Here we want to vaporize water at room temperature, which will require more heat than at "100^\u2218C" .
Heat flow is a path function, so we can separate this into specific steps. All of this is done at constant pressure, so the heat flow is equal to the enthalpy, a state function, and the order of these steps doesn't matter.
We set a "boiling point" at "25^\u2218C", and thus have two steps:
1. Heat from "10^\u2218C" to "25^\u2218C"
2. Vaporize at "25^\u2218C"
Step 1 would be a simple heating at constant pressure:
"q_1=mC_P\u0394T"
where
m is mass in g ,
"C_P" is the specific heat capacity at constant atmospheric pressure in
"J\/g^\u2218C"
ΔT is the change in temperature until the phase change temperature.
In this case we specify "T_f=25^\u2218C"
"\\implies q_1 =50*4.184*(25-10)"
"q_1=3138 J=3.138kJ"
Step 2 would be vaporization at constant pressure again, but at a CONSTANT, lower temperature than usual.Recall that
"q=\u0394H"
at constant pressure (provided they have the same units).
Thus, we just have:
"q_2=n\u0394H_{vap}T"
where,
n is number of moles of water
"\\Delta H_{vap}" is heat of vaporization in "kJ\/mol"
T is the temperature at which this phase change occurs.
"\\implies q_2=(50\/18)*(44)*(25)"
"q_2=3055.555kJ"
"\u2206H =q_1+q_2"
"\u2206H=3.138+3055.555"
"\u2206H=3058.693kJ" (Answer)
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