Enthalpy

Submitted by ChemPRIME Staff on Thu, 12/16/2010 - 15:06


In chemistry we are interested not only in those changes occurring in a closed container at constant volume but also in those occurring in an open container at constant (i.e., atmospheric) pressure. When a change occurs at constant pressure, there is another energy factor we must consider in addition to the heatEnergy transferred as a result of a temperature difference; a form of energy stored in the movement of atomic-sized particles. absorbed and the change in internal energy. This is the expansion workA mechanical process in which energy is transferred to or from an object, changing the state of motion of the object. wexp which the system does as its volume expands against the external pressure.

In order to understand the nature and magnitude of this expansion work, let us consider the simple example illustrated in Fig. 1. Here a sample of oxygen gasA state of matter in which a substance occupies the full volume of its container and changes shape to match the shape of the container. In a gas the distance between particles is much greater than the diameters of the particles themselves; hence the distances between particles can change as necessary so that the matter uniformly occupies its container. is heated at a constant pressure P from an initial temperatureA physical property that indicates whether one object can transfer thermal energy to another object. T1 to a final temperature T2 by means of an electrical heating coil. The gas is confined in a cylinder by a piston, and the pressure is maintained by placing a weightA measure of the gravitational force on an object; directly proportional to mass. of the correct magnitude on top of the piston. The whole apparatus is maintained in a vacuum so that there is no atmospheric pressure to consider in addition to the effect of the weight and piston.

When the heating coil in this apparatus is switched on, the temperature rises and the gas expands in compliance with Charles’ law, lifting the piston and weight in the process. Energy must he supplied from the heating coil not only to increase the energy of the oxygen molecules but also to lift the weight. In other words,


qp = ΔU + wexp      (1)


where      qp = heat absorbed

             ΔU = change in internal energy

            wexp = expansion work, i.e., work done in lifting the weight

            To calculate the magnitude of this expansion work, we begin with the definition of pressure:


P=\frac{\text{force}}{\text{area}}=\frac{F}{A}
or
F = PA


Figure 1 When a sample of gas is heated at constant pressure, energy must be supplied to expand the gas as well as to increase its internal energy.


where F is the total farce exerted by the weight and piston on the oxygen gas and A is the area of the piston. As the gas sample is heated, the volume increases from an initial value V1 to a final value V2, while the piston and its weight move from a height h1 to a height h2. The work done is thus given by the expression


wexp = force exerted × distance moved

       = (P × A) × (h2h1)

       = P × (A × h2 A × h1)


However, since the volume of a cylinder is the area of the baseIn Arrhenius theory, a substance that increases the concentration of hydroxide ions in an aqueous solution. In Bronsted-Lowry theory, a hydrogen-ion (proton) acceptor. In Lewis theory, a species that donates a pair of electrons to form a covalent bond. times the height,


           A × h1 = V1      initial volume of gas

and      A × h2 = V2      final volume

Thus       wexp = P × (V2V1)

or           wexp = P ΔV      (2)


Inserting this value for wexp into Eq. (1), we obtain the final result


qp = ΔU + P ΔV      (3)


It is important to realize that the expansion work P ΔV does not depend on our sample being in the apparatus of Fig. 1 in which there is an obvious gain in the potential energy of a weight. If instead of a weight we allowed the atmosphereA unit of pressure equal to 101.325 kPa or 760 mmHg; abbreviated atm. Also, the mixture of gases surrounding the earth. to exert a pressure P on the gas, the result would still be P ΔV. In this second case, instead of lifting a visible weight, the expanding gas would push back the atmosphere and hence be lifting invisible air molecules. The work done, and hence the increase in the potential energy of the atmosphere, would still be P ΔV.

This simple example of an expanding gas helps us to see what is involved in the general case of a chemical or physical changeA process, such as melting, in which the composition of all substances remains unchanged. occurring at constant pressure. In any such case the heat energy absorbed by the system, qp, will always exactly account for the increase in internal energy ΔU and the expansion work P ΔV. In other words the relationship


qp = ΔU + P ΔV      (3)


is valid in the general case.



EXAMPLE 1 When 1 mol liquidA state of matter in which the atomic-scale particles remain close together but are able to change their positions so that the matter takes the shape of its container H2O is boiled at 100°C and 101.3 kPa (1.000 atm) pressure, its volume expands from 19.8 cm3 in the liquid state to 30.16 dm³ in the gaseous state. The heat energy absorbed by the vaporizationThe formation of a vapor from a liquid; evaporation or boiling. process is found experimentally to be 40.67 kJ. Calculate the increase in internal energy ΔU of H2O.


SolutionA mixture of one or more substances dissolved in a solvent to give a homogeneous mixture. We must first calculate the expansion work P ΔV.


wexp = P × (V2V1)

       = 101.3 kPa × (30.16 dm3 – 0.0198 dm3) = 3053 kPa dm3


In the section on Pressure, we see that 1Pa × 1 dm3 = 1 J, and we have

wexp = 3053 J = 3.055 kJ


Also, since

qp = ΔU + P ΔV


we have

ΔU = qpP ΔV = 40.67 kJ – 3.05 kJ = 37.63 kJ


Note: As we see in the sections on Properties of Organic Compounds and Other Covalent Substances and Solids, Liquids, and Solutions, the vaporization of a liquid is always an endothermicIn chemical thermodynamics, describes a process in which energy is transferred from the surroundings to the system as a result of a temperature difference. process. Since the molecules attract each other, energy must be supplied to separate them as vaporization occurs. However, not all the energy supplied when a liquid boils goes to increasing the potential energy of the molecules. A significant proportion is needed to increase the potential energy of the air as well.



It is far easier to carry out most chemical reactions in a container open to the atmosphere than in a closed system like a bomb calorimeterA sturdy, rigid container (bomb) and associated device for measuring the heat energy transferred out of or into a chemical system in which a reaction occurs; the sturdy bomb maintains constant volume.. However, when a reaction is carried out at constant atmospheric pressure, it is necessary to measure P, V1 and V2 (as in Example 1) as well as qp in order to calculate the change in internal energy from the equation ΔU = qpP ΔV. These extra measurements are a nuisance, and they can be avoided by introducing a new quantity which is related to the internal energy but also includes the potential energy of the atmosphere. This quantity is also used in the sections on Using Chemical Equations in Calculations. It is called the enthalpy, symbol H, and is defined by


H = U + PV      (4)


From Eq. (4) we can see that the enthalpy is always larger than the internal energy by a quantity PV. This extra energy is added to take account of the fact that whenever a body of volume V is introduced into the atmosphere, the potential energy of the atmosphere is increased by PV [by the same argument used to derive Eq. (2)]. The enthalpy is thus of the form


Enthalpy = internal energy + potential energy of atmosphere      (5)


When a system undergoes a chemical or physical change at constant pressure, the change in enthalpy is given by


Change in enthalpy = change in internal energy + change in potential energy of atmosphere      (6)


The change in enthalpy thus includes both the energy changes for which heat energy must be supplied from the surroundings. In more formal language


ΔH = ΔU + Δ(PV) = ΔU + (P2V2P1V1)      (7)


If we consider conditions of constant pressure, P2 = P1 = P, and


ΔH = ΔU + (PV2PV1) = ΔU + P(V2V1) = ΔU + P ΔV

but from Eq. (3)


qp = ΔU + P ΔV
Thus
qp = ΔH      (8)


In other words, the heat energy absorbed by a system in any change at constant pressure is equal to the increase in its enthalpy. The change in enthalpy ΔH can be obtained from a single experimental measurement: the heat energy absorbed at constant pressure.