Unit 5: Chemical Thermodynamics
NCERT Chemistry Class 11: Chapter 5
"It is the only physical theory of universal content concerning which I am convinced that, within the framework of the applicability of its basic concepts, it will never be overthrown."
Albert Einstein on Thermodynamics
Chemical energy stored within molecular bonds can be transformed into thermal energy, mechanical work, or electrical work. When natural gas (methane) burns in air, chemical potential energy is liberated as heat. In an automobile engine or rocket thruster, that chemical energy is converted into directed mechanical work through gas expansion. In a galvanic cell, it produces electrical work to power external circuits.
The branch of physical science concerned with these quantitative energy transformations and the equilibrium states of matter is chemical thermodynamics.
Thermodynamics is governed by foundational characteristics that distinguish it from chemical kinetics and mechanics:
- Macroscopic Scope: Thermodynamics deals exclusively with bulk systems comprising vast ensembles of particles (on the order of Avogadro's constant, NA≈6.022×1023). It does not require knowledge of individual atomic trajectories, molecular velocities, or quantum eigenstate transitions.
- Path-Independent State Functions: Thermodynamic analysis is concerned with the initial and final equilibrium states of a system. It does not depend on the specific pathway or mechanism connecting those states.
- No Kinetic Information: Thermodynamics answers whether a process has the thermodynamic potential to occur spontaneously, how much heat or work will be exchanged, and where the chemical equilibrium position lies. It provides zero information regarding the reaction rate or time required to reach that equilibrium. A mixture of hydrogen and oxygen gas at 298 K is thermodynamically unstable with respect to water formation, yet the reaction proceeds at an imperceptible rate in the absence of a catalyst.
Thermodynamics addresses three primary questions:
- How do we calculate the energy changes accompanying physical transformations and chemical reactions?
- What fundamental physical principle dictates whether a reaction will proceed spontaneously without continuous external assistance?
- To what extent will reactants convert into products before reaching dynamic equilibrium?
How to Use the Interactive Lab Modules:
Alongside this chapter, you have access to seven interactive simulation tools in the right-hand workspace:
- System Boundary Simulator: Manipulate Open, Closed, and Isolated boundaries; observe real-time exchange of matter and energy.
- Energy Transfer & Thermodynamic Sign Lab: Conduct Joule paddle-wheel churning and electrical coil heating; track q, w, and ΔU with IUPAC sign conventions.
- Piston Gas & Indicator Lab: Compress and expand gases irreversibly or reversibly; visualize indicator PV diagrams and evaluate w=−∫pexdV.
- Reaction Calorimeter & Temperature Lab: Measure heat evolved at constant volume in a bomb calorimeter (ΔU=qV) versus constant pressure (ΔH=qp).
- Hess's Law Puzzle & Reaction Builder: Combine and scale intermediate reactions to construct target enthalpy cycles path-independently.
- Bond Breaking & Making Lab: Sever reactant covalent bonds and forge product bonds to calculate approximate gas-phase enthalpies.
- Molecular Disorder & Gibbs Spontaneity Simulator: Track particle microstates across solid, liquid, and gas phases; manipulate ΔH, ΔS, and temperature to map the four quadrants of spontaneity and evaluate equilibrium constants K.
Follow the Interactive Simulation Experiment callouts integrated into each section.
To formulate thermodynamic laws quantitatively, precise terminology must be established for defining the portion of the universe under study and the nature of its boundaries.
5.1.1 The System, Surroundings, and Boundary
| Thermodynamic Entity | Formal Definition | Laboratory Example |
|---|
| System | The specific part of the universe chosen for thermodynamic investigation, containing reactants, products, and solvent. | The aqueous solution of reactants inside a conical flask. |
| Surroundings | The entire remainder of the universe outside the system boundaries that can exchange energy or matter with the system. | The water bath, laboratory bench, ambient air, and measuring instruments in thermal contact with the flask. |
| Boundary | The real physical or imaginary geometrical surface separating the system from its surroundings across which matter or energy can pass. | The borosilicate glass walls of the flask and the open liquid-air interface at the neck. |
Mathematically, the relationship is expressed as:
Universe=System+Surroundings
In practical laboratory measurements, changes occurring within a chemical system affect only the immediate neighborhood of the system. Therefore, the effective surroundings comprise only that finite region capable of exchanging energy or matter with the system.
Boundaries are classified based on physical properties:
- Diathermic (Conducting) Boundary: Permits heat exchange between system and surroundings driven by temperature gradients (for example, a copper vessel).
- Adiabatic (Insulated) Boundary: Completely prevents heat transfer between system and surroundings (q=0, such as the silvered vacuum walls of a Dewar flask).
- Rigid Boundary: Possesses fixed volume and cannot be displaced, preventing pressure-volume work (dV=0).
- Flexible Boundary: Allows volumetric expansion or contraction against external pressure (such as a gas cylinder fitted with a mobile piston).
5.1.2 Classification of Thermodynamic Systems
Systems are classified according to whether their boundaries permit the exchange of matter, energy, or neither:
| System Type | Exchange of Matter | Exchange of Energy | Laboratory Demonstration |
|---|
| Open System | Allowed | Allowed | A beaker of boiling water without a lid. Steam escapes to surroundings, and heat conducts through the base. |
| Closed System | Prohibited | Allowed | A sealed copper flask containing hot liquid. Mass cannot escape, but thermal energy dissipates into the surroundings. |
| Isolated System | Prohibited | Prohibited | Hot tea stored in a perfectly insulated thermos flask. Neither matter nor heat crosses the boundary. |
Key Principle: The Energy of an Isolated System is Conserved
For any completely isolated system, because no mass, heat, or work can cross the boundary, the total energy remains strictly invariant: ΔUisolated=0.
Interactive Simulation Experiment: System Boundary Simulator
Open the System Boundary tab in the right-hand simulation suite:
- Select the Open System preset. Introduce heat via the burner control. Observe water molecules evaporating across the boundary into the surroundings while energy transfers.
- Switch to Closed System. Note that a sealed barrier prevents mass transfer, yet heat continues to equilibrate through diathermic walls.
- Switch to Isolated System. Verify that both the mass counter and the internal energy monitor remain locked at fixed values regardless of external thermal fluctuations.
5.1.3 The State of the System and State Functions
In classical mechanics, the state of a particle is fully specified by identifying its instantaneous position coordinates (x,y,z) and momentum components (px,py,pz). In thermodynamics, a vastly simpler macroscopic approach is utilized.
The state of a thermodynamic system is completely described by quoting a small set of measurable macroscopic bulk properties:
- Pressure (p)
- Temperature (T)
- Volume (V)
- Amount of substance (n)
- Chemical composition
For a single-phase homogeneous pure substance, fixing any two independent macroscopic variables (such as p and T) uniquely fixes all other variables according to an equation of state (for an ideal gas, pV=nRT).
State Functions versus Path Functions
| Characteristic | State Function (State Variable) | Path Function |
|---|
| Dependence | Depends exclusively on the instantaneous thermodynamic state of the system, independent of the past history or pathway taken to reach that state. | Depends directly on the specific path, mechanism, or steps taken to transition between initial and final states. |
| Mathematical Property | Exact differential (df); cyclic integral is zero: ∮df=0. | Inexact differential (δf); cyclic integral is generally non-zero: ∮δf=0. |
| Finite Change | Δf=ffinal−finitial | Cannot be expressed as a difference of two state values: q and w. |
| Examples | Internal Energy (U), Enthalpy (H), Entropy (S), Gibbs Free Energy (G), Pressure (p), Volume (V), Temperature (T). | Heat (q), Mechanical Work (w), Electrical Work (welec). |
Conceptual Analogy:
Elevation above sea level is a state function: whether you climb a mountain via a vertical cliff face or take a winding, gentle trail, the net change in altitude Δh=hsummit−hbase is identical. The total distance walked and muscular energy expended depend directly on the route chosen and are path functions.
5.1.4 Extensive and Intensive Properties
Macroscopic properties of matter are categorized based on their dependence on system size or amount of material:
| Classification | Definition | Classic Properties | Partition Experiment |
|---|
| Extensive Property | A property whose magnitude depends directly on the total quantity, mass, or size of matter present in the system. | Mass (m), Volume (V), Internal Energy (U), Enthalpy (H), Heat Capacity (C), Entropy (S), Gibbs Energy (G). | If a container of gas of volume V is bisected by an impermeable partition, the volume in each half becomes V/2. |
| Intensive Property | A property whose magnitude is completely independent of the total quantity or size of matter in the system. | Temperature (T), Pressure (p), Density (ρ), Refractive Index, Molar Heat Capacity (Cm), Specific Heat (c), Surface Tension, Viscosity. | Upon bisecting the container of gas, the temperature T and pressure p in each half remain identical to the original system. |
Critical Mathematical Property:
The ratio of any two extensive properties is an intensive property:
- Mass (extensive) divided by Volume (extensive) yields Density (intensive): ρ=Vm.
- Heat Capacity (extensive) divided by Moles (extensive) yields Molar Heat Capacity (intensive): Cm=nC.
- Enthalpy (extensive) divided by Moles (extensive) yields Molar Enthalpy (intensive): Hm=nH.
5.2.1 Internal Energy (U) as a State Function
When a chemical or physical system exchanges energy with its surroundings, we introduce a quantity representing the total intrinsic energy residing within the system: the internal energy, denoted by U.
At the microscopic atomic level, internal energy is the sum of:
- Kinetic Energy Contributions: Translational, rotational, and vibrational motions of molecules, along with the orbital movements and spins of electrons.
- Potential Energy Contributions: Electrostatic attractions and repulsions between atomic nuclei and electrons, chemical bonding energies, and intermolecular attractive forces (dispersion, dipole-dipole, hydrogen bonding).
U=Etranslational+Erotational+Evibrational+Eelectronic+Ebonding+Eintermolecular
Because of the extreme complexity of subatomic interactions and relativistic mass-energy equivalents, it is impossible to evaluate the absolute numerical value of U for any macroscopic system. In chemical thermodynamics, an absolute value is never required. We measure only changes in internal energy:
ΔU=Ufinal−Uinitial
The internal energy of a system can change through three distinct interactions:
- Heat passes into or out of the system.
- Work is done on or by the system.
- Matter enters or leaves the system.
5.2.2 Changing Internal Energy by Work: Adiabatic Processes
Consider a system containing a quantity of liquid water enclosed in a rigid, thermally insulated container equipped with adiabatic walls (q=0).
Between 1840 and 1850, James Prescott Joule performed classic experiments to investigate mechanical and electrical equivalents of heat:
- Pathway 1 (Mechanical Paddle Work): Mechanical work (w=1.0 kJ) was performed on the water by rotating a set of paddles, churning the viscous liquid. The temperature rose from TA to TB, causing a change in internal energy: ΔU=UB−UA.
- Pathway 2 (Electrical Work): An identical quantity of electrical work (w=1.0 kJ) was supplied to the water by passing current through an immersion resistor. The recorded temperature increase was identical: ΔT=TB−TA.
Joule discovered that regardless of how adiabatic work is performed, a given quantity of work done on the system produces an identical change in state as measured by the temperature increment:
ΔU=U2−U1=wad
This experimental invariance proves that internal energy U is a characteristic state function: the adiabatic work depends solely on the initial and final states, independent of the path taken.
5.2.3 Changing Internal Energy by Heat
Internal energy can also be altered without doing mechanical or electrical work, by putting the system in thermal contact with surroundings at a different temperature through thermally conducting (diathermic) walls.
Energy transferred across a boundary solely as a result of a temperature difference between the system and surroundings is defined as heat, denoted by q.
If water at temperature TA is enclosed in a rigid, fixed-volume copper container and placed in a large water bath maintained at temperature TB (TB>TA), heat flows into the system until thermal equilibrium is established. Because the vessel is rigid, no mechanical expansion work can occur (w=0). Under these conditions:
ΔU=qV
Where the subscript V denotes heat transferred at constant volume.
5.2.4 The First Law of Thermodynamics
When a closed system undergoes a change of state involving both heat exchange (q) and mechanical/electrical work (w), the net change in internal energy is given by the algebraic sum:
ΔU=q+w
This formulation constitutes the mathematical statement of the First Law of Thermodynamics.
Statements of the First Law of Thermodynamics:
- The total energy of an isolated system remains constant over time.
- Energy can neither be created nor destroyed; it can only be transformed from one physical or chemical form into another.
- A perpetual motion machine of the first kind (a machine that produces continuous mechanical work without consuming an equivalent quantity of energy) is physically impossible.
For an isolated system, no heat or work can be exchanged with the surroundings (q=0,w=0). Therefore:
ΔUisolated=0
Although q and w individually depend on the path chosen, their algebraic sum ΔU=q+w is strictly path-independent.
5.2.5 IUPAC Sign Conventions in Chemical Thermodynamics
To maintain mathematical consistency across all equations, chemical thermodynamics adopts the standard IUPAC Sign Convention:
| Quantity | Algebraic Sign | Physical Interpretation |
|---|
| Heat absorbed by system (q>0) | Positive (+) | Thermal energy enters the system from surroundings; internal energy increases. |
| Heat released by system (q<0) | Negative (−) | Thermal energy exits the system to surroundings; internal energy decreases. |
| Work done ON the system (w>0) | Positive (+) | Surroundings compress the system or perform work; internal energy increases. |
| Work done BY the system (w<0) | Negative (−) | System expands against surroundings or does work; internal energy decreases. |
Important Caution: Physics vs. Chemistry Sign Convention for Work:
In many classical physics textbooks, work done by the system is defined with a positive sign, yielding ΔU=q−wphysics. In modern chemical thermodynamics and IUPAC standards, all energy inputs into the system carry a positive sign, so ΔU=q+w, where w=−pexΔV.
NCERT Problem 5.1 (Step-by-Step Solution):
Express the change in internal energy of a system when:
(i) No heat is absorbed by the system from the surroundings, but work (w) is done on the system. What type of wall does the system have?
(ii) No work is done on the system, but q amount of heat is taken out from the system and given to the surroundings. What type of wall does the system have?
(iii) w amount of work is done by the system and q amount of heat is supplied to the system. What type of system would it be?
Step 1: Given Quantities & Unit Harmonization
- Case (i): q=0, work done on system =+w.
- Case (ii): w=0, heat released to surroundings =−q.
- Case (iii): Work done by system =−w, heat absorbed =+q.
Step 2: Fundamental Governing Formula
ΔU=q+w
Step 3: Direct Substitution & Arithmetic Computation
- (i) ΔU=0+w=wad. Because q=0, the container possesses an adiabatic wall.
- (ii) ΔU=−q+0=−q. Because heat transfers across the boundary in response to temperature differences, the container possesses a thermally conducting (diathermic) wall.
- (iii) ΔU=q−w. Because energy transfers across the boundary as both heat and work, but matter is contained, this represents a closed system.
Step 4: Physical Significance & Laboratory Insight
The physical nature of the boundary governs which energy transfer modes are accessible to a system during a state transition.
NCERT Problem 5.7 (Step-by-Step Solution):
In a process, 701 J of heat is absorbed by a system and 394 J of work is done by the system. What is the change in internal energy for the process?
Step 1: Given Quantities & Unit Harmonization
- Heat absorbed by system: q=+701 J
- Work done by system: w=−394 J
Step 2: Fundamental Governing Formula
ΔU=q+w
Step 3: Direct Substitution & Arithmetic Computation
ΔU=(+701 J)+(−394 J)=+307 J
Step 4: Physical Significance & Laboratory Insight
Although the system expanded against its surroundings and expended 394 J of mechanical work, the thermal energy influx of 701 J exceeded the work done, producing a net increase of 307 J in the internal energy of the system.
In chemical processes, the most common form of mechanical work is pressure-volume (pV) work, occurring when gases expand or contract against an external resisting pressure.
5.3.1 Derivation of Expansion Work
Consider a cylinder fitted with a frictionless, massless mobile piston of cross-sectional area A, containing an ideal gas at pressure p.
Suppose the external opposing pressure exerted on the outer face of the piston is pex.
- The opposing force acting on the piston is:
Fopp=pex⋅A
- If the gas expands and displaces the piston outward by a distance l, the work done by the system against the resisting force is:
w=−Force×Distance=−(pex⋅A)⋅l
- The change in volume is the area multiplied by displacement: ΔV=A⋅l=Vf−Vi.
- Substituting gives the fundamental expression for mechanical work against a constant external pressure:
w=−pexΔV=−pex(Vf−Vi)
Verification of Sign Conventions:
- During Gas Compression: Vf<Vi⟹ΔV<0.
w=−pex(−ΔV)=+pex∣ΔV∣>0.
Work is done on the system, and w is mathematically positive.
- During Gas Expansion: Vf>Vi⟹ΔV>0.
w=−pex(+ΔV)<0.
Work is done by the system, and w is mathematically negative.
5.3.2 Multi-Step and Reversible Processes
If compression or expansion occurs in a single sudden step against a constant external pressure, the magnitude of work equals the area of the rectangle pex⋅(Vf−Vi) on an indicator PV diagram.
If the external pressure is adjusted in a series of finite intermediate stages:
w=−∑pexΔV
When the pressure changes in infinite infinitesimal increments, the process becomes thermodynamically reversible:
Reversible Process Definition:
A process is said to be reversible if it is conducted infinitely slowly through a continuous succession of equilibrium states, such that the driving force exceeds the opposing force by only an infinitesimal amount (dp), and the process can be reversed in direction at any instant by an infinitesimal modification of external parameters.
For a reversible expansion:
pex=pin−dp
For a reversible compression:
pex=pin+dp
Substituting into the work integral:
wrev=−∫ViVf(pin±dp)dV
Because the product of two infinitesimal differentials dp⋅dV is negligibly small, this reduces to:
wrev=−∫ViVfpindV
5.3.3 Isothermal Reversible Expansion of an Ideal Gas
For n moles of an ideal gas undergoing an isothermal process (T=constant), the ideal gas law gives:
p=VnRT
Substituting into the work integral:
wrev=−∫ViVfVnRTdV=−nRTln(ViVf)
Converting from natural logarithm to common base-10 logarithm:
wrev=−2.303nRTlog10(ViVf)
According to Boyle's Law, at constant temperature piVi=pfVf⟹ViVf=pfpi. Thus:
wrev=−2.303nRTlog10(pfpi)
Maximum Work Theorem:
For any isothermal expansion between specified initial and final volumes, a reversible pathway extracts the maximum possible work from the gas: ∣wrev∣>∣wirrev∣. Conversely, compressing a gas reversibly requires the minimum possible work.
5.3.4 Free Expansion of an Ideal Gas
Expansion of a gas into an evacuated vessel (vacuum) is termed free expansion. Because the opposing external pressure is zero (pex=0):
w=−pexΔV=−0×ΔV=0
In 1843, Joule verified experimentally that when an ideal gas undergoes free expansion inside an isolated water bath, no temperature change occurs. Therefore:
ΔT=0⟹ΔU=0
Applying the First Law of Thermodynamics:
ΔU=q+w⟹0=q+0⟹q=0
Thus, during isothermal free expansion of an ideal gas into vacuum, no work is performed and no heat is absorbed or evolved.
| Thermodynamic Process | Conditions Imposed | Heat (q) | Work (w) | Internal Energy Change (ΔU) |
|---|
| Isothermal Reversible Expansion | T=const,pex=p±dp | q=+2.303nRTlog(Vf/Vi) | w=−2.303nRTlog(Vf/Vi) | ΔU=0 |
| Isothermal Irreversible Expansion | T=const,pex=const | q=+pex(Vf−Vi) | w=−pex(Vf−Vi) | ΔU=0 |
| Isothermal Free Expansion | pex=0 (vacuum) | q=0 | w=0 | ΔU=0 |
| Adiabatic Reversible Process | q=0 | q=0 | w=ΔU | ΔU=nCV(Tf−Ti) |
| Isochoric Process | V=const,ΔV=0 | qV=ΔU | w=0 | ΔU=qV |
NCERT Problem 5.2 (Step-by-Step Solution):
Two litres of an ideal gas at a pressure of 10 atm expands isothermally at 25∘C into a vacuum until its total volume is 10 litres. How much heat is absorbed and how much work is done in the expansion?
Step 1: Given Quantities & Unit Harmonization
- Initial volume: Vi=2 L
- Final volume: Vf=10 L
- External resisting pressure: pex=0 atm (vacuum)
- Temperature: T=25∘C=298.15 K=constant
Step 2: Fundamental Governing Formula
w=−pex(Vf−Vi),ΔU=q+w
Step 3: Direct Substitution & Arithmetic Computation
w=−0×(10−2) L=0 J
For an isothermal expansion of an ideal gas, ΔU=0:
q=−w=0 J
Step 4: Physical Significance & Laboratory Insight
Because the opposing pressure is zero, the expanding gas meets no resistance. Consequently, no work is performed, and no thermal energy is drawn from the surroundings.
NCERT Problem 5.3 (Step-by-Step Solution):
Consider the same expansion as Problem 5.2, but this time conducted against a constant external pressure of 1 atm.
Step 1: Given Quantities & Unit Harmonization
- Vi=2 L,Vf=10 L,ΔV=8 L
- External pressure: pex=1 atm
- Unit conversion: 1 L⋅atm=101.325 J
Step 2: Fundamental Governing Formula
w=−pexΔV,q=−w (for isothermal ideal gas)
Step 3: Direct Substitution & Arithmetic Computation
w=−1 atm×(10−2) L=−8 L⋅atm
Converting to joules:
w=−8×101.325 J=−810.6 J
Heat absorbed:
q=−w=+8 L⋅atm=+810.6 J
Step 4: Physical Significance & Laboratory Insight
Expansion against a finite resisting pressure forces the gas to do work on the surroundings. To maintain constant temperature, the gas absorbs an equivalent quantity of heat (810.6 J) from the thermal reservoir.
NCERT Problem 5.4 (Step-by-Step Solution):
Consider the expansion given in Problem 5.2, for 1 mol of an ideal gas conducted reversibly.
Step 1: Given Quantities & Unit Harmonization
- n=1.0 mol
- T=298.15 K
- Vi=2.0 L,Vf=10.0 L⟹ViVf=5.0
- R=8.314 J⋅K−1⋅mol−1 (or 0.08206 L⋅atm⋅K−1⋅mol−1)
- log10(5)=0.6990
Step 2: Fundamental Governing Formula
wrev=−2.303nRTlog10(ViVf)
Step 3: Direct Substitution & Arithmetic Computation
In L⋅atm:
wrev=−2.303×(1.0)×(0.08206)×(298.15)×0.6990=−39.37 L⋅atm
In Joules:
wrev=−2.303×(1.0 mol)×(8.314 J⋅K−1⋅mol−1)×(298.15 K)×0.6990
wrev=−3988.4 J=−3.988 kJ
Because the process is isothermal (ΔU=0):
q=−wrev=+39.37 L⋅atm=+3.988 kJ
Step 4: Physical Significance & Laboratory Insight
Notice that reversible work (−39.37 L⋅atm) is nearly five times greater in magnitude than single-step irreversible work (−8.0 L⋅atm). An infinite number of infinitesimal steps extracts maximum mechanical work from the gas.
Interactive Simulation Experiment: Piston Gas & Indicator Lab
Open the Piston & Gas tab in the simulation suite:
- Set initial volume to 2.0 L and pressure to 10.0 atm.
- Choose Single-Step Irreversible Expansion against 1.0 atm. Note the shaded rectangular work area (w=−8.0 L⋅atm).
- Reset and select Reversible Isothermal Expansion. Watch the piston move smoothly through multiple equilibrium points. Observe that the work area under the hyperbolic PV curve expands to −39.37 L⋅atm.
5.4.1 Definition of Enthalpy as a State Function
In a chemistry laboratory, the majority of chemical reactions are carried out in open vessels (beakers, flasks, test tubes) under constant atmospheric pressure (p=constant), rather than in sealed constant-volume bombs.
Applying the First Law under constant pressure conditions:
ΔU=qp+w=qp−pΔV
Rearranging for heat absorbed at constant pressure:
qp=ΔU+pΔV
Writing ΔU=U2−U1 and ΔV=V2−V1:
qp=(U2−U1)+p(V2−V1)=(U2+pV2)−(U1+pV1)
This prompts the introduction of a new thermodynamic state function, the Enthalpy (H), derived from the Greek word enthalpien (meaning to heat or warm):
H=U+pV
Because U, p, and V are all state functions, H is strictly a state function. Therefore, the enthalpy change for a finite process is:
ΔH=H2−H1=qp
Key Principle:
The change in enthalpy of a system during a chemical or physical transformation is quantitatively equal to the heat absorbed or released at constant pressure.
- Exothermic Reaction: System releases heat to surroundings ⟹qp<0⟹ΔH<0.
- Endothermic Reaction: System absorbs heat from surroundings ⟹qp>0⟹ΔH>0.
5.4.2 Relationship Between DeltaH and DeltaU
Differentiating the enthalpy equation for a finite transformation:
ΔH=ΔU+Δ(pV)
If pressure is maintained constant:
ΔH=ΔU+pΔV
For chemical reactions involving only condensed phases (solids and liquids), volume changes upon heating or reacting are minuscule (ΔV≈0). Consequently, for solid-liquid reactions:
ΔH≈ΔU
However, when chemical reactions involve gases, the volume occupied by gaseous products can differ substantially from gaseous reactants. Assuming ideal gas behavior for all gaseous components (pV=nRT):
pVA=nARTandpVB=nBRT
Subtracting the reactant state from the product state:
p(VB−VA)=(nB−nA)RT⟹pΔV=ΔngRT
Where Δng is defined as:
Δng=∑ngaseous products−∑ngaseous reactants
Substituting into the enthalpy equation yields the core relationship:
ΔH=ΔU+ΔngRT
| Reaction Type | Stoichiometric Change | Enthalpy vs. Internal Energy | Classic Chemical Example |
|---|
| Δng=0 | Gaseous moles conserved | ΔH=ΔU | H2(g)+Cl2(g)→2HCl(g) |
| Δng>0 | Gaseous moles expand | ΔH>ΔU | PCl5(g)→PCl3(g)+Cl2(g) |
| Δng<0 | Gaseous moles contract | ΔH<ΔU | N2(g)+3H2(g)→2NH3(g) |
NCERT Problem 5.5 (Step-by-Step Solution):
If water vapour is assumed to be a perfect gas, molar enthalpy change for vaporisation of 1 mol of water at 1 bar and 100∘C is 41.00 kJ⋅mol−1. Calculate the internal energy change when 1 mol of water is vaporised at 1 bar pressure and 100∘C.
Step 1: Given Quantities & Unit Harmonization
- Chemical transformation: H2O(l)→H2O(g)
- Enthalpy of vaporization: ΔvapH=+41.00 kJ⋅mol−1
- Temperature: T=100∘C=373.15 K
- Gas constant: R=8.314 J⋅K−1⋅mol−1=8.314×10−3 kJ⋅K−1⋅mol−1
- Change in gaseous moles: Δng=1 mol (gas)−0 mol (liquid)=+1.0 mol
Step 2: Fundamental Governing Formula
ΔH=ΔU+ΔngRT⟹ΔU=ΔH−ΔngRT
Step 3: Direct Substitution & Arithmetic Computation
Compute the work of expansion:
ΔngRT=(1.0 mol)×(8.314×10−3 kJ⋅K−1⋅mol−1)×(373.15 K)=3.102 kJ⋅mol−1
Compute internal energy change:
ΔU=41.00 kJ⋅mol−1−3.102 kJ⋅mol−1=37.898 kJ⋅mol−1≈37.90 kJ⋅mol−1
Step 4: Physical Significance & Laboratory Insight
Of the 41.00 kJ of thermal energy supplied to vaporize one mole of liquid water at 100∘C, 37.90 kJ is utilized internally to overcome intermolecular hydrogen bonding networks, while 3.10 kJ is expended pushing back the ambient atmosphere (pΔV work).
5.4.3 Heat Capacity and Specific Heat
When heat is absorbed by a substance, its temperature increases. The temperature increment ΔT is directly proportional to the quantity of heat transferred:
q=CΔT
The proportionality factor C is termed the heat capacity of the system:
- It is an extensive property with units of J⋅K−1.
- When C is large, absorbing a large quantity of thermal energy produces only a small temperature change (for instance, liquid water).
To establish an intensive property independent of sample size:
- Specific Heat Capacity (c): The quantity of heat required to raise the temperature of one unit mass (1 g or 1 kg) of a substance by one Kelvin:
q=m⋅c⋅ΔT
Units: J⋅g−1⋅K−1 or J⋅kg−1⋅K−1.
- Molar Heat Capacity (Cm): The quantity of heat required to raise the temperature of one mole of a substance by one Kelvin:
Cm=nC,q=n⋅Cm⋅ΔT
Units: J⋅K−1⋅mol−1.
5.4.4 Derivation of the Meyer Relation (Cp−CV=R) for an Ideal Gas
Because the state of a gas can be altered under conditions of constant volume or constant pressure, two distinct heat capacities are defined:
- Heat Capacity at Constant Volume (CV):
qV=ΔU=CVΔT⟹CV=(∂T∂U)V
- Heat Capacity at Constant Pressure (Cp):
qp=ΔH=CpΔT⟹Cp=(∂T∂H)p
To derive their relationship for 1 mole of an ideal gas:
- From the definition of enthalpy:
H=U+pV
- For one mole of an ideal gas, pV=RT. Substituting gives:
H=U+RT
- Differentiating with respect to temperature:
dTdH=dTdU+R
- Substituting Cp=dTdH and CV=dTdU:
Cp=CV+R⟹Cp−CV=R
Physical Reason Why Cp>CV:
When an ideal gas is heated at constant volume, all supplied heat is converted into molecular kinetic energy, raising the temperature directly (no work is performed). When heated at constant pressure, the gas expands against the atmosphere, so extra energy must be supplied to perform mechanical expansion work (pΔV=RΔT) while achieving the same temperature rise.
NCERT Problem 5.9 (Step-by-Step Solution):
Calculate the number of kJ of heat necessary to raise the temperature of 60.0 g of aluminium from 35∘C to 55∘C. Molar heat capacity of Al is 24 J⋅mol−1⋅K−1. Molar mass of Al=27.0 g/mol.
Step 1: Given Quantities & Unit Harmonization
- Mass of aluminium: m=60.0 g
- Molar mass: M=27.0 g/mol
- Initial temperature: T1=35∘C
- Final temperature: T2=55∘C⟹ΔT=(55−35)=20 K
- Molar heat capacity: Cm=24.0 J⋅mol−1⋅K−1
Step 2: Fundamental Governing Formula
n=Mm,q=n⋅Cm⋅ΔT
Step 3: Direct Substitution & Arithmetic Computation
n=27.0 g/mol60.0 g=2.222 mol
q=(2.222 mol)×(24.0 J⋅mol−1⋅K−1)×(20 K)=1066.67 J=1.067 kJ
Step 4: Physical Significance & Laboratory Insight
Supplying 1.067 kJ of energy elevates the lattice vibrational kinetic energies of 2.222 moles of aluminium atoms across the 20 K temperature interval.
Energy changes accompanying physical transformations or chemical reactions are determined experimentally using calorimetry.
5.5.1 Constant-Volume Bomb Calorimetry (DeltaU Measurement)
To measure the heat of combustion at constant volume, a bomb calorimeter is employed:
- A known mass of combustible sample is placed in a platinum cup inside a heavy-walled, sealed steel pressure vessel (the bomb).
- The bomb is charged with pure dioxygen under high pressure (≈25 to 30 atm) and submerged in a thermally insulated water bath equipped with a precision thermometer and mechanical stirrer.
- The sample is ignited electrically. The heat liberated passes into the surrounding water and calorimeter components.
- Because the steel bomb is rigid and completely sealed:
ΔV=0⟹w=−pexΔV=0
- From the First Law:
ΔU=qV
- The total heat absorbed by the calorimeter is:
qcalorimeter=CV⋅ΔT
- By conservation of energy, the heat liberated by the combustion reaction is:
qreaction=−qcalorimeter=−CV⋅ΔT
5.5.2 Constant-Pressure Calorimetry (DeltaH Measurement)
For reactions conducted in aqueous solutions (such as acid-base neutralization or precipitation), heat is measured in a coffee cup calorimeter operating under ambient atmospheric pressure:
- The polystyrene cup provides thermal insulation while remaining open to the atmosphere.
- Pressure remains constant (p=patm).
- The heat measured directly reflects the enthalpy of reaction:
qp=ΔrH=−msolution⋅cs⋅ΔT
NCERT Problem 5.6 (Step-by-Step Solution):
1.0 g of graphite is burnt in a bomb calorimeter in excess of oxygen at 298 K and 1 atm pressure according to the equation:
C(graphite)+O2(g)→CO2(g)
During the reaction, temperature rises from 298.0 K to 299.0 K. If the heat capacity of the bomb calorimeter is 20.7 kJ/K, what is the enthalpy change for the above reaction at 298 K and 1 atm?
Step 1: Given Quantities & Unit Harmonization
- Mass of graphite: m=1.0 g
- Molar mass of carbon: M=12.01 g/mol
- Temperature rise: ΔT=(299.0−298.0)=1.0 K
- Calorimeter heat capacity: CV=20.7 kJ/K
Step 2: Fundamental Governing Formula
qreaction=−CV⋅ΔT,ΔU=nqreaction,ΔH=ΔU+ΔngRT
Step 3: Direct Substitution & Arithmetic Computation
Heat absorbed by calorimeter:
q=CV×ΔT=20.7 kJ/K×1.0 K=20.7 kJ
Heat of reaction for 1.0 g:
qreaction=−20.7 kJ
Moles of carbon burned:
n=12.01 g/mol1.0 g=0.08326 mol
Molar internal energy change:
ΔU=1.0 g−20.7 kJ×12.01 g/mol=−2.486×102 kJ/mol=−248.6 kJ/mol
Evaluate Δng for C(s)+O2(g)→CO2(g):
Δng=1 mol (CO2)−1 mol (O2)=0
Therefore:
ΔH=ΔU+(0)RT=ΔU=−2.486×102 kJ/mol=−248.6 kJ/mol
Step 4: Physical Significance & Laboratory Insight
Because the number of moles of gas is identically conserved during complete combustion of graphite to carbon dioxide, no pressure-volume expansion work is performed. Hence, the constant-volume energy change ΔU and constant-pressure enthalpy change ΔH are numerically identical.
NCERT Problem 5.8 (Step-by-Step Solution):
The reaction of cyanamide, NH2CN(s), with dioxygen was carried out in a bomb calorimeter, and ΔU was found to be −742.7 kJ⋅mol−1 at 298 K. Calculate enthalpy change for the reaction at 298 K:
NH2CN(s)+23O2(g)→N2(g)+CO2(g)+H2O(l)
Step 1: Given Quantities & Unit Harmonization
- ΔU=−742.7 kJ⋅mol−1
- T=298.15 K
- R=8.314×10−3 kJ⋅K−1⋅mol−1
- Gaseous products: 1 mol N2+1 mol CO2=2 mol
- Gaseous reactants: 23 mol O2=1.5 mol
- Gaseous change: Δng=2−1.5=+0.5 mol
Step 2: Fundamental Governing Formula
ΔH=ΔU+ΔngRT
Step 3: Direct Substitution & Arithmetic Computation
ΔngRT=(0.5 mol)×(8.314×10−3 kJ⋅K−1⋅mol−1)×(298.15 K)=+1.240 kJ⋅mol−1
ΔH=−742.7 kJ⋅mol−1+1.240 kJ⋅mol−1=−741.46 kJ⋅mol−1≈−741.5 kJ⋅mol−1
Step 4: Physical Significance & Laboratory Insight
Because half a mole of gas is generated during combustion, the system performs expansion work against the surroundings at constant pressure, making the enthalpy change slightly less negative (less exothermic) than the constant-volume internal energy change.
Interactive Simulation Experiment: Reaction Calorimeter & Temperature Lab
Open the Calorimeter tab in the simulation suite:
- Select the Combustion of Graphite preset in the Bomb Calorimeter mode.
- Observe the virtual temperature sensor rise from 298.0 K to 299.0 K.
- Verify that the computer-logged heat output matches qV=−20.7 kJ.
- Switch to Reaction Temperature Lab and compare an exothermic profile (neutralization of HCl+NaOH, temperature rises, ΔH<0) against an endothermic profile (dissolution of NH4NO3, temperature drops, ΔH>0).
5.6.1 Standard State Convention
Because the enthalpy change of a reaction varies with temperature and pressure, standard thermodynamic reference conditions are established:
Standard State Definition:
The standard state of a chemical substance at a specified temperature (customarily 298.15 K=25∘C) is its pure, stable form of aggregation at a pressure of exactly 1 bar (105 Pa).
- For a gas: Pure gas behaving ideally at p=1 bar.
- For a liquid or solid: Pure substance at p=1 bar.
- For a solute in solution: Standard concentration of 1.0 mol⋅L−1 (1 M) at p=1 bar.
Standard state quantities are designated by the superscript symbol ∘ (or ⊖), for example: ΔrH∘.
5.6.2 Standard Enthalpy of Formation (ΔfH∘)
Standard Molar Enthalpy of Formation Definition:
The standard enthalpy change accompanying the formation of exactly one mole of a chemical compound in its standard state from its constituent elements in their most stable reference states of aggregation at 298.15 K and 1 bar pressure.
By international thermodynamic convention:
ΔfH∘[element in its reference state]=0.00 kJ⋅mol−1
| Element | Most Stable Reference State at 298 K, 1 bar | Standard Enthalpy of Formation (ΔfH∘) |
|---|
| Carbon | Graphite, C(graphite, s) | 0.00 kJ/mol |
| Carbon | Diamond, C(diamond, s) | +1.89 kJ/mol (Not reference state) |
| Oxygen | Dioxygen gas, O2(g) | 0.00 kJ/mol |
| Oxygen | Ozone gas, O3(g) | +142.7 kJ/mol (Not reference state) |
| Hydrogen | Dihydrogen gas, H2(g) | 0.00 kJ/mol |
| Bromine | Liquid dibromine, Br2(l) | 0.00 kJ/mol |
| Chlorine | Dichlorine gas, Cl2(g) | 0.00 kJ/mol |
| Sulfur | Rhombic sulfur, Sα(rhombic, s) | 0.00 kJ/mol |
Enthalpy of Reaction from Standard Enthalpies of Formation
For any generalized chemical reaction:
∑biReactantsi→∑aiProductsi
The standard reaction enthalpy is computed via:
ΔrH∘=∑aiΔfH∘(products)−∑biΔfH∘(reactants)
Where ai and bi represent stoichiometric coefficients from the balanced chemical equation.
5.6.3 Hess's Law of Constant Heat Summation
Because enthalpy is a state function, the net enthalpy change between an initial state (reactants) and a final state (products) is completely path-independent.
Hess's Law of Constant Heat Summation:
If a chemical reaction can be expressed as the algebraic sum of a sequence of intermediate chemical reactions, the standard reaction enthalpy for the overall process is equal to the algebraic sum of the standard reaction enthalpies of each individual intermediate step at the same temperature:
ΔrH∘=ΔrH1∘+ΔrH2∘+ΔrH3∘+⋯
Rules for Manipulating Thermochemical Equations:
- Reversing an Equation: When a thermochemical reaction is written in reverse, the algebraic sign of ΔrH∘ must be inverted:
N2(g)+3H2(g)→2NH3(g),ΔrH∘=−92.4 kJ/mol
2NH3(g)→N2(g)+3H2(g),ΔrH∘=+92.4 kJ/mol
- Scaling Coefficients: Multiplying all stoichiometric coefficients in a balanced equation by a factor c scales the magnitude of ΔrH∘ by the same factor c.
- Algebraic Addition: When adding equations, chemical species appearing identically on both the reactant and product sides cancel out as spectator species.
NCERT Problem 5.9 (Step-by-Step Solution):
The combustion of one mole of benzene takes place at 298 K and 1 atm. After combustion, CO2(g) and H2O(l) are produced and 3267.0 kJ of heat is liberated. Calculate the standard enthalpy of formation, ΔfH∘ of benzene. Standard enthalpies of formation of CO2(g) and H2O(l) are −393.5 kJ⋅mol−1 and −285.83 kJ⋅mol−1 respectively.
Step 1: Given Quantities & Unit Harmonization
Target reaction (formation of benzene):
6C(graphite)+3H2(g)→C6H6(l),ΔfH∘=?
Given thermochemical data:
(1) C6H6(l)+215O2(g)→6CO2(g)+3H2O(l),ΔcH∘=−3267.0 kJ/mol
(2) C(graphite)+O2(g)→CO2(g),ΔfH∘=−393.5 kJ/mol
(3) H2(g)+21O2(g)→H2O(l),ΔfH∘=−285.83 kJ/mol
Step 2: Fundamental Governing Formula
Method A (Hess's Law Summation):
Target =6×(2)+3×(3)−(1)
Method B (Formation Formula):
ΔrH∘=∑ΔfH∘(products)−∑ΔfH∘(reactants)
Step 3: Direct Substitution & Arithmetic Computation
Using Method B on the combustion reaction (1):
ΔcH∘=[6ΔfH∘(CO2)+3ΔfH∘(H2O)]−[ΔfH∘(C6H6)+215ΔfH∘(O2)]
Substituting known values (ΔfH∘(O2)=0):
−3267.0=[6(−393.5)+3(−285.83)]−[ΔfH∘(C6H6)+0]
−3267.0=[−2361.0−857.49]−ΔfH∘(C6H6)
−3267.0=−3218.49−ΔfH∘(C6H6)
ΔfH∘(C6H6)=−3218.49+3267.0=+48.51 kJ⋅mol−1
Step 4: Physical Significance & Laboratory Insight
The standard enthalpy of formation of liquid benzene is positive (+48.51 kJ/mol), establishing that benzene is an endothermic compound with higher potential energy than its constituent elements in their reference states.
Interactive Simulation Experiment: Hess's Law Puzzle & Reaction Builder
Open the Hess's Law tab in the simulation suite:
- Select the Benzene Formation puzzle.
- Use the multiplier slider to scale the carbon combustion equation by 6. Observe the enthalpy card dynamically scale to −2361.0 kJ.
- Scale the water formation equation by 3 (enthalpy becomes −857.49 kJ).
- Click Invert Direction on the benzene combustion equation; observe the sign invert from −3267.0 kJ to +3267.0 kJ.
- Click Sum Reactions. Verify spectator O2,CO2,H2O cancel out, leaving the net target reaction with ΔfH∘=+48.51 kJ/mol.
5.7.1 Enthalpy of Phase Transformations
| Transformation | Process Description | NCERT Example | Standard Enthalpy Value |
|---|
| Enthalpy of Fusion (ΔfusH∘) | Heat required to melt one mole of a solid substance at its melting point under standard pressure (1 bar). | H2O(s)→H2O(l) at 273.15 K | +6.01 kJ⋅mol−1 |
| Enthalpy of Vaporization (ΔvapH∘) | Heat required to vaporize one mole of a liquid at its boiling point under standard pressure (1 bar). | H2O(l)→H2O(g) at 373.15 K | +40.79 kJ⋅mol−1 |
| Enthalpy of Sublimation (ΔsubH∘) | Enthalpy change when one mole of a solid transforms directly into vapor under standard pressure (1 bar). | CO2(s, dry ice)→CO2(g) at 195 K | +25.2 kJ⋅mol−1 |
Phase transformations obey Hess's Law:
ΔsubH∘=ΔfusH∘+ΔvapH∘
The magnitude of ΔvapH∘ directly reflects the strength of intermolecular forces in the condensed phase. Water exhibits a high vaporization enthalpy (40.79 kJ/mol) due to extensive three-dimensional hydrogen bonding networks, whereas acetone requires only 29.1 kJ/mol due to weaker dipole-dipole attractions.
5.7.2 Enthalpy of Combustion (ΔcH∘)
Standard Enthalpy of Combustion Definition:
The enthalpy change accompanying the complete combustion of one mole of a substance in its standard state with excess dioxygen, with all reactants and products measured in their standard states at the specified temperature.
Combustion reactions are invariably exothermic (ΔcH∘<0). They represent the energetic foundation of industrial manufacturing, heating, and biological metabolism:
- Complete combustion of butane in LPG cylinders:
C4H10(g)+213O2(g)→4CO2(g)+5H2O(l),ΔcH∘=−2658.0 kJ⋅mol−1
- Cellular respiration of D-glucose in living organisms:
C6H12O6(s)+6O2(g)→6CO2(g)+6H2O(l),ΔcH∘=−2802.0 kJ⋅mol−1
5.7.3 Enthalpy of Atomization (ΔaH∘)
The enthalpy change accompanying the complete cleavage of all chemical bonds in one mole of a substance to obtain isolated atoms in the gas phase:
- For diatomic molecules, it is equal to the bond dissociation enthalpy:
H2(g)→2H(g),ΔaH∘=+435.0 kJ⋅mol−1
- For metals, it equals the enthalpy of sublimation:
Na(s)→Na(g),ΔaH∘=+108.4 kJ⋅mol−1
- For polyatomic molecules, it equals the sum of all bond dissociation energies:
CH4(g)→C(g)+4H(g),ΔaH∘=+1665.0 kJ⋅mol−1
5.7.4 Bond Enthalpy (ΔbondH∘)
In chemical reactions, old bonds in reactant molecules are severed (requiring energy input, an endothermic process) and new bonds in product molecules are forged (liberating energy, an exothermic process).
Two distinct terms are utilized depending on molecular complexity:
- Bond Dissociation Enthalpy: The enthalpy required to break one mole of a specific covalent bond in a gaseous diatomic molecule.
Cl2(g)→2Cl(g),ΔCl−ClH∘=+242.0 kJ⋅mol−1
- Mean (Average) Bond Enthalpy: In polyatomic molecules, stepwise bond cleavage reveals that each successive bond requires a different quantity of energy due to electronic redistribution in the remaining radical fragments:
- Step 1: CH4(g)→CH3(g)+H(g),ΔH1=+427 kJ/mol
- Step 2: CH3(g)→CH2(g)+H(g),ΔH2=+439 kJ/mol
- Step 3: CH2(g)→CH(g)+H(g),ΔH3=+452 kJ/mol
- Step 4: CH(g)→C(g)+H(g),ΔH4=+347 kJ/mol
Total atomization enthalpy: ΔaH∘=427+439+452+347=1665 kJ/mol.
The mean bond enthalpy for the C−H bond is the arithmetic average:
ΔC−HH∘=41ΔaH∘=41665=416.25 kJ⋅mol−1
Estimating Enthalpy of Reaction from Bond Enthalpies:
For all-gas-phase reactions, the standard enthalpy of reaction can be approximated:
ΔrH∘≈∑Bond Enthalpies of Reactants (bonds broken)−∑Bond Enthalpies of Products (bonds formed)
Interactive Simulation Experiment: Bond Breaking & Making Lab
Open the Bond Enthalpy tab in the simulation suite:
- Select the reaction CH4(g)+2O2(g)→CO2(g)+2H2O(g).
- Click Break Reactant Bonds. The tool severs 4×C−H (4×414=1656 kJ) and 2×O=O (2×498=996 kJ). Energy absorbed: +2652 kJ.
- Click Form Product Bonds. The tool creates 2×C=O (2×741=1482 kJ) and 4×O−H (4×464=1856 kJ). Energy liberated: −3338 kJ.
- Observe the net energy balance: ΔrH∘≈2652−3338=−686 kJ/mol.
5.7.5 Lattice Enthalpy and the Born-Haber Cycle
Lattice Enthalpy (ΔlatticeH∘) Definition:
The enthalpy change accompanying the complete dissociation of one mole of a solid ionic crystalline compound into its constituent isolated gaseous ions:
MX(s)→M+(g)+X−(g),ΔlatticeH∘>0
Because gaseous ions cannot be pulled apart directly in a calorimeter without solvent or surface interactions, lattice enthalpies are evaluated indirectly using a thermodynamic closed cycle devised by Max Born and Fritz Haber: the Born-Haber Cycle.
Deconstruction of the Born-Haber Cycle for Sodium Chloride (mathrmNaCl):
- Sublimation of Metallic Sodium:
Na(s)→Na(g),ΔsubH∘=+108.4 kJ/mol
- Ionization of Gaseous Sodium Atoms:
Na(g)→Na+(g)+e−,ΔiH∘=+496.0 kJ/mol
- Dissociation of Dichlorine Molecules:
21Cl2(g)→Cl(g),21ΔbondH∘=+121.0 kJ/mol
- Electron Gain by Gaseous Chlorine Atoms:
Cl(g)+e−→Cl−(g),ΔegH∘=−348.6 kJ/mol
- Condensation of Gaseous Ions into Crystal Lattice:
Na+(g)+Cl−(g)→NaCl(s),−ΔlatticeH∘
- Direct Standard Formation Reaction:
Na(s)+21Cl2(g)→NaCl(s),ΔfH∘=−411.2 kJ/mol
Applying Hess's Law around the closed cycle:
ΔfH∘=ΔsubH∘+ΔiH∘+21ΔbondH∘+ΔegH∘−ΔlatticeH∘
Rearranging to solve for the lattice dissociation enthalpy of NaCl:
ΔlatticeH∘=ΔsubH∘+ΔiH∘+21ΔbondH∘+ΔegH∘−ΔfH∘
ΔlatticeH∘=108.4+496.0+121.0−348.6−(−411.2)=+788.0 kJ⋅mol−1
Enthalpy of Solution and Hydration:
When an ionic solid dissolves in water, two competing energetic processes take place:
- The ionic lattice must be torn apart into gaseous ions: requires input of ΔlatticeH∘.
- The separated gaseous ions are solvated by polar water dipoles: releases ΔhydH∘.
ΔsolH∘=ΔlatticeH∘+ΔhydH∘
For NaCl:
ΔsolH∘=(+788.0 kJ/mol)+(−784.0 kJ/mol)=+4.0 kJ⋅mol−1
The net dissolution process is slightly endothermic (+4.0 kJ/mol), causing a slight drop in temperature when table salt dissolves in water.
5.8.1 The Physical Limitation of the First Law
The First Law of Thermodynamics establishes the strict conservation of energy (ΔU=q+w), but it places zero restriction on the direction in which natural processes unfold:
- When a hot copper block is brought into contact with a cold copper block, heat flows spontaneously from the hot body to the cold body until thermal equilibrium is attained. The reverse process (heat spontaneously flowing from the cold block to make the hot block hotter) would conserve total energy perfectly, yet it never occurs in nature.
- When the valve between an evacuated flask and a gas-filled flask is opened, gas expands spontaneously to occupy the total available volume. The gas never spontaneously compresses itself back into a single flask.
- A drop of ink placed in water diffuses until uniformly distributed; it never un-diffuses back into an isolated droplet.
A process that has the natural potential to occur without the continuous intervention of an external driving agency is termed a spontaneous process. Spontaneous processes are inherently irreversible.
5.8.2 Is Decrease in Enthalpy the Criterion for Spontaneity?
In classical mechanics, physical systems spontaneously minimize their potential energy: water flows downhill, a stretched spring contracts, and a falling stone strikes the ground.
By analogy, early thermochemists postulated that chemical reactions might proceed spontaneously solely in the direction of lower enthalpy (exothermic reactions, ΔH<0):
21N2(g)+23H2(g)→NH3(g),ΔrH∘=−46.1 kJ/mol(Spontaneous)
H2(g)+21O2(g)→H2O(l),ΔrH∘=−285.8 kJ/mol(Spontaneous)
However, numerous endothermic processes (ΔH>0) occur spontaneously in nature:
- Evaporation of liquid water at room temperature:
H2O(l)→H2O(g),ΔvapH∘=+44.01 kJ/mol(Spontaneous)
- Dissolution of ammonium nitrate in water:
NH4NO3(s)+aq→NH4+(aq)+NO3−(aq),ΔH>0(Spontaneous)
- Thermal decomposition of limestone at high temperatures:
CaCO3(s)→CaO(s)+CO2(g),ΔrH∘=+178.3 kJ/mol(Spontaneous above 1100 K)
Furthermore, when two inert ideal gases diffuse into each other inside an isolated chamber, the enthalpy change is exactly zero (ΔH=0), yet the mixing process is completely spontaneous and irreversible.
Conclusion:
A decrease in enthalpy is a contributing factor, but not the sole criterion for spontaneity. A second thermodynamic driving force is required.
5.8.3 The Concept of Entropy (S)
Consider the spontaneous interdiffusion of two gases (A and B) initially separated by a partition. Before removal of the partition, gas A is confined to the left half and gas B to the right half. The state is highly ordered and predictable: any molecule sampled from the left is guaranteed to be A.
When the partition is withdrawn, molecules diffuse randomly until uniformly dispersed. Sampling a molecule now carries statistical uncertainty. The system has transitioned from an ordered state to a disordered, chaotic state.
To quantify the degree of disorder, randomness, and energetic dispersal in a system, we introduce a thermodynamic state function: Entropy, denoted by S.
Thermodynamic Definition of Entropy Change
When thermal energy is added to a system, it increases random molecular motions (translation, rotation, vibration), increasing disorder. The randomizing effect of heat depends directly on the temperature at which it is introduced:
- Adding 100 J of heat to a cold system (low temperature, where particles are quiet) introduces a dramatic increase in disorder.
- Adding the same 100 J of heat to a hot system (high temperature, where particles are already violently chaotic) produces only a negligible percentage increase in disorder.
Therefore, the change in entropy is inversely proportional to temperature. For a reversible transformation:
ΔS=Tqrev
Units of entropy: J⋅K−1 (or J⋅K−1⋅mol−1 for molar entropy).
5.8.4 The Second Law of Thermodynamics
The Second Law of Thermodynamics:
In any spontaneous (naturally occurring) process, the total entropy of the universe (system plus surroundings) must strictly increase:
ΔStotal=ΔSsystem+ΔSsurroundings>0
At thermodynamic equilibrium:
ΔStotal=0
For a non-spontaneous process:
ΔStotal<0
Entropy of Physical States:
For any substance, the degree of spatial and energetic disorder follows the sequence:
Ssolid≪Sliquid≪Sgas
- In a crystalline solid, atoms are locked into rigid lattice sites with minimal entropy.
- In a liquid, molecules translate and tumble while remaining in close contact.
- In a gas, molecules fly freely across vast intermolecular volumes, maximizing spatial disorder and entropy.
NCERT Problem 5.10 (Step-by-Step Solution):
Predict in which of the following processes entropy increases or decreases:
(i) A liquid crystallizes into a solid.
(ii) Temperature of a crystalline solid is raised from 0 K to 115 K.
(iii) 2NaHCO3(s)→Na2CO3(s)+CO2(g)+H2O(g)
(iv) H2(g)→2H(g)
Step 1: Given Quantities & Qualitative Criteria
State change criteria: Formation of gases or increased temperature increases entropy; crystallization or decreasing temperature decreases entropy.
Step 2: Fundamental Governing Formula
ΔS=Sfinal−Sinitial
Step 3: Direct Analysis & Reasoning
- (i) Entropy Decreases (ΔS<0): Upon freezing, mobile liquid molecules become locked into a highly ordered crystalline lattice, reducing randomness.
- (ii) Entropy Increases (ΔS>0): At 0 K, constituent particles are static. As temperature rises to 115 K, thermal energy excites lattice vibrations, increasing disorder.
- (iii) Entropy Increases (ΔS>0): Two moles of solid reactant decompose to yield one mole of solid plus two moles of gas (Δng=+2). Gaseous products possess vastly higher entropy than solids.
- (iv) Entropy Increases (ΔS>0): One mole of diatomic molecules dissociates into two moles of independent gaseous atoms. The doubling of particles increases configurational microstates.
Step 4: Physical Significance & Laboratory Insight
Tracking changes in the number of gaseous moles (Δng) provides a reliable qualitative indicator of the sign of ΔrS∘.
NCERT Problem 5.11 (Step-by-Step Solution):
For the oxidation of iron:
4Fe(s)+3O2(g)→2Fe2O3(s)
The entropy change of the system is −549.4 J⋅K−1⋅mol−1 at 298 K. In spite of the negative entropy change of the system, why is this reaction spontaneous? (Given ΔrH∘=−1648.0×103 J⋅mol−1).
Step 1: Given Quantities & Unit Harmonization
- ΔSsystem=−549.4 J⋅K−1⋅mol−1
- ΔrH∘=−1648.0×103 J⋅mol−1
- T=298.15 K
Step 2: Fundamental Governing Formula
The heat liberated by the exothermic reaction is absorbed by the surroundings at constant pressure:
qsurroundings=−ΔrH∘
ΔSsurroundings=Tqsurroundings=T−ΔrH∘
ΔStotal=ΔSsystem+ΔSsurroundings
Step 3: Direct Substitution & Arithmetic Computation
ΔSsurroundings=298.15 K−(−1648.0×103 J⋅mol−1)=+5527.4 J⋅K−1⋅mol−1
ΔStotal=−549.4+5527.4=+4978.0 J⋅K−1⋅mol−1
Step 4: Physical Significance & Laboratory Insight
Although iron and oxygen gas become locked into an ordered crystalline oxide lattice (decreasing the system entropy), the massive quantity of heat released into the surroundings (1648 kJ) creates enormous thermal agitation in the ambient environment. Because ΔSsurroundings≫∣ΔSsystem∣, the net entropy change of the universe is overwhelmingly positive (+4978 J/K), driving the spontaneous rusting of iron.
Evaluating the spontaneity of a chemical reaction using ΔStotal=ΔSsys+ΔSsurr requires calculating entropy changes for both the reaction vessel and the entire surrounding universe.
To evaluate spontaneity using properties pertaining exclusively to the system, the American mathematical physicist Josiah Willard Gibbs defined a new thermodynamic function: the Gibbs Energy (or Gibbs Free Energy), denoted by G:
G=H−TS
Because H, T, and S are state functions, G is an extensive property and a state function.
5.9.1 Derivation of the Gibbs Equation
For an isothermal transformation (T=constant):
ΔGsys=ΔHsys−TΔSsys
We know from Section 5.8 that the entropy change of the surroundings is:
ΔSsurr=Tqsurr=T−ΔHsys
Substituting into the total entropy expression:
ΔStotal=ΔSsys+ΔSsurr=ΔSsys−TΔHsys
Multiplying through by absolute temperature T:
TΔStotal=TΔSsys−ΔHsys=−(ΔHsys−TΔSsys)
Recognizing the right-hand term as −ΔGsys:
TΔStotal=−ΔGsys⟹ΔGsys=−TΔStotal
5.9.2 Criterion for Spontaneity at Constant T and p
Because absolute temperature T is always positive (T>0 K), the algebraic sign of ΔGsys is strictly opposite to that of ΔStotal:
| Value of ΔG | Value of ΔStotal | Spontaneity Status | Physical Interpretation |
|---|
| ΔG<0 | ΔStotal>0 | Spontaneous (Exergonic) | Reaction proceeds spontaneously in the forward direction as written. |
| ΔG>0 | ΔStotal<0 | Non-Spontaneous (Endergonic) | Forward reaction cannot occur; reverse reaction is spontaneous. |
| ΔG=0 | ΔStotal=0 | Dynamic Equilibrium | System is at chemical equilibrium; no net reaction occurs. |
Physical Meaning of "Free" Energy:
In any process, the total enthalpy change ΔH represents total heat exchanged. The quantity TΔS represents bound energy that must be dissipated into molecular disorder and cannot be harnessed. Therefore, ΔG=ΔH−TΔS represents the net usable energy available to perform non-expansion (useful) work:
−ΔG=wuseful, max
5.9.3 Effect of Temperature on Reaction Spontaneity
The Gibbs-Helmholtz equation ΔrG∘=ΔrH∘−TΔrS∘ involves a competition between the enthalpy factor (favoring ΔH<0) and the entropy factor (favoring ΔS>0):
| Case | ΔrH∘ | ΔrS∘ | Sign of ΔrG∘ | Temperature Dependence & Spontaneity (NCERT Table 5.4) |
|---|
| Case 1 | Negative (−) | Positive (+) | Negative (−) | Spontaneous at all temperatures. Enthalpy and entropy factors both favor spontaneity. (2O3(g)→3O2(g)) |
| Case 2 | Negative (−) | Negative (−) | Negative (−) at low T<br>Positive (+) at high T | Spontaneous at low temperatures; non-spontaneous at high temperatures. (TΔS term dominates at elevated T). (Exothermic syntheses: N2+3H2→2NH3) |
| Case 3 | Positive (+) | Positive (+) | Positive (+) at low T<br>Negative (−) at high T | Non-spontaneous at low temperatures; becomes spontaneous at high temperatures. (TΔS outweighs ΔH). (Melting of ice, decomposition of CaCO3) |
| Case 4 | Positive (+) | Negative (−) | Positive (+) | Non-spontaneous at all temperatures. Both enthalpy and entropy oppose reaction. Forward reaction impossible. (3O2(g)→2O3(g)) |
Equilibrium Crossover Temperature (Teq):
For Cases 2 and 3, setting ΔrG∘=0 identifies the transition temperature where the reaction switches between spontaneity and non-spontaneity:
0=ΔrH∘−TeqΔrS∘⟹Teq=ΔrS∘ΔrH∘
5.9.4 The Third Law of Thermodynamics
As the temperature of a substance decreases, molecular thermal agitation (translation, rotation, vibration) slows down.
In 1906, Walther Nernst formulated the principle governing the low-temperature limit of entropy:
The Third Law of Thermodynamics:
The entropy of any pure, perfectly crystalline substance approaches zero as the absolute temperature approaches zero Kelvin:
limT→0 KS=0
Physical Foundation:
At absolute zero (0 K), all thermal motion ceases. For a perfect crystal, every constituent atom is located at its unique, lowest-energy lattice coordinate. In statistical mechanics, this corresponds to a single thermodynamic microstate (W=1). Applying Boltzmann's entropy formula:
S=kBlnW=kBln(1)=0
The Third Law enables evaluation of the absolute molar entropy (S∘) of pure substances by integrating heat capacity data from 0 K to temperature T:
S∘(T)=∫0TTCpdT+∑TphaseΔHphase
For a reversible chemical reaction proceeding toward equilibrium:
A+B⇌C+D
As reactants convert to products, the Gibbs energy of the reaction mixture decreases continuously until it reaches a minimum value. At this minimum, the slope of Gibbs energy with respect to reaction extent is zero:
ΔrG=0
5.10.1 Relationship Between ΔrG∘ and Equilibrium Constant (K)
The actual Gibbs energy change ΔrG at any arbitrary non-equilibrium composition is related to the standard Gibbs energy change ΔrG∘ by the relation:
ΔrG=ΔrG∘+RTlnQ
Where Q is the reaction quotient. At dynamic chemical equilibrium, ΔrG=0 and Q=K:
0=ΔrG∘+RTlnK
Rearranging yields the fundamental thermodynamic equation connecting thermodynamics to chemical equilibrium:
ΔrG∘=−RTlnK
Converting to common base-10 logarithms:
ΔrG∘=−2.303RTlog10K
Solving for the equilibrium constant K:
K=e−RTΔrG∘=10−2.303RTΔrG∘
| Standard Gibbs Energy | Equilibrium Constant | Reaction Extent at Equilibrium |
|---|
| ΔrG∘<0 (strongly negative) | K≫1 | Products predominate heavily; reaction proceeds to near completion. |
| ΔrG∘=0 | K=1 | Reactants and products are present in comparable concentrations. |
| ΔrG∘>0 (strongly positive) | K≪1 | Reactants predominate heavily; negligible product formation. |
NCERT Problem 5.12 (Step-by-Step Solution):
Calculate ΔrG∘ for conversion of oxygen to ozone, 23O2(g)→O3(g) at 298 K, if Kp for this conversion is 2.47×10−29.
Step 1: Given Quantities & Unit Harmonization
- Reaction: 23O2(g)→O3(g)
- Temperature: T=298.15 K
- Equilibrium constant: Kp=2.47×10−29
- Gas constant: R=8.314 J⋅K−1⋅mol−1
Step 2: Fundamental Governing Formula
ΔrG∘=−2.303RTlog10(Kp)
Step 3: Direct Substitution & Arithmetic Computation
log10(2.47×10−29)=log10(2.47)−29=0.3927−29=−28.6073
ΔrG∘=−2.303×(8.314 J⋅K−1⋅mol−1)×(298.15 K)×(−28.6073)
ΔrG∘=−5708.8×(−28.6073)=+163313 J⋅mol−1=+163.31 kJ⋅mol−1≈+163 kJ⋅mol−1
Step 4: Physical Significance & Laboratory Insight
The enormous positive value of ΔrG∘ (+163.3 kJ/mol) aligns with the minuscule equilibrium constant (10−29). Ozone will not form spontaneously from atmospheric dioxygen at room temperature without electrical discharge or ultraviolet photolysis.
NCERT Problem 5.13 (Step-by-Step Solution):
Find out the value of the equilibrium constant for the following reaction at 298 K:
2NH3(g)+CO2(g)⇌NH2CONH2(aq)+H2O(l)
Standard Gibbs energy change, ΔrG∘ at the given temperature is −13.6 kJ⋅mol−1.
Step 1: Given Quantities & Unit Harmonization
- ΔrG∘=−13.6 kJ⋅mol−1=−13600 J⋅mol−1
- T=298.15 K
- R=8.314 J⋅K−1⋅mol−1
Step 2: Fundamental Governing Formula
log10K=2.303RT−ΔrG∘
Step 3: Direct Substitution & Arithmetic Computation
log10K=2.303×(8.314 J⋅K−1⋅mol−1)×(298.15 K)−(−13600 J⋅mol−1)=5708.813600=2.3823
Taking the antilogarithm:
K=102.3823=100.3823×102≈2.41×102
Step 4: Physical Significance & Laboratory Insight
Because ΔrG∘ is negative, K>1 (2.4×102), confirming that the industrial synthesis of urea from ammonia and carbon dioxide is thermodynamically favorable at 298 K.
NCERT Problem 5.14 (Step-by-Step Solution):
At 60∘C, dinitrogen tetroxide is 50% dissociated. Calculate the standard free energy change at this temperature and at one atmosphere.
N2O4(g)⇌2NO2(g)
Step 1: Given Quantities & Unit Harmonization
- Total pressure: ptotal=1.0 atm
- Temperature: T=60∘C=333.15 K
- Degree of dissociation: α=0.50
Step 2: Fundamental Governing Formula
For the dissociation N2O4⇌2NO2:
- Initial moles: 1 mole of N2O4, 0 mole of NO2.
- Equilibrium moles: (1−α) moles of N2O4, 2α moles of NO2.
- Total equilibrium moles: ntotal=(1−α)+2α=1+α.
Mole fractions:
xN2O4=1+α1−α,xNO2=1+α2α
Partial pressures (pi=xi⋅ptotal):
Kp=pN2O4(pNO2)2=(1−α2)4α2ptotal
ΔrG∘=−RTlnKp=−2.303RTlog10Kp
Step 3: Direct Substitution & Arithmetic Computation
For α=0.50:
xN2O4=1+0.51−0.5=1.50.5=31
xNO2=1+0.52(0.5)=1.51.0=32
Partial pressures: pN2O4=31 atm, pNO2=32 atm.
Kp=1/3(2/3)2=1/34/9=34=1.333 atm
Compute ΔrG∘:
ΔrG∘=−2.303×(8.314 J⋅K−1⋅mol−1)×(333.15 K)×log10(1.333)
log10(1.333)=0.1249
ΔrG∘=−2.303×8.314×333.15×0.1249=−796.8 J⋅mol−1≈−0.797 kJ⋅mol−1
Step 4: Physical Significance & Laboratory Insight
Because ΔrG∘ is slightly negative at 60∘C (−0.80 kJ/mol), the equilibrium constant Kp>1, reflecting a moderate tendency for N2O4 to dissociate into brown nitrogen dioxide vapor at elevated temperatures.
Interactive Simulation Experiment: Molecular Disorder & Gibbs Spontaneity Simulator
Open the Entropy & Spontaneity tab in the simulation suite:
- In the Molecular Disorder mode, drag the temperature slider from 0 K to 500 K.
- At 0 K, observe complete crystal lattice immobility (S=0, verifying Third Law).
- Increase temperature to view vibrational motion, melting to liquid, and gas vaporization with dispersed microstates.
- Switch to Spontaneity Simulator. Set ΔH=+40 kJ/mol and ΔS=+120 J⋅K−1⋅mol−1.
- Observe the real-time ΔG indicator gauge. At T=250 K, ΔG=+10 kJ/mol (non-spontaneous, red gauge).
- Slide temperature above the crossover Teq=12040000=333.3 K. Observe ΔG turn negative (spontaneous, green gauge), illustrating Case 3 from Table 5.4.
Exercise 5.1
Question: Choose the correct answer. A thermodynamic state function is a quantity:
(i) used to determine heat changes
(ii) whose value is independent of path
(iii) used to determine pressure-volume work
(iv) whose value depends on temperature only
Solution:
(ii) whose value is independent of path.
Rationale: By definition, a state function depends exclusively on the current equilibrium state of the system and not on the pathway or sequence of steps taken to reach that state.
Exercise 5.2
Question: For the process to occur under adiabatic conditions, the correct condition is:
(i) ΔT=0
(ii) Δp=0
(iii) q=0
(iv) w=0
Solution:
(iii) q=0.
Rationale: An adiabatic process is strictly defined as one in which no heat transfers across the system boundary (q=0). The temperature can and usually does change due to internal work.
Exercise 5.3
Question: The enthalpies of all elements in their standard states are:
(i) unity
(ii) zero
(iii) <0
(iv) different for each element
Solution:
(ii) zero.
Rationale: By international thermodynamic convention, the standard molar enthalpy of formation of an element in its most stable reference form of aggregation at 298.15 K and 1 bar is assigned a value of zero.
Exercise 5.4
Question: ΔU∘ of combustion of methane is −X kJ⋅mol−1. The value of ΔH∘ is:
(i) =ΔU∘
(ii) >ΔU∘
(iii) <ΔU∘
(iv) =0
Solution:
(iii) <ΔU∘.
Rationale: The thermochemical combustion reaction is:
CH4(g)+2O2(g)→CO2(g)+2H2O(l)
Δng=1 mol (CO2)−(1+2) mol (reactants)=1−3=−2
ΔH∘=ΔU∘+ΔngRT=−X+(−2RT)=−X−2RT
Because 2RT>0, ΔH∘ is more negative than ΔU∘, so ΔH∘<ΔU∘.
Exercise 5.5
Question: The enthalpy of combustion of methane, graphite, and dihydrogen at 298 K are −890.3 kJ⋅mol−1, −393.5 kJ⋅mol−1, and −285.8 kJ⋅mol−1 respectively. Enthalpy of formation of CH4(g) will be:
(i) −74.8 kJ⋅mol−1
(ii) −52.27 kJ⋅mol−1
(iii) +74.8 kJ⋅mol−1
(iv) +52.26 kJ⋅mol−1
Solution:
(i) −74.8 kJ⋅mol−1.
Step-by-Step Breakdown:
Target formation equation:
C(graphite)+2H2(g)→CH4(g),ΔfH∘=?
Given combustion reactions:
(1) CH4(g)+2O2(g)→CO2(g)+2H2O(l),ΔH1=−890.3 kJ/mol
(2) C(graphite)+O2(g)→CO2(g),ΔH2=−393.5 kJ/mol
(3) H2(g)+21O2(g)→H2O(l),ΔH3=−285.8 kJ/mol
Target equation =(2)+2×(3)−(1):
ΔfH∘=ΔH2+2ΔH3−ΔH1
ΔfH∘=−393.5+2(−285.8)−(−890.3)=−393.5−571.6+890.3=−965.1+890.3=−74.8 kJ⋅mol−1
Exercise 5.6
Question: A reaction, A+B→C+D+q is found to have a positive entropy change. The reaction will be:
(i) possible at high temperature
(ii) possible only at low temperature
(iii) not possible at any temperature
(iv) possible at any temperature
Solution:
(iv) possible at any temperature.
Rationale: The liberation of heat (+q) indicates an exothermic reaction: ΔH<0. The entropy change is positive: ΔS>0. In the Gibbs equation:
ΔG=ΔH−TΔS=(negative)−T(positive)<0
Because both terms are negative, ΔG is negative at all values of absolute temperature T. The reaction is spontaneous at any temperature.
Exercise 5.7
Question: In a process, 701 J of heat is absorbed by a system and 394 J of work is done by the system. What is the change in internal energy for the process?
Solution:
- q=+701 J (absorbed)
- w=−394 J (done by system)
ΔU=q+w=(+701 J)+(−394 J)=+307 J
Exercise 5.8
Question: The reaction of cyanamide, NH2CN(s), with dioxygen was carried out in a bomb calorimeter, and ΔU was found to be −742.7 kJ⋅mol−1 at 298 K. Calculate enthalpy change for the reaction at 298 K:
NH2CN(s)+23O2(g)→N2(g)+CO2(g)+H2O(l)
Solution:
Δng=(1+1)−1.5=+0.5 mol
ΔH=ΔU+ΔngRT=−742.7 kJ/mol+(0.5×8.314×10−3×298.15) kJ/mol
ΔH=−742.7+1.24=−741.46 kJ⋅mol−1≈−741.5 kJ⋅mol−1
Exercise 5.9
Question: Calculate the number of kJ of heat necessary to raise the temperature of 60.0 g of aluminium from 35∘C to 55∘C. Molar heat capacity of Al is 24 J⋅mol−1⋅K−1.
Solution:
n=27.0 g/mol60.0 g=2.222 mol
ΔT=55−35=20 K
q=n⋅Cm⋅ΔT=(2.222 mol)×(24 J⋅mol−1⋅K−1)×(20 K)=1066.67 J=1.067 kJ
Exercise 5.10
Question: Calculate the enthalpy change on freezing of 1.0 mol of water at 10.0∘C to ice at −10.0∘C. Given ΔfusH=6.03 kJ⋅mol−1 at 0∘C, Cp[H2O(l)]=75.3 J⋅mol−1⋅K−1, and Cp[H2O(s)]=36.8 J⋅mol−1⋅K−1.
Solution:
The transformation is divided into three thermodynamic steps:
- Step 1: Cooling liquid water from 10.0∘C (283.15 K) to 0∘C (273.15 K):
ΔH1=n⋅Cp[H2O(l)]⋅(0−10)=(1.0 mol)×(75.3 J⋅mol−1⋅K−1)×(−10 K)=−753 J=−0.753 kJ
- Step 2: Freezing water at 0∘C into ice (reverse of fusion):
ΔH2=−ΔfusH=−6.03 kJ⋅mol−1
- Step 3: Cooling ice from 0∘C (273.15 K) to −10.0∘C (263.15 K):
ΔH3=n⋅Cp[H2O(s)]⋅(−10−0)=(1.0 mol)×(36.8 J⋅mol−1⋅K−1)×(−10 K)=−368 J=−0.368 kJ
Total enthalpy change:
ΔH=ΔH1+ΔH2+ΔH3=−0.753−6.03−0.368=−7.151 kJ⋅mol−1
Exercise 5.11
Question: Enthalpy of combustion of carbon to CO2 is −393.5 kJ⋅mol−1. Calculate the heat released upon formation of 35.2 g of CO2 from carbon and dioxygen gas.
Solution:
Reaction: C(s)+O2(g)→CO2(g),ΔH=−393.5 kJ/mol
Molar mass of CO2=12.01+2(16.00)=44.01 g/mol.
Moles of CO2 formed:
n=44.01 g/mol35.2 g=0.7998 mol≈0.80 mol
Heat released:
q=n×∣ΔH∣=0.7998 mol×393.5 kJ/mol=314.73 kJ≈315 kJ
Exercise 5.12
Question: Enthalpies of formation of CO(g), CO2(g), N2O(g), and N2O4(g) are −110, −393, +81, and +9.7 kJ⋅mol−1 respectively. Find the value of ΔrH for the reaction:
N2O4(g)+3CO(g)→N2O(g)+3CO2(g)
Solution:
ΔrH=[ΔfH(N2O)+3ΔfH(CO2)]−[ΔfH(N2O4)+3ΔfH(CO)]
ΔrH=[81+3(−393)]−[9.7+3(−110)]
ΔrH=[81−1179]−[9.7−330]=−1098−(−320.3)=−1098+320.3=−777.7 kJ⋅mol−1
Exercise 5.13
Question: Given:
N2(g)+3H2(g)→2NH3(g),ΔrH∘=−92.4 kJ⋅mol−1
What is the standard enthalpy of formation of NH3 gas?
Solution:
Standard enthalpy of formation is defined per one mole of substance formed from reference elements:
ΔfH∘(NH3)=2ΔrH∘=2−92.4 kJ/mol=−46.2 kJ⋅mol−1
Exercise 5.14
Question: Calculate the standard enthalpy of formation of CH3OH(l) from the following data:
(1) CH3OH(l)+23O2(g)→CO2(g)+2H2O(l),ΔrH∘=−726 kJ⋅mol−1
(2) C(graphite)+O2(g)→CO2(g),ΔcH∘=−393 kJ⋅mol−1
(3) H2(g)+21O2(g)→H2O(l),ΔfH∘=−286 kJ⋅mol−1
Solution:
Target equation:
C(graphite)+2H2(g)+21O2(g)→CH3OH(l),ΔfH∘=?
Target =(2)+2×(3)−(1):
ΔfH∘=(−393)+2(−286)−(−726)
ΔfH∘=−393−572+726=−965+726=−239 kJ⋅mol−1
Exercise 5.15
Question: Calculate the enthalpy change for the process:
CCl4(g)→C(g)+4Cl(g)
and calculate bond enthalpy of C−Cl in CCl4(g).
Given:
- ΔvapH∘(CCl4)=30.5 kJ⋅mol−1
- ΔfH∘(CCl4)=−135.5 kJ⋅mol−1
- ΔaH∘(C)=715.0 kJ⋅mol−1
- ΔaH∘(Cl2)=242.0 kJ⋅mol−1
Solution:
Standard enthalpy of formation reaction for liquid carbon tetrachloride:
C(graphite)+2Cl2(g)→CCl4(l),ΔfH∘=−135.5 kJ/mol
Vaporizing liquid CCl4:
CCl4(l)→CCl4(g),ΔvapH∘=+30.5 kJ/mol
Adding gives formation of gaseous CCl4:
C(graphite)+2Cl2(g)→CCl4(g),ΔfH∘[CCl4(g)]=−135.5+30.5=−105.0 kJ/mol
Now consider atomizing the constituent elements into isolated gaseous atoms:
- Atomization of carbon: C(graphite)→C(g),ΔH=+715.0 kJ/mol
- Atomization of chlorine: 2Cl2(g)→4Cl(g),ΔH=2×242.0=+484.0 kJ/mol
Total enthalpy of gaseous atoms from elements:
ΔHatoms=715.0+484.0=+1199.0 kJ/mol
For the atomization reaction CCl4(g)→C(g)+4Cl(g):
ΔaH∘=ΔHatoms−ΔfH∘[CCl4(g)]=1199.0−(−105.0)=1199.0+105.0=1304.0 kJ⋅mol−1
Mean bond enthalpy of C−Cl:
ΔC−ClH∘=4ΔaH∘=41304.0=326.0 kJ⋅mol−1
Exercise 5.16
Question: For an isolated system, ΔU=0, what will be ΔS?
Solution:
For an isolated system, no energy or matter can be exchanged with the surroundings. For any spontaneous or natural irreversible process occurring within an isolated system, the entropy must increase according to the Second Law:
ΔS>0
At thermodynamic equilibrium, ΔS=0. Hence, for any spontaneous change in an isolated system, ΔS is strictly positive.
Exercise 5.17
Question: For the reaction at 298 K,
2A+B→C
ΔH=400 kJ⋅mol−1 and ΔS=0.2 kJ⋅K−1⋅mol−1. At what temperature will the reaction become spontaneous considering ΔH and ΔS to be constant over the temperature range?
Solution:
For spontaneity, ΔG<0:
ΔG=ΔH−TΔS<0⟹ΔH<TΔS⟹T>ΔSΔH
Substituting values:
T>0.2 kJ⋅K−1⋅mol−1400 kJ⋅mol−1=2000 K
The reaction will become spontaneous at temperatures strictly above 2000 K.
Exercise 5.18
Question: For the reaction,
2Cl(g)→Cl2(g)
what are the signs of ΔH and ΔS?
Solution:
- Sign of ΔH is Negative (−): Chemical bond formation releases energy (exothermic process).
- Sign of ΔS is Negative (−): Two moles of randomly moving isolated gaseous chlorine atoms combine to form one mole of structured diatomic chlorine molecules, reducing randomness and translational microstates.
Exercise 5.19
Question: For the reaction:
2A(g)+B(g)→2D(g)
ΔU∘=−10.5 kJ and ΔS∘=−44.1 J⋅K−1 at 298 K. Calculate ΔG∘ for the reaction, and predict whether the reaction may occur spontaneously.
Solution:
Δng=2−(2+1)=−1.0 mol
ΔH∘=ΔU∘+ΔngRT=−10.5 kJ+(−1.0 mol)×(8.314×10−3 kJ⋅K−1⋅mol−1)×(298.15 K)
ΔH∘=−10.5 kJ−2.479 kJ=−12.979 kJ
Now evaluate ΔG∘:
ΔG∘=ΔH∘−TΔS∘
TΔS∘=(298.15 K)×(−44.1×10−3 kJ⋅K−1)=−13.148 kJ
ΔG∘=−12.979 kJ−(−13.148 kJ)=−12.979+13.148=+0.169 kJ
Because ΔG∘>0 (+0.17 kJ), the reaction is non-spontaneous at standard conditions and 298 K.
Exercise 5.20
Question: The equilibrium constant for a reaction is 10. What will be the value of ΔG∘? (R=8.314 J⋅K−1⋅mol−1,T=300 K).
Solution:
ΔrG∘=−2.303RTlog10K
ΔrG∘=−2.303×(8.314 J⋅K−1⋅mol−1)×(300 K)×log10(10)
Because log10(10)=1:
ΔrG∘=−5744.14 J⋅mol−1=−5.744 kJ⋅mol−1
Exercise 5.21
Question: Comment on the thermodynamic stability of NO(g), given:
21N2(g)+21O2(g)→NO(g),ΔrH∘=+90 kJ⋅mol−1
NO(g)+21O2(g)→NO2(g),ΔrH∘=−74 kJ⋅mol−1
Solution:
- The standard enthalpy of formation of NO(g) is positive (+90 kJ/mol), meaning it is an endothermic compound and thermodynamically unstable with respect to decomposition into elemental N2 and O2.
- Furthermore, the oxidation of NO(g) to NO2(g) is exothermic (ΔrH∘=−74 kJ/mol), meaning NO(g) is unstable in the presence of excess oxygen and readily oxidizes to reddish-brown NO2 gas.
Exercise 5.22
Question: Calculate the entropy change in surroundings when 1.00 mol of H2O(l) is formed under standard conditions. Given ΔfH∘=−286.0 kJ⋅mol−1.
Solution:
The standard formation of liquid water:
H2(g)+21O2(g)→H2O(l),ΔrH∘=−286.0 kJ⋅mol−1
Because the process is exothermic, heat absorbed by the surroundings at constant pressure and 298.15 K is:
qsurr=−ΔrH∘=−(−286.0 kJ)=+286.0 kJ=+286000 J
Entropy change in the surroundings:
ΔSsurr=Tqsurr=298.15 K+286000 J=+959.25 J⋅K−1⋅mol−1≈+959.3 J⋅K−1⋅mol−1
| Concept / Quantity | Governing Mathematical Equation | Physical Meaning & IUPAC Sign Convention |
|---|
| First Law of Thermodynamics | ΔU=q+w | Total energy conservation. q>0 when absorbed; w>0 when work is done on the system. |
| Irreversible Expansion Work | w=−pexΔV=−pex(Vf−Vi) | Work done against constant resisting external pressure pex. |
| Reversible Isothermal Work | wrev=−2.303nRTlog10(ViVf) | Maximum work extracted through infinite equilibrium expansion steps. |
| Free Expansion into Vacuum | pex=0⟹w=0,q=0,ΔU=0 | Gas expands into vacuum without work or heat exchange. |
| Enthalpy State Function | H=U+pV | Total heat content. At constant pressure: ΔH=qp. |
| Enthalpy and Internal Energy | ΔH=ΔU+ΔngRT | Relationship for ideal gas reactions where Δng=∑ng,prod−∑ng,react. |
| Molar Heat Capacity Relation | Cp−CV=R | Difference between constant-pressure and constant-volume heat capacities for 1 mol of ideal gas. |
| Bomb Calorimeter (Constant V) | qV=ΔU=−CV⋅ΔT | Heat evolved at rigid constant volume measures change in internal energy directly. |
| Reaction Enthalpy from Formation | ΔrH∘=∑aiΔfH∘(prod)−∑biΔfH∘(react) | Standard reaction enthalpy from element formation enthalpies (reference elements =0). |
| Hess's Law of Heat Summation | ΔrH∘=ΔrH1∘+ΔrH2∘+⋯ | Path-independence of enthalpy allows algebraic addition of intermediate thermochemical equations. |
| Reaction Enthalpy from Bond Enthalpies | ΔrH∘≈∑BE(reactants)−∑BE(products) | Approximate gas-phase reaction enthalpy from bond cleavage and formation energies. |
| Lattice Enthalpy (Born-Haber Cycle) | ΔfH∘=ΔsubH∘+ΔiH∘+21ΔbondH∘+ΔegH∘−ΔlatticeH∘ | Thermodynamic cycle relating ionic solid lattice energy to elemental formation and gaseous ion properties. |
| Enthalpy of Solution | ΔsolH∘=ΔlatticeH∘+ΔhydH∘ | Balance between lattice breakdown and ionic hydration energy. |
| Entropy of Reversible Process | ΔS=Tqrev | Quantitative measure of thermal energy dispersal and molecular randomness. |
| Second Law of Thermodynamics | ΔStotal=ΔSsys+ΔSsurr>0 | Spontaneous processes strictly increase the total entropy of the universe. |
| Gibbs Free Energy Equation | ΔG=ΔH−TΔS | Single-system criterion for spontaneity at constant temperature and pressure. |
| Spontaneity Criterion | ΔG<0⟹Spontaneous<br>ΔG=0⟹Equilibrium<br>ΔG>0⟹Non-Spontaneous | Master condition for chemical and physical spontaneity at constant T,p. |
| Third Law of Thermodynamics | limT→0 KS=0 | Entropy of a pure, perfect crystalline solid approaches zero at absolute zero. |
| Gibbs Energy and Equilibrium Constant | ΔrG∘=−RTlnK=−2.303RTlog10K | Link between standard free energy and the chemical equilibrium position. |