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The document classifies waves based on various criteria such as: 1) Rate of variation - surges, intermediate waves, long waves 2) Controlling force - gravity, capillary, gravity and friction 3) Frequency of occurrence - simple solitary waves, wave trains, wave groups It also discusses the direction of movement, wave surface elevation, form, periodic/oscillatory nature, translatory or orbital motion, transverse or longitudinal propagation, and behavior in deep or shallow water. Classification is important for analyzing unsteady open channel flows.

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0% found this document useful (0 votes)
101 views4 pages

37 3 PDF

The document classifies waves based on various criteria such as: 1) Rate of variation - surges, intermediate waves, long waves 2) Controlling force - gravity, capillary, gravity and friction 3) Frequency of occurrence - simple solitary waves, wave trains, wave groups It also discusses the direction of movement, wave surface elevation, form, periodic/oscillatory nature, translatory or orbital motion, transverse or longitudinal propagation, and behavior in deep or shallow water. Classification is important for analyzing unsteady open channel flows.

Uploaded by

Raza
Copyright
© © All Rights Reserved
We take content rights seriously. If you suspect this is your content, claim it here.
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Hydraulics Prof. B.S.

Thandaveswara

37.3 Classification of waves


Translatory, longitudinal shallow water waves can be classified based on different

criteria as shown in table below. (Ref. unsteady flow in open channels edited by

Mahmood K and Yevjevich V. Vol 1, 1975).

Table: Criteria for classification of wave

Criteria Classification

Surges (Moving hydraulic jugs - hydraulic bore)


(1) Rate of
variation Intermediate waves

Long waves

capillary wave

gl
Gravity C 2 =

(2) Controlling
force
(
gL 2πσ
)
2πy
C2 = ___ + ____ tanh ____ (for shallow water waves)
2π ρL ρL
Capillary wave

(
gL 2πσ
C2 = ___ + ____
2π ρL ) (for deep wave)

Gravity and friction

3a
η = 2a S ec h 2 ( x − ct )
Simple solitary 2 y3
(Single form of gravity wave )
Undisturbed water flow
a
η
(3) Frequency of
occurrence

The Solitary Wave

Indian Institute of Technology Madras


Hydraulics Prof. B.S. Thandaveswara

Mutiple

Wave train
cg

Wave Groups
Downstream
Relative to channel bed slope
Upstream

Vw Vw Vw
y V2 V2 y V2 y V2 y
2 V1 y1 y1 V1 2 y1 V1 2 y V1 2
1

Type A - Advancing Type B - Advancing Type B - Advancing Type B - Advancing


downstream upstream upstream upstream
(positive surge) (positive surge) (positive surge) (positive surge)

Vw = c + V1 Vw = c - V1 Vw = c + V1 Vw = c - V1
(4) Direction of
movement

V - Vw+V2 Vw - V2 +V
y w V2 Vw - V1 V +V y Vw - V1 y y Vw 2 Vw+V1
2 y1 y w 1 2 y1 2 2 y1
1

Type A Type B Type C Type D

Four Types of rapidly varied uniformly progressive flow. (Top)


Unsteady flows; (bottom) the corresponding flows that appear steady to
an observer following the wavefront.

Downstream
Relative to underlying flow
Upstream

(5) Wave
surface
elevation

Indian Institute of Technology Madras


Hydraulics Prof. B.S. Thandaveswara

Positive(higher) uniformly
progressive wave (sluice gate)
Relative to level of underlying flow Surge
Negative(lower) Type C (Sluice gate)
and D is operated Demand Surge
Positive-negative (when Sluice is operated these these appear in pairs)

Occur Tidal in rivers


Type A, B occur in Tidal rivers
Rejected Surge

(6) Form Single-faced (Monoclinical progressive rising wave)


Symmetrical
Two-faced
Asymmetrical

FLOOD
WAVE
Q

Time

Mean Water Level L

η a
(7) Periodic or
oscillatory wave
A Periodic y

Definition Sketch for Oscillatory Wave Motion

Particles constantly progressing the wave movement (Example: Sea waves)

(8) Translatory
Orbital

Circular particle Orbits in Deep Water

Indian Institute of Technology Madras


Hydraulics Prof. B.S. Thandaveswara

(9) Transverse
wave
Longitudinal
wave

L
Mean water level
(10) Deep water
wave
Stokesian wave
Cnoidal wave y
Shallow water y'
wave

Elliptical Particle Orbits in Shallow Water


Mean water level

Typical Cnoidal Wave Profile

(11) Mechanical
Oscillation Finite amplitude due to initial disturbance
(pulsating flows) Mechanical oscillation
Kinematic wave Surface instability
Eg: Roll wave (progressive wave train)
Diffusive wave Steep slopes F > 2.0
Dynamic wave

(12)Rapidly
varying Progressing Surges, bores, depression
unsteady flow
Gradually Floods in reservoirs and in channels / rivers
varying
unsteady flow

Indian Institute of Technology Madras

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