Principles of Geotechnical Engineering (MindTap Course List)
9th Edition
ISBN: 9781305970939
Author: Braja M. Das, Khaled Sobhan
Publisher: Cengage Learning
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Chapter 7, Problem 7.10P
To determine
Find the hydraulic conductivity of the sand layer.
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the cross section of a levee, shown below, which is 650 m long and is underlain by a 2.5-m-thick permeable sand layer. It was observed that the quantity of water flowing through the sand layer into the collection ditch is 13.5 m3 /hr. What is the hydraulic conductivity of the sand layer?
Figure below shows the cross section of a levee that is 500 m long and is underlain by a 2-m-thick permeable sand layer. It was observed that the quantity of water flowing through the sand layer into the collection ditch is 250 m^3/day.
Refer to Problem 8.4. Using the flow net drawn, calculate the hydraulic uplift force at the base of the hydraulic structure per meter length (measured along the axis of the structure).8.24 For the hydraulic structure shown in Figure 8.24, draw a flow net for flow through the permeable layer and calculate the seepage loss in m3/day/m.
Chapter 7 Solutions
Principles of Geotechnical Engineering (MindTap Course List)
Ch. 7 - Prob. 7.1PCh. 7 - Prob. 7.2PCh. 7 - Prob. 7.3PCh. 7 - Prob. 7.4PCh. 7 - Prob. 7.5PCh. 7 - Prob. 7.6PCh. 7 - Prob. 7.7PCh. 7 - Prob. 7.8PCh. 7 - Prob. 7.9PCh. 7 - Prob. 7.10P
Ch. 7 - Prob. 7.11PCh. 7 - Prob. 7.12PCh. 7 - Prob. 7.13PCh. 7 - Prob. 7.14PCh. 7 - Prob. 7.15PCh. 7 - Prob. 7.16PCh. 7 - Prob. 7.17PCh. 7 - Prob. 7.18PCh. 7 - Prob. 7.19PCh. 7 - Prob. 7.20PCh. 7 - Prob. 7.21PCh. 7 - Refer to Figure 7.24. The following data were...Ch. 7 - Prob. 7.23PCh. 7 - Prob. 7.1CTP
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- The figure below represents a system with flow in the horizontal direction. Find the value of each pressure charge, level charge, and total charge in A, B, C, D, E, F, G, plus the real and approximate velocity of water flow plotting all of the above, given that soil porosity = 0.33 and transmittance coefficient = 0.50 cm/secarrow_forwardA confined aquifer has a thickness of 85 ft. An 86-in diameter well drilled to the bottom of the aquifer, as shown in fig 3-10, if the hydraulic conductivity of the aquifer is 10 ft / day, and if water is originally 170 ft deep in the well, calculate approximately the maximum rate of flow that can be pumped from the well without dewatering any part of the aquifer. Assume 1000 ft reasonable value for the radius of influence. What will be the average velocity ( Darcy velocity ) of flow in the aquifer at a distance 20 ft from the center of the well?arrow_forwardHow do the frequency of exceedance and the return period affect the design of hydraulic structures?arrow_forward
- Refer to Figure 7.24. The following data were collected during the field permeability measurement of a confined aquifer using a pumping test. Determine the hydraulic conductivity of the permeable layer. Use Eq. (7.49). Thickness of the aquifer, H = 4.5 m Piezometric level and radial distance of the first observation well: h1 = 2.9 m; r1 = 17.8 m Piezometric level and radial distance of the second observation well: h2 = 1.8 m; r2 = 8.1 m Rate of discharge from pumping, q = 0.5 m3/minarrow_forwardWater is stored in the reservoir of a trapezoidal dam with a vertical upstream height of 6 meters. If the pressure is 3.14 kPa at the lowest position, determine the depth of the water. How much would the hydrostatic force change if silica contamination causes the water's specific gravity to rise? (Specific gravity of contaminated water = 1.1)arrow_forwardA well with a 0.25-m diameter fully penetrates an unconfined aquifer that is 20 m thick. The well has a discharge of 0.015 m ・ s−1 and a drawdown of 8 m. If the flow is steady and the hydraulic conductivity is 1.5 × 10−4 m ・ s−1, what is the height of the piezometric surface above the confining layer at a site 80 inches from the well?arrow_forward
- From the figure shows an unconfined non homogeneous aquifer between two water bodies at depth of 50 m and 45 m. respectively. Compute the average coefficient of permeability of the aquifer and the rate of flow.arrow_forwardA confined aquifer underlies an unconfined aquifer as shown. Compute the equivalent horizontal coeff. of permebility Compute the hydraulic gradient Compute the flow rate from one stream to another per meter widtharrow_forwardCALCULATION USING DARCY'S LAW 1) An aquifer has 2 piezometers installed (A and B) and the distance between them is 1km, the hydraulic loads are 850m and 625m respectively. The average hydraulic conductivity of the aquifer is 3.9 x 10-2 m/day and the effective porosity is 25%, calculate how long in years it takes for the water to walk between piezometer A and B.arrow_forward
- If a pumping well extracts water at a rate of 0.1 cumecs from a confined, homogeneous aquifer of 33.1 m thick and porosity of 0.04, what is the magnitude of the apparent groundwater velocity in m/d at 132 m from the well?arrow_forwardA confined aquifer is 18.5 m thick. The hydraulic head drops 2.99 m between two wellsthat are 823 m apart. If the hydraulic conductivity of the aquifer is 4.35 m/d, how many cubicmeters of water are moving through the aquifer per unit width?arrow_forwardHow much subsidence would you expect from an elastic confined aquifer that hasa specific storage of 2.6 x 10-5 m-1, a decline in pressure of 225 kPa, an aquifer thickness of180 m, and a porosity of 24 percent? Assume the aquifer temperature is 20 °C. Just looking for a push in the right direction. Thanksarrow_forward
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