For a drainage basin of 600 km², isohyetals drawn for a storm gave the following datą:; . 15-12 12-9 6-3 3-1 Isohyetals (interval) (cm) Inter-isohyetal area (km³) 9-6 92 128 120 175 85 (A) 1.741 cm B 7.41 cm C) 7.14 cm D) 4.71 cm

For a drainage basin of 600 km², isohyetals drawn for a storm gave the following datą:; . 15-12 12-9 6-3 3-1 Isohyetals (interval) (cm) Inter-isohyetal area (km³) 9-6 92 128 120 175 85 (A) 1.741 cm B 7.41 cm C) 7.14 cm D) 4.71 cm

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

Estimate the average depth.

For a drainage basin of 600 km², isohyetals drawn for a storm gave the following datą:; .
15-12
12-9
6-3
3-1
Isohyetals (interval) (cm)
Inter-isohyetal area (km³)
9-6
92
128
120
175
85
(A) 1.741 cm
B 7.41 cm
C) 7.14 cm
D 4.71 cm

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