Index - 217

eISSN - 1944-7973

pISSN - 0043-1397

DOI - 10.1029/wr017i004p01028

Subject(s) - groundwater recharge , aquifer , water table , hydraulic conductivity , geology , transient (computer programming) , isotropy , geotechnical engineering , table (database) , groundwater model , homogeneous , soil science , groundwater , hydrology (agriculture) , mechanics , thermodynamics , physics , soil water , quantum mechanics , computer science , data mining , operating system

A mathematical model of the water table fluctuation in an unconfined aquifer subjected to a typical localized transient recharge is presented. The aquifer is taken to be homogeneous, isotropic, underlain by a horizontal impermeable base, and linked with a surface reservoir on one side. Sensitivity characteristics of the water table due to variations in the rate of recharge, hydraulic conductivity, and specific yield are illustrated with the help of a numerical example.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here

Accelerating Research