Homework Answers
Question 5: (25 marks) A fully penetrating pumping well is located in a confined aquifer that can be considered to have an infinite extent in all directions. There is no recharge to the aquifer a...
Question 5: (25 marks) A fully penetrating pumping well is located in a confined aquifer that can be considered to have an infinite extent in all directions. There is no recharge to the aquifer and no other pumping wells in the area. There are two observation wells located at 100 and 500 m, respectively, from the pumping wells. The aquifer and the pumping well have the following properties: Depth to top of aquifer: 50 m Aquifer thickness: 5 m Aquifer...
The drawdown doserved at a confined aquifer well after pumping it during 1400 minutes at a...
The drawdown doserved at a confined aquifer well after pumping it during 1400 minutes at a flow rate of 500 gal/min is 20.39 ft. The drawdowns observed at the same time at two observation wells located at 10 ft and 100 ft from the pumped well are 20 and 19.7 ft, respectively. Find the transmissivity of the aquifer and the well radius. Answ: T-8.8x105 gpd/ft, r-0.5 ft. 3.
1. (2 points) A well in a uniform, homogeneous, isotropic confined aquifer is pumped at a...
1. (2 points) A well in a uniform, homogeneous, isotropic confined aquifer is pumped at a rate of 815 L/min. After 3 days it looks as if the water levels have stabilized in observation wells at distances of 20 m and 200 m from the pumping well. The drawdown in the well at 20 m is 6.5 m and the drawdown in the well at 200 m is 3.5 m. a) Use the Thiem solution to determine the aquifer transmissivity....
1) Three 610 mm wells are located on a straight line 304.8 m apart in an artesian aquifer With T- 3974 m^3/d/m and S 3 x 10^-5. The pumps are to be pumped for 10 days. Suppose we want to restrict...
1) Three 610 mm wells are located on a straight line 304.8 m apart in an artesian aquifer With T- 3974 m^3/d/m and S 3 x 10^-5. The pumps are to be pumped for 10 days. Suppose we want to restrict the drawdown in each of the wells to 18.3m. What will be the coresponding discharge for the individual wells?
1) Three 610 mm wells are located on a straight line 304.8 m apart in an artesian aquifer With T-...
A well is pumping near a barrier boundary at a rate of 0.05 m3/s from a confined aquifer 20 m thi...
A well is pumping near a barrier boundary at a rate of 0.05 m3/s
from a confined aquifer 20 m thick. The hydraulic conductivity of
the aquifer is 5 x 10-4 m/s, and its storativity is 4 x 10-5.
Determine the drawdown in the observation well after 30 hours of
continuous pumping. What is the fraction of the drawdown
attributable to the barrier boundary?
River fi Гр-240 m 30° 300 m 300 m
River fi Гр-240 m 30° 300 m...
Question 4 A well 50 cm in diameter penetrates 33 m below the static water table....
Question 4 A well 50 cm in diameter penetrates 33 m below the static water table. After a long period of pumping at a rate of 80 m2/h, the drawdowns in two observation wells A and B, 18 and 45 m from the pumped well, were found to be 1.8 and 1.1 m respectively. Determine the hydraulic conductivity of the aquifer (in m/d) . the expected drawdown in the pumped well . the radius of influence of the pumped well,...
estion 4 a. A well 50 cm in diameter penetrates 33 m below the static water...
estion 4 a. A well 50 cm in diameter penetrates 33 m below the static water table. After a long period of pumping at a rate of 80 m/h, the drawdowns in two observation wells A and B, 18 and 45 m from the pumped well, were found to be 1.8 and 1.1 m respectively. Determine . the hydraulic conductivity of the aquifer (in m/d) the expected drawdown in the pumped well the radius of influence of the pumped well,...
2 3) [40] A discharge Q (l/s) is being pumped for a very long duration from...
2 3) [40] A discharge Q (l/s) is being pumped for a very long duration from a confined aquifer of m (m) thickness by a pumping well of ro(cm) radius. The water table has dropped by s=5.4m and sz=3.3 m, respectively in two observation wells at distances of r1=25m and rz=71m from the pumping well a) Determine the hydraulic conductivity K and the conduction coefficient (transmissivity) T of the aquifer. b) Calculate the drop so in the pumping well in...
WSE3701
QUESTION 2 Discuss how porosity and particle size affect a well’s ability to provide enough quantities of water. (10) QUESTION 3 Calculate the transmissivity of an artesian aquifer that has a thickness of 5.5 m and is pumped at a rate of 1.52 m3 /min. There are two observation wells located at 150 m and 280 m away with drawdowns of 0.8 and 0.72 m respectively. (10) QUESTION 4 An aquifer has T = 175 m2 /day, S = 1.3 x10-4, and provides a flow...
Water, with density of 1000 kg/m3 and kinematic viscosity of 1.0 x 10- m2/s, is pumped through a ...
Water, with density of 1000 kg/m3 and kinematic viscosity of 1.0 x 10- m2/s, is pumped through a total length of 60 m of pipe from a lower reservoir to a higher reservoir. The inner diameter of the pipe is 30 cm. Both reservoirs are open to the atmosphere, and the water surface of the higher reservoir is 10 m above that of the lower reservoir. The entrance from the lower reservoir to the pipe is sharp-edged, and along the...
Question 5: (25 marks) A fully penetrating pumping well is located in a confined aquifer that can be considered to have an infinite extent in all directions. There is no recharge to the aquifer and no other pumping wells in the area. There are two observation wells located at 100 and 500 m, respectively, from the pumping wells. The aquifer and the pumping well have the following properties: Depth to top of aquifer: 50 m Aquifer thickness: 5 m Aquifer...
The drawdown doserved at a confined aquifer well after pumping it during 1400 minutes at a flow rate of 500 gal/min is 20.39 ft. The drawdowns observed at the same time at two observation wells located at 10 ft and 100 ft from the pumped well are 20 and 19.7 ft, respectively. Find the transmissivity of the aquifer and the well radius. Answ: T-8.8x105 gpd/ft, r-0.5 ft. 3.
1) Three 610 mm wells are located on a straight line 304.8 m apart in an artesian aquifer With T- 3974 m^3/d/m and S 3 x 10^-5. The pumps are to be pumped for 10 days. Suppose we want to restrict the drawdown in each of the wells to 18.3m. What will be the coresponding discharge for the individual wells?
1) Three 610 mm wells are located on a straight line 304.8 m apart in an artesian aquifer With T-...
A well is pumping near a barrier boundary at a rate of 0.05 m3/s
from a confined aquifer 20 m thick. The hydraulic conductivity of
the aquifer is 5 x 10-4 m/s, and its storativity is 4 x 10-5.
Determine the drawdown in the observation well after 30 hours of
continuous pumping. What is the fraction of the drawdown
attributable to the barrier boundary?
River fi Гр-240 m 30° 300 m 300 m
River fi Гр-240 m 30° 300 m...
Question 4 A well 50 cm in diameter penetrates 33 m below the static water table. After a long period of pumping at a rate of 80 m2/h, the drawdowns in two observation wells A and B, 18 and 45 m from the pumped well, were found to be 1.8 and 1.1 m respectively. Determine the hydraulic conductivity of the aquifer (in m/d) . the expected drawdown in the pumped well . the radius of influence of the pumped well,...
estion 4 a. A well 50 cm in diameter penetrates 33 m below the static water table. After a long period of pumping at a rate of 80 m/h, the drawdowns in two observation wells A and B, 18 and 45 m from the pumped well, were found to be 1.8 and 1.1 m respectively. Determine . the hydraulic conductivity of the aquifer (in m/d) the expected drawdown in the pumped well the radius of influence of the pumped well,...
2 3) [40] A discharge Q (l/s) is being pumped for a very long duration from a confined aquifer of m (m) thickness by a pumping well of ro(cm) radius. The water table has dropped by s=5.4m and sz=3.3 m, respectively in two observation wells at distances of r1=25m and rz=71m from the pumping well a) Determine the hydraulic conductivity K and the conduction coefficient (transmissivity) T of the aquifer. b) Calculate the drop so in the pumping well in...
Water, with density of 1000 kg/m3 and kinematic viscosity of 1.0 x 10- m2/s, is pumped through a total length of 60 m of pipe from a lower reservoir to a higher reservoir. The inner diameter of the pipe is 30 cm. Both reservoirs are open to the atmosphere, and the water surface of the higher reservoir is 10 m above that of the lower reservoir. The entrance from the lower reservoir to the pipe is sharp-edged, and along the...
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