EVAPORATION
Submitted to :
Dr. Aniruddha D Ghare
Professor, Civil Engineering
VNIT Nagpur
Submitted by:
Gaurav Gautam
MT21WRE012
Visvesvaraya National Institute of Technology , Nagpur
APPLIED SURFACE HYDROLOGY
CONTENT
• Atmometer
i. Design
ii. Types
iii. Use and Maintenance
iv. Advantages & Disadvantages
• Pan Evaporation
i. Observation on pan
ii. Pan coefficient
iii. Factors affecting Pan coefficient
iv. Types of pan
v. Numerical Problem
ATMOMETER
• An atmometer is a scientific instrument used for measuring the rate of water evaporation from
a wet surface to the atmosphere .
• This is a device that can give direct measurement of evaporation .
• Atmometers are mainly used by farmers and growers to measure evapotranspiration rates of
crops at any field location .
• Atmometers are not common because of there small size and also they do not have sufficient
exposure .
• The rate of evaporation observed from an atmometers is on higher side than that from any other
method .
DESIGN
• Atmometer basically consists of a wet , porous ceramic cup
mounted on the top a cylindrical water reservoir .
• The ceramic cup is covered with a green fabric that stimulates the
canopy of a crop .
• The reservoir is filled with distilled water that evaporates out of the
ceramic cup and is pulled through a suction tube that extends to the
bottom of the reservoir .
• Underneath the fabric , the ceramic cup is covered by the special
membrane that keeps rain water from seeping into the ceramic cup.
• A rigid wire extending from the top keep birds from perching on top
of the gauge .
Source :- Paper Atmometer – based irrigation scheduling system for drip – irrigated onion (Allium
cepa L.)
The following normal types of atmometers :-
1) Livingstone atmometer
• It consists of 50 mm diameter spherical surface of 2.5 mm thick
porous material .
• The bottle is filled with distilled water that is supplied
continuously to the porous bulb .
• The loss of water from the bottle is due to the evaporation .
2) Piche atmometer
• It consists of graduated glass tube of 15 mm diameter and 300 mm in length .
• It is filled with water and covered with filter paper .
• The tube is kept in an inverted position so that there is a continuous supply of
water to the filter paper .
• The loss of water from the glass tube is the loss due to evaporation .
USE and MAINTENANCE
• An atmometer is fairly easy to install and use .
• It is usually mounted on a wooden post about 1000 mm above the ground in an area
representative of the weather and field conditions .
• The plate of the atmometer should be placed in direct sunlight so the evaporation rates are not
affected .
• It should not be placed near tall trees or buildings, as they can affect the amount of exposure
that the atmometer has to environmental factors, which affect evapotranspiration rates .
• To measure the amount of water that has evaporated, calculate the change in water level on the
gauge by subtracting the final water level from the initial water level.
ADVANTAGES
• Low cost
• Easy operation
• Convenience
• No computer or power required
DISADVANTAGES
• Bad weather can occur damage to
the device
• Constant need to refill water supply
• Gauge must be read manually (only
on manual model)
PAN EVAPORATION
• The estimation of observation can be done by taking actual evaporation from pan and
correlating these result with reservoir .
• Pan :- A pan is a metal container , square or circular , and of uniform cross-section . Normally,
it is circular having diameter ranging from 300 – 1500 mm .
• The pan is filled with water and the loss of water from this pan in a specific period is measured.
• The rate of evaporation observed here is correlated to the evaporation from reservoir .
OBSERVATIONS ON PAN
• In the first method , the pan is filled up to a specific level and the loss of water is calculated by
observing the level of water over a specified time. Knowing the cross-section of the pan and the
reduction in the water level , the loss due to evaporation over a specified time can be calculated .
The water levels in the pan are taken accurately by a hook gauge .
• In the second method , the pan is filled up to specific level . This level is maintained constant by
adding water to the pan periodically to meet the evaporation loss . The loss due to evaporation over
that period is the quantity of water added to the pan to maintain a constant level .
PAN COEFFICIENT
• The observation from a pan are extrapolated to a reservoir by using a pan coefficient .
• It may be defined as follows :
Pan coefficient = Rate of Evaporation from the reservoir
Rate of Evaporation from the pan
• The value of pan coefficient is always less than 1.0 ( because in case of a pan , a very small area
is exposed to atmosphere and secondly , the metal container absorb more energy and in turn is
utilized for evaporation .
• It is dimensionless .
Factors Affecting Pan coefficient
The following factor affect the pan coefficient :
• Type of Pan ( Diameter , Depth of water , Height of rim above
water level , colour , material )
• Pan Environment ( Location )
• Climate ( Humidity & windspeed ) .
TYPES OF PAN
• Class A Evaporation Pan
• ISI Standard Pan
• Colorado Sunken Pan
• US Geological Survey Floating Pan
Class A Evaporation Pan
• It is the standard pan of 1210 mm diameter and 255 mm depth used by the US weather Bureau and
is known as Class A Land Pan .
• The depth of water is maintained between 18 cm and 20
cm. The pan is normally made up of unpainted galvanised
iron sheet .
• Monel metal is used where corrosion is problem .
• The pan is placed on the wooden platform of 15 cm
height above the ground to allow free circulation of air
below the pan .
• Evaporation measurement are made by measuring the depth of water with a hook gauge in stilling
well .
ISI Standard Pan
• This pan evaporimeter specified by IS:5973-1970 , also
known as Modified Class A Pan .
• Pan of 1220 mm in diameter with 255 mm of depth .
• Pan is made up of copper sheet of 0.9 mm thickness , tinned
inside and painted white outside .
• The pan is placed is placed on the square wooden platform
of width 1225 mm height 100 mm above ground level to
allow free air circulation below the pan
• A fixed point gauge indicates the level of water .
Colorado Sunken Pan
• This pan , having 920 mm square side and 460 mm deep and it is made up of unpainted
galvanised iron sheet and buried into the ground with 50mm of the top .
• The chief advantage of the sunken pan is that radiation and
aerodynamic characteristics are similar to those of a lake .
• However, it has the following disadvantages also :
i. Difficult to detect leaks
ii. Extra care is needed to keep the surrounding area free
from tall grass, dust ,etc .
iii. Expensive to install .
US Geological Survey Floating Pan
• A square pan of 900 mm sides and 450 mm deep .
• It is supported by drum floats in the middle of the raft of size 4.25m 4.87 m ,
• It is set to float in a lake with a view to simulate the characteristics of large body of water .
• Water level in the pan is maintained at the same level as that in the lake , leaving a rim of 75 mm .
S.NO TYPES OF PAN VALUE RANGE
1. Class A Land Pan 0.70 0.60-0.80
2. ISI Pan ( Modified Class A ) 0.80 0.65-1.10
3. Colorado Sunken Pan 0.78 075-0.86
4. USGS Floating Pan 0.80 0.70-0.82
Value of Pan Coefficient
Ques : A Class A pan was setup adjacent to a lake . The depth of water in a pan at the
beginning of a certain week was 195 mm . In that week there was a rainfall of 45 mm and
15 mm of water was removed from the pan to keep the water level within the specified
range .
If the depth of water in the end of week was 190 mm .Calculate the pan Evaporation using a
suitable Pan coefficient .
Estimate Lake evaporation in that week .
Soln :
• Initial Reading = 195 mm
• Rainfall = 45 mm
• Removed Water = 15 mm
• Cp for Class A Pan = 0.7
• Total Water in the pan = 195+45 = 240 mm
• Water Remaining After removal = 240-15 =225 mm
• Water Evaporated = 225 -190 =35 mm
• Lake Evaporation = Cp × Pan Evaporation
= 0.7 × 35 = 24.5 mm
References :
• Elementary Engineering Hydrology: By Deodar .
• Elementary Hydrology: By K Subramanya .
• Google .
THANK YOU

ATMOMETER AND PAN EVAPORATION

  • 1.
    EVAPORATION Submitted to : Dr.Aniruddha D Ghare Professor, Civil Engineering VNIT Nagpur Submitted by: Gaurav Gautam MT21WRE012 Visvesvaraya National Institute of Technology , Nagpur APPLIED SURFACE HYDROLOGY
  • 2.
    CONTENT • Atmometer i. Design ii.Types iii. Use and Maintenance iv. Advantages & Disadvantages • Pan Evaporation i. Observation on pan ii. Pan coefficient iii. Factors affecting Pan coefficient iv. Types of pan v. Numerical Problem
  • 3.
    ATMOMETER • An atmometeris a scientific instrument used for measuring the rate of water evaporation from a wet surface to the atmosphere . • This is a device that can give direct measurement of evaporation . • Atmometers are mainly used by farmers and growers to measure evapotranspiration rates of crops at any field location . • Atmometers are not common because of there small size and also they do not have sufficient exposure . • The rate of evaporation observed from an atmometers is on higher side than that from any other method .
  • 4.
    DESIGN • Atmometer basicallyconsists of a wet , porous ceramic cup mounted on the top a cylindrical water reservoir . • The ceramic cup is covered with a green fabric that stimulates the canopy of a crop . • The reservoir is filled with distilled water that evaporates out of the ceramic cup and is pulled through a suction tube that extends to the bottom of the reservoir . • Underneath the fabric , the ceramic cup is covered by the special membrane that keeps rain water from seeping into the ceramic cup. • A rigid wire extending from the top keep birds from perching on top of the gauge . Source :- Paper Atmometer – based irrigation scheduling system for drip – irrigated onion (Allium cepa L.)
  • 5.
    The following normaltypes of atmometers :- 1) Livingstone atmometer • It consists of 50 mm diameter spherical surface of 2.5 mm thick porous material . • The bottle is filled with distilled water that is supplied continuously to the porous bulb . • The loss of water from the bottle is due to the evaporation .
  • 6.
    2) Piche atmometer •It consists of graduated glass tube of 15 mm diameter and 300 mm in length . • It is filled with water and covered with filter paper . • The tube is kept in an inverted position so that there is a continuous supply of water to the filter paper . • The loss of water from the glass tube is the loss due to evaporation .
  • 7.
    USE and MAINTENANCE •An atmometer is fairly easy to install and use . • It is usually mounted on a wooden post about 1000 mm above the ground in an area representative of the weather and field conditions . • The plate of the atmometer should be placed in direct sunlight so the evaporation rates are not affected . • It should not be placed near tall trees or buildings, as they can affect the amount of exposure that the atmometer has to environmental factors, which affect evapotranspiration rates . • To measure the amount of water that has evaporated, calculate the change in water level on the gauge by subtracting the final water level from the initial water level.
  • 8.
    ADVANTAGES • Low cost •Easy operation • Convenience • No computer or power required DISADVANTAGES • Bad weather can occur damage to the device • Constant need to refill water supply • Gauge must be read manually (only on manual model)
  • 9.
    PAN EVAPORATION • Theestimation of observation can be done by taking actual evaporation from pan and correlating these result with reservoir . • Pan :- A pan is a metal container , square or circular , and of uniform cross-section . Normally, it is circular having diameter ranging from 300 – 1500 mm . • The pan is filled with water and the loss of water from this pan in a specific period is measured. • The rate of evaporation observed here is correlated to the evaporation from reservoir .
  • 10.
    OBSERVATIONS ON PAN •In the first method , the pan is filled up to a specific level and the loss of water is calculated by observing the level of water over a specified time. Knowing the cross-section of the pan and the reduction in the water level , the loss due to evaporation over a specified time can be calculated . The water levels in the pan are taken accurately by a hook gauge . • In the second method , the pan is filled up to specific level . This level is maintained constant by adding water to the pan periodically to meet the evaporation loss . The loss due to evaporation over that period is the quantity of water added to the pan to maintain a constant level .
  • 11.
    PAN COEFFICIENT • Theobservation from a pan are extrapolated to a reservoir by using a pan coefficient . • It may be defined as follows : Pan coefficient = Rate of Evaporation from the reservoir Rate of Evaporation from the pan • The value of pan coefficient is always less than 1.0 ( because in case of a pan , a very small area is exposed to atmosphere and secondly , the metal container absorb more energy and in turn is utilized for evaporation . • It is dimensionless .
  • 12.
    Factors Affecting Pancoefficient The following factor affect the pan coefficient : • Type of Pan ( Diameter , Depth of water , Height of rim above water level , colour , material ) • Pan Environment ( Location ) • Climate ( Humidity & windspeed ) .
  • 13.
    TYPES OF PAN •Class A Evaporation Pan • ISI Standard Pan • Colorado Sunken Pan • US Geological Survey Floating Pan
  • 14.
    Class A EvaporationPan • It is the standard pan of 1210 mm diameter and 255 mm depth used by the US weather Bureau and is known as Class A Land Pan . • The depth of water is maintained between 18 cm and 20 cm. The pan is normally made up of unpainted galvanised iron sheet . • Monel metal is used where corrosion is problem . • The pan is placed on the wooden platform of 15 cm height above the ground to allow free circulation of air below the pan . • Evaporation measurement are made by measuring the depth of water with a hook gauge in stilling well .
  • 15.
    ISI Standard Pan •This pan evaporimeter specified by IS:5973-1970 , also known as Modified Class A Pan . • Pan of 1220 mm in diameter with 255 mm of depth . • Pan is made up of copper sheet of 0.9 mm thickness , tinned inside and painted white outside . • The pan is placed is placed on the square wooden platform of width 1225 mm height 100 mm above ground level to allow free air circulation below the pan • A fixed point gauge indicates the level of water .
  • 16.
    Colorado Sunken Pan •This pan , having 920 mm square side and 460 mm deep and it is made up of unpainted galvanised iron sheet and buried into the ground with 50mm of the top . • The chief advantage of the sunken pan is that radiation and aerodynamic characteristics are similar to those of a lake . • However, it has the following disadvantages also : i. Difficult to detect leaks ii. Extra care is needed to keep the surrounding area free from tall grass, dust ,etc . iii. Expensive to install .
  • 17.
    US Geological SurveyFloating Pan • A square pan of 900 mm sides and 450 mm deep . • It is supported by drum floats in the middle of the raft of size 4.25m 4.87 m , • It is set to float in a lake with a view to simulate the characteristics of large body of water . • Water level in the pan is maintained at the same level as that in the lake , leaving a rim of 75 mm .
  • 18.
    S.NO TYPES OFPAN VALUE RANGE 1. Class A Land Pan 0.70 0.60-0.80 2. ISI Pan ( Modified Class A ) 0.80 0.65-1.10 3. Colorado Sunken Pan 0.78 075-0.86 4. USGS Floating Pan 0.80 0.70-0.82 Value of Pan Coefficient
  • 19.
    Ques : AClass A pan was setup adjacent to a lake . The depth of water in a pan at the beginning of a certain week was 195 mm . In that week there was a rainfall of 45 mm and 15 mm of water was removed from the pan to keep the water level within the specified range . If the depth of water in the end of week was 190 mm .Calculate the pan Evaporation using a suitable Pan coefficient . Estimate Lake evaporation in that week .
  • 20.
    Soln : • InitialReading = 195 mm • Rainfall = 45 mm • Removed Water = 15 mm • Cp for Class A Pan = 0.7 • Total Water in the pan = 195+45 = 240 mm • Water Remaining After removal = 240-15 =225 mm • Water Evaporated = 225 -190 =35 mm • Lake Evaporation = Cp × Pan Evaporation = 0.7 × 35 = 24.5 mm
  • 21.
    References : • ElementaryEngineering Hydrology: By Deodar . • Elementary Hydrology: By K Subramanya . • Google .
  • 22.