CHEP 121 Lecture Notes on the First Law of Thermodynamics

MANICALAND STATE UNIVERSITY OF APPLIED SCIENCES

FACULTY OF ENGINEERING, APPLIED SCIENCES AND TECHNOLOGY

Chemical Engineering Thermodynamics CHEP 121 Lecture Notes: First Law of Thermodynamics By Muhezwa C.

Internal Energy and the First Law of Thermodynamics

  • Molecules in motion possess:
    • Kinetic Energy:
    • Types: translation, rotation, internal vibration.
    • Potential Energy:
    • Due to intermolecular forces (attraction or repulsion between molecules).
  • Internal Energy (U):
    • Sum of total kinetic energy from molecular motion and potential energy from intermolecular forces.
    • Excludes energy from the gross position or movement of the system as a whole.
  • While determining absolute internal energy is challenging, only changes in internal energy matter for thermodynamic analysis.

Representation of the First Law of Thermodynamics

  • The First Law, or Principle of Conservation of Energy, states that:
    • Total energy of a system and its surroundings is constant.
    • Energy appears in different forms but total quantity remains fixed.
    • Energy transitions (one form disappearing and another appearing) are constant.
  • Initially a postulate; has become a recognized law due to strong experimental evidence.

The First Law of Thermodynamics

  • Statement: The total energy of any system and its surroundings is conserved.
  • Definitions:
    • System: The portion of the universe chosen for analysis; includes everything within its boundaries.
    • Surroundings: Everything outside the system.
  • Energy changes in the system may include changes in:
    • Internal energy
    • Potential Energy (PE)
    • Kinetic Energy (KE)
  • Heat (Q) and Work (W):
    • Forms of energy in transit across system boundaries.
  • Closed System:
    • No material transfer across boundaries; total energy change in surroundings equals heat and work exchanged with the system.

Mathematical Expressions in Thermodynamics

  • For closed systems, energy balance equations are:
    • Change in energy of surroundings: ext(EnergyofSurroundings)=±Q±Wext{∆(Energy of Surroundings)} = ±Q ± W …………(3.1)
    • Change in energy of the system: ext(EnergyofSystem)=KE+PE+Uext{∆(Energy of System)} = ∆KE + ∆PE + ∆U ………. (3.2)
  • Combining equations yields the First Law for Closed Systems:
    • KE+PE+U=±Q±W∆KE + ∆PE + ∆U = ±Q ± W …………(3.3)

Sign Convention

  • Adopting Sign Convention:
    • Heat transferred to the system from surroundings is positive.
    • Work done by the system to surroundings is negative.
  • Equation (3.3) modifies to:
    • KE+PE+U=QW∆KE + ∆PE + ∆U = Q - W ………… (3.4)
  • If changes in KE & PE are negligible:
    • U=QW∆U = Q - W …………(3.5)
  • For differential changes:
    • dU=δQδWdU = δQ - δW …………(3.6)

Internal Energy: Implications on the First Law

  • Internal Energy (U) is a state function:
    • Path independence when computing QWQ - W, depending only on initial and final states.
  • Useful in calculating energy requirements for processes in:
    • Heat exchangers, pumps, compressors, distillation columns, etc.
  • State functions like U can be tabulated for any process, utilizing thermodynamic principles productively.

Thermodynamic Processes

  • A system can experience various thermodynamic changes, adjusting Pressure (P), Volume (V), and Temperature (T).
  • PV Diagram Representation:
    • Work done under PV curves is equivalent to the area under the curve:
    • W > 0 for expansion
    • W < 0 for compression.

Isothermal Process

  • Definition: Process occurring at constant temperature (ΔT = 0).
  • Assumption: System remains in contact with a heat reservoir, ensuring thermal equilibrium is maintained.
  • For Ideal Gases:
    • Since ΔTΔT is zero, then ΔU=0ΔU = 0, thus:
    • From the First Law, Q=WQ = W
    • Any energy entering (Q) must leave as work (W).

Isothermal Process on a P-V Diagram

  • Visualization:
    • Includes states A and B at constant temperature T1.
  • Equation for work in an isothermal process:
    • W=QW=-Q, reflecting energy conservation.

Iso-volumetric Process (Isochoric)

  • Definition: Constant volume process.
  • Work: No volume change implies:
    • W=0W = 0
  • Internal energy change relation:
    • ΔU=QΔU = Q (energy transferred is entirely as heat).
  • Example: Heating gas in a closed, rigid container.

Iso-volumetric Process on a P-V Diagram

  • Illustration:
    • Volume remains constant; process denoted by the same point on the curve.
  • Similarly, Work remains zero (W = 0) and Heat is equal to the internal energy change.

Adiabatic Process

  • Definition: Process with no heat exchange (Q = 0).
  • Relation between changes:
    • ΔU=WextorΔU=W– ΔU = W ext{ or } ΔU = -W
  • Conditions for expansion and compression:
    • Expansion: Work done by the system (W positive) implies ΔUΔU is negative.
    • Compression: Work done on the system (W negative) thus ΔUΔU is positive.

Adiabatic Process on a P-V Diagram

  • Visual Representation:
    • Notable isotherms and adiabat relationship:
    • Work effect shown during volumetric changes.

Isobaric Process

  • Definition: Process occurring at constant pressure.
  • Energy changes (ΔU, W, Q) can be non-zero:
    • Work from ideal gas calculated as: W=PΔVW = P ΔV
  • Everyday example: Water boiling in a saucepan, reflecting constant pressure.

Isobaric Process on a P-V Diagram

  • Demonstration:
    • Work calculated as W=P(V2V1)W = -P(V2 - V1)
  • Pressure remains constant; changes in volume occur under work done.

Enthalpy (H)

  • Definition: Enthalpy is defined as: HU+PVH ≡ U + PV ……………………………(1)
    • Represents internal energy plus the product of pressure and volume.
  • Enthalpy is a state function as all the contributing factors are state functions.
  • The differential form is expressed as:
    • dH=dU+d(PV)dH = dU + d(PV)
  • Integrated form from equation (1):
    • ΔH=ΔU+pΔVΔH = ΔU + pΔV when transformed during constant pressure.
  • At constant pressure, heat Q can be stated as:
    • Therefore for processes under constant pressure: ΔH=QΔH = Q.
  • An advantage of knowing enthalpy is its usefulness in energy balances for processes such as:
    • Heat exchangers, chemical reactors, pumps, turbines, etc.

Example on Calculation of ΔU and ΔH

  • Calculating for 1 kg of water vaporized at 100°C and 101.33 kPa:
    • Change identified by specific volumes of liquid (0.00104 m³·kg⁻¹) and vapor (1.673 m³·kg⁻¹).
  • Energy addition: Q=2256.9kJQ = 2256.9 kJ
  • Using Formulas:
    • ΔH=Q=2256.9kJΔH = Q = 2256.9 kJ
    • For ΔUΔU using pressure-volume work:
    • PAV=101.33extkPaimes(1.6730.001)extm3=169.4extkJPAV = 101.33 ext{kPa} imes (1.673 - 0.001) ext{m}^3 = 169.4 ext{kJ}
    • Thus, calculating internal energy:
    • ΔU=2256.9169.4=2087.5extkJΔU = 2256.9 - 169.4 = 2087.5 ext{kJ}

Heat Capacity

  • Definition: Heat capacity is categorized into two types for homogeneous fluids:
    • C₍V₎: Heat capacity at constant volume, defined as:
    • CV=32RC_V = \frac{3}{2} R.
    • C₍P₎: Heat capacity at constant pressure, defined as:
    • CP=52RC_P = \frac{5}{2} R.
  • For constant volume processes:
    • Q=nCVΔT=ΔUQ = nC_VΔT = ΔU.
  • The universal gas constant: R=8.314extJ/molKR = 8.314 ext{J/mol·K}.

Heat Capacity at Constant Volume

  • Heat capacity derivation considers state functions CVS with respect to Temp and Volume:
    • ΔU=CV(T2T1)ΔU = C_V(T_2 - T_1).
  • No process dependency means C_V is independently evaluated.

Heat Capacity at Constant Pressure

  • Definition encompasses both molar and specific heat capacities regarding enthalpy H:
    • ΔH=CP(T2T1)ΔH = C_P (T_2 - T_1),
  • C_P serves as a state function that doesn't vary with the process.

Equations of State and Heat Capacities

  • Case Study: N₂ gas at 273 K and 1 atm; adding 3000 J of heat causes 832 J of work:
    • Tasks include:
    • (i) Final state of the gas
    • (ii) Values for ΔUΔU and ΔHΔH during state change
    • (iii) Values of specific heat capacities c₍V₎ and c₍P₎ for N₂ assuming ideal gas behavior, reversible change of state.