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Water in Soils: One Dimensional Flow of Water through Soils

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Academic year: 2023

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Braja M Das, Principal of Geotechnical

Engineering , fourth edition, PWS Publishing Company, 1998, Boston

Muni Budu, Soil Mechanics and Foundations , 2nd edition, John Wiley & Sons, 2007, USA

R.F. Craig, Soil Mechanics , (English & terjemahan Prof.Dr.Ir Budi S Supandji)

Cernica, J.N., Soil Mechanics , John Wiley & Sons, 1995

Holtz, R.D., Kovacs, W.D., An introduction to

Geotechnical Engineering , Prentice Hall, N.J.,

1981

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Bernoulli’s law

Darcy’s law

Flow

Determining hydraulic conductivity

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Common knowledge:

Water flow from higher place to the lower

places

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g z v h u

w

 2

2

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g z v h u

w

 2

2

Pressure

Head Velocity

Head

Elevation Total Head

Head

In soil, the velocity of the flow is very small, it can be neglected

u z h

w

 

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L ih

B

A h

h

h  

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P = 0 (= P

atm

)

Pressure Head (increases with depth below surface)

Elevation

Head

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Elevation Head ith height above datum)

Elevation

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P = 0 (= P

atm

)

Total Head (constant: hydrostatic equilibrium)

Elevation

Head Elevation datum

Total head = Pressure

head + Elevation head

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Hydorstatic Pressure

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Classifications : one, two or three dimensional

◦ One dimensional flow :

 flow with fluid parameter such as pressure, velocity, constant temperature toward intersection

perpendicular to flow direction

◦ Two dimensional flow :

 cofferdam cells (sheet pile wall), concrete dam; earth dam and levees

◦ Three dimensional flow:

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i k

v  

v = discharge velocity

k = hydraulic conductivity i = hydraulic gradient

A v

q  

q = flow rate

A = cross sectional area

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 

     

V V V

v L

A

L A A

v A

A A

v v

A v A

A v q

A A

A

A v vA q

v s v

v s v

v s v

s

v s s

v s v

v s

 

 

 

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The hydraulic conductivity of soils depends on several factors: fluid viscosity, pore size distribution, grain-size distribution, void ratio, roughness of mineral particles, and degree of soil saturation.

In clayey soils, structure plays an important

role in hydraulic conductivity.

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Constant Head Test

Falling Head Test

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The constant head test method is used for permeable soils (k>10-4 cm/s), and the falling head test is mainly used for less permeable soils (k<10-4 cm/s).

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Permeability of granular soils (U.S.

Dept of Navy, 1971)

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Variation of void ratio with hydraulic

conductivity of clayey soil (Tavenas et al, 1983)

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 

eq

H H H H n

H

k H k H k H k H

k H

n

 1 ...

3 2

1 2 3

1

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 

 

 

 

 

 

 

 

 

 

 

 

 

Vn

n V

V V

eq V

k H k

H k

H k

H k H

...

3 2

1

3 2

1

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Flow takes place laterally and vertically through the sides of the canal and vertically below the canal,

 Determine the equivalent hydraulic conductivity in the horizontal and vertical directions. The vertical and

horizontal hydraulic conductivities for each layer are assumed to be the same.

 Calculate the ratio of the equivalent horizontal hydraulic conductivity to the equivalent vertical hydraulic

conductivity for flow through the sides of the canal.

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Referensi

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