Abstract
The aquifer under the Indus basin of Pakistan is of marine origin and the native groundwater is saline which is overlain by a freshwater layer. The upper freshwater layer is formed as a result of seepage from rivers, canals, field irrigation losses and precipitation. About 6.42 million ha area has freshwater layer of variable thickness.
Cite
CITATION STYLE
APA
SAEED, M. M., ASGHAR, M. N., & BRUEN, M. (2003). Options for Skimming Fresh Groundwater in the Indus Basin of Pakistan: A Review. Journal of Groundwater Hydrology, 45(3), 259–278. https://doi.org/10.5917/jagh1987.45.259
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free