Classical Definition of the First Law of Thermodynamics
The classical statement of the first law is foundational for closed systems:
For a closed system, the cyclic integral of heat transfer is equal to the cyclic integral of work.
Key Concepts
- Closed system: Permits energy transfer across boundaries but no mass transfer
- Cyclic integral: An integral evaluated for a thermodynamic cycle
For a deeper understanding of energy transfers in such systems, see Understanding Internal Energy: Heat and Work in Thermodynamics.
Understanding the Thermodynamic Cycle
- A thermodynamic cycle occurs when all mechanical and thermodynamic properties return to their starting point
- Visualized on a P-V diagram as a closed loop from state 1 back to state 1
- Real-world example: Reciprocating engine cycles (intake → compression → power → exhaust, repeating)
Path Integrals in Cycles
The cyclic integral is evaluated as a sum of path segments:
- Heat transfer: ∫12 δQ + ∫23 δQ + ... + ∫n1 δQ
- Work: ∫12 δW + ∫23 δW + ... + ∫n1 δW
- The classical first law states: ∮ δQ = ∮ δW
Demonstration: Path Independence of Energy
Using a simple two-state system (states 1 and 2) with three possible paths (A, B, C):
Cycle A-B
- ∫12 δQ_A + ∫21 δQ_B = ∫12 δW_A + ∫21 δW_B
Cycle A-C
- ∫12 δQ_A + ∫21 δQ_C = ∫12 δW_A + ∫21 δW_C
Key Result
Subtracting these equations eliminates the A path components, leaving:
- ∫21 δQ_B - ∫21 δQ_C = ∫21 δW_B - ∫21 δW_C
- This simplifies to: (δQ - δW) on path B = (δQ - δW) on path C
Critical Conclusion: The quantity (δQ - δW) is independent of path and equals a constant, the change in energy level between the two states (dE). To see this principle applied in engines and other devices, check out Understanding Thermodynamics: A Comprehensive Overview.
Connecting Classical and Pragmatic Approaches
| Classical Statement | Derived Relationship | |----------------|---------------------| | ∮ δQ = ∮ δW | δQ - δW = dE (independent of path) |
Important Distinctions
- ∫ δW = amount of work, not W2 - W1 (W2 - W1 has no meaning)
- ∫ δQ = amount of heat, not Q2 - Q1 (Q2 - Q1 has no meaning)
- ∫ dE = change in energy level (E2 - E1)
- Heat and work are path quantities; energy is a state property
For more details on energy as a state function, see Understanding the First Law of Thermodynamics: Energy Conversion Explained.
Practical Forms of the First Law
-
Energy balance form (convention: heat in positive, work out positive):
Q - W = ΔE = ΔU + ΔKE + ΔPE (units: Joules)
-
Rate form (time derivative):
Q̇ - Ẇ = dE/dt
Most practical form for engineering analysis
-
Specific form (per unit mass):
q12 - w12 = e2 - e1 (units: kJ/kg)
Solve for specific values, then multiply by total mass
Explore these forms and their applications further in Complete Thermodynamics & Thermochemistry Concepts Explained.
Summary Checklist
- [ ] Classical first law: ∮ δQ = ∮ δW for closed systems
- [ ] Cyclic integral = sum of path integrals around a thermodynamic cycle
- [ ] Energy change (dE) is path-independent
- [ ] Heat and work are amounts, not changes
- [ ] Practical equation: Q - W = ΔE (or Q̇ - Ẇ = dE/dt)
For a recap of closed vs. isolated systems, see First Law of Thermodynamics: Closed & Isolated Systems Explained with Examples.
we've already taken a pragmatic approach to coming up with a statement of the first law of thermodynamics
if you recall we came up with a statement for an isolated system and for a closed system that was in
terms of the works and heat transfer and the change in energy before we start doing examples using the first law of
thermodynamics i want to go back to the very classical definition of the first law
so the classical definition is very simply for a closed system the cyclic integral of heat transfer is
equal to the cyclic integral of work now a closed system we understand a closed system is
a system that permits the transfer of energy across the boundaries but not the passage of mass
so the other piece we have to understand is what is a cyclic integral so to demonstrate what a cyclic integral
is i've drawn this very simple diagram and i've drawn a point one and a path with a whole bunch of numbers here
a cyclic integral is an integral evaluated for a thermodynamic cycle so this is interesting so cyclic
integral we've got that linked now now we've introduced another term the thermodynamic cycle
so a thermodynamic cycle is one where the mechanical and thermodynamic properties return to their
starting point so this diagram demonstrates or illustrates what a thermodynamic cycle
is so we've got this point one on a pv diagram and i've indicated the path by the little arrow and it just
follows the path and comes back to the beginning okay something like a reciprocating
engine is a great example of a cycle that keeps returning to where it starts right it goes intake compression power
exhaust intake compression power exhaust so it keeps repeating itself so
this isn't really a foreign concept to anybody now how do we actually do the evaluation
well when i say um uh it's an integral evaluated across the cycle that means that it's got to be a path
integral and in calculus you you define that you're looking at a path integral by
putting this little path symbol on the integral so the path integral of the heat transfer
is simply a sum of all of the segments so the the integral not the path but the
integral from one to two plus the integral from two to three and on and on and on until we're
at the integral from n back to one which is the last one and the path integral of the work across
the same process is one to two of the work two to three of the work
and on and on all the way to n to one that gets us back to the starting point so what the first law of thermodynamics
tells us the classical statement is that these are the two integrals we're interested in
and the path integral of heat transfer is equal to the path integral of the work so the path
integrals are analogous to the cyclic integrals so this is the classical statement of the
first law so the next thing we're going to do is show how we get back to that other
statement we had by starting with this statement of the first law of thermodynamics
let's do this evaluation on a very simple system so i'm drawing another pv diagram between two states
one and two and i've got three different paths that can be taken to go from state one to
state two or vice versa so path a leads from one to two and then paths b
or c lead back to path one so either root a b or a ac is a thermodynamic cycle so as long as
we take the cyclic integrals we should have you know a definition of the first law so let's look at cycle a b
cycle a b is um the integral of heat a plus the integral of heat b is equal to
the integral of work a the integral of work b cyclic integral heat transfer cyclic
integral work it's just the segments of the complete path added up
now let's look at cycle ac same thing integral 1 to 2 on path a but this time integral 2 1 on path c for heat transfer
same thing for work one two on a two one on path c now if we subtract these two statements
the a's all disappear because q a q a w a w a both from one to two all gone so the only thing that's left
is integrals from two to one along paths b and c so the integral of heat transfer b
minus e transfer c because we're subtracting is equal to the work b minus the work c
we can rearrange that and put everything from path b on the left everything from path c on the right
everything is evaluated across the same uh well from the same two states two to one
and so because these integrals are equal it also means that the integrands must be equal
if the integration across two states of an integral is the same if they're equivalent then
it has to mean that there's equivalence between the integrands so that means that we can say that this
del q minus del w on path b is equal to del q minus del w on path c and this is a constant because we could
have done any number of other paths from two to one we would have got the same thing we have a whole list of these
and what the they equal is a constant and this constant is the difference in the energy level
from state one to state two or in this case two to one okay so this is a very important
statement we've used the classical definition of the first law we've conducted the cyclic integral
we've evaluated them for these three are these two different possible thermodynamic cycles
and we've come up with this statement that these quantities independent of the path are a constant
as long as you're working between the same two states and that's equal to d e
so just to clean up the connection between the classical statement of the first law
and the pragmatic approach that we use to to develop the first law uh we have the cyclic integral of work
equals the cyclic integral of heat transfer classical definition we've shown that
um if you conduct or evaluate the cyclic integrals on a thermodynamic cycle that there is equivalence
and the difference between you know the different types of paths is simply equal to the change in the
level of energy between the two states we've shown that now just a note and i've already
mentioned this in a previous lecture you've got to keep in mind
that the integral of del w is an amount of work it's not w2 minus w1
whereas if you did the integral from one to two of d e or du or dh or anything else
then it is a change in the level of energy or or whatever other quantity the
distinction though with heat and mass transfer is that amounts of heat and amounts of work
result in changes in the level of energy so we have to really keep in mind that i use this dell
to indicate that we're finding an amount of work not a change this is really meaningless
right here has no meaning whatsoever analogously for heat transfer so let's just you know close this little
segment by looking at different forms of the first line we've already been here about
eight lectures ago we looked at something that looked exactly like this so for a convention where
we've got you know any kind of closed system we've got our control volume drawn around it
and our convention for heat is positive heat goes in positive work goes out and we've got an
amount of mass and an energy level that changes depending on what we do with the
boundaries so using that convention q minus w is equal to changes in energy and
remember the energy is captured by internal kinetic and potential this is in joules
if we uh differentiate with respect to time then we see the rate at which you add
heat minus the rate at which you do work is equal to the rate of change of energy in the system
this is a very useful form of the first law it's the one that i like to use the most
and another form if you divide this statement by the mass or by the mass flux
you actually i put it in terms of lowercase letters so little q one two little w one two is
equal to lowercase e one two and this just puts it in terms of kilojoules per kilogram
okay so you solve it you solve the amounts of energy and work required to you know make some change to a kilogram
of the substance and then you find the total amount of heat and work by multiplying those values by the mass
of the system
The classical statement holds that for a closed system undergoing a thermodynamic cycle, the cyclic integral of heat transfer equals the cyclic integral of work, expressed as ∮ δQ = ∮ δW. This means that over a complete cycle, any net heat added to the system is fully converted into net work output, and vice versa, with no net change in the system's energy.
A thermodynamic cycle occurs when all mechanical and thermodynamic properties of a system, such as pressure and temperature, return to their initial values after a series of processes. On a P-V diagram, this is visualized as a closed loop starting and ending at the same state point, like the intake-compression-power-exhaust sequence in a reciprocating engine.
By comparing two different cycles (e.g., path A-B and A-C) connecting the same states 1 and 2, the first law shows that (δQ - δW) on path B equals (δQ - δW) on path C. This implies the quantity dE = δQ - δW depends solely on the initial and final states, not the path taken, proving that energy is a state property.
Heat (δQ) and work (δW) are path quantities that represent amounts of energy transferred during a process, and their integrals (∫ δQ, ∫ δW) give total amounts, not changes (e.g., Q₂ - Q₁ is meaningless). In contrast, energy (E) is a state property, so its integral dE yields a change (E₂ - E₁) independent of the process path.
The most common forms are: the energy balance (Q - W = ΔE = ΔU + ΔKE + ΔPE), the rate form for transient systems (Q̇ - Ẇ = dE/dt), and the specific form per unit mass (q₁₂ - w₁₂ = e₂ - e₁). The rate form is especially useful for real-time analysis, while the specific form simplifies calculations by first solving for per-unit values.
To apply the cyclic integral, sum the path integrals of heat (∫₁² δQ + ∫₂³ δQ + … + ∫ₙ¹ δQ) and work (∫₁² δW + ∫₂³ δW + … + ∫ₙ¹ δW) around the entire cycle. According to the first law, these two sums are equal (∮ δQ = ∮ δW), confirming energy conservation over the cycle.
The First Law provides a fundamental energy balance for closed systems, such as reciprocating engines, where only energy (heat and work) crosses boundaries. By equating the cyclic integrals of heat and work, engineers can predict performance, efficiency, and energy changes, ensuring designs meet practical constraints without mass transfer.
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