GENERAL CHEMISTRY 2 • CHEMICAL KINETICS

Reaction Rate & Units — Define reaction rate and interpret rate units

Understanding how fast reactions proceed and expressing that speed in rigorous, stoichiometrically consistent units.

Historical Context & Motivation

Chemists have long recognized that reactions differ dramatically in speed—some, like the rusting of iron, unfold over years, while others, like the neutralization of a strong acid by a strong base, are essentially instantaneous. Yet for most of chemistry's early history, the discipline focused almost exclusively on what reactions produce (thermodynamic products) rather than how quickly they get there. The formal study of chemical kinetics—the branch of chemistry concerned with the rates and mechanisms of chemical reactions—emerged only in the mid-nineteenth century, as quantitative experimental methods matured enough to track concentration changes over time.

1850
Wilhelmy's Sucrose Hydrolysis
Ludwig Wilhelmy performed one of the first quantitative kinetic studies, measuring the rate of sucrose inversion in acid solution using a polarimeter. He demonstrated that the rate was proportional to the concentration of sucrose remaining—establishing the concept of a first-order rate law.
1864
Guldberg & Waage — Law of Mass Action
Cato Guldberg and Peter Waage proposed that the rate of a reaction depends on the active masses (concentrations) of the reactants, formalizing the relationship between concentration and rate that underpins modern rate expressions.
1889
Arrhenius Equation
Svante Arrhenius linked reaction rates to temperature through the now-famous equation k = A·e−Eₐ/RT, introducing the concept of activation energy and providing a physical basis for why rate constants change with temperature.
1913
Michaelis–Menten Kinetics
Leonor Michaelis and Maud Menten applied kinetic rate analysis to enzyme-catalyzed reactions, showing that enzyme kinetics could be described by saturation curves—extending chemical kinetics into biochemistry and demonstrating the universality of rate concepts.
1935
Transition State Theory
Henry Eyring and colleagues developed transition state theory, providing a statistical-mechanical framework for predicting rate constants from molecular properties. This theory gave kinetics a firm theoretical foundation and connected macroscopic rates to microscopic molecular behavior.

At the heart of all these developments lies a deceptively simple question: How do we quantify the speed of a chemical reaction? Before we can discuss rate laws, reaction orders, or mechanisms, we must first define precisely what we mean by reaction rate, choose appropriate units, and understand how stoichiometry links the rates of disappearance and appearance of different species. That foundational work is the focus of this lesson.

Core Principles & Definitions

A reaction rate quantifies the change in concentration of a reactant or product per unit time. Because reactants are consumed and products are formed, we adopt sign conventions and stoichiometric coefficients to ensure that the rate is always expressed as a positive quantity that is the same regardless of which species we choose to monitor. The following foundational ideas organize the treatment.

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Average Rate vs. Instantaneous Rate

The average rate is the change in concentration Δ[X] over a finite time interval Δt. The instantaneous rate is the limit of this ratio as Δt → 0—geometrically, it is the slope of the tangent line to the concentration-time curve at a specific moment.
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Sign Convention

Because reactant concentrations decrease (Δ[reactant] < 0), we prepend a negative sign to make the rate positive: rate = −Δ[reactant]/Δt. Product concentrations naturally increase, so no sign adjustment is needed: rate = +Δ[product]/Δt.
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Stoichiometric Normalization

Different species in a balanced equation disappear or appear at rates proportional to their stoichiometric coefficients. To obtain a single, unambiguous rate, we divide each species' rate of change by its coefficient: rate = −(1/a)·Δ[A]/Δt = −(1/b)·Δ[B]/Δt = +(1/c)·Δ[C]/Δt.
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Units of Rate

Since rate = Δ(concentration)/Δ(time), the SI unit is mol·L⁻¹·s⁻¹ (equivalently M/s or M·s⁻¹). Depending on the timescale, minutes or hours may replace seconds, and pressure units (atm, Pa) may replace molarity for gas-phase reactions.
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Experimental Measurement

Rates are measured by monitoring a physical property—absorbance, pressure, conductivity, mass loss—that correlates with concentration. The choice of observable depends on the system, but the resulting data always reduce to concentration vs. time curves from which rates are extracted.
✦ KEY TAKEAWAY
Think of reaction rate like reporting the speed of traffic flow on a highway. Each lane (species) moves at a different car-count per minute, but when you normalize by the number of lanes each vehicle occupies (stoichiometric coefficient), every observer agrees on a single, unified traffic flow rate. Similarly, dividing by stoichiometric coefficients ensures all species in a reaction yield the same overall reaction rate, regardless of which species you choose to monitor.

Visual Explanation — Concentration vs. Time

The most informative single graph in chemical kinetics is the concentration vs. time plot. By plotting [reactant] and [product] on the y-axis against elapsed time on the x-axis, we obtain curves whose slopes encode the reaction rate at every moment. The diagram below illustrates this for a generic reaction A → B, highlighting how the average rate over an interval differs from the instantaneous rate at a point.

The pink curve shows [A] decreasing over time while the cyan curve shows [B] increasing. The dashed secant line between two points on the [A] curve represents the average rate over Δt = 20 s. The green tangent line at an early time point gives the instantaneous rate at that moment.

Several features of this plot deserve emphasis. First, notice that the [A] curve is concave up and the [B] curve is concave down—both curves flatten as the reaction approaches completion (or equilibrium), reflecting the fact that the rate generally decreases as reactant is consumed. Second, the slope of the secant line joining two data points gives only the average rate over that interval, and it will depend on which two points you select. The tangent line at a single point eliminates this ambiguity—its slope is the instantaneous rate, obtained mathematically as the derivative d[A]/dt. In practice, the initial instantaneous rate (the slope at t = 0) is especially useful because concentrations are known precisely and competing reverse reactions or secondary processes have not yet become significant.

Mathematical Framework

The mathematical definition of reaction rate must accommodate three issues simultaneously: the sign convention (rates are always positive), the stoichiometry of the balanced equation, and the distinction between average and instantaneous rates. We address each in turn through the equations below.

AVERAGE RATE OF DISAPPEARANCE
Average rate of disappearance of A = −Δ[A] / Δt = −([A]₂ − [A]₁) / (t₂ − t₁)
Here [A]₁ and [A]₂ are molar concentrations at times t₁ and t₂. The negative sign ensures a positive value because [A]₂ < [A]₁ for a reactant being consumed.
INSTANTANEOUS RATE
Instantaneous rate = −d[A] / dt
The instantaneous rate is the limit of the average rate as Δt → 0 and equals the magnitude of the slope of the tangent to the [A] vs. t curve. In calculus terms, it is the negative of the first derivative of concentration with respect to time.
UNIQUE REACTION RATE (STOICHIOMETRIC FORM)
For aA + bB → cC + dD: rate = −(1/a)(d[A]/dt) = −(1/b)(d[B]/dt) = +(1/c)(d[C]/dt) = +(1/d)(d[D]/dt)
Dividing each species' rate of concentration change by its stoichiometric coefficient yields a single, unique reaction rate independent of which species is monitored. The lowercase letters a, b, c, d are the stoichiometric coefficients from the balanced equation.
⚠️ Important Convention
Many textbooks define the "rate of reaction" using the stoichiometric form above, while the "rate of disappearance of A" or "rate of appearance of C" refers to the un-normalized quantity (−d[A]/dt or +d[C]/dt, respectively). Always read carefully whether a problem asks for the reaction rate or the rate of disappearance/appearance of a specific species—they differ by a factor of the stoichiometric coefficient.
UNITS OF REACTION RATE
Rate = Δ(concentration) / Δ(time) → mol·L⁻¹·s⁻¹ (equivalently M/s or M·s⁻¹)
Alternative time units (min⁻¹, h⁻¹) may be used depending on the timescale. For gas-phase reactions, pressure-based units such as atm·s⁻¹ or Pa·s⁻¹ are common because partial pressure is proportional to molar concentration via the ideal gas law.

Stoichiometric Rate Relationships in Detail

One of the most common sources of error in kinetics problems is forgetting to account for stoichiometric coefficients when relating the rates of different species. Consider the reaction 2 N2O5(g) → 4 NO2(g) + O2(g). Because 2 mol of N2O5 decompose for every 1 mol of O2 formed, N2O5 disappears twice as fast as O2 appears. The diagram below maps these relationships visually.

Each species' rate of change equals the unique reaction rate multiplied by its stoichiometric coefficient. When rate = 1.0 × 10⁻³ M/s, N2O5 disappears at 2.0 × 10⁻³ M/s (×2), NO2 appears at 4.0 × 10⁻³ M/s (×4), and O2 appears at 1.0 × 10⁻³ M/s (×1).
Rate relationships for the decomposition of N₂O₅
SpeciesCoefficientRate ExpressionIf rate = 1.0 × 10⁻³ M/s
N₂O₅2 (reactant)−(1/2) d[N₂O₅]/dt−d[N₂O₅]/dt = 2.0 × 10⁻³ M/s
NO₂4 (product)+(1/4) d[NO₂]/dt+d[NO₂]/dt = 4.0 × 10⁻³ M/s
O₂1 (product)+d[O₂]/dt+d[O₂]/dt = 1.0 × 10⁻³ M/s

Worked Example

The following worked example integrates stoichiometric normalization, unit analysis, and the average-rate concept.

Calculating Average Rates for the Haber Process
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Step 1 — Write the Balanced EquationThe synthesis of ammonia is described by: N2(g) + 3 H2(g) → 2 NH3(g). The stoichiometric coefficients are a = 1 (N₂), b = 3 (H₂), and c = 2 (NH₃).
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Step 2 — Identify Given DataSuppose that over a 10.0-second interval, the concentration of H2 drops from 0.450 M to 0.390 M. We are asked to find (a) the average rate of disappearance of H₂, (b) the unique reaction rate, and (c) the average rate of appearance of NH₃.
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Step 3 — Average Rate of Disappearance of H₂−Δ[H₂]/Δt = −(0.390 − 0.450) / 10.0 = −(−0.060) / 10.0 = 0.0060 M/s. The rate of disappearance of H₂ is 6.0 × 10⁻³ M·s⁻¹.
−Δ[H₂]/Δt = 6.0 × 10⁻³ M·s⁻¹
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Step 4 — Unique Reaction RateUsing the stoichiometric form: rate = −(1/3)(Δ[H₂]/Δt) = (1/3)(6.0 × 10⁻³) = 2.0 × 10⁻³ M·s⁻¹. Because H₂ has a coefficient of 3, the reaction proceeds one-third as fast as H₂ is consumed.
Reaction rate = 2.0 × 10⁻³ M·s⁻¹
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Step 5 — Rate of Appearance of NH₃From the unique rate: rate = +(1/2)(Δ[NH₃]/Δt), so Δ[NH₃]/Δt = 2 × rate = 2 × (2.0 × 10⁻³) = 4.0 × 10⁻³ M·s⁻¹. Notice that NH₃ appears at twice the unique reaction rate because its coefficient is 2.
+Δ[NH₃]/Δt = 4.0 × 10⁻³ M·s⁻¹
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Step 6 — Verify with Stoichiometric RatiosCheck: the ratio (rate of disappearance of H₂) : (rate of appearance of NH₃) = 6.0 × 10⁻³ : 4.0 × 10⁻³ = 3 : 2, which matches the stoichiometric coefficients (3 H₂ : 2 NH₃). ✓ This internal consistency confirms our calculations.

Average vs. Instantaneous vs. Initial Rates

In experimental kinetics, three related but distinct quantities are invoked frequently: the average rate, the instantaneous rate, and the initial rate. Understanding the strengths and limitations of each is essential for designing experiments and interpreting data correctly.

Comparison of the three rate types commonly used in kinetics
Rate TypeDefinitionStrengthsLimitations
Average RateΔ[X]/Δt over a finite time intervalEasy to calculate from discrete data points; no calculus requiredDepends on interval chosen; may mask rate changes within the interval
Instantaneous Rated[X]/dt at a specific time tGives the true rate at a precise moment; connects to rate law directlyRequires a tangent or derivative, which can be sensitive to data scatter
Initial RateInstantaneous rate at t = 0Concentrations are exactly known; reverse reactions negligible; no product interferenceRequires rapid measurement or extrapolation to t = 0; may miss later-stage behavior
✦ KEY TAKEAWAY
The initial rate method is the workhorse of experimental kinetics because it provides data under the cleanest conditions: you know exactly what concentrations you started with, and neither reverse reactions nor secondary product build-up have had time to complicate matters. Think of it like clocking a sprinter's first few strides out of the blocks—free from wind fatigue or strategy adjustments, those early data points best reveal the runner's raw capability (i.e., the intrinsic rate law).

Connection to Rate Laws & the Rate Constant

Defining and computing reaction rates is only the first step. The deeper goal of chemical kinetics is to express the rate as a function of concentration through a rate law of the form rate = k[A]m[B]n, where k is the rate constant and m, n are the reaction orders with respect to each reactant (determined experimentally, not from stoichiometry). The units of k must make the overall expression dimensionally consistent with the rate units of M·s⁻¹, and this requirement provides a useful check on the overall reaction order.

Units of the rate constant k as a function of overall reaction order
Overall Reaction OrderRate Law FormUnits of k
0 (zeroth order)rate = kM·s⁻¹ (mol·L⁻¹·s⁻¹)
1 (first order)rate = k[A]s⁻¹
2 (second order)rate = k[A]² or k[A][B]M⁻¹·s⁻¹ (L·mol⁻¹·s⁻¹)
3 (third order)rate = k[A]²[B] etc.M⁻²·s⁻¹ (L²·mol⁻²·s⁻¹)
💡 Dimensional Analysis Tip
A quick formula for the units of k for an overall order n is: k has units of M1−n·s⁻¹. For example, for n = 2: M1−2·s⁻¹ = M⁻¹·s⁻¹. This relationship is derived by requiring that k × [concentration]n = M·s⁻¹, and it serves as a powerful dimensional consistency check.

This table previews the content of the next several lessons in chemical kinetics. The key point for now is that the reaction rate we have defined in this lesson is precisely the quantity that rate laws describe, and the units of the rate constant are always determined by the requirement that the rate law be dimensionally homogeneous, yielding concentration per time on both sides of the equation.

Practice Problems

PROBLEM 1 — CONCEPTUAL
For the reaction 2 SO2(g) + O2(g) → 2 SO3(g), if the rate of disappearance of O₂ is 3.5 × 10⁻⁴ M/s, is the rate of disappearance of SO₂ faster, slower, or the same? Explain using stoichiometric reasoning.
PROBLEM 2 — BASIC CALCULATION
The concentration of a reactant A decreases from 0.800 M to 0.600 M over 50.0 seconds. Calculate the average rate of disappearance of A. Express your answer in M·s⁻¹.
PROBLEM 3 — INTERMEDIATE
Consider the reaction 5 Br⁻(aq) + BrO₃⁻(aq) + 6 H⁺(aq) → 3 Br₂(aq) + 3 H₂O(l). If the rate of disappearance of Br⁻ is 2.50 × 10⁻² M·s⁻¹, determine: (a) the unique reaction rate, (b) the rate of disappearance of H⁺, and (c) the rate of appearance of Br₂.
PROBLEM 4 — APPLIED
A pharmaceutical chemist monitors the degradation of drug X in solution. She finds that [X] drops from 1.20 × 10⁻⁴ M to 0.85 × 10⁻⁴ M over 4.0 hours. (a) Express the average rate in M·min⁻¹ and M·s⁻¹. (b) If the degradation follows X → Y + Z (unimolecular decomposition), what is the average rate of appearance of Y in M·h⁻¹?
PROBLEM 5 — CRITICAL THINKING
A student measures the average rate of disappearance of reactant A over three successive 10-second intervals and obtains 8.0 × 10⁻³, 5.2 × 10⁻³, and 3.4 × 10⁻³ M·s⁻¹. She claims the instantaneous rate at t = 15 s (midpoint of the second interval) is exactly 5.2 × 10⁻³ M·s⁻¹. Critically evaluate her claim. Under what conditions would this approximation be most accurate, and when might it fail badly?

Lesson Summary

The reaction rate measures how quickly reactant concentrations decrease or product concentrations increase, expressed as the change in concentration per unit time. The average rate (Δ[X]/Δt) approximates behavior over a finite interval, while the instantaneous rate (d[X]/dt) captures the exact rate at a given moment as the slope of the tangent to the concentration-time curve. The initial rate—the instantaneous rate at t = 0—is experimentally favored because concentrations are precisely known and complicating factors are minimized.

A negative sign is affixed to reactant rate expressions to ensure all rates are positive, and dividing by stoichiometric coefficients yields a single, unambiguous unique reaction rate. The standard unit is mol·L⁻¹·s⁻¹ (M·s⁻¹), though alternative time or concentration units are used depending on the timescale and phase of the system. These foundational definitions set the stage for rate laws, where the reaction rate is expressed as a function of concentration through the rate constant k, whose units depend on the overall reaction order (M1−n·s⁻¹).

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