The proposed dam shown in figure is 90 m long and the coefficient of permeability of the soil is 0.0013 mm/sec. The quantity of water (m³) that will be lost per day by seepage is (rounded to the nearest number). 8.5m Flow lines 1.2m Equipotential lines 12.5m-

The proposed dam shown in figure is 90 m long and the coefficient of permeability of the soil is 0.0013 mm/sec. The quantity of water (m³) that will be lost per day by seepage is (rounded to the nearest number). 8.5m Flow lines 1.2m Equipotential lines 12.5m-

Structural Analysis

6th Edition

ISBN:9781337630931

Author:KASSIMALI, Aslam.

Publisher:KASSIMALI, Aslam.

Chapter2: Loads On Structures

Section: Chapter Questions

Problem 1P

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Concept explainers

Sediment transport

Sediment transport or Soil transport is the movement of solid particles, usually due to the combination of gravitational forces acting on the sediment, and the movement of the liquid at which the sediment enters. Soil erosion occurs in natural systems where the particles are sandstones (sand, rocks), mud, or clay; the liquid is air, water, or ice; and the gravitational force that works to move particles to the landing surface. Sediment transportation or soil migration due to the movement of liquids occurs in rivers, lakes, lakes, oceans, and other bodies of water as a result of currents and waves. Transportation is also caused by glaciers as they flow, and to places on earth under the influence of wind. Soil erosion due to gravity alone is possible in most sloping areas, including hills, scarves, cliffs, and the continental shelf — the continental boundary of the slope.

Question

The proposed dam shown in figure is 90
m long and the coefficient of
permeability of the soil is 0.0013
mm/sec. The quantity of water (m³) that
will be lost per day by seepage is
(rounded to the nearest number).
8.5m
Flow lines
1.2m
h2m/0.6m
Equipotential
lines
12.5m-

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