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Evaporation
Heat of Reaction
Energy Balance
Mrs Nadia Junaid
Distribution of Water on Earth
• Most of the Earth’s water is in oceans.
• Oceans contain salt water and covers most of the earth’s
surface.
• Of the final 1%, only 4/10 of water comes from rivers, a major
source of the water we use.
Click on the graph to learn more!
Most of Earth’s water is in the oceans, which
cover most of Earth’s surface.
• Liquid water evaporates, turns into water vapor and back into a
liquid when cooled or as a solid if cooled below the freezing point
of water.
• Water vapor in the air moves and can form fog or clouds, and can
fall to Earth as rain, hail, sleet, or snow.
• The amount of fresh water located in rivers, lakes, underground
sources, and glaciers is limited and that its availability can be
extended by recycling and decreasing water use.
Clouds Formation
What is a cloud?
~ It is a thick mass of suspended water drops or
ice crystals
Clouds Identification
• 1. The altitude at which they occur
2. Color
3. Density
4. Shape
5. Degree of cover
FOG
Fog : Clouds at ground level
Evaporation, Condensation and Precipitation:
The main processes of the water cycle
WATER CYCLE
Energy and Phase Changes
Evaporation
• The transformation of a liquid into a gas.
• The sun’s heat raising the temperature of
water and turning it into a gas.
• Water from earth’s rivers, and oceans that is
heated and travels through the air as a gas.
Stages of Evaporation
1. Water is warmed
by the sun
3. Water particles rise as a gas
or vapor
2. As the water
heats, it turns
into a gas.
Condensation
• Water vapor particles rising through the air.
• You can't see it, but air contains a lot of water.
• When air gets cold, the water vapor condenses into
clouds.
• Warm air can hold more water vapor than cold air.
– When warm air holds a lot of water vapor, the air feels sticky
and damp.
• The amount of water in the air is called humidity.
The Stages of Condensation
1. Water vapor particles rising
2. Particles forming groups
3. Water particles grouped to form bonds
Precipitation is…
• …the process by which
water falls back down to
earth as rain, snow, or
hail.
• Depending on the
temperature, water may
fall to earth as:
– liquid (rain),
– semi-solid (snow),
– solid (hail)
Factors affecting evaporation
• evaporation the escape of more energetic
molecules from the surface of a liquid.
• Relate evaporation to the consequent cooling.
• Demonstrate understanding of how
temperature, surface area and air flow over a
surface influence evaporation
Evaporation
Evaporation
Consider a beaker of water at room
temperature
Evaporation
The molecules of water are moving around at
different speeds, some fast, some slow.
speed of
molecule (m/s)
# of molecules at
a particular speed
Average
speed
Evaporation
If a molecule is at the surface, and moving fast
enough, it may escape the liquid. This is called
evaporation.
Freedom!
Evaporation
Since the average speed of the remaining molecules must
now be lower, the temperature of the liquid drops (since
temperature is a measure of the kinetic energy of the
molecules).
Freedom!
Evaporation
Evaporation can thus take place at any
temperature.
Increasing the rate of evaporation
Increasing the
temperature.
Increasing the rate of evaporation
Increasing the
temperature
means that more
molecules are
moving fast
enough to escape.
Increasing the rate of evaporation
Increasing the
surface area
Increasing the rate of evaporation
Increasing the
surface area
means that more
molecules are at
the surface.
Increasing the rate of evaporation
Increasing the air
flow over the
surface
Increasing the rate of evaporation
Increasing the air
flow over the
surface so that
molecules are
carried away
before they can
fall back into the
liquid
Increasing the rate of evaporation
Decreasing the
humidity of the
surrounding
atmosphere
Increasing the rate of evaporation
Decreasing the
humidity of the
surrounding
atmosphere to
stop water
molecules from
the atmosphere
entering the liquid.
Factors Influencing Evaporation
• Energy supply for vaporization
(latent heat)
– Solar radiation
• Transport of vapor away from
evaporative surface
– Wind velocity over surface
– Specific humidity gradient above
surface
• Vegetated surfaces
– Supply of moisture to the surface
– Evapotranspiration (ET)
• Potential Evapotranspiration (PET)
– moisture supply is not limited
nR
E
Net radiation
Evaporation
Air Flow
u
Boiling
• Boiling is a cooling process
• Temperature is 100
degrees C no matter how
much heat we give the
water.
• Water boils as fast as it is
being warmed by heating.
• The steam carries away the
heat.
Boiling Water
• At what temperature does water boil in the
mountains?
Energy in Condensation/Vaporization
• The Heat of Vaporization is 540 calories per
gram of condensed water at 100 degrees.
EVAPORATION
• Definition: Process by which water is changed from the liquid
or solid state into the gaseous state through the transfer of
heat energy (AMERICAN SOCIETY OF CHEMICAL, 1949).
• It occurs when some water molecules attain sufficient kinetic
energy to break through the water surface and escape into
the atmosphere (~ 600 cal needed to evaporate 1 gram of
water).
• Depends on the supply of heat energy and the vapor pressure
gradient (which, in turn, depends on water and air
temperatures, wind, atmospheric pressure, solar radiation,
etc).
Under which of the following conditions will
water evaporate the slowest?
a) Humidity = 95% b) Humidity = 80%
c) Humidity = 30% d) Humidity = 70%
At which of the following ground temperatures will
the WATER evaporate the fastest?
a) 50°C b) 15°C
c) 29°C d) 87°C
Your little sister forgot to turn off the water in the bathroom sink. The
water overflowed and soaked the carpet. You want to dry the carpet
out before your mother gets home. At which level should you turn on
the fan?
a) low b) high
c) medium d) The carpet would dry
out faster without a fan.
Students are investigating whether wind affects the rate at
which the sponge will dry. Which experiment is best to use
in answering their question?
a) b)
c) d)
Each of the following containers hold exactly10
ounces of water. From which container will water
evaporate the fastest?
a) b)
c) d)
Which letter represents evaporation?
In which state is the fog?
a) Melting
b) Freezing
c) Boiling
d) Evaporating
e) Condensing
f) Sublimating
In which state is the moisture on the
bottle?
a) Melting
b) Freezing
c) Boiling
d) Evaporating
e) Condensing
f) Sublimating
In which state is the moisture on the leaf
petals?
a) Melting
b) Freezing
c) Boiling
d) Evaporating
e) Condensing
f) Sublimating
In which state is the water in the tea pot?
a) Melting
b) Freezing
c) Boiling
d) Evaporating
e) Condensing
f) Sublimating
FACTORS affecting Evaporation
Factor 1 - Temperature
The higher the temperature the faster the rate
of evaporation.
Which part will evaporate faster?
A B
Factor 2 - Wind
• The more wind or air circulation the faster the
rate of evaporation.
Which part will evaporate faster?
A B
Factor 3 – Exposed Surface Area
The larger the exposed surface area the faster
the evaporation rate.
The water will evaporate more quickly from the
beaker on the right with the wider opening.
3 inches
1 inch
If each beaker contains 8 ounces of water, which
beaker will evaporate the quickest?
Factor 4 - Humidity
• When humidity (the amount of water vapor in
the air) is high, evaporation is slower.
In which location would laundry hanging
on a line dry the quickest?
A) Desert
Humidity = 30%
B) Nice Day
Humidity =60%
C) Rainy Day
Humidity = 100%
D) Tropics
Humidity = 90%
Heat of REACTION
Thermochemistry
• Thermodynamics is the science of the
relationship between heat and other forms of
energy.
• Thermochemistry is the study of the quantity of
heat absorbed or evolved by chemical reactions.
Energy
• There are three broad concepts of energy:
• Kinetic Energy is the energy associated with an
object by virtue of its motion.
• Potential Energy is the energy an object has by
virtue of its position in a field of force.
• Internal Energy is the sum of the kinetic and
potential energies of the particles making up a
substance.
We will look at each of these in detail.
Energy
• Internal Energy is the energy of the
particles making up a substance.
• The total energy of a system is the sum of its
kinetic energy, potential energy, and internal
energy, U.
UEEE pktot 
Energy
• The Law of Conservation of Energy: Energy may
be converted from one form to another, but the
total quantities of energy remain constant.
The First Law of Thermodynamics:
You can’t get something
from nothing!
Heat of Reaction
• In chemical reactions, heat is often
transferred from the “system” to its
“surroundings,” or vice versa.
• The substance or mixture of substances under
study in which a change occurs is called the
thermodynamic system (or simply system.)
• The surroundings are everything in the vicinity
of the thermodynamic system.
Heat of Reaction
• Heat is defined as the energy that flows
into or out of a system because of a
difference in temperature between the
system and its surroundings.
• Heat flows from a region of higher
temperature to one of lower temperature;
once the temperatures become equal, heat
flow stops.
Heat of Reaction
• Heat is denoted by the symbol q.
– The sign of q is positive if heat is absorbed by
the system.
– The sign of q is negative if heat is evolved by
the system.
• Heat of Reaction is the value of q required to
return a system to the given temperature at
the completion of the reaction.
Heat of Reaction
• An exothermic process is a chemical
reaction or physical change in which heat is
evolved (q is negative).
• An endothermic process is a chemical
reaction or physical change in which heat is
absorbed (q is positive).
Endothermic
and
exothermic.
Heat of Reaction
• Exothermicity
– “out of” a system
Dq < 0
• Endothermicity
– “into” a system
Dq > 0
Energy
System
Surroundings
Energy
System
Surroundings
70
Reaction Conditions
Reaction conditions for a chemical reaction
require
 collisions between reacting molecules
 collisions with sufficient energy to break
the bonds in the reactants
 the breaking of bonds between atoms of
the reactants
 the forming of new bonds to give products
71
Chemical Reactions
In the reaction H2(g) + I2(g) 2HI(g),
 the reactants H2 and I2 collide
 the bonds of H2 and I2 break
 the bonds for HI form
H2 + I2 collision bonds break HI
new bonds form
72
Activation Energy
Activation energy
 is the minimum energy required upon
collision for a reaction to take place
73
Heat of Reaction
The heat of reaction
 is the amount of heat
absorbed or released
during a reaction
 is the difference in the
energy of the reactants
and the products
 Has the symbol ΔH
ΔH = ΔHproducts −
ΔHreactants
74
Exothermic Reactions
In an exothermic reaction,
 the energy of the products is
less than the energy of the
reactants
 heat of reaction is released
 heat is a product
C(s) + O2(g) CO2(g) + 394 kJ
ΔH = –394 kJ/mole (heat released)
75
Endothermic Reactions
In an endothermic reaction,
 heat is absorbed
 the energy of the products
is greater than the energy
of the reactants
 heat is a reactant
N2(g) + O2(g) + 180 kJ 2NO(g)
ΔH = 180 kJ (heat added)
76
Summary
Reaction Energy Heat Sign of
Type Change in Reaction ΔH
Endothermic Heat absorbed Reactant side +
Exothermic Heat released Product side –
ENERGY BALANCE
Law of Conservation of Energy
• The law of conservation of energy states that
energy cannot be created or destroyed, but
only changed from one form to another.
Hess’s Law
• Hess’s Law states that the heat change of a
reaction depends only on the initial and final
states of the reaction and is independent of the
route by which the reaction may occur.
• for a reaction described by a given equation, the
heat of reaction equals the sum of the heats of
formation of the products of the reaction less the
sum of the heats of formation of the reactants of
the reaction.
• ΔHr = ΔHf (products) - ΔHf (reactants)
ENERGY BALANCE
According to law of conservation of energy : it is always remain conserved.
So Energy is balanced
A Problem of energy balance
• Suppose a piece of iron requires 6.70 J of
heat to raise its temperature by one degree
Celsius. The quantity of heat required to
raise the temperature of the piece of iron
from 25.0 oC to 35.0 oC is:
)C0.25C0.35()C/J70.6(TCq ooo
D
J0.67q 
• In above problem, Energy added to the system
is calculated, and energy accumulated by the
system is found by the formula , and overall
energy of the system is conserved.

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Biogeo chemical processes

  • 1. Evaporation Heat of Reaction Energy Balance Mrs Nadia Junaid
  • 2. Distribution of Water on Earth • Most of the Earth’s water is in oceans. • Oceans contain salt water and covers most of the earth’s surface. • Of the final 1%, only 4/10 of water comes from rivers, a major source of the water we use. Click on the graph to learn more!
  • 3. Most of Earth’s water is in the oceans, which cover most of Earth’s surface. • Liquid water evaporates, turns into water vapor and back into a liquid when cooled or as a solid if cooled below the freezing point of water. • Water vapor in the air moves and can form fog or clouds, and can fall to Earth as rain, hail, sleet, or snow. • The amount of fresh water located in rivers, lakes, underground sources, and glaciers is limited and that its availability can be extended by recycling and decreasing water use.
  • 4.
  • 6. What is a cloud? ~ It is a thick mass of suspended water drops or ice crystals
  • 7. Clouds Identification • 1. The altitude at which they occur 2. Color 3. Density 4. Shape 5. Degree of cover
  • 8. FOG
  • 9. Fog : Clouds at ground level
  • 10.
  • 11. Evaporation, Condensation and Precipitation: The main processes of the water cycle
  • 13. Energy and Phase Changes
  • 14.
  • 15. Evaporation • The transformation of a liquid into a gas. • The sun’s heat raising the temperature of water and turning it into a gas. • Water from earth’s rivers, and oceans that is heated and travels through the air as a gas.
  • 16. Stages of Evaporation 1. Water is warmed by the sun 3. Water particles rise as a gas or vapor 2. As the water heats, it turns into a gas.
  • 17. Condensation • Water vapor particles rising through the air. • You can't see it, but air contains a lot of water. • When air gets cold, the water vapor condenses into clouds. • Warm air can hold more water vapor than cold air. – When warm air holds a lot of water vapor, the air feels sticky and damp. • The amount of water in the air is called humidity.
  • 18. The Stages of Condensation 1. Water vapor particles rising 2. Particles forming groups 3. Water particles grouped to form bonds
  • 19. Precipitation is… • …the process by which water falls back down to earth as rain, snow, or hail. • Depending on the temperature, water may fall to earth as: – liquid (rain), – semi-solid (snow), – solid (hail)
  • 20. Factors affecting evaporation • evaporation the escape of more energetic molecules from the surface of a liquid. • Relate evaporation to the consequent cooling. • Demonstrate understanding of how temperature, surface area and air flow over a surface influence evaporation
  • 22. Evaporation Consider a beaker of water at room temperature
  • 23. Evaporation The molecules of water are moving around at different speeds, some fast, some slow. speed of molecule (m/s) # of molecules at a particular speed Average speed
  • 24. Evaporation If a molecule is at the surface, and moving fast enough, it may escape the liquid. This is called evaporation. Freedom!
  • 25. Evaporation Since the average speed of the remaining molecules must now be lower, the temperature of the liquid drops (since temperature is a measure of the kinetic energy of the molecules). Freedom!
  • 26. Evaporation Evaporation can thus take place at any temperature.
  • 27. Increasing the rate of evaporation Increasing the temperature.
  • 28. Increasing the rate of evaporation Increasing the temperature means that more molecules are moving fast enough to escape.
  • 29. Increasing the rate of evaporation Increasing the surface area
  • 30. Increasing the rate of evaporation Increasing the surface area means that more molecules are at the surface.
  • 31. Increasing the rate of evaporation Increasing the air flow over the surface
  • 32. Increasing the rate of evaporation Increasing the air flow over the surface so that molecules are carried away before they can fall back into the liquid
  • 33. Increasing the rate of evaporation Decreasing the humidity of the surrounding atmosphere
  • 34. Increasing the rate of evaporation Decreasing the humidity of the surrounding atmosphere to stop water molecules from the atmosphere entering the liquid.
  • 35. Factors Influencing Evaporation • Energy supply for vaporization (latent heat) – Solar radiation • Transport of vapor away from evaporative surface – Wind velocity over surface – Specific humidity gradient above surface • Vegetated surfaces – Supply of moisture to the surface – Evapotranspiration (ET) • Potential Evapotranspiration (PET) – moisture supply is not limited nR E Net radiation Evaporation Air Flow u
  • 36. Boiling • Boiling is a cooling process • Temperature is 100 degrees C no matter how much heat we give the water. • Water boils as fast as it is being warmed by heating. • The steam carries away the heat.
  • 37. Boiling Water • At what temperature does water boil in the mountains?
  • 38. Energy in Condensation/Vaporization • The Heat of Vaporization is 540 calories per gram of condensed water at 100 degrees.
  • 39. EVAPORATION • Definition: Process by which water is changed from the liquid or solid state into the gaseous state through the transfer of heat energy (AMERICAN SOCIETY OF CHEMICAL, 1949). • It occurs when some water molecules attain sufficient kinetic energy to break through the water surface and escape into the atmosphere (~ 600 cal needed to evaporate 1 gram of water). • Depends on the supply of heat energy and the vapor pressure gradient (which, in turn, depends on water and air temperatures, wind, atmospheric pressure, solar radiation, etc).
  • 40. Under which of the following conditions will water evaporate the slowest? a) Humidity = 95% b) Humidity = 80% c) Humidity = 30% d) Humidity = 70%
  • 41. At which of the following ground temperatures will the WATER evaporate the fastest? a) 50°C b) 15°C c) 29°C d) 87°C
  • 42. Your little sister forgot to turn off the water in the bathroom sink. The water overflowed and soaked the carpet. You want to dry the carpet out before your mother gets home. At which level should you turn on the fan? a) low b) high c) medium d) The carpet would dry out faster without a fan.
  • 43. Students are investigating whether wind affects the rate at which the sponge will dry. Which experiment is best to use in answering their question? a) b) c) d)
  • 44. Each of the following containers hold exactly10 ounces of water. From which container will water evaporate the fastest? a) b) c) d)
  • 45. Which letter represents evaporation?
  • 46. In which state is the fog? a) Melting b) Freezing c) Boiling d) Evaporating e) Condensing f) Sublimating
  • 47. In which state is the moisture on the bottle? a) Melting b) Freezing c) Boiling d) Evaporating e) Condensing f) Sublimating
  • 48. In which state is the moisture on the leaf petals? a) Melting b) Freezing c) Boiling d) Evaporating e) Condensing f) Sublimating
  • 49. In which state is the water in the tea pot? a) Melting b) Freezing c) Boiling d) Evaporating e) Condensing f) Sublimating
  • 51. Factor 1 - Temperature The higher the temperature the faster the rate of evaporation.
  • 52. Which part will evaporate faster? A B
  • 53. Factor 2 - Wind • The more wind or air circulation the faster the rate of evaporation.
  • 54. Which part will evaporate faster? A B
  • 55. Factor 3 – Exposed Surface Area The larger the exposed surface area the faster the evaporation rate. The water will evaporate more quickly from the beaker on the right with the wider opening. 3 inches 1 inch
  • 56. If each beaker contains 8 ounces of water, which beaker will evaporate the quickest?
  • 57. Factor 4 - Humidity • When humidity (the amount of water vapor in the air) is high, evaporation is slower.
  • 58. In which location would laundry hanging on a line dry the quickest? A) Desert Humidity = 30% B) Nice Day Humidity =60% C) Rainy Day Humidity = 100% D) Tropics Humidity = 90%
  • 60. Thermochemistry • Thermodynamics is the science of the relationship between heat and other forms of energy. • Thermochemistry is the study of the quantity of heat absorbed or evolved by chemical reactions.
  • 61. Energy • There are three broad concepts of energy: • Kinetic Energy is the energy associated with an object by virtue of its motion. • Potential Energy is the energy an object has by virtue of its position in a field of force. • Internal Energy is the sum of the kinetic and potential energies of the particles making up a substance. We will look at each of these in detail.
  • 62. Energy • Internal Energy is the energy of the particles making up a substance. • The total energy of a system is the sum of its kinetic energy, potential energy, and internal energy, U. UEEE pktot 
  • 63. Energy • The Law of Conservation of Energy: Energy may be converted from one form to another, but the total quantities of energy remain constant. The First Law of Thermodynamics: You can’t get something from nothing!
  • 64. Heat of Reaction • In chemical reactions, heat is often transferred from the “system” to its “surroundings,” or vice versa. • The substance or mixture of substances under study in which a change occurs is called the thermodynamic system (or simply system.) • The surroundings are everything in the vicinity of the thermodynamic system.
  • 65. Heat of Reaction • Heat is defined as the energy that flows into or out of a system because of a difference in temperature between the system and its surroundings. • Heat flows from a region of higher temperature to one of lower temperature; once the temperatures become equal, heat flow stops.
  • 66. Heat of Reaction • Heat is denoted by the symbol q. – The sign of q is positive if heat is absorbed by the system. – The sign of q is negative if heat is evolved by the system. • Heat of Reaction is the value of q required to return a system to the given temperature at the completion of the reaction.
  • 67. Heat of Reaction • An exothermic process is a chemical reaction or physical change in which heat is evolved (q is negative). • An endothermic process is a chemical reaction or physical change in which heat is absorbed (q is positive).
  • 69. Heat of Reaction • Exothermicity – “out of” a system Dq < 0 • Endothermicity – “into” a system Dq > 0 Energy System Surroundings Energy System Surroundings
  • 70. 70 Reaction Conditions Reaction conditions for a chemical reaction require  collisions between reacting molecules  collisions with sufficient energy to break the bonds in the reactants  the breaking of bonds between atoms of the reactants  the forming of new bonds to give products
  • 71. 71 Chemical Reactions In the reaction H2(g) + I2(g) 2HI(g),  the reactants H2 and I2 collide  the bonds of H2 and I2 break  the bonds for HI form H2 + I2 collision bonds break HI new bonds form
  • 72. 72 Activation Energy Activation energy  is the minimum energy required upon collision for a reaction to take place
  • 73. 73 Heat of Reaction The heat of reaction  is the amount of heat absorbed or released during a reaction  is the difference in the energy of the reactants and the products  Has the symbol ΔH ΔH = ΔHproducts − ΔHreactants
  • 74. 74 Exothermic Reactions In an exothermic reaction,  the energy of the products is less than the energy of the reactants  heat of reaction is released  heat is a product C(s) + O2(g) CO2(g) + 394 kJ ΔH = –394 kJ/mole (heat released)
  • 75. 75 Endothermic Reactions In an endothermic reaction,  heat is absorbed  the energy of the products is greater than the energy of the reactants  heat is a reactant N2(g) + O2(g) + 180 kJ 2NO(g) ΔH = 180 kJ (heat added)
  • 76. 76 Summary Reaction Energy Heat Sign of Type Change in Reaction ΔH Endothermic Heat absorbed Reactant side + Exothermic Heat released Product side –
  • 78. Law of Conservation of Energy • The law of conservation of energy states that energy cannot be created or destroyed, but only changed from one form to another.
  • 79. Hess’s Law • Hess’s Law states that the heat change of a reaction depends only on the initial and final states of the reaction and is independent of the route by which the reaction may occur. • for a reaction described by a given equation, the heat of reaction equals the sum of the heats of formation of the products of the reaction less the sum of the heats of formation of the reactants of the reaction. • ΔHr = ΔHf (products) - ΔHf (reactants)
  • 80. ENERGY BALANCE According to law of conservation of energy : it is always remain conserved. So Energy is balanced
  • 81. A Problem of energy balance • Suppose a piece of iron requires 6.70 J of heat to raise its temperature by one degree Celsius. The quantity of heat required to raise the temperature of the piece of iron from 25.0 oC to 35.0 oC is: )C0.25C0.35()C/J70.6(TCq ooo D J0.67q 
  • 82. • In above problem, Energy added to the system is calculated, and energy accumulated by the system is found by the formula , and overall energy of the system is conserved.