thermochemistry
Student Learning Objectives (SLOs) - Thermochemistry Part 1
Apply the First Law of Thermodynamics to determine signs on heat (q) and work (w).
Differentiate between path and state functions.
Differentiate between endothermic and exothermic processes.
Apply stoichiometric relationships between enthalpy and a balanced chemical equation to determine unknowns, such as grams of product, moles of reactant, change in energy, etc.
Introduction to Thermochemistry
Changes in matter accompanied by changes in energy.
Thermochemistry: The study of heat involved in chemical reactions.
Example: The small chemical heater, which uses the exothermic reaction of magnesium (Mg) and water to produce heat without light or smoke. A ‘tea bag’ filled with Mg is used: just add water and wait 10 minutes for the temperature to reach 60° C (source: www.CEN-ONLINE.ORG).
Basic Concepts in Thermodynamics
Thermodynamics: The study of energy and its interconversions.
First Law of Thermodynamics: States that the total energy of the universe is constant, also known as the Law of Conservation of Energy.
Energy Transfer Equation:
Heat and Work
Heat (q): Energy transferred due to a change in temperature.
-q indicates that heat has left the system (heat is lost).
+q indicates that heat has entered the system (heat is gained).
Work (w): Energy transferred when an object moves due to a force.
The relationship for energy in the context of thermodynamics is given as:
Class Concept Check
Predict the sign of q related to the system (and surroundings) using examples:
An ice cube melting in a beverage cools the drink (q is negative for the system).
Sweat evaporating on the skin cools the body (q is negative for the system).
Thermodynamic Functions
There are two kinds of thermodynamic functions:
State Function: A property of the system fixed by its current conditions and independent of the system’s history.
Path Function: A property that depends on how a particular change occurred.
The energy is classified as a state function:
Enthalpy (ΔH)
Enthalpy (ΔH): Another state function representing the change in heat (q) experienced by the system at constant pressure.
A thermochemical equation presents a chemical equation including the enthalpy of reaction:
Example:
The sign on ΔH indicates whether heat is released (given off) or absorbed.
Exothermic vs. Endothermic Reactions
Exothermic Reaction: A system that transfers heat to its surroundings, indicated by -ΔH.
Example Reaction:
Endothermic Reaction: A reaction that absorbs heat from its surroundings, indicated by +ΔH.
Example Reaction:
Using Thermochemical Equations
Example: Given the reaction with units of ΔH relate to coefficients from the balanced equation.
Inverting the moles will change the heat associated with the reaction:
If 4 moles of react, calculate heat (q) required.
If 286 kJ of heat is absorbed (as endothermic), determine how many moles of hydrogen gas form.
Distinction between Heat (q) and Enthalpy (ΔH)
Heat (q) (measured in kJ) relates to the mass or moles you start with in a problem (like pantry items).
ΔH (measured in kJ per mole from coefficient) is the rate of heat gain/loss during a process.
Relationship:
Example Calculation of Heat Required
It takes 74 kJ to heat enough liquid for a cup of tea. Determine mass of methane (CH4) to burn for this heat.
Given Reaction: (exothermic).
Example Heat Exchange Calculation
Calculate heat exchanged when 11.0 g of forms from the combustion of propane.
Given Reaction:
Student Learning Objectives (SLOs) - Thermochemistry Part 2
Calculate heat, temperature, mass, and heat capacity using the formulas: and for both the system and surroundings (excluding pressure-volume work).
Rank substances based on predicted temperature change using heat capacities.
Solve for change in temperature in constant pressure calorimetry settings.
Solve for ΔHrxn using Hess’s Law, ΔHf, and calorimetry.
Additional Methods for Determining ΔH
Various methods to solve for ΔH:
Calorimetry
Hess’s Law
Heat of formation
Calorimetry Overview
In laboratory measurements, q can be derived to determine ΔH:
Conduct the reaction at constant pressure.
Create surroundings to retain all heat produced or absorbed.
Measure temperature change (ΔT) using a thermometer and relate to heat quantity using the specific heat capacity of the substance.
Calorimetry: In a closed, insulated system (no energy entry or exit).
Specific Heat Capacity
Specific Heat Capacity (c): The amount of heat needed to increase the temperature of 1 gram of a substance by 1 K (or °C).
For liquid water, specific heat is:
Mathematical Example of Specific Heat
The relationship between heat (q), mass (m), and change in temperature (ΔT) is shown in the equation:
Relating Heat of Surroundings and System
The contents of the calorimeter represent the surroundings, hence:
The chemical reaction refers to the system, thus:
A sign change is required to relate and for appropriate calculations, plus ensure units consistency (q in Joules but ΔH in kJ).
Calorimetry Calculations
General formulas for calorimetry calculations:
Example Problem of Calorimetry
Example: Dissolution of 22.2 g of CaCl2 (molar mass = 111.08 g/mol) in water contained in a calorimeter, where the temperature of water rises by 7.14 °C. Compute ΔH for the dissolution process.
Given specific heat of water:
Further Example for Determining Temperature Changes
Calculation involving 18.4 g of (molar mass = 158.6 g/mol) added to 585 g of water at an initial temperature of 35.1 °C, where the reaction is:
Student Learning Objectives (SLOs) - Thermochemistry Part 3
Solve for ΔHrxn using Hess's Law, ΔHf, and calorimetry.
Hess's Law of Heat Summation
Hess’s Law states that the ΔH of an overall process is the sum of the enthalpy changes of its different steps, represented as:
It allows us to break down an overall unknown process into individual steps with known ΔH values.
A crucial advantage is that ΔH is a state function, allowing easy summation of changes.
Thermochemical equations must be provided to calculate the target ΔH.
Empirical Application of Hess's Law
Example Reactions to showcase Hess's Law:
Tricks for Thermochemical Equations and Hess's Law
To manipulate thermochemical equations with Hess’s Law:
Sign Change: If the direction of the reaction is reversed, the sign of ΔH must be reversed.
Magnitude Change: If the amount of reactants or products is altered, then the magnitude of ΔH must be correspondingly adjusted.
Fractional Coefficients: Allows for adjustments provided ΔH relationships are maintained due to the state function property.
Example: Given - When reversed, becomes:
Advanced Calculation with Hess's Law
Determine the enthalpy change via Hess’s law using known reactions:
For example:
Query:
Calculation Example of Enthalpy Change
Calculate the enthalpy change for target:
Given the following equations:
Standard Enthalpy of Formation (ΔHºf)
The Standard Enthalpy of Formation (ΔHºf) is defined as the enthalpy change when one mole of a substance in its standard state is created from its most stable form of constituents in their standard states.
The standard state for a substance means the pure form at 25ºC and 1 atm pressure (for solutions, it is 1M).
Example: Carbon exists as graphite rather than diamond.
Reactions:
Reaction Enthalpy Calculation Using ΔHºf
Reaction Calculation Formula:
Example: For reaction - Calculation to find - Given Standard Enthalpy Data:
Another application: Solve for the enthalpy of formation for a compound given its ΔHrxn.