This Presentation covers the topic of surface and subsurface tile drainage which is the part of canal irrigation. The content covered in this has been explained thoroughly with theory and Diagrams related to the topics and consists of various pictures to explain the content completely .Thank you.
This Presentation covers the topic of surface and subsurface tile drainage which is the part of canal irrigation. The content covered in this has been explained thoroughly with theory and Diagrams related to the topics and consists of various pictures to explain the content completely .Thank you.
For More Visit - www.civilengineeringadda.com
Irrigation Efficiency
Water conveyance Efficiency
It takes into account, conveyance or transit losses such as seepage through canal and evaporation through it.
η_c=W_f/W_r ×100
Where, Wf = water delivered to the field
Wr = water delivered from river or stream
Water Application Efficiency
It is the ratio of water stored in root zone to the water delivered to the field.
η_a=W_s/W_f ×100
Where, WS = water weight stored in root zone
WS = Wf – deep percolation – runoff
Wf = water delivered to the field
This efficiency is also called as farm efficiency and it depends on the irrigation technique that has been adopted.
Water use efficiency
It is the ratio of water used beneficially or consumptively to the water delivered to the field.
η_u=W_u/W_f ×100
Where, Wf = water delivered to the field
WU = consumptively used water
Water Storage Efficiency
This is the ratio of actual water stored in the root zone to the water needed to be stored to bring the moisture content upto field capacity.
Water Distribution efficiency
This evaluate the degree to which water is uniformly distributed to the root zone throughout the field area.
η_d=(1-y/d)×100
Where, d = average depth
y = Average numerical deviation in the depth of water stored from the average depth stored during irrigation
Question – the depths of penetration along the length of a border strip at points 30 m apart were proved. There observed values are 2 m, 1.9 m, 1.8 m, 1.6 m and 1.5 m. Compute the water distribution efficiency.
Solution –
Water distribution efficiency,
η_d=(1-y/d)×100
Where, d = average depth
d = (2+1.9+1.8+1.6+1.5)/5=1.76
And y = average numerical deviation
y = 1/5((2-1.76)+(1.9-1.76)+(1.8-1.76)+(1.76-1.6)+(1.76-1.5)=0.168
Therefore,
η_d=(1-0.168/1.76)×100
η_d=90.45%
Consumptive Use Efficiency
It is the ratio of water used consumptively to the net amount of water from the root zone.
Gully Erosion Control Measures
Temporary check dam
Brushwood dams
One row or single post brush wood dam
Double row post brush wood dams.
Semi permanent dams
Loose rock dam
Netting dam
Log check dam
Permanent check dam
Drop Spillway
Drop inlet spillway
Chute spillway
Parshall Flume..
It is an important topic in Hydraulic .. In irrigation purpose, Waste Water treatment, Aeration, Industrial water Treatment plant, etc , It is used..
For More Visit - www.civilengineeringadda.com
Irrigation Efficiency
Water conveyance Efficiency
It takes into account, conveyance or transit losses such as seepage through canal and evaporation through it.
η_c=W_f/W_r ×100
Where, Wf = water delivered to the field
Wr = water delivered from river or stream
Water Application Efficiency
It is the ratio of water stored in root zone to the water delivered to the field.
η_a=W_s/W_f ×100
Where, WS = water weight stored in root zone
WS = Wf – deep percolation – runoff
Wf = water delivered to the field
This efficiency is also called as farm efficiency and it depends on the irrigation technique that has been adopted.
Water use efficiency
It is the ratio of water used beneficially or consumptively to the water delivered to the field.
η_u=W_u/W_f ×100
Where, Wf = water delivered to the field
WU = consumptively used water
Water Storage Efficiency
This is the ratio of actual water stored in the root zone to the water needed to be stored to bring the moisture content upto field capacity.
Water Distribution efficiency
This evaluate the degree to which water is uniformly distributed to the root zone throughout the field area.
η_d=(1-y/d)×100
Where, d = average depth
y = Average numerical deviation in the depth of water stored from the average depth stored during irrigation
Question – the depths of penetration along the length of a border strip at points 30 m apart were proved. There observed values are 2 m, 1.9 m, 1.8 m, 1.6 m and 1.5 m. Compute the water distribution efficiency.
Solution –
Water distribution efficiency,
η_d=(1-y/d)×100
Where, d = average depth
d = (2+1.9+1.8+1.6+1.5)/5=1.76
And y = average numerical deviation
y = 1/5((2-1.76)+(1.9-1.76)+(1.8-1.76)+(1.76-1.6)+(1.76-1.5)=0.168
Therefore,
η_d=(1-0.168/1.76)×100
η_d=90.45%
Consumptive Use Efficiency
It is the ratio of water used consumptively to the net amount of water from the root zone.
Gully Erosion Control Measures
Temporary check dam
Brushwood dams
One row or single post brush wood dam
Double row post brush wood dams.
Semi permanent dams
Loose rock dam
Netting dam
Log check dam
Permanent check dam
Drop Spillway
Drop inlet spillway
Chute spillway
Parshall Flume..
It is an important topic in Hydraulic .. In irrigation purpose, Waste Water treatment, Aeration, Industrial water Treatment plant, etc , It is used..
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5. Placed at suitable depth and grade
below the ground surface
Lowers the capillary surface and
water table
Aerates the root zone
6. 1.Advantages of Subsurface Drains
Provides aeration to root zone
Improves soil structure and
maintains soil temperature
Avails land for early cultivation
Facilitates easy movement of farm
machines
7. Removes undesirable salts from
root zone
Decreases chances of flood hazards
Occupies no surface land
Small capacity drains are required
Less maintenance cost compared to
surface drains
8. 2. Disadvantages of subsurface drains
Require high initial cost
Requires steeper gradient
Repair works are costly and
inconvenient
Only seepage water is removed
Construction is difficult
9. 3. Subsurface drainage methods
Tile drains
Mole drains
Drainage wells
Deep open drains
Combination of tile and
mole drains
10. 4. Investigations for subsurface drainage
Topographic map of the area
Data of soil physiochemical properties
Position of ground water table and its
fluctuation
Quality of groundwater
11. Logs of soil and subsurface material
Crops to be grown and their drainage
requirements
Irrigation practices and their
requirements
12. 5. Groundwater studies for planning
subsurface drainage
3 parameters:
oDepth and fluctuation of groundwater
table
oQuality of groundwater
oHydraulic conductivity of the subsoil
material
13. DESIGN OF TILE DRAINAGE SYSTEM
Consists of :
1. Layout of the system
2. Depth and spacing of the drain
3. Size and grade of the tile lines
4. Material of tiles
5. Envelope materials and accessory
structures
6. Installation of tile drains
14. 1. Layout of tile drainage system
Drainage system comprises of laterals,
main drains and an outlet
Laterals
Main drains
Outlet
15. Different layouts of tile drainage
system:
a) Natural system
b) Parallel system
c) Herringbone system
d) Grid iron system
e) Random system
16. f) Intercepting system
g) Double system
h) Grouping system
i) Composite system
j) Zig zag system
k) Sink hole system
23. 2. Depth and spacing of tile drains
Depth and spacing are closely inter related
Depends on:
Texture of soil
Hydraulic conductivity
Types of crops grown
Extend of surface drainage
24. Outlet conditions
Topography of land
Salt content of soil
Agronomic practices
Drain depth: From ground surface to the
bottom of the tile, usually 1-1.5m
Tiles are placed above impermeable layer,
if any
25. Deeper the drain, wider the spacing, lesser
the number of drains required
Drain spacing-
’Hooghouts drain spacing formula’
S2 = 4K/R [H2-2hd+2Hd-h2]
where,
d- Depth to the impermeable layer
from the drain bottom
h- Height of water in the drain
26. H-Height of water in midway between 2
drains
S- Drain spacing
D-Distance from the impermeable layer to the
maximum height of water between the
drains
K- Hydraulic conductivity
R- Replenishment rate
27. 3. Size and grade of the tile drains
Drains are designed based on
Manning's formula
Drains are laid on longitudinal slope:
0.05-3%
Working grade: 0.2%
Size of tiles pipes: 30-90cm long,
10-15cm diameter
28. Diameter of tile drains,
d = 5.3(Dc)0.375 A0.375 S-0.1875
where,
d- Internal diameter of tile drain, cm
Dc – Drainage coefficient, cm/day
A-Drainage area, ha
S- Hydraulic gradient or tile grade, m/m
29. 4. Material of tiles
Clay, Concrete, PVC/Plastic pipes, Bituminous fibre or
steel
Pipe material should be:
Resistant to weathering and freezing
Have high density
Have sufficient strength to withstand static and
dynamic loads
Have uniformity in shape and wall thickness
30. 5. Envelope materials and accessory
structures
a) Envelope materials:
Materials that cover the drains placed
in less pervious strata
Gravel, coarse sand etc.
Prevents inflow of soil into the drains
Increases effective drain diameter
32. Recommendations for gravel envelope
(USBR):
For uniform soils,
D50 of envelope/D50 of soil = 5 to 10
For graded soils,
D50 of envelope/ D50 of soil = 12 to 58
33. b) Manholes and sedimentation basins:
Vertical structures
Installed at regular intervals along the
tile lines
Constructed by concrete or brick
masonry
Helps in cleaning and inspection
34. A man can enter and
work within it
Placed about 60 cm
below ground surface
Covered by
concrete block
35. c) Inlet to tile drains:
Allows water into the drain
Two types:
Blind inlet- cheaper but chances of
clogging
Surface inlet- have provisions to
prevent the trash
entering into the drains but costly
37. d) Outlet for drains:
Water from tile drains are discharged into
big size surface drains
Either by gravity or pumping
Gravity outlet- invert level of tile drain is
higher than fully supply level of surface
drain
Pump outlet- bed level of the outlet is
higher tan the discharging tile drain
38. e) Installation of tile drains:
Consists of:
Excavation of a trench
Laying the tile at predetermined grade,
depth and spacing
Putting the envelope material and
backfilling the soil
Installation of tile should start from out let
41. MULTIPLE WELL SYSTEM
Multiple wells are installed in a common
area of influence
Cone of depressions overlap each other
Results in increased drawdown in each well
Provides more drainage effect