Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Aquifer - Water Table Aquitard Model for Hard Rock Areas


Affiliations
1 Department of Civil Engineering, Indian Institute of Science, Bangalore 560 012, India
     

   Subscribe/Renew Journal


Two layered models are gellerally accepted to represent groundwater flow in fractured media. This paper presents a rigorous numerical analysis of an aquifer - water table aquitard system, which may be applied for hard rock areas. In this study, the water table aquitard considered is compressible and the system is of two-layered nature. The model is quasi three dimensional and takes into account the vertical variations of head in the aquitard. The water table is treated as an unknown boundary.

A new iterative scheme for analysing aquifer-water table aquitard system has been presented. It has been found that rigorous analysis may be necessary in the well field solutions while approximate methods are sufficient for a regional study in hard rock areas.


Subscription Login to verify subscription
User
Notifications
Font Size

Abstract Views: 167

PDF Views: 3




  • Aquifer - Water Table Aquitard Model for Hard Rock Areas

Abstract Views: 167  |  PDF Views: 3

Authors

K. Sridharan
Department of Civil Engineering, Indian Institute of Science, Bangalore 560 012, India
M. S. Mohan Kumar
Department of Civil Engineering, Indian Institute of Science, Bangalore 560 012, India
N. S. Lakshmana Rao
Department of Civil Engineering, Indian Institute of Science, Bangalore 560 012, India

Abstract


Two layered models are gellerally accepted to represent groundwater flow in fractured media. This paper presents a rigorous numerical analysis of an aquifer - water table aquitard system, which may be applied for hard rock areas. In this study, the water table aquitard considered is compressible and the system is of two-layered nature. The model is quasi three dimensional and takes into account the vertical variations of head in the aquitard. The water table is treated as an unknown boundary.

A new iterative scheme for analysing aquifer-water table aquitard system has been presented. It has been found that rigorous analysis may be necessary in the well field solutions while approximate methods are sufficient for a regional study in hard rock areas.