Two reservoirs are connected through a homogeneous and isotropic aquifer having hydraulic conductivity (K) of 25 m/day and effective porosity (n) of 0.3 as shown in the figure (not to scale). Groundwater is flowing in the aquifer at the steady-state. 7 Reservoir 1 30 m 10⁰ Aquifuge 5 m Aquiclude Aquifer 2km K= 25 m/day 10 m n = 0.3 Datum V Reservoir 2 If the water in Reservoir 1 is contaminated then the time (in days, round off to one decimal place) taken by the contaminated water to reach to Reservoir 2 will be

Structural Analysis
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ISBN:9781337630931
Author:KASSIMALI, Aslam.
Publisher:KASSIMALI, Aslam.
Chapter2: Loads On Structures
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Two reservoirs are connected through a homogeneous and isotropic aquifer having
hydraulic conductivity (K) of 25 m/day and effective porosity (n) of 0.3 as shown in the
figure (not to scale). Groundwater is flowing in the aquifer at the steady-state.
2
Reservoir 1
10⁰
30 m
Aquifuge
Aquiclude
5 m Aquifer K = 25 m/day 10 m
m = 0.3
2km
Datum
Reservoir 2
If the water in Reservoir 1 is contaminated then the time (in days, round off to one decimal
place) taken by the contaminated water to reach to Reservoir 2 will be
Transcribed Image Text:Two reservoirs are connected through a homogeneous and isotropic aquifer having hydraulic conductivity (K) of 25 m/day and effective porosity (n) of 0.3 as shown in the figure (not to scale). Groundwater is flowing in the aquifer at the steady-state. 2 Reservoir 1 10⁰ 30 m Aquifuge Aquiclude 5 m Aquifer K = 25 m/day 10 m m = 0.3 2km Datum Reservoir 2 If the water in Reservoir 1 is contaminated then the time (in days, round off to one decimal place) taken by the contaminated water to reach to Reservoir 2 will be
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