Energy Balance Essentials: Isolated Systems, Enthalpy, and Partial Pressures
Internal energy, thermal energy, and chemical energy
- U = total energy; composed of thermal (kinetic) energy and chemical energy (bond energy).
- Chemical energy is negative in the sense of potential energy wells; bond formation lowers the system's chemical energy.
- Energy balance in a closed system: ΔU=q+w=ΔU<em>chem+ΔU</em>thermal.
- Isolated system (no heat or work exchange): ΔU<em>total=0⇒ΔU</em>thermal=−ΔUchem.
- If chemical energy decreases (more negative) due to bond strengthening, the thermal energy increases by the same amount in an isolated system.
- If the system is not isolated, the excess thermal energy can be transferred as heat to the surroundings or as work; the budget remains balanced with the outside world.
- In a fixed-volume, insulated container: q=0,w=0⇒ΔU=0. The chemical-to-thermal energy transfer still occurs internally as needed.
- Practical takeaway: the heat you feel inside the system depends on whether heat can leave the system.
Enthalpy and constant-pressure processes
- Enthalpy defined: h=u+pv where $u$ is internal energy per unit substance and $v$ is specific volume.
- Change in enthalpy: Δh=Δu+pΔv.
- At constant pressure with only PV-work (no non-PV work): qp=Δh.
- Enthalpy is a state function; heat is a boundary quantity. In many reactions, Δu dominates and Δh≈Δu, with a small correction from $p\Delta v$.
- When volume changes are small or pressure is constant, enthalpy provides a convenient energy accounting at constant pressure.
Partial pressures and open vs closed systems
- For mixtures of gases, total pressure is the sum of individual partial pressures: P=∑<em>iP</em>i.
- For ideal gases, P<em>i=x</em>iP where $x_i$ is the mole fraction of component $i$.
- In open (open to surroundings) experiments, the gas tends to equilibrate with the external pressure, performing or receiving PV-work as it expands or contracts.
- In open systems, a work term ($w$) often appears due to volume change against external pressure; this is automatically accounted for when considering enthalpy.
Worked intuition and example notes
- Exothermic reaction in an insulated container: heat stays in the system; the products (system) heat up; the internal energy increases due to the loss of chemical energy.
- Exothermic reaction in contact with surroundings: heat can leave the system; the thermal energy of the system may decrease or rise less, depending on environment.
- Real breathing example: respiration releases chemical energy, warming the exhaled air; excess heat is transferred to surroundings.
- General energy-tracking rule (isolated vs open):
- Isolated and fixed volume: ΔU=0⇒ΔU<em>thermal=−ΔU</em>chem.
- Open or connected to environment: heat and/or work can move between system and surroundings; enthalpy helps track energy when volume can change under constant external pressure.
Quick example (conceptual, using shown numbers)
- If a reaction changes chemical energy from $-5.03\,\text{eV}$ to $-16.48\,\text{eV}$:
- ΔUchem=(−16.48)−(−5.03)=−11.45 eV.
- In an isolated system: ΔU<em>thermal=−ΔU</em>chem=+11.45 eV.
- If the system is not isolated, this 11.45 eV may be carried away as heat to the surroundings or stored as thermal energy, depending on the environment and constraints.
Homework-oriented takeaways
- You will be asked to track energy through a chemical change:
- Compute ΔU<em>chem=U</em>chem, final−Uchem, initial.
- Determine whether the accompanying change in thermal energy ΔUthermal stays in the system (isolated) or leaves to the surroundings (open).
- If the container is fixed and insulated: ΔU=0⇒ΔU<em>thermal=−ΔU</em>chem.
- If the container is at constant external pressure: use enthalpy: qp=Δh=Δu+pΔv.
- For glucose burning or similar reactions, you’ll need the balanced equation and standard molar volumes at STP to evaluate PV-work contributions when using enthalpy.
- First Law: ΔU=q+w
- Energy components: ΔU=ΔU<em>chem+ΔU</em>thermal
- Isolated, fixed volume: ΔU=0⇒ΔU<em>thermal=−ΔU</em>chem
- Enthalpy: h=u+pv;Δh=Δu+pΔv
- Constant pressure, PV-work only: qp=Δh
- Partial pressures for ideal gases: P=∑<em>iP</em>i;P<em>i=x</em>iP