- 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.
A state function depends only on the initial and final states of the system, not on the path used to reach the state.
(ii) whose value is independent of path.
- i. ΔT = 0
- ii. Δp = 0
- iii. q = 0
- iv. w = 0
An adiabatic process is one in which no heat is exchanged between system and surroundings. Therefore q = 0.
(iii) q = 0.
- i. unity
- ii. zero
- iii. < 0
- iv. different for each element
By convention, the standard enthalpy of formation of an element in its standard state is taken as zero.
(ii) zero.
- i. = ΔU°
- ii. > ΔU°
- iii. < ΔU°
- iv. = 0
For CH4(g) + 2O2(g) → CO2(g) + 2H2O(l), Δng = 1 - 3 = -2. Since ΔH = ΔU + ΔngRT, ΔH = ΔU - 2RT. Therefore ΔH is more negative than ΔU, i.e. ΔH < ΔU.
(iii) < ΔU°.
- i. -74.8 kJ mol^-1
- ii. -52.27 kJ mol^-1
- iii. +74.8 kJ mol^-1
- iv. +52.26 kJ mol^-1.
For CH4(g) + 2O2(g) → CO2(g) + 2H2O(l), ΔcH = [ΔfH(CO2) + 2ΔfH(H2O)] - ΔfH(CH4). Thus -890.3 = [-393.5 + 2(-285.8)] - ΔfH(CH4) = -965.1 - ΔfH(CH4). Hence ΔfH(CH4) = -74.8 kJ mol^-1.
(i) -74.8 kJ mol^-1.
- i. possible at high temperature
- ii. possible only at low temperature
- iii. not possible at any temperature
- v. possible at any temperature
Heat q appears on the product side, so the reaction is exothermic and ΔH is negative. Since ΔS is positive, ΔG = ΔH - TΔS is negative at all temperatures. Therefore the reaction is spontaneous at any temperature.
(v) possible at any temperature.
Heat absorbed by the system is q = +701 J. Work done by the system is w = -394 J. From the first law, ΔU = q + w = 701 - 394 = 307 J.
+307 J.
For NH2CN(s) + 3/2 O2(g) → N2(g) + CO2(g) + H2O(l), use ΔH = ΔU + ΔngRT. Gaseous product moles = 1 mol N2 + 1 mol CO2 = 2 mol. Gaseous reactant moles = 1.5 mol O2; solid cyanamide and liquid water do not count. Thus Δng = 0.5. ΔH = -742.7 + (0.5)(8.314)(298)/1000 = -742.7 + 1.24 = -741.5 kJ mol^-1.
-741.5 kJ mol^-1.
Moles of Al = 60.0/27.0 = 2.22 mol. ΔT = 20 K. Heat required q = nCΔT = (2.22)(24)(20) = 1.07 x 10^3 J = 1.07 kJ.
1.07 kJ.
Cool liquid water from 10°C to 0°C: q1 = (1)(75.3)(0 - 10) = -753 J. Freeze at 0°C: q2 = -6.03 kJ = -6030 J. Cool ice from 0°C to -10°C: q3 = (1)(36.8)(-10 - 0) = -368 J. Total q = -753 - 6030 - 368 = -7151 J = -7.15 kJ.
-7.15 kJ mol^-1.
Moles of CO2 = 35.2/44.0 = 0.800 mol. Heat released = 0.800 x 393.5 = 314.8 kJ. The enthalpy change is -314.8 kJ for this amount.
314.8 kJ of heat is released.
ΔrH = ΣΔfH(products) - ΣΔfH(reactants). Products: 81 + 3(-393) = -1098 kJ mol^-1. Reactants: 9.7 + 3(-110) = -320.3 kJ mol^-1. Therefore ΔrH = -1098 - (-320.3) = -777.7 kJ mol^-1.
-777.7 kJ mol^-1.
The given reaction forms 2 mol NH3 from elements in their standard states. Therefore ΔfH° per mole of NH3 = -92.4/2 = -46.2 kJ mol^-1.
-46.2 kJ mol^-1.
For CH3OH(l) + 3/2 O2(g) → CO2(g) + 2H2O(l), -726 = [ΔfH(CO2) + 2ΔfH(H2O)] - ΔfH(CH3OH). Substitute values: -726 = [-393 + 2(-286)] - x = -965 - x. Hence x = -239 kJ mol^-1.
-239 kJ mol^-1.
The formation enthalpy of CCl4(g) is ΔfH°[CCl4(l)] + ΔvapH° = -135.5 + 30.5 = -105.0 kJ mol^-1. Atomising elements to C(g) + 4Cl(g) needs 715.0 + 2(242) = 1199 kJ mol^-1. Therefore CCl4(g) → C(g) + 4Cl(g) has ΔH = 1199 - (-105.0) = 1304 kJ mol^-1. Average C-Cl bond enthalpy = 1304/4 = 326 kJ mol^-1.
ΔH = 1304 kJ mol^-1; average C-Cl bond enthalpy = 326 kJ mol^-1.
The second law states that entropy of an isolated system increases for a spontaneous process and becomes maximum at equilibrium. Therefore ΔU = 0 alone does not make ΔS zero; the natural direction has ΔS positive until equilibrium is reached.
For a spontaneous process in an isolated system, ΔS > 0; at equilibrium, ΔS = 0.
For spontaneity, ΔG = ΔH - TΔS < 0. Thus T > ΔH/ΔS = 400/0.2 = 2000 K. At 2000 K the reaction is at the threshold; above 2000 K it becomes spontaneous.
Above 2000 K.
Formation of a Cl-Cl bond from chlorine atoms releases energy, so ΔH < 0. Two gaseous atoms combine to form one gaseous molecule, decreasing disorder, so ΔS < 0.
ΔH is negative and ΔS is negative.
Here Δng = 2 - 3 = -1. At 298 K, ΔH° = ΔU° + ΔngRT = -10.5 - (8.314 x 298/1000) = -12.98 kJ. Convert entropy: ΔS° = -44.1 J K^-1 = -0.0441 kJ K^-1. ΔG° = ΔH° - TΔS° = -12.98 - 298(-0.0441) = +0.16 kJ. Since ΔG° is positive, the reaction is not spontaneous under standard conditions.
ΔG° is about +0.16 kJ mol^-1 at 298 K; the reaction is not spontaneous under standard conditions.
Use ΔG° = -RT ln K. With K = 10, T = 300 K and R = 8.314 J K^-1 mol^-1, ΔG° = -(8.314)(300)ln10 = -5744 J mol^-1 = -5.74 kJ mol^-1.
-5.74 kJ mol^-1.
Formation of NO from N2 and O2 is endothermic, with ΔrH° = +90 kJ mol^-1, so NO is not very stable thermodynamically relative to the elements. Its oxidation to NO2 is exothermic, ΔrH° = -74 kJ mol^-1, showing that NO tends to form the more stable oxide NO2 in oxygen.
NO(g) is thermodynamically unstable with respect to its elements and can be oxidised exothermically to NO2.
The system releases 286 kJ mol^-1 to the surroundings. At 298 K, ΔSsurr = -ΔHsys/T = -(-286000 J mol^-1)/298 K = +960 J K^-1 mol^-1.
+960 J K^-1 mol^-1.