GVF - profile classification

0.0(0)
Studied by 0 people
call kaiCall Kai
learnLearn
examPractice Test
spaced repetitionSpaced Repetition
heart puzzleMatch
flashcardsFlashcards
GameKnowt Play
Card Sorting

1/19

flashcard set

Earn XP

Description and Tags

20 Terms

1
New cards

describe the main features of the GVF profile of water surface

  • it joins 2 normal depths

  • it crosses critical depth

  • it is gradual, the curve is possibly over a few hundred meters long


2
New cards

how can the different situations which cause GVF be identified and classified?

  • examine the slope and the resulting normal and critical depths


3
New cards

what is the critical slope (Sc)?

in uniform flow, for a given Q there will be a slope which normal depth=critical depth, this is the critical slope

4
New cards

what is the critical slope given by for a wide channel (bยปยปy)

Sc = (gn2)/(yc1/3)

5
New cards

what are the different classifications for open channels in GVF studies?

  • mild

  • steep

  • critical

  • horizontal

  • adverse


6
New cards

what are the classifications derived from?

whether the normal depth in uniform flow is sub-critical, super-critical or critical

  • or by comparing the critical slope


7
New cards

define S0 for horizontal and adverse channels

  • horizontal channel โ†’ S0=0

  • adverse channel โ†’ S0<0


8
New cards

what 3 things does the GVF equation tell us regarding depth change

  1. S0 - Sf > 0 if y is greater than normal depth

  2. 1 - Fr2 > 0 if y is greater than critical depth

  3. dy/dx < 0 (depth increasing) if y lies between normal and critical depths


9
New cards

the depth space is divided into 3 regions by the normal and critical depths, what are the regions defined by (letter + digit)?

mild slope:

  • M1 (above normal depth)

  • M2 (between normal depth and critical depth)

  • M3 (below critical depth)


steep slope

  • S1 (above critical depth)

  • S2 (between critical depth and normal depth)

  • S3 (below normal depth)


10
New cards

describe the M1 profile

  • y increases along the channel

  • y is greater than yn so Sf<S0

  • y is greater than yc so Fr<1

  • flow is subcritical


11
New cards

describe the M2 profile

  • y decreased along channel

  • y is less than yn so Sf>S0

  • y is greater than yc so Fr <1

  • flow is subcritical


12
New cards

describe the M3 profile

y increases along channel

  • y is less than yn so Sf>S0

  • y is less than yc so Fr >1

  • flow is supercritical


13
New cards

describe the S1 profile

  • y increases along channel

  • y is greater than yn so Sf<S0

  • y is greater than yc so Fr < 1

  • flow is subcritical


14
New cards

describe the S2 profile

y decreases along channel

  • y is greater than yn so Sf<S0

  • y is less than yc so Fr >1

  • flow is supercritical


15
New cards

describe the S3 profile

y increases along channel

  • y is less than yn so Sf>S0

  • y is less than yc so Fr >1

  • flow is supercritical


16
New cards

what is a control point?

a location where there is a known relationship between water depth and discharge

  • provide a location to start a GVF calculation


17
New cards

what are the general rules for supercritical and subcritical flow

  • supercritical is controlled by upstream conditions

  • subcritical is controlled by downstream conditions


18
New cards

given a long enough stretch of channel, what will flow try to do?

revert to normal flow

19
New cards

where does a hydraulic jump occur?

between 2 regions of GVF at a point where the jump conditions for the sequent depths is correct

20
New cards

what can be assumed about a hydraulic jump where the slope is mild?

if there is no influential downstream control, a hydraulic jump can be assumed to jump directly to normal depth