Abstract
Radioactive tracer, Iodine-131, was used to detrermine the groundwater flow velocity at CHASNUPP site by applying multi-well technique. During the experiment the water table was monitored in the detection wells and the groundwater regime was found unstable due to fluctions in the water level of Chashma-Jehlum Link Canal flowing nearby the area under study. The ground water flow velocity was estimated to be about 4.8 cm per day under the prevailing conditions. (author).
Citation Formats
Hussain, S D, Ahmed, M, Rafiq, M, and Ahmed, N.
Measurement of groundwater flow velocity at CHASNUPP site using radio-tracer technique.
Pakistan: N. p.,
1991.
Web.
Hussain, S D, Ahmed, M, Rafiq, M, & Ahmed, N.
Measurement of groundwater flow velocity at CHASNUPP site using radio-tracer technique.
Pakistan.
Hussain, S D, Ahmed, M, Rafiq, M, and Ahmed, N.
1991.
"Measurement of groundwater flow velocity at CHASNUPP site using radio-tracer technique."
Pakistan.
@misc{etde_10117452,
title = {Measurement of groundwater flow velocity at CHASNUPP site using radio-tracer technique}
author = {Hussain, S D, Ahmed, M, Rafiq, M, and Ahmed, N}
abstractNote = {Radioactive tracer, Iodine-131, was used to detrermine the groundwater flow velocity at CHASNUPP site by applying multi-well technique. During the experiment the water table was monitored in the detection wells and the groundwater regime was found unstable due to fluctions in the water level of Chashma-Jehlum Link Canal flowing nearby the area under study. The ground water flow velocity was estimated to be about 4.8 cm per day under the prevailing conditions. (author).}
place = {Pakistan}
year = {1991}
month = {Jun}
}
title = {Measurement of groundwater flow velocity at CHASNUPP site using radio-tracer technique}
author = {Hussain, S D, Ahmed, M, Rafiq, M, and Ahmed, N}
abstractNote = {Radioactive tracer, Iodine-131, was used to detrermine the groundwater flow velocity at CHASNUPP site by applying multi-well technique. During the experiment the water table was monitored in the detection wells and the groundwater regime was found unstable due to fluctions in the water level of Chashma-Jehlum Link Canal flowing nearby the area under study. The ground water flow velocity was estimated to be about 4.8 cm per day under the prevailing conditions. (author).}
place = {Pakistan}
year = {1991}
month = {Jun}
}