Diesel Cycle: Difference between revisions

From wikiluntti
 
(11 intermediate revisions by the same user not shown)
Line 30: Line 30:
=== Diesel Cycle and Ideal Gas ===
=== Diesel Cycle and Ideal Gas ===


For a closed system, the total change in energy of a system is the sum of the work done and the heat added <math>dU = \delta W + \delta Q</math>, and the reversible work done on a system by changing the volume is <math>\delta W = - p dV</math>.
There are three (3) different processes:
# Isentropic <math>dU = nC_v dT = -pdV</math>
# Isobaric <math>Q = \Delta U + p \Delta V</math>
# Isochoric <math>\Delta Q = m c_v \Delta T</math>


If the system is reversible and adiabatic (isentropic) <math>\delta Q = 0</math>, which gives  
where the specific heat capacity at constant volume is <math>c_v = \frac{dQ/dT}{m}</math>.
 
 
For a closed system, the total change in energy of a system is the sum of the work done and the heat added <math>dU = \delta W + \delta Q</math>, and the reversible work done on a system by changing the volume is <math>\delta W = - p dV</math>. Furthermore, for any transformation of an ideal gas, it is always true that <math>dU = nC_v dT</math>.
 
 
 
If the system is reversible and adiabatic ('''isentropic''') <math>\delta Q = 0</math>, which gives  


<math>
<math>
Line 38: Line 48:
</math>
</math>


Furthermore, for any transformation of an ideal gas, it is always true that <math>dU = nC_v dT</math>, giving


<math>
<math>
dU = nC_v dT = -pdV  
dU = nC_v dT = -pdV  
</math>
</math>


For the constant pressure ('''isobaric process''') <math>\Delta p = 0</math> we have <math>W = \int p dV = p \Delta V</math>, and by applying the ideal gas law, we get <math>W = n R \Delta T</math>.


=== Real gas: Air ===
For the '''Isochoric process''' <math>\Delta V=0</math>, and thus we have <math>dQ = dU = mc_v dT</math> which gives <math>\Delta Q = m c_v\Delta T</math>.


1. Basic ideal gas model (good first approximation)
<math>


Air is usually approximated as an ideal gas with:
</math>


Gas constant:
=== Real gas: Air ===
 
R≈287 J/(kg\cdotpK)
R≈287J/(kg\cdotpK)
Equation of state:
 
p=ρRT
p=ρRT


Basic ideal gas model (good first approximation). Air is usually approximated as an ideal gas with:
* Gas constant:
** R≈287 J/(kg\cdotpK)
** R≈287J/(kg\cdotpK)
* Equation of state:
* p=ρRT
This works well at:
This works well at:
* pressures near atmospheric
* temperatures roughly 200–500 K


pressures near atmospheric
temperatures roughly 200–500 K
2. “Generalized” ideal gas → temperature-dependent properties


To go beyond the simple model, you allow properties like heat capacity to vary with temperature:
“Generalized” ideal gas → temperature-dependent properties. To go beyond the simple model, you allow properties like heat capacity to vary with temperature:
 
Heat capacity
cp(T)
c
p
 
(T)
 
For air, a common approximation is a polynomial:
 
cp(T)=a+bT+cT2+dT3
c
p
 
(T)=a+bT+cT
2
+dT
3


Heat capacity. For air, a common approximation is a polynomial
<math>
c_p(T)=a+bT.
</math>
Typical coefficients (for dry air, ~200–1000 K range):
Typical coefficients (for dry air, ~200–1000 K range):
 
* a≈1005
a≈1005
* b≈0.1
a≈1005
b≈0.1
b≈0.1
higher-order terms small depending on fit
 
More accurate forms come from NASA polynomials:
More accurate forms come from NASA polynomials:
<math>
\frac{c_p}R=a_1+a_2T+a_3T^2+a_4T^3+a_5T^4
</math>
Which are widely used in CFD and thermodynamics.


cpR=a1+a2T+a3T2+a4T3+a5T4
Compressibility factor Z (real gas correction). If you want a generalized ideal gas, you often introduce <math>p=Z\rho RT</math>. Where
R
* Z=1 → ideal gas
c
* Z≠1 → real gas behavior
p
 
 
=a
1
 
+a
2
 
T+a
3
 
T
2
+a
4
 
T
3
+a
5
 
T
4
 
These are widely used in CFD and thermodynamics.
 
3. Compressibility factor  
Z
Z (real gas correction)
 
If you want a generalized ideal gas, you often introduce:
 
p=ZρRT
p=ZρRT
 
Where:
 
Z=1
Z=1 → ideal gas
Z≠1
Z
=1 → real gas behavior
 
For air:
For air:
* At normal conditions:  Z≈1
* At high pressure: use virial expansion
<math>
Z=1+\frac{B(T)}V+\frac{C(T)}{V^2}+ \cdots
\approx 1+ \frac{B(T)}{RT}p.
</math>


At normal conditions:
Z≈1
Z≈1
At high pressure: use virial expansion
Virial equation:
Z=1+B(T)V+C(T)V2+⋯
Z=1+
V
B(T)


+
Mixture-based formulation (more fundamental). Air is a mixture mainly of:
V
* N₂ (~78%)
2
* O₂ (~21%)
C(T)
* Ar (~1%)


+⋯
<math>
 
\begin{align}
Usually truncated to:
R &=\sum_i y_i R_i \\
 
c_p & = \sum_i y_ i c_{p,i}(T)
Z≈1+B(T)RTp
\end{align}
Z≈1+
</math>
RT
B(T)
 
p
4. Mixture-based formulation (more fundamental)
 
Air is a mixture mainly of:
 
N₂ (~78%)
O₂ (~21%)
Ar (~1%)
 
You can model it as:
 
R=∑iyiRi
R=
i
 
y
i
 
R
i
 
cp=∑iyicp,i(T)
c
p
 
=
i
 
y
i
 
c
p,i
 
(T)
 
This is the most physically grounded “generalized ideal gas” model.
 
5. When to use which model
Simple engineering → constant
R,cp
R,c
p
 
Moderate accuracy (aerodynamics, engines) →
cp(T)
c
p
 
(T)
High pressure / high temperature → include
Z
Z
High fidelity (CFD, combustion) → mixture + NASA polynomials
Bottom line
 
Yes—air is commonly treated as a generalized ideal gas by:
 
Keeping
p=ρRT
p=ρRT
Allowing:
cp=cp(T)
c
p
 
=c
p
 
(T)
possibly
Z≠1
Z
=1


== Realistic Diesel Cycle ==
== Realistic Diesel Cycle ==

Latest revision as of 21:36, 30 March 2026

Introduction

1

Ratio of specific heats (heat capacity ratio) is defined as

pV diagram

  1. Isentropic (adiabatic) expansion
  2. Isochoric cooling (Qout): Heat rejection. Power stroke ends, heat rejection starts.
  3. Isobaric compression: Exhaust
  4. Isobaric expansion: Intake
  5. Isentropic (adiabatic) compression
  6. Isobaric heating (Qin): Combustion of fuel (heat is added in a constant pressure;)

Engine displacement is the cylinder volume swept by all of the pistons of a piston engine, excluding the combustion chambers. A combustion chamber is part of an internal combustion engine in which the fuel/air mix is burned.

Only air is compressed, and then diesel fuel is injected directly into that hot, high-pressure air.

  • Cylinder pressure: ~30–80 bar
  • Injection pressure: ~1,000–2,500+ bar

Diesel Cycle and Ideal Gas

There are three (3) different processes:

  1. Isentropic
  2. Isobaric
  3. Isochoric

where the specific heat capacity at constant volume is .


For a closed system, the total change in energy of a system is the sum of the work done and the heat added , and the reversible work done on a system by changing the volume is . Furthermore, for any transformation of an ideal gas, it is always true that .


If the system is reversible and adiabatic (isentropic) , which gives


For the constant pressure (isobaric process) we have , and by applying the ideal gas law, we get .

For the Isochoric process , and thus we have which gives .

Real gas: Air

Basic ideal gas model (good first approximation). Air is usually approximated as an ideal gas with:

  • Gas constant:
    • R≈287 J/(kg\cdotpK)
    • R≈287J/(kg\cdotpK)
  • Equation of state:
  • p=ρRT

This works well at:

  • pressures near atmospheric
  • temperatures roughly 200–500 K


“Generalized” ideal gas → temperature-dependent properties. To go beyond the simple model, you allow properties like heat capacity to vary with temperature:

Heat capacity. For air, a common approximation is a polynomial Typical coefficients (for dry air, ~200–1000 K range):

  • a≈1005
  • b≈0.1

More accurate forms come from NASA polynomials: Which are widely used in CFD and thermodynamics.

Compressibility factor Z (real gas correction). If you want a generalized ideal gas, you often introduce . Where

  • Z=1 → ideal gas
  • Z≠1 → real gas behavior

For air:

  • At normal conditions: Z≈1
  • At high pressure: use virial expansion


Mixture-based formulation (more fundamental). Air is a mixture mainly of:

  • N₂ (~78%)
  • O₂ (~21%)
  • Ar (~1%)

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \begin{align} R &=\sum_i y_i R_i \\ c_p & = \sum_i y_ i c_{p,i}(T) \end{align} }

Realistic Diesel Cycle

Ratio of specific heats γ

Caption text
Condition γ (approx.)
Stoichiometric ~1.30–1.33
Moderate lean ~1.33–1.37
Very lean (diesel) ~1.37–1.40

Injection pressures

  • Older systems: 200–500 bar
  • Modern common-rail: 1,000–2,500 bar
  • Latest systems: up to ~3,000 bar
  • Air pressure in cylinder: ~30–80 bar, which is the pressure of the combustion chamber.
  • Temperature: ~700–1000 K

Diesel-air Mixture

Only diesel is ejected into the cylinder. Clean air comes in during the intake stroke.

The heat capacity ratio (known as the adiabatic index) for a diesel-air mixture is typically around 1.4.

Air-fuel ratio
14.5:1 Near-stoichiometric; good combustion efficiency but higher emissions.
16:1 Balanced performance; good power output and efficiency.
18:1 Lean burn; improved fuel economy but potential for higher NOx emissions.


Diesel is a complicated compound, but it’s commonly approximated as a hydrocarbon like C12H23 (or C12H26). Air is about 21% O2 and 79% N2. Without nitrogen, the stoichiometric ratio is about

C12​H23​+17.75O2​→12CO2​+11.5H2​O

and by including nitrogen, we get

C12​H23​+17.75( O2 + 3.76 N2 )​→12CO2​+11.5H2​O + 66.74 N2.

The molar masses

  • Fuel: 167 g/mol
  • Air: 137.28 g/mol

And the total air needed is 17.72 x 137.28 = 2436 g, which gives air-to-fuel-ratio to

MB data

Motor: OM648.

Mercedes Benz W211 (2003)

  • Engine displacement: 3222 cm3 = 0.003222 m3
  • Bore x Stroke: 88.0 x 88.4 mm3
  • Compression Ratio: 18.0

Bore x stroke gives V = 6xπ(8.8/2)2 x 8.84 cm3 = 3225.95cm3, which is rather close.

1

1

1