Work potential
- For conversion of thermal energy to electricity or mechanical work,
energy alone is not enough.
- A 1 K temperature change in the oceans would supply 17000 CMO!
- But at the average surface temperature, the thermal conversion
efficiency would be ~0.003.
- We really want the work potential of an energy source.
- Names: exergy, availability, lost work,
second law analysis
How much work can be extracted in going from one state to
another?
Or, how much work is required in going from one state to another?
Work Potential: KE, PE
The wind blows at 10 m/s, what is the work potential per unit
mass?
What is the work potential in a 5.1 meter high waterfall?
Work potential: heat transfer
We transfer 1 kW of power from a thermal energy source at 500 K.
What is the work potential?
Need to define the surrounding state, so, 300 \(K\), say.
WP here is simply 1 kW times the Carnot efficiency: \[W = 1\,\mbox{kW} ⋅ \underbrace{(1 -
300/500)}_{η_c} = 0.40\,\mbox{kW}\]
Work potential: air, change state
Air
T (K) |
573 |
300 |
P (atm) |
10 |
1 |
S (J/kg\(⋅\)K) |
6892 |
6892 |
H (kJ/kg) |
282 |
1.91 |
How much work can be extracted in moving from state 1 to state
2?
Isentropic
Work is just \(Δ H\)
That is, the maximum 1\(^{st}\)
law work can be extracted
Work potential: steam, change state
Water
Phase |
supercritical |
liquid |
T (K) |
800 |
300 |
P (atm) |
10 |
1 |
S (J/kg\(⋅\)K) |
11350 |
3913 |
H (kJ/kg) |
-12434 |
-15858 |
How much work can be extracted in moving from state 1 to state
2?
- First law: \(Δ H = W + Q\)
- Max work for min Q
- Second law: \(Q_{min}=T_{min}Δ
S\)
Lost work
- Consider an unsteady, open system
- Energy balance \[\begin{align}
\frac{d(mu)_{sys}}{dt} &= \dot{W} + \dot{Q} + \sum_i\dot{m}_iu_i \\
&=\sum_i\dot{m}_iPv_i + \dot{W}_\phi + \sum_j\dot{Q}_j +
\sum_i\dot{m}_iu_i
\end{align}\]
Here, \(\dot{W}_\phi\) is “other”
work not including injection work (which goes into enthalpy).
\[\frac{d(mu)_{sys}}{dt} =
\sum_i\dot{m}_ih_i + \dot{W}_\phi + \sum_j\dot{Q}_j\]
Lost work
- Entropy balance
- Here, we define the system so that it exchanges heat with the
surrounding reservoirs \(j\) at the
respective reservoir temperature. In this way, all irreversibilities are
within the system, and \(\dot{S}_{sys} +
\dot{S}_{surr} = \dot{S}_{irrev}\). \[\frac{d(ms)_{sys}}{dt} = \sum_i\dot{m}s_i +
\underbrace{\sum_j\dot{S}_{j,HT}}_{\sum_j\dot{Q}_j/T_j} +
\dot{S}_{irrev}\]
\[\frac{d(ms)_{sys}}{dt} =
\sum_i\dot{m}_is_i + \sum_j\dot{Q}_j/T_j + \dot{S}_{irrev}\]
Lost work
- The term \(\dot{S}_{irrev}\) is
identified as the lost work divided by the surrounding
temperature \(T_0\): \[\dot{S}_{irrev} = \frac{W_L}{T_0}\]
- We multiply the entropy balance by \(T_0\) and subtract the result from the
energy balance. This gives a relation for the combined first and second
laws: \[\frac{d(m(u-T_0s))_{sys}}{dt} =
\sum_i\dot{m}_i(h_i-T_0s_i) + \sum_jQ_j\left(1-\frac{T_0}{T_j}\right) +
\dot{W}_\phi -\dot{W}_L\]
- Solve for \(\dot{W}_\phi\): \[\dot{W}_\phi =
\left[\frac{d(m(u-T_0s))_{sys}}{dt} - \sum_i\dot{m}_i(h_i-T_0s_i) -
\sum_jQ_j\left(1-\frac{T_0}{T_j}\right)\right] + \dot{W}_L\]
Lost work
- Again: \[\dot{W}_\phi =
\frac{d(m(u-T_0s))_{sys}}{dt} - \sum_i\dot{m}_i(h_i-T_0s_i) -
\sum_jQ_j\left(1-\frac{T_0}{T_j}\right) + \dot{W}_L\]
- If the lost work is zero, then we have a reversible process, by
which:
\[\dot{W}_{\phi,rev} =
\frac{d(m(u-T_0s))_{sys}}{dt} - \sum_i\dot{m}_i(h_i-T_0s_i) -
\sum_jQ_j\left(1-\frac{T_0}{T_j}\right)\]
- \(Q\) is positive into the
system
- \(\dot{m}\) is positive into the
system
- \(\dot{W}_{\phi,rev}\) is positive
into the system