10.1 Reaction Rates, Rate Laws, and Integrated Rate Equations
Key Takeaways
Reaction rate is defined unambiguously by normalizing the rate of concentration change by the stoichiometric coefficient: .
Differential rate laws relate rate to species concentrations (), where reaction orders () are determined experimentally and the units of the rate constant follow .
Integrated rate equations model concentration decay over time: zero-order (), first-order (), and second-order ().
Half-life expressions provide immediate diagnostic signatures for reaction order: (zero-order, drops with concentration), (first-order, strictly concentration-independent), and (second-order, inversely proportional to ).
Radioactive decay is an exact first-order process (), underpinning geochronological and archaeological dating methodologies including radiocarbon dating ().
Reaction Rates, Rate Laws, and Integrated Rate Equations
Chemical kinetics investigates the rates of chemical processes, the physical and chemical variables that alter these rates, and the microscopic molecular mechanisms connecting reactants to products. While chemical thermodynamics determines the spontaneous direction and theoretical equilibrium yield of a reaction (), it reveals nothing about the timescale required to attain equilibrium. On the PRC Chemist Licensure Examination, mastery of chemical kinetics demands rigorous proficiency with stoichiometric rate definitions, differential and integrated rate laws, graphical transformations, half-life relationships, experimental rate-order evaluations, and radioactive decay processes.
1. Stoichiometric Definition of Reaction Rate
For a general homogeneous reaction occurring in a closed system at constant volume:
the rate of disappearance of reactants and rate of appearance of products are stoichiometrically coupled. To avoid ambiguous rates that depend arbitrarily on which chemical species is monitored, the IUPAC defines the rate of reaction () as the time derivative of the extent of reaction () divided by system volume (), or the rate of change of concentration divided by the stoichiometric coefficient (, taken as negative for reactants and positive for products):
Instantaneous vs. Average Rates
- Average Rate: Calculated over a finite macroscopic time interval :
- Instantaneous Rate: The derivative evaluated at an infinitesimal instant (the tangent slope of the concentration-time curve at that specific point):
- Initial Rate (): The instantaneous rate at the exact commencement of the reaction (), prior to any significant depletion of initial reactants or interference from reverse reactions and product inhibition.
Stoichiometric Rate Conversion Example
Consider the gas-phase decomposition of dinitrogen pentoxide: If the rate of decomposition of is measured as , the rates of appearance of products are:
2. Differential Rate Laws and Reaction Orders
A differential rate law expresses the instantaneous reaction rate as a mathematical function of the instantaneous concentrations of reacting species:
- Rate Constant (): A proportionality constant specific to a given reaction at a specified temperature. It is strictly independent of reactant concentrations, but varies exponentially with temperature and ionic strength.
- Partial Orders (): The powers to which individual concentrations are raised. The partial order with respect to component is , with respect to is . Reaction orders are strictly experimental quantities; they cannot be deduced from the stoichiometric coefficients of an overall balanced chemical equation (unless the reaction is known to proceed via a single elementary step).
- Overall Reaction Order (): The algebraic sum of all partial orders: Reaction orders can be positive integers (), negative numbers (indicating inhibition), or fractional values (common in free-radical gas reactions, e.g., the thermal synthesis of phosgene follows with overall order ).
Dimensional Analysis of the Rate Constant
Because reaction rate always carries units of concentration per unit time (typically or ), the dimensional units of depend directly on the overall reaction order :
| Overall Order () | Dimensional Units of | Alternative SI Representation |
|---|---|---|
| 0 (Zero-order) | ||
| 1 (First-order) | ||
| 2 (Second-order) | ||
| 3 (Third-order) | ||
| (Half-order) |
Tip
Licensure exam questions frequently hide the reaction order inside the stated numerical units of . Whenever a problem gives , you immediately know without checking that the reaction is first-order.
3. Integrated Rate Equations and Half-Life Derivations
Integrated rate laws express reactant concentration directly as an explicit function of continuous reaction time . Let us examine the three fundamental classical rate laws for reactions of the type .
1. Zero-Order Reactions
A zero-order reaction proceeds at a constant velocity that is entirely independent of reactant concentration (common in surface-catalyzed heterogeneous reactions where active sites are fully saturated, and enzyme reactions under substrate saturation):
Integrating from initial concentration at to at time :
- Linear Graphical Plot: Plotting versus yields a straight line with slope and -intercept .
- Half-Life (): The time required for the concentration to drop to half its initial value (): Crucial Diagnostic: For a zero-order reaction, the half-life is directly proportional to the initial reactant concentration. Successive half-lives become progressively shorter (). The reaction terminates completely in finite time .
2. First-Order Reactions
A first-order reaction has a rate directly proportional to the first power of concentration:
Separating variables and integrating:
Converting to base-10 logarithms:
- Linear Graphical Plot: Plotting versus yields a straight line with slope and -intercept . (Or plotting vs with slope ).
- Half-Life (): Substituting : Crucial Diagnostic: For a first-order process, the half-life is strictly independent of the initial concentration. Every successive half-life takes the exact same duration (). After half-lives, the remaining fraction is .
3. Second-Order Reactions (Single Reactant: )
When the reaction rate depends on the square of a single reactant concentration:
Separating variables and integrating:
- Linear Graphical Plot: Plotting versus yields a straight line with positive slope and -intercept .
- Half-Life (): Substituting : Crucial Diagnostic: For a second-order reaction, the half-life is inversely proportional to the initial concentration. Each successive half-life is double the preceding one (). As the reactant dilutes, the collision probability falls quadratically, drastically prolonging the decay.
4. Second-Order Reactions (Two Reactants: )
When the rate law is first-order in and first-order in () with unequal initial concentrations ():
Let be the concentration of and that has reacted at time , such that and : Integrating by partial fractions yields the integrated rate law: Plotting versus yields a straight line with slope .
4. Comprehensive Comparison of Integrated Rate Laws
| Kinetic Property | Zero-Order () | First-Order () | Second-Order (, single reactant) |
|---|---|---|---|
| Differential Law | |||
| Integrated Law | |||
| Exponential Form | — | ||
| Linear Plot | vs. | vs. | vs. |
| Slope of Linear Plot | |||
| -Intercept | |||
| Half-Life () | |||
| Dependence of on | Directly proportional () | Independent () | Inversely proportional () |
| Successive Half-Lives | (halving) | (constant) | (doubling) |
| Units of |
5. Experimental Methods of Determining Reaction Order
1. Initial Rates Method (Method of Initial Rates)
In this classic quantitative method, multiple kinetic trials are executed with systematically varied initial reactant concentrations. Because the rates are evaluated at , reaction products have not yet accumulated, eliminating reverse reactions.
Taking natural logarithms:
Worked Step-by-Step Problem: Initial Rates Analysis
Experimental Data: Determine the rate law and rate constant for at :
- Run 1: , ,
- Run 2: , ,
- Run 3: , ,
Step 1: Determine order with respect to (using Runs 1 and 2):
Step 2: Determine order with respect to (using Runs 1 and 3):
Step 3: State rate law and overall order:
Step 4: Compute rate constant with units using Run 1:
2. Graphical Method
Experimental concentration-versus-time data are transformed into three parallel graphs:
- vs.
- vs.
- vs. The plot exhibiting strict linearity (highest correlation coefficient ) identifies the true order ( or ), and the slope gives the numerical magnitude of .
3. Half-Life Dependence Method
For any reaction of arbitrary overall order (where ): Comparing two distinct initial concentrations and with measured half-lives and :
4. Isolation Method (Flood Method) and Pseudo-Order Kinetics
When a reaction involves multiple reactants (e.g., ), measuring individual orders simultaneously is challenging. In the isolation method, reactants and are added in vast stoichiometric excess relative to (, typically to excess). As reactant is consumed completely, the concentrations of and change by an imperceptible percentage and remain effectively constant:
The reaction behaves as a pseudo--order process. For instance, acid-catalyzed ester hydrolysis in dilute aqueous solution involves water as both solvent and reactant (). Because is effectively invariant, the second-order process collapses to pseudo-first-order kinetics with , where .
6. Radioactive Decay Kinetics and Radiocarbon Dating
Nuclear transmutation and radioactive decay processes are pure first-order kinetic phenomena occurring at the atomic nucleus, completely independent of chemical environment, pressure, or temperature.
Governing Equations
Let be the number of undecayed radioactive nuclei at time :
where is the decay constant (equivalent to first-order ), related to half-life by:
Activity ()
The activity is the disintegration rate:
- Units: Becquerel () and Curie (). Specific activity is typically expressed in disintegrations per minute per gram of total carbon ().
Radiocarbon () Dating Principles
- Atmospheric cosmic-ray neutrons react with atmospheric :
- Radioactive () oxidizes to and incorporates into the biosphere via photosynthesis and the food chain, establishing a steady-state specific activity in living organisms of approximately .
- Upon death, carbon exchange ceases. The decays via beta emission (), causing the residual specific activity to decline exponentially:
Worked Step-by-Step Calculation: Archaeological Artifact Dating
Scenario: A buried wood fragment recovered from a lake-sediment core has a measured specific activity of . If fresh wood has a specific activity of and , calculate the archaeological age of the wood.
Step 1: Compute fraction of remaining activity: Notice that , which corresponds to exactly two elapsed half-lives.
Step 2: Calculate age rigorously using the exponential decay equation: Conclusion: The wood died approximately ago.
For the gas-phase reaction 2 NO(g) + Br2(g) -> 2 NOBr(g) at 273 K, initial rate data were recorded across three experiments: Run 1 ([NO]_0 = 0.10 M, [Br2]_0 = 0.10 M, Initial Rate = 1.30 x 10^-3 M/s); Run 2 ([NO]_0 = 0.20 M, [Br2]_0 = 0.10 M, Initial Rate = 5.20 x 10^-3 M/s); Run 3 ([NO]_0 = 0.20 M, [Br2]_0 = 0.30 M, Initial Rate = 1.56 x 10^-2 M/s). What is the experimental rate law, overall reaction order, and numerical rate constant k?
Rate = k[NO][Br2], overall order = 2, and k = 0.130 M^-1*s^-1
Rate = k[NO][Br2]^2, overall order = 3, and k = 0.650 M^-2*s^-1
Rate = k[NO]^2[Br2], overall order = 3, and k = 1.30 M^-2*s^-1
Rate = k[NO]^2[Br2]^2, overall order = 4, and k = 13.0 M^-3*s^-1
The gas-phase dimerization of 1,3-butadiene (2 C4H6 -> C8H12) is second-order with respect to 1,3-butadiene with rate constant k = 0.0140 M^-1*s^-1 at 500 K. If the initial concentration of 1,3-butadiene is 0.0500 M, what is the initial half-life (t_1/2) and the total time required for 75.0% of the butadiene to react?
t_1/2 = 49.5 s and t_75% = 99.0 s
t_1/2 = 714 s and t_75% = 2143 s
t_1/2 = 1429 s and t_75% = 4286 s
t_1/2 = 1429 s and t_75% = 2857 s
An archaeological charcoal sample recovered from an excavation site in Palawan, Philippines exhibits a 14C specific activity of 2.40 disintegrations per minute per gram of carbon (dpm/g C). Modern living biological carbon has a steady-state activity of 15.30 dpm/g C. Given that the half-life of 14C is 5730 years, what is the estimated archaeological age of the charcoal specimen?
7640 years
15310 years
11460 years
22920 years
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