Time-drawdown data collected at a distance of 30 m from a well pumping at a rate of 1000 m³/day are as follows. Calculate the transmissivity and the storativity. t, min 1 2 3 4 5 6 7 10 20 40 80 100 300 500 1000 0.03 0.15 0.30 0.39 0.48 0.61 0.72 0.91 1.38 1.91 2.41 2.60 3.45 3.87 4.39 s, m a) Use Theis Method b) Use modified Theis Method (Cooper-Jacob Method) c) d) Regenerate the drawdowns value found in (a) and compared with the given data. Compute the root mean square error between the calculated drawdown and observation values. Regenerate the drawdowns value found in (b) and compared with the given data. Compute the root mean square error between the calculated drawdown and observation values.
Time-drawdown data collected at a distance of 30 m from a well pumping at a rate of 1000 m³/day are as follows. Calculate the transmissivity and the storativity. t, min 1 2 3 4 5 6 7 10 20 40 80 100 300 500 1000 0.03 0.15 0.30 0.39 0.48 0.61 0.72 0.91 1.38 1.91 2.41 2.60 3.45 3.87 4.39 s, m a) Use Theis Method b) Use modified Theis Method (Cooper-Jacob Method) c) d) Regenerate the drawdowns value found in (a) and compared with the given data. Compute the root mean square error between the calculated drawdown and observation values. Regenerate the drawdowns value found in (b) and compared with the given data. Compute the root mean square error between the calculated drawdown and observation values.
Chapter2: Loads On Structures
Section: Chapter Questions
Problem 1P
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Question
![Time-drawdown data collected at a distance of 30 m from a well pumping at a rate of 1000
m³/day are as follows. Calculate the transmissivity and the storativity.
t, min 1
2
3
4
5
6
7 10 20
40 80 100 300 500 1000
s, m
0.03 0.15 0.30 0.39 0.48 0.61 0.72 0.91 1.38 1.91 2.41 2.60 3.45 3.87
4.39
a) Use Theis Method
b) Use modified Theis Method (Cooper-Jacob Method)
c) Regenerate the drawdowns value found in (a) and compared with the given data. Compute
the root mean square error between the calculated drawdown and observation values.
d) Regenerate the drawdowns value found in (b) and compared with the given data.
Compute the root mean square error between the calculated drawdown and observation
values.](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F35e8d6e3-8597-43d8-a90c-971420eb5676%2F8a4366c6-d4a3-436c-854f-a69f99095baf%2Fadf1d1_processed.png&w=3840&q=75)
Transcribed Image Text:Time-drawdown data collected at a distance of 30 m from a well pumping at a rate of 1000
m³/day are as follows. Calculate the transmissivity and the storativity.
t, min 1
2
3
4
5
6
7 10 20
40 80 100 300 500 1000
s, m
0.03 0.15 0.30 0.39 0.48 0.61 0.72 0.91 1.38 1.91 2.41 2.60 3.45 3.87
4.39
a) Use Theis Method
b) Use modified Theis Method (Cooper-Jacob Method)
c) Regenerate the drawdowns value found in (a) and compared with the given data. Compute
the root mean square error between the calculated drawdown and observation values.
d) Regenerate the drawdowns value found in (b) and compared with the given data.
Compute the root mean square error between the calculated drawdown and observation
values.
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