steady state drainage

15
Steady State Steady State Drainage Drainage Department of Agricultural and Biological Engineering University of Illinois at Urbana- Champaign

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Steady State Drainage. Department of Agricultural and Biological Engineering. University of Illinois at Urbana-Champaign. Darcy’s Law. h 1. L. h 2. q: [L/T]. K: [L/T]. L, h: [L]. Bubbling tube. Water inlet tubes. Water. Air. Storage tube. Bubbles. Air at. atmospheric. pressure. - PowerPoint PPT Presentation

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Page 1: Steady  State Drainage

Steady State Steady State DrainageDrainage

Department of Agricultural and Biological

Engineering University of Illinois at Urbana-Champaign

Page 2: Steady  State Drainage

L)h - h( K = q 21

Lh1

h2

Darcy’s LawDarcy’s Law

q: [L/T] K: [L/T] L, h: [L]

Page 3: Steady  State Drainage

Bubbling tube

Water inlet tubes

Outlet tube

Outlet holes

Storage tube

Air seal plugSoil

Water

AirBubbles

Water level fixedby bubbling tube

Air at atmosphericpressure

Page 4: Steady  State Drainage

Inner Cylinder

Outer Cylinder

Mariotte Bottle

Bubbling Tube

Soil

Page 5: Steady  State Drainage

H1

H2

H3

Hn

Hn+1

K1

K2

Kn

D1

D2

Dn

q

EQUIVALENT K FOR VERTICAL FLOWEQUIVALENT K FOR VERTICAL FLOWWhen flow is

perpendicular to a series of soil layers, the flux through each layer is the

same.

D = D1 + D2 +...+Dn

n

n

2

2

1

1e

KD

KD

KD

D K

...

D)H - H( K = q 1n1

e

Page 6: Steady  State Drainage

9 ft4 ft K = 2 ft/d

2 ft K = 4 ft/d

3 ft K = 3 ft/d

Ke?

ft/d 2.573.59

42

24

33

9 K e

Page 7: Steady  State Drainage

Q2

Hb

K1

K2

Kn

D1

D2

Dn

EQUIVALENT K FOR HORIZONTAL FLOWEQUIVALENT K FOR HORIZONTAL FLOW

When flow is parallel to a series of soil layers, the discharge through unit thickness of the system is the

sum of the discharges through the

layers..

n21

nn2211L DDD

KDKDKD K

...

...L

)H - H( K = q baL

Ha

Q1

Qn

L

Page 8: Steady  State Drainage

IMPERMEABLE LAYER

h

m

d S

2r

Hooghoudt EquationHooghoudt Equation

2e

S)2d4Km(m

q

de

Page 9: Steady  State Drainage

Hooghoudt EquationHooghoudt Equation

2e

S)2d4Km(m

q

1,3,5,....n S4n

S4n

01n0

e

)e(1n

e48)

rπS

(ln8

)S

dnπ2coth(ln16)

rπS

(ln8

Sπd

πd

πd

Page 10: Steady  State Drainage

Estimating Spacing Estimating Spacing using using The Hooghoudt The Hooghoudt EquationEquation

2e

S)2d4Km(m

q

i)2d4Km(m

S e2

i = Drainage Coefficient

Page 11: Steady  State Drainage
Page 12: Steady  State Drainage

0.4 1.2

S

6.0

Soil surface

Impervious layer

Water table

For drainage design the following information is available:

depth of tile = 1.2 m; depth to water table = 0.8 m; depth to impermeable layer = 7.2 m; drainage

coefficient = 0.007 m; hydraulic conductivity = 0.8 m/day. Estimate the required drain spacing

Page 13: Steady  State Drainage

0.4 1.2

S

6.0

Soil surface

Impervious layer

Water table

For drainage design the following information is available:

depth of tile = 4 ft; depth to water table = 1 ft; depth to impermeable layer = 12 ft; drainage coefficient = 3/8 inches; hydraulic conductivity = 2 inch/hr. Estimate the

required drain spacing

3 4

8

Page 14: Steady  State Drainage

IMPERMEABLE LAYER

h

b

d S

2r

t

Kirkham EquationKirkham Equation

gSr)bK(t4

q

Page 15: Steady  State Drainage

)2/)2(cos()2/cosh(

)2/)2(cos()2/cosh(ln

)2/cos()2/cosh(

)2/cos()2/cosh(ln2

)4/tan(

)4/)2(tan(ln2

1 hrdhmS

hrdhmS

hrhmS

hrhmS

hd

hrd

m

g

gSr)bK(t4

q

Kirkham EquationKirkham Equation