This document summarizes the methodology used to determine the water requirements of rice crops in Venkatapuram village. It provides background on rice cultivation and methods for calculating irrigation water needs. Key details include: the project area is Venkatapuram village in Andhra Pradesh; rainfall and climate data were collected for the area; the consumptive use of rice was calculated as 143.98 cm using the Blaney-Criddle method; the total water required for rice over the growing season is estimated to be 896,833.60 cubic meters with a required discharge of 0.06 cubic meters/second; and evapotranspiration was calculated as 1155.79 mm/season for rice using the Penman method.
The water balanced of a place, whether it be an agricultural field, watershed, or continent, can be determined by calculating the input, output, and storage changes of water at the Earth's surface. The major input of water is from precipitation and output is evapotranspiration. The water balance is intended for use as a screening tool to further evaluates water resources allocations within the watershed and to identify water balance components that may require further analysis during the next levels of watersheds planning. The study area chosen for the present study area is Doddavalabhi sub watershed which falls in Kolar taluk of Kolar district. The study areas geographically lies between 760 8’ 0” E and 760 23’ 0” E longitude and 120 20’ 0” N and 120 28’ 0” N latitudes with an area 15.20 sq.km. For the determination of crop water requirement for Kolar major crops considered are ragi and groundnut with the crop period of 120 days and 140 days respectively. The year and monthly wise potential evapotranspiration and actual evapotranspiration is calculated by using penman method, blaney-criddle method, pan evaporation and radiation methods. The year wise potential evapotranspiration calculated by Blaney-criddle is maximum 645.66 mm during 2014, in this year monthly PET is maximum in July month ie 150.4mm. The year wise potential evapotranspiration calculated by Pan Evaporation is maximum 236.43 mm during 2014, in this year monthly PET is maximum in July month ie 56.67mm. The Year wise actual evapotranspiration is also maximum during 2014 for both ragi and groundnut. Hence Blaney criddle method is best suitable since it provides the most satisfactory results compared to other methods because this method is suggested for areas where available climatic data cover air temperature data only.
This presentation contains some of the factors affecting the duty of irrigation water and also the measures to improve the duty. Hope this will found very helpful to you...
Introduction:
Necessity of irrigation- scope of irrigation engineering- benefits and ill effects of irrigation- irrigation development in India- types of irrigation systems, Soil-water plant relationship: Classification of soil water- soil
moisture contents- depth of soil water available to plants-permanent
and ultimate wilting point
Water requirements of crops:
Depth of water applied during irrigation- Duty of water and deltaimprovement
of duty- command area and intensity of irrigation consumptive use of water and evapotranspiration- irrigation efficiencies- assessment of irrigation water
The water balanced of a place, whether it be an agricultural field, watershed, or continent, can be determined by calculating the input, output, and storage changes of water at the Earth's surface. The major input of water is from precipitation and output is evapotranspiration. The water balance is intended for use as a screening tool to further evaluates water resources allocations within the watershed and to identify water balance components that may require further analysis during the next levels of watersheds planning. The study area chosen for the present study area is Doddavalabhi sub watershed which falls in Kolar taluk of Kolar district. The study areas geographically lies between 760 8’ 0” E and 760 23’ 0” E longitude and 120 20’ 0” N and 120 28’ 0” N latitudes with an area 15.20 sq.km. For the determination of crop water requirement for Kolar major crops considered are ragi and groundnut with the crop period of 120 days and 140 days respectively. The year and monthly wise potential evapotranspiration and actual evapotranspiration is calculated by using penman method, blaney-criddle method, pan evaporation and radiation methods. The year wise potential evapotranspiration calculated by Blaney-criddle is maximum 645.66 mm during 2014, in this year monthly PET is maximum in July month ie 150.4mm. The year wise potential evapotranspiration calculated by Pan Evaporation is maximum 236.43 mm during 2014, in this year monthly PET is maximum in July month ie 56.67mm. The Year wise actual evapotranspiration is also maximum during 2014 for both ragi and groundnut. Hence Blaney criddle method is best suitable since it provides the most satisfactory results compared to other methods because this method is suggested for areas where available climatic data cover air temperature data only.
This presentation contains some of the factors affecting the duty of irrigation water and also the measures to improve the duty. Hope this will found very helpful to you...
Introduction:
Necessity of irrigation- scope of irrigation engineering- benefits and ill effects of irrigation- irrigation development in India- types of irrigation systems, Soil-water plant relationship: Classification of soil water- soil
moisture contents- depth of soil water available to plants-permanent
and ultimate wilting point
Water requirements of crops:
Depth of water applied during irrigation- Duty of water and deltaimprovement
of duty- command area and intensity of irrigation consumptive use of water and evapotranspiration- irrigation efficiencies- assessment of irrigation water
soil plant water relationship determinationhailu55
The relationship is related to the properties of soil and plants
that affect the movement, retention and use of water.
A simple analogy:
Soil – Water Reservoir
Plant Roots – pump with many inlets
As the rate of pumping depends on the character of the pump,
the rate of extraction of water from the soil by the plant depends
on the character of the soil.
Soil Water Classification
Gravitational water:
It is the water in the large pores that moves downward freely under the influence of gravity
It drains out so fast that it is not available to the crops.
The time of draining out varies from one day in sandy soils to three days in clay soils.
Capillary Water:
It is the amount of water retained by the soil after gravitational water has drained out.
It is the water in the small pores which moves because of capillary forces and is called capillary water.
Capillary water is the major source of water available for the plant
Hygroscopic Water
Soil moisture further reduced by ET until no longer moves because of capillary forces.
The remaining water which is held on particle surfaces so tightly is called hygroscopic water.
Here, the water is held by adhesive force. And therefore, it is unavailable to the plant.
soil water constants
Field Capacity (FC)
Following saturation when all macro pores are drained by gravity and drainage ceases, usually defined 2 days following saturation by rainfall.
Measured as the moisture content at -5 kPa (0.05 bar or 0.5 m tension)
Permanent Wilting point (PWP)
The point where plants cannot extract any more water – only very small pores are filled with water.
Defined as the moisture content at -1500 kPa (15 bar or 150 m tension)
Total Available Water
Total Available Water (TAW): the water available to crops
expressed in mm/m (mm of water per meter depth of soil).
TAW = (FC – PWP)*b*Dz
Readily Available Water (RAW):
This is the level to which the available water in the soil can be used up without causing stress in the crop.
For most crops, 50 to 60% of the total available water is taken as readily available.
RAW = MAD*TAW
Where, MAD = maximum allowable deficit
Crop Water Requirement
CU is the controlling factor for irrigation scheduling.
That is, CU determines the quantity of water to be added by irrigation and helps in day to day management of irrigation systems.
Actually, total water demand of crops is made up of:
i) Crop water use: includes evaporation and transpiration
ii) Leaching requirement: a fraction of water to be added to remove salts from the root zone.
iii) Losses of water due to deep seepage in canals and losses due to the inefficiency of application.
ETc = Evaporation + Transpiration
ETc is normally expressed in mm/day.
Factors Affecting ETc:
Weather parameters (To, RH, Wind, etc.)
Crop Characteristics (type, variety and length of growing period)
Management and Environmental aspects
(control of diseases, soil salinity, etc.)
Runoff is one of the most significant hydrological variables used in most of the water resources applications. Physiographically the area is characterized by undulating topography with plains and valleys. The Soil Conservation Service Curve Numbers also known as hydrologic soil group method were used in this study. This method is adaptable and suitable approach for quick runoff estimation and is approximately easy to use with minimum data and it gives good result. From the study yearly rainfall and runoff were estimated easily. The study area covers an area of 466.02 km2, having maximum length of 36.5 km. The maximum and minimum elevation of the basin is 569 m and 341 m above MSL, respectively.
Solution Manual for Water Supply and Pollution Control – Warren Viessman, Mar...HenningEnoksen
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Solution Manual for Water Supply and Pollution Control - 8th Edition
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> Present and future status of water and population
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2. CONTENT OF PRESENTATION
INTRODUCTION
REVIEW OF LITERATURE
PROJECT AREA & METHODOLOGY
RESULT AND CONCLUSION
3. INTRODUCTION
Introduction on rice crop : Rice is the seed of the grass species Oryza
sativa (Asian rice) or Oryza glaberrima (African rice). India is the third largest
contry to produce rice in the world. Rice is the basic need in human life.
Irrigation Water requirement : The primary objective of irrigation is
to provide plants with sufficient water to obtain optimum yields and a high
quality harvested product. The required timing and amount of applied water is
determined by the prevailing climatic conditions, the crop and its stage of
growth, soil properties (such as water holding capacity) and the extent of root
development. Water within the crop root zone is the source of water for crop
evapotranspiration. Thus, it is important to consider the field water balance to
determine the irrigation water requirements.
4. REVIEW OF LITERATURE
PREPARATION OF LAND : Land preparation starts with removal of
shrubs and stumps from rice fields. The land is then ploughed using hand hoes
such as jembe/panga, oxen or tractors. Power and equipment are required
for tillage in different soil types are varied. It is essential to plough when land
is dry to reduce weeds. However in difficult soils such as virgin lands there
may be need to wet the field before ploughing. It is generally recommended
that two ploughs and one harrow or rotovation are sufficient for soil
disturbance long before planting to establish.
5. DEPTH AND TIME OF IRRIGATION :The depth and time of
irrigation is given by the expression below.
y =
Fc .d. γs
γw
Let, y = depth of water available in root zone
d = depth of root zone in meters
Fc = field capacity of soil expressed as a ratio
γs = Density or unit weight of soil
γw = Density or unit weight of water
Time of irrigation is given by the expression below.
T=
2.778A ×dw
q
Let, A = area of land
q = discharge of water
dw = available moisture depth
6. CROP AND CROP SEASON IN INDIA :In India, the northern and
north eastern regions have two distinct cropping seasons. The first coinciding
mostly with the South western monsoon is called kharif. Which spans mostly
from July to October. The other, called Rabi, spans generally over October to
March. The summer season crops are planted sometime between April and
June. In southern part of India, there is no such distinct season, but each
region has its own classification of seasons.
DUTY, DELTA & BASE PERIOD :
1. Delta: Delta is the total depth of water required-by a crop during the entire
period Of crop in the field, and is denoted by a symbolΔ .
2. Base Period: It is the time in days counted from the period of first watering
for a crop before sowing the crop (known as pre sowing irrigation) and the
last watering before harvesting the crop.
3. Duty: Duty is defined as the area irrigated by a unit discharge during the Base
period of crop or in other words Duty may be defined as the area irrigated by
an average discharge of 1 cumec for a specified number of days.
7. RELATIONSHIP BETWEEN DUTY AND DELTA :
Let D = Duty in hectares/cumec,
∆= Total depth of water (in meters), and
B = Base period in days
If we take a field of area D hectares; water supplied to the field corresponding to
the water depth ∆ meters will be
=∆ x D hectares meters = D x ∆ x 104 cubic meters . . . (1)
(b) Again for the same field of D hectares, one cumec of water is required to
flow during the entire base period. Hence, water supplied to this field
= 1 x (B x 24 x 60 x 60) m3 . . . (2)
Equating Equation (1) And (2) we get,
D×∆×104 = B×24×60×60
∆=
8.64 B
D
8. CONSUMPTIVE USE OF WATER :Consumptive use for a particular
crop may be defined as the total amount of water used by the plant in
transpiration (building of plant tissues, etc.) and evaporation from
adjacent soils or from plant leaves, in any specified time. The values of
consumptive use (Cu) may be different for different crops, and may be
different for the same crop at different times and places.
Blaney-Criddle method :
Cu=
k.p
40
[I.8t + 32]
Cu= Monthly consumptive use in cm.
k = Crop factor
t = Mean monthly temperature in °C.
p = Monthly per cent of annual day light hours that occur during the period.
If,
𝑝
40
[I.8t + 32] is represented by f, we get
Cu= k. f
9. Table3: Monthly daytime percentage hours (p)
Table2: Monthly crop coefficient factor k (for use in Blaney-Criddle method)
10. Penman method :
The penman formula is a semi-empirical equation combining mass transfer (Ea) and
energy budget (H) methods. The formula was developed by Penman in 1948 and is
still widely used for calculating the potential evaporation using synoptic
meteorological data.
According to Penman the potential evaporation Eo (in mm/day) can be calculated
as:
Et =
A.H+ α Ea
A+α
Also,
Ea = 0.002187(160 + u2) (es – ea)
Table4: saturated vapour pressure of water
11. Table5: mean monthly solar radiation incident on earth outer space
Table6: maximum possible hours of bright sunshine in hours
12. ASSESSMENT OF IRRIGATION WATER :The different type of
Assessment of irrigation water are described below
1. Assessment on area basis: A rate arrived at in this method is called a crop rate.
In a mostly all the canal irrigated tracts are assessed for irrigation charges under
this system. In this system charges are levied on the area which is actually
irrigated. The rate of payment of charges is not some for all states.
2. Volumetric assessment: In this method charges are levied on actual volume of
water supplied to the cultivators. This is ideal system under which cultivators has
incentive for using water economically. However this method has no practical
value induce up till now.
3. Assessment on seasonal basis: In this water charging are mainly based on crop
season. The rate depend on the type of crop grown in the season in that
particular tract.
4. Composite rate: Sometimes land revenue and irrigation revenue are combined.
It is then called a composite rate. This method of assessment is not very
commonly used but still it is in practice in some states of India.
13. PROJECT AREA & METHODOLOGY
LOCATION OF PROJECT AREA :Venkatapuram is a Village in
Renigunta Mandal in Chittoor District of Andhra Pradesh State, India. It
belongs to Rayalaseema region. It is located 79 KM towards North from
District headquarters Chittoor. 7 KM from Renigunta. And the Longitude,
Latitude values are (79.4967, 13.6629)
MAP OF PROJECT AREA :
14. RAINFALL DATA OF AREA:
YEAR 1997 1998 1999 2000 2001 2002 2003 2004 2005
JANUARY 12.2 10.4 6.2 0 0 0 0 0 0
FEBRUARY 22.2 12.4 7.8 1.0 0 0 0 0 0
MARCH 45.9 38.6 35.2 27.2 5.8 2.4 .8 0 0
APRIL 152.2 117.8 72.6 40.4 32.5 27.6 26.4 20.8 19.2
MAY 195 181.9 180 103.7 82.2 75.8 75.6 74.2 50
JUNE 378.8 189.6 180.8 157 101.4 99.2 88.2 87 78.8
JULY 399.5 250 2112 179.7 164.6 163.2 139.4 134.5 123.2
AUGUST 343 250.5 227.4 178.9 169.3 154.7 146.8 138.6 137.8
SEPTEMBER 306.4 270.9 230.1 209.0 198.4 183.6 180.8 143 137.2
OCTOBER 339.6 289.6 288.2 280 272.6 215 198.4 184 176.2
NOVEMBER 360 267.8 238.9 237 220.4 176.8 175.8 173.5 146
DECEMBER 188 176.4 152 122.4 75.2 69.4 65.2 62 48.4
18. ESTIMATION :
Field irrigation requirement (FIR)/ consumptive use (cu) : Data
collected for rice crop
MONTH MONTHLY
TEMPERATURE
0c
MONTHLY % OF DAY
TIME HOURS OF THE
YEAR
USEFULL
RANFALL (CM)
July 32.778 12.76 6.8
August 31 12.55 16.8
September 30 12.2 37.45
October 29 11.833 46.08
November 27 11.5 19.41
f=
𝑝
40
[I.8t + 32]
MONTH T0c P% F
July 32.778 12.76 29.03
August 31 12.55 27.55
September 30 12.2 26.23
October 29 11.833 24.91
November 27 11.5 23.17
∑𝑓 = 130.89
19. Cu= k×∑f = 1.1×130.89 = 143.98 cm
Re = 6.8+16.8+37.45+46.08+19.41 = 126.54 cm
CIR = CU – Re = 143.98-126.54 = 17.44 cm
NIR=CIR (since no water is used for deep percolation)
FIR =
NIR
ŋa
=
17.44
0.7
= 24.91 cm
AMOUNT OF WATER REQUIRED : The amount of water required for irrigation
of rice crop in venkatapuram village is
Volume = Area × delta = 1.3×68.9872 = 89.68 hectare-m = 896833.60 m3
Discharge = area/duty = 68.9872/1216.25 = 0.06 m3/s
Crop Base period, B
(days)
Delta,∆
(m)
Duty
D=
8.64 B
∆
Area
(hectare)
Volume
(m3)
Discharge
(m3/s)
Rice 183 1.3 1216.25 68.9872 896833.60 0.06
20. EVAPOTRANSPIRATION : Evapotranspiration is calculated by penman
method. estimation for rice crop in 2017 is done below
Et =
A.H+ α Ea
A+α
July August September October November Average
54% 60% 67% 72% 80% 67%
Table for Relative Humidity (RH) in 2017
July August September October November Average
8.1 mph 6.9 mph 5.1 mph 4.5 mph 5.6 mph 6.04 mph
Table for wind speed (u) in 2017
α = 0.49 mmhg/0c
A = 1.85 (from table 3)
es =31.81 mmhg (from table 3)
Now,
ea = es × RH = 31.81 ×
67
100
= 21.31 mmhg
u2= u (
2
Z
)1/7 = u = 6.04 mph = 233.29 km/day
Ea = 0.002187(160 + u2) (es – ea)
Ea = 0.002187 (160+233.29) (31.81-21.31) = 9.03 mm/day
21. We know, RA= 14.1, Ø=13.6288, r=0.2, n=12.17, 𝜎=2.01×10-9 mm/day, T= 273+29.96=
302.96 k
H= RA (1-r) (0.29cosØ + 0.55n/N) – α (Tα) 4 (0.56-0.092√ea) (0.10+0.9n/N)
H= 14.1 (1-0.2) (0.29cos13.6288+0.55
12.17
12.1
) -2.01×10-9(302.96)4 (0.56-0.092√21.31)
(0.10+0.9
12.17
12.1
) = 7.04 mmhg/day
Et =
1.85×7.04+0.49×9.03
1.85+0.49
= 7.46 mm of water per month = 1155.79 mm of water/season
DEPTH AND TIME OF IRRIGATION :
Depth of Water stored =
Fc .d .γd
γw
=
0.27×15×0.9
9.81
= 0.37 m
Available moisture depth (dw) =
d .γd
γw
(Fc − wc) =
0.9×15
9.81
(0.27 − 0.13) = 0.19 m
Depth of Irrigation =
d .γd
γw
(Fc − w) =
0.9×15
9.81
(0.27 − 0.14) = 0.18 m
Time to Irrigate Field:
t=
2.778 A ×dw
q
=
2.778×68.9872×0.19
0.06
= 606.88 hours = 25.29 days
22. ASSESSMENT OF IRRIGATION :
Assessment of irrigation water is the revenue that should be paid to the
government by using water from irrigation canals. In venkatapuram village
assessment on area basis is followed that means at the end of the crop period a
demand statement for each farmer are prepared. For failure of crops for reasons
beyond the control of the irrigator or for shortage of water supply, remission may
be given to the farmer.
23. RESULT AND CONCLUSION
Water requirement of Crop is the most important factor governing the loss in crop
production in India. It had been so long that, most of farmer in our country is not
provide with proper irrigation water supply. They mostly depend on Rainfall water, due
to increase in global warming and other adverse effect on environment, rate of Rainfall
is in decreasing rate so that Farmers are in great problem.
Based on the experiment and the data estimated for the irrigation field of
venkatapuram village, Andhra Pradesh in 2017, following conclusion are made.
1. The Field Irrigation Requirement (FIR) of Rice crop for whole crop season is 24.91
cm.
2. The consumptive use of water for rice crop is 143.98 cm.
3. The total volume of water required for irrigating field is 896833.60 m3.
4. The evapotranspiration (Et) is 7.45 mm of water per month and 1155.79 mm of
water per season of rice crop.
5. Depth of water stored in root Zone (d) is 0.37 m.
6. The available moisture depth (dw) is 0.19 m.
7. The depth of irrigation water is 0.18 m.
8. Time to irrigate field is 25.29 days.
9. Assessment on area basis or crop rate basis is followed by the farmer of the
venkatapuram village.
24. It should be concluded that all the data obtained is calculated. We can see that
farmer of this village is largely depended on irrigation water. The soil is clay loam
so that the production of rice crop in this area is very good. But other crops like
maize, tobacco etc. production is not suitable.
FUTURE SCOPE :In future, the production of rice in this area will be
high because new irrigation structure had been constructed in the locality.
And youth of this village are quite focused to continue there ancestor farming
occupation.