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BELLWORK‐
heat
flow
in
pool

  When
you
enter
a
swimming
 pool,
the
water
may
feel
quite
  cold.
ABer
a
while,
though,
your
body
“gets
used
to
it,”
and
  the
water
no
longer
feels
so
cold.
Use
the
concept
of
heat
to
    explain
what
is
going
on.
The specific heat capacity (c) of any
substance is the amount of heat
required to raise the temperature of
1gram of that substance by 1°C.


• Every substance has its own
  specific heat.
Water has a high specific heat.
c= 4.184 J/(g·°C)
Water can absorb or release a
lot of heat before changing
temperature
The heat absorbed during a change in
 temperature is calculated using the
 equation



         Specific   Mass of    Change
  Heat
         heat       sample     in temp
  (J)
         capacity   (g)        (°C)
         J/(g·°C)
                     ΔT= Tfinal-Tinitial
PracIce
How
much
energy
is
required
to
raise
50g
   of
water
from
25°C
to
40°C?




q
=
c

m

ΔT





q
=
unknown




c
=
4.18J/(g°C)
for
water




m
=
50g




ΔT
=
15°C          q = 4.18 x 50 x 15
                         = 3135 J of energy
∆Hfus = the
quanIty
of
heat
absorbed

             during
melIng
   


=
the
quanIty
of
heat
released

             during
freezing.
For water
H2O(s)  H2O(l)    ∆Hfus = 6.01kJ/mol


H2O(l)  H2O(s)   ∆Hfus = -6.01kJ/mol
How
many
grams
of
ice
at
0°C
will
melt
       if
2.25kJ
of
heat
are
added?
  Known
  • iniIal
and
final
temps
are
0
°C
  • 
ΔHfus
=

6.01kJ/mol
  • 
ΔH
=
2.25kJ

2.25 kJ x     1mol = 0.374 moles would
            6.01kJ      be melted
How
much
energy
is
needed
to
melt
50g
of
ice?
  Known                      The heat of
  • ΔHfus
=

6.01kJ/mol      fusion is PER
  • 50g                      MOLE so
                             convert grams
                             to moles

50g
H2O


x





1mole




 2.8 moles x 6.01 kJ
                        =
          







18g                   1mole

                              =16.8 kJ
The
quanIty
of
heat
absorbed
by
a
 evaporaIng
liquid
is
exactly
the
same
as
 the
quanIty
of
heat
released
when
the
 vapor
condenses
=
∆Hvap

 For water
 H2O(l)  H2O(g)     ∆Hvap = 40.7kJ/mol


 H2O(g)  H2O(l)      ∆Hvap= -40.7kJ/mol
Phase
change
occurs
at
                    a
specific
temperature
                    (aka
the
melIng
point
                    and
boiling
point)


Temperature
is
constant
during
a
phase
change
Temperature
is
constant
during
a
phase
change


  During
a
phase
change
heat
is
  used
to
overcome
  intermolecular
a`racIons.
The
ΔHvap
is
always
                         larger
than
ΔHfus



∆Hfus

is
the
energy
required
to
overcome
some

  intermolecular
a`racIons.

∆Hvap

is
the
energy
required
to
overcome
all
  intermolecular
a`racIons.
IN YOUR NOTES--
Include a labeled drawing of
the water curve and all of
the notes in black and red
on the slides to follow.
To
calculate
energy
changes
(ΔH)
for
a
state
change
     




moles
x
ΔHfus





OR





moles
x
ΔHvap
To
calculate
energy
required
to
increase
or
decrease
          temperature
within
a
single
state
                    q=
c
m
ΔT

                                               




Use
                                               




the
                                               specific
                              Use
the          heat
of
                              specific
heat       Energy
                                               steam
                              of
liquid
                              water

            Use
the
            specific
heat
            of
ice
To
calculate
the
energy
change
over
more
than
one
secIon
of
the
curve…
     Calculate
the
energy
for
each
step
and
add
them
together.
Calculate
the
ΔH
associated
with
changing
100g
of
steam
at
125°C
to
ice
at
‐50
°C.

                                           125°C




              1.Determine
if
a
phase
change
occurs
                within
the
temperature
range.
                • water
will
condense
at
100°C
                • water
will
freeze
at
0
°C
      ‐50°C
Calculate
the
ΔH
associated
with
changing
100g
of
steam
at
125°C
to
ice
at
‐50
°C.

                                         125°C



              2.
Split
problem
into
steps.
                    125
°C
steam

100
°C
steam
                    steam

water
                    100
°C
water

0
°C
water
      ‐50°C         water

ice
                    0
°C
ice

‐50
°C
ice
3.
Calculate
the
enthalpy
change
for
each
step.
      125
°C
steam

100
°C
steam
  q
=
1.89 J/(g°C)
x
100g
x
‐25°C
=
‐4725J
     steam

water
  100g
x
1
mol/18g
=
5.55mol
x
40.7kJ/mol
=
‐226kJ
      100
°C
water

0
°C
water
  q
=
4.18 J/(g°C)
x
100g
x
‐100°C
=
‐41,800J
     water

ice
  5.55mol
x
6.01
kJ/mol
=
‐33.4kJ
      0
°C
ice

‐50
°C
ice
  q
=
2.10 J/(g°C)
x
100g
x
‐50°C
=
‐10,500J
4.
Add
the
values
for
each
step
to
get

 the
total
energy
change

  





‐4725J     =
‐4.725
kJ
+

 


‐226kJ
+



‐41,800J      =
‐41.8
kJ
+








‐33.4kJ
+



‐10,500J      =
‐10.5
kJ
Whoops!
The
units
aren’t
the
same!!
4.
Add
the
values
for
each
step
to
get

    the
total
energy
change
            



‐4.725
kJ
    +

 ‐226







kJ
                           The
total
enthalpy
    +








‐41.8




kJ
                           change
and
the
    +








‐33.4




kJ
                           changes
in
each
step
    +








‐10.5




kJ
                           are
all
negaIve
ΔHtotal
=
‐316.4
kJ        values
because
                           cooling
water
is
an
                           exothermic
process
EXOTHERMIC STATE CHANGES
 Heat comes out of substance(system)
 ∆H is negative
 Happens in a freezer
 Freezing(solidification) & condensation

ENDOTHERMIC STATE CHANGES
 Heat goes into substance
 ∆H is positive
 Happens on a stove
 Melting(fusion), vaporization, sublimation
The
insulated
device
used
to
measure
heat
changes
in
chemical
or
physical
processes
is
called
a
calorimeter.

                     qwater = - qrxn
                     The heat change for
                     the water in the
                     calorimeter is equal
                     to the heat change
                     of the reaction but
                     opposite in sign.
CalculaIons
for
Honors
Only
Lecture 17b- Water Curve Calcs
Lecture 17b- Water Curve Calcs
Lecture 17b- Water Curve Calcs

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Lecture 17b- Water Curve Calcs