Integrated Rate Law Calculator

Calculate concentration, time, and rate constants for different reaction orders

Integrated Rate Laws

Calculate concentration, time, or rate constant for zero, first, and second order reactions.

Select Reaction Order:

Calculate:

Example Problems:

Understanding Integrated Rate Laws

Zero Order:

Concentration decreases linearly with time. Common in surface-catalyzed reactions and enzyme kinetics when substrate is saturated. Half-life decreases as reaction proceeds.

First Order:

Concentration decreases exponentially with time. Common in radioactive decay and many decomposition reactions. Half-life is constant (independent of concentration).

Second Order:

1/[A] increases linearly with time. Common in gas-phase reactions and dimerizations. Half-life increases as reaction proceeds (takes longer when concentration is lower).

Graphical Analysis:

  • Zero order: Plot [A] vs t → straight line (slope = -k)
  • First order: Plot ln[A] vs t → straight line (slope = -k)
  • Second order: Plot 1/[A] vs t → straight line (slope = k)

What are Integrated Rate Laws?

Integrated rate laws are mathematical equations that relate the concentration of a reactant to time. Unlike differential rate laws (which express rate as a function of concentration), integrated rate laws allow us to predict concentrations at any point in time.

The form of the integrated rate law depends on the order of the reaction with respect to the reactant. The three most common cases are:

  • Zero order: Rate is independent of concentration
  • First order: Rate is directly proportional to concentration
  • Second order: Rate is proportional to concentration squared

Key Concept:

Integrated rate laws are derived by integrating the differential rate law. They provide a direct relationship between concentration and time, making them extremely useful for experimental kinetics and predicting reaction progress.

The Three Reaction Orders

Zero Order Reactions

Differential Rate Law:

Rate = k

Integrated Rate Law:

[A] = [A]₀ - kt

(Linear decrease in concentration with time)

Half-Life:

t½ = [A]₀ / (2k)

(Decreases as reaction proceeds - depends on initial concentration)

Graphical Analysis:

Plot [A] vs t → straight line with slope = -k

Examples:

  • Photochemical reactions (constant light intensity)
  • Enzyme-catalyzed reactions at high substrate concentration
  • Surface-catalyzed reactions when surface is saturated

First Order Reactions

Differential Rate Law:

Rate = k[A]

Integrated Rate Law:

ln[A] = ln[A]₀ - kt

or [A] = [A]₀e^(-kt)

(Exponential decrease in concentration with time)

Half-Life:

t½ = ln(2) / k = 0.693 / k

(Constant - independent of concentration!)

Graphical Analysis:

Plot ln[A] vs t → straight line with slope = -k

Examples:

  • Radioactive decay (all radioactive nuclei)
  • Decomposition of N₂O₅, H₂O₂
  • Many unimolecular gas-phase reactions
  • Enzyme reactions at low substrate concentration

Second Order Reactions

Differential Rate Law:

Rate = k[A]²

Integrated Rate Law:

1/[A] = 1/[A]₀ + kt

(Reciprocal of concentration increases linearly with time)

Half-Life:

t½ = 1 / (k[A]₀)

(Increases as reaction proceeds - depends on initial concentration)

Graphical Analysis:

Plot 1/[A] vs t → straight line with slope = k

Examples:

  • Dimerization reactions (2A → A₂)
  • Gas-phase reactions: NO₂ → NO + O
  • Many bimolecular reactions when [A] = [B]

Comparison of Reaction Orders

PropertyZero OrderFirst OrderSecond Order
Rate LawRate = kRate = k[A]Rate = k[A]²
Integrated Form[A] = [A]₀ - ktln[A] = ln[A]₀ - kt1/[A] = 1/[A]₀ + kt
Half-Life[A]₀/(2k)0.693/k1/(k[A]₀)
Linear Plot[A] vs tln[A] vs t1/[A] vs t
Slope of Plot-k-k+k
Units of kM·s⁻¹s⁻¹M⁻¹·s⁻¹
t½ DependenceDecreasesConstantIncreases

Worked Example: First Order Reaction

Problem:

The decomposition of N₂O₅ is first order with k = 5.7 × 10⁻⁴ s⁻¹. If the initial concentration is 0.100 M, what will be the concentration after 2000 seconds?

Given Information:

  • Reaction order: First order
  • [A]₀ = 0.100 M
  • k = 5.7 × 10⁻⁴ s⁻¹
  • t = 2000 s
  • Find: [A] at t = 2000 s

Solution:

Step 1: Write the integrated rate law for first order

[A] = [A]₀ e^(-kt)

Step 2: Substitute values

[A] = (0.100 M) × e^(-(5.7×10⁻⁴ s⁻¹)(2000 s))

Step 3: Calculate the exponent

-kt = -(5.7×10⁻⁴)(2000) = -1.14

Step 4: Calculate e^(-1.14)

e^(-1.14) = 0.3198

Step 5: Calculate final concentration

[A] = (0.100 M)(0.3198) = 0.0320 M

Answer:

After 2000 seconds, the concentration will be 0.0320 M, which is about 32% of the original concentration.

Note: The half-life for this reaction is t½ = 0.693/k = 0.693/(5.7×10⁻⁴) = 1216 s. Since 2000 s is slightly more than one half-life, having about 32% remaining (slightly less than 50%) makes sense.

Real-World Applications

1. Drug Pharmacokinetics

Most drug metabolism follows first-order kinetics. Integrated rate laws help determine dosing schedules, predict drug concentrations in blood over time, and calculate how long it takes for a drug to be eliminated from the body.

2. Radioactive Dating

Radioactive decay is first-order. Carbon-14 dating uses the integrated rate law to determine the age of archaeological artifacts. By measuring remaining C-14 and knowing its half-life (5,730 years), we can calculate the age of organic materials.

3. Environmental Chemistry

Degradation of pollutants often follows first-order kinetics. Integrated rate laws predict how long it takes for pesticide residues, pharmaceutical contaminants, or oil spills to degrade to safe levels in soil and water.

4. Food Science

Food spoilage reactions (vitamin degradation, flavor loss, color changes) often follow first-order kinetics. Integrated rate laws help determine shelf life, optimal storage conditions, and expiration dates for food products.

5. Chemical Engineering

Industrial reactor design requires integrated rate laws to determine reactor size, residence time, and optimal operating conditions. Engineers use these equations to scale up processes from laboratory to production scale.

6. Atmospheric Chemistry

Ozone depletion, greenhouse gas reactions, and smog formation all involve reactions with specific rate laws. Integrated rate laws help model atmospheric changes and predict future concentrations of important atmospheric species.

Problem-Solving Strategy

Step 1: Identify the Reaction Order

  • Given explicitly in the problem
  • Determined from rate law (check exponent on [A])
  • Found from experimental data using graphical method
  • Inferred from units of rate constant k

Step 2: Write the Appropriate Integrated Rate Law

  • Zero order: [A] = [A]₀ - kt
  • First order: ln[A] = ln[A]₀ - kt or [A] = [A]₀e^(-kt)
  • Second order: 1/[A] = 1/[A]₀ + kt

Step 3: Identify Known and Unknown Variables

  • [A]₀ = initial concentration
  • [A] = concentration at time t
  • k = rate constant
  • t = time
  • Determine which three you know and which one you need to find

Step 4: Substitute and Solve

  • Plug in known values into the integrated rate law
  • Rearrange to solve for the unknown
  • Be careful with units - they must be consistent
  • For first order with ln: use natural log (ln), not log₁₀

Step 5: Check Your Answer

  • [A] should be less than [A]₀ (concentration decreases)
  • Time should be positive
  • Rate constant k should be positive
  • Compare to half-life if known: does the answer make sense?
  • Check units of final answer

Common Mistakes to Avoid

❌ Using log₁₀ Instead of ln for First Order

The integrated rate law for first order uses natural logarithm (ln), not log base 10.

Correct: ln[A] = ln[A]₀ - kt

❌ Forgetting e^x When Solving First Order

After calculating ln[A], you must use e^x to get back to [A].

Correct: If ln[A] = -1.5, then [A] = e^(-1.5) = 0.223, not -1.5

❌ Incorrect Sign in Rate Law

For zero order: [A] = [A]₀ minus kt (not plus). For second order: 1/[A] = 1/[A]₀ plus kt.

Remember: Concentration always decreases, but the mathematical form varies by order.

❌ Inconsistent Units

If k is in s⁻¹, time must be in seconds. If k is in min⁻¹, time must be in minutes.

Correct approach: Convert all units to match before calculating.

❌ Confusing [A] and [A]₀

[A]₀ is always the initial concentration (at t=0). [A] is the concentration at time t.

Remember: The subscript 0 means "initial" or "at time zero".

❌ Wrong Equation for Reaction Order

Using a first-order equation for a second-order reaction (or vice versa) will give completely wrong results.

Correct approach: Always verify the reaction order before choosing the equation.

Quick Reference Guide

Zero Order

[A] = [A]₀ - kt

t½ = [A]₀/(2k)

Plot [A] vs t → line
Slope = -k
Units: M·s⁻¹

First Order

[A] = [A]₀e^(-kt)

t½ = 0.693/k

Plot ln[A] vs t → line
Slope = -k
Units: s⁻¹

Second Order

1/[A] = 1/[A]₀ + kt

t½ = 1/(k[A]₀)

Plot 1/[A] vs t → line
Slope = k
Units: M⁻¹·s⁻¹