⚗️ Reaction Order Calculator
Solve zero order, first order, and second order reaction kinetics — calculate concentration at any time, find rate constant k, compute half-life for all reaction orders, and determine reaction order from experimental data with full step-by-step integrated rate law working.
[A] = [A]₀ − kt
ln[A] = ln[A]₀ − kt
1/[A] = 1/[A]₀ + kt
Enter concentration vs time data — the calculator tests zero order ([A] vs t) and first order (ln[A] vs t) linearity, computes R² values, and identifies the reaction order.
| Time (s) | Concentration [A] (M) |
|---|
Zero Order vs First Order Reactions — Key Differences
The most important distinction: zero order half-life depends on initial concentration while first order half-life is constant and independent of concentration. This single fact separates the two reaction orders in every kinetics course.
| Property | 🟦 Zero Order | 🟨 First Order |
|---|---|---|
| Rate Law | rate = k |
rate = k[A] |
| Integrated Rate Law | [A] = [A]₀ − kt |
ln[A] = ln[A]₀ − kt |
| Concentration Form | Linear: [A] vs t | Exponential: [A] = [A]₀e^(−kt) |
| Graph [A] vs t | Straight line (negative slope −k) | Exponential decay curve |
| Graph ln[A] vs t | Curved (non-linear) | Straight line (slope = −k) |
| Units of k | M·s⁻¹ or mol/(L·s) | s⁻¹ or 1/s |
| Half-life Formula | t½ = [A]₀/(2k) |
t½ = 0.693/k |
| Half-life depends on [A]₀? | ✅ YES — Depends on [A]₀ | ❌ NO — Always constant |
| Successive half-lives | Each one is SHORTER (less reactant) | Each one is IDENTICAL (constant) |
| Examples | Photochemistry, surface reactions, saturated enzymes | Radioactive decay, drug metabolism, organic decomposition |
Zero Order Reactions — Rate = k
In a zero order reaction (also written zeroth order), the reaction rate is completely independent of the reactant concentration. No matter how much or how little [A] is present, the reaction proceeds at the same constant rate k. This typically occurs when a catalyst, enzyme, or light-source is saturated — the rate is limited by something other than the amount of reactant.
rate = −d[A]/dt = k
Integrate: −∫d[A] = ∫k dt
−([A] − [A]₀) = kt
[A] = [A]₀ − kt ✓
Plot [A] vs time → straight line
Slope = −k (units: M/s)
y-intercept = [A]₀
x-intercept = t_complete = [A]₀/k
| Example | Values | Calculation | Result |
|---|---|---|---|
| Find [A] at t=10 s | [A]₀=0.5M, k=0.02 M/s | [A]=0.5−(0.02×10)=0.5−0.2 | 0.3 M |
| Find half-life | [A]₀=1.0M, k=0.05 M/min | t½=1.0/(2×0.05)=1.0/0.1 | 10 min |
| Find k | [A]₀=0.8M, [A]=0.5M, t=15s | k=(0.8−0.5)/15=0.3/15 | 0.02 M/s |
First Order Reactions — Rate = k[A]
A first order reaction has a rate directly proportional to the reactant concentration [A]. As [A] decreases, the rate decreases proportionally — producing the characteristic exponential decay curve. First order kinetics is the most common reaction order in chemistry and biology.
rate = −d[A]/dt = k[A]
Separate: −d[A]/[A] = k dt
Integrate: −ln[A] = kt + C
At t=0: C = −ln[A]₀
ln[A] = ln[A]₀ − kt ✓
[A] vs t → exponential curve
ln[A] vs t → straight line
Slope of ln[A] plot = −k (s⁻¹)
y-intercept of ln[A] plot = ln[A]₀
| Example | Values | Calculation | Result |
|---|---|---|---|
| Find [A] at t=10 s | [A]₀=1.0M, k=0.1 s⁻¹ | [A]=1.0×e^(−0.1×10)=e^(−1) | 0.368 M (36.8%) |
| Find time t | [A]₀=0.5M, [A]=0.125M, k=0.2 min⁻¹ | t=ln(0.5/0.125)/0.2=ln(4)/0.2 | 6.93 min |
| Find half-life | k=0.05 hour⁻¹ | t½=0.693/0.05 | 13.86 hours |
| Find k | [A]₀=1.0M, [A]=0.25M, t=20 s | k=ln(1.0/0.25)/20=ln(4)/20 | 0.0693 s⁻¹ |
Half-Life Formula: Zero Order vs First Order
- DEPENDS on initial concentration [A]₀
- More starting material → longer half-life
- 1 M takes 10 min; 2 M takes 20 min (same k)
- Each successive half-life is shorter
- Reaction reaches zero in finite time
- INDEPENDENT of initial concentration [A]₀
- Same half-life for any starting amount
- 1 M or 0.001 M: same t½
- Every half-life is identical
- Concentration approaches zero asymptotically
The formulas t½ = [A]₀/(2k) and t½ = 0.693/k capture the fundamental difference: zero order half-life depends on [A]₀; first order half-life does not.
| [A]₀ | k (M/s zero; s⁻¹ first) | Zero t½ (s) | First t½ (s) |
|---|---|---|---|
| 0.5 M | 0.05 | 5.0 s | 13.86 s |
| 1.0 M | 0.05 | 10.0 s | 13.86 s |
| 2.0 M | 0.05 | 20.0 s | 13.86 s |
| 5.0 M | 0.05 | 50.0 s | 13.86 s |
Same k = 0.05 for both orders. Zero order t½ changes with [A]₀; first order t½ stays constant at 13.86 s.
Integrated Rate Law Equations — Complete Formula Reference
The integrated rate law equations are derived by integrating the differential rate law. The key relationships: [A] = [A]₀ − kt (zero order), ln[A] = ln[A]₀ − kt (first order), and 1/[A] = 1/[A]₀ + kt (second order).
| Reaction Order | Rate Law | Integrated Form | Alternative Form | Linear Plot | Slope |
|---|---|---|---|---|---|
| Zero Order | rate = k |
[A] = [A]₀ − kt |
— | [A] vs t | −k |
| First Order | rate = k[A] |
ln[A] = ln[A]₀ − kt |
[A] = [A]₀e^(−kt) |
ln[A] vs t | −k |
| Second Order | rate = k[A]² |
1/[A] = 1/[A]₀ + kt |
[A] = 1/(1/[A]₀ + kt) |
1/[A] vs t | +k |
How to Find Rate Constant k — All Three Reaction Orders
| Reaction Order | Formula for k | Units of k | How to find from graph |
|---|---|---|---|
| Zero Order | k = ([A]₀ − [A])/t |
M·s⁻¹ | Slope of [A] vs t (negative) |
| First Order | k = ln([A]₀/[A])/t |
s⁻¹ | −Slope of ln[A] vs t |
| Second Order | k = (1/[A] − 1/[A]₀)/t |
M⁻¹·s⁻¹ | Slope of 1/[A] vs t (positive) |
[A]₀=1.0M, [A]=0.6M at t=20s
k = (1.0−0.6)/20 = 0.4/20 = 0.020 M/s
[A]₀=1.0M, [A]=0.368M at t=10s
k = ln(1.0/0.368)/10 = 1.000/10 = 0.100 s⁻¹
[A]₀=0.5M, [A]=0.357M at t=8s
k = (1/0.357−1/0.5)/8 = (2.80−2.0)/8 = 0.100 M⁻¹s⁻¹
Zero, First and Second Order Reactions — Complete Comparison
Master reference table for all three reaction orders — the most important table in chemical kinetics.
| Property | 🟦 Zero Order | 🟨 First Order | 🟪 Second Order |
|---|---|---|---|
| Rate law | rate = k | rate = k[A] | rate = k[A]² |
| Integrated rate law | [A] = [A]₀ − kt | ln[A] = ln[A]₀ − kt | 1/[A] = 1/[A]₀ + kt |
| Linear plot | [A] vs t | ln[A] vs t | 1/[A] vs t |
| Slope of linear plot | −k | −k | +k |
| Units of k | M·s⁻¹ | s⁻¹ | M⁻¹·s⁻¹ |
| Half-life formula | t½ = [A]₀/2k | t½ = 0.693/k | t½ = 1/k[A]₀ |
| Half-life depends on [A]₀? | ✅ YES | ❌ NO (constant) | ✅ YES |
| Successive half-lives | Decrease (shorter each time) | Constant (same every time) | Increase (double each time) |
| Real examples | Photochemistry, surface reactions | Radioactive decay, drug metabolism | NO₂ decomposition, ozone |
How to Determine Reaction Order — Method Explained
The graphical method for determining reaction order uses the integrated rate laws as tests. The plot that produces a straight line identifies the reaction order.
| Time (s) | [A] (M) | ln[A] | 1/[A] (M⁻¹) |
|---|---|---|---|
| 0 | 1.000 | 0.000 | 1.000 |
| 10 | 0.905 | −0.100 | 1.105 |
| 20 | 0.819 | −0.200 | 1.221 |
| 30 | 0.741 | −0.300 | 1.350 |
| 50 | 0.607 | −0.500 | 1.647 |
| → ln[A] vs t is perfectly linear: this is a FIRST ORDER reaction, k = 0.010 s⁻¹ | |||
Real-World Applications — Where Zero and First Order Reactions Happen
🟦 Zero Order Examples
When light intensity limits the reaction, rate equals the photon flux regardless of reactant concentration. Photosynthesis approaches zero order when CO₂ is abundant and light is limiting.
When enzyme active sites are fully saturated with substrate, adding more substrate has no effect. The rate is k (determined by enzyme turnover) — zero order with respect to substrate. [A] = [A]₀ − kt applies perfectly.
Heterogeneous catalysis on a solid surface proceeds at zero order when the surface is fully covered. The rate depends on catalyst surface area, not reactant concentration. The zero order formula rate = k describes this precisely.
🟨 First Order Examples
Carbon-14 has a constant half-life of 5,730 years. No matter how much C-14 you start with, half decays in 5,730 years. After 11,460 years: 25% remains. After 17,190 years: 12.5%. This constant half-life — from t½ = 0.693/k — is why C-14 dating works precisely.
Most drugs are eliminated from the bloodstream at a rate proportional to their concentration — first order kinetics. Ibuprofen half-life: ~2 hours. After 10 hours (5 half-lives): only 3.1% remains. Dosing schedules use t½ = 0.693/k to maintain therapeutic levels.
Ozone (O₃) decomposition in the stratosphere follows first order kinetics. The rate = k[O₃] means ozone concentration decays exponentially as [A] = [A]₀e^(−kt). Catalytic destruction by CFCs follows the same first order mathematics.
Worked Examples
[A]₀=0.5M, k=0.02 M/s, t=10s. Formula: [A] = [A]₀ − kt. Substitute: [A] = 0.5 − (0.02×10) = 0.5 − 0.2 = 0.30 M. Concentration reduced by 40% in 10 seconds at constant rate of 0.02 M per second.
[A]₀=0.8M, [A]=0.6M at t=10s. Rearrange [A]=[A]₀−kt: k=([A]₀−[A])/t = (0.8−0.6)/10 = 0.20/10 = 0.020 M/s. Units of k for zero order are always M/s (or mol·L⁻¹·s⁻¹).
[A]₀=1.0M, k=0.05 M/min. Formula: t½=[A]₀/(2k) = 1.0/(2×0.05) = 1.0/0.10 = 10.0 minutes. At t=10 min: [A]=0.5M. At t=20 min: [A]=0M. Total reaction time = [A]₀/k = 1.0/0.05 = 20 minutes.
[A]₀=1.0M, k=0.1 s⁻¹, t=10s. [A]=1.0×e^(−0.1×10)=e^(−1.0)=0.368M. Using ln form: ln[A]=ln(1.0)−(0.1)(10)=0−1=−1, so [A]=e^(−1)=0.368M. 36.8% of initial concentration remains.
[A]₀=0.5M, [A]=0.125M, k=0.2 min⁻¹. Rearrange: kt=ln([A]₀/[A])=ln(0.5/0.125)=ln(4)=1.386. t=1.386/0.2=6.93 minutes. Equivalently: 0.125/0.5=0.25=(1/2)², so 2 half-lives → t=2×(0.693/0.2)=6.93 min ✓
Plot [A] vs t → curved exponential. Plot ln[A] vs t → straight line with R²=0.9998. Conclusion: first order reaction. From slope of ln[A] plot: slope=−k=−0.050, so k=0.050 s⁻¹. Half-life=0.693/0.050=13.86 s.
k=0.05 hour⁻¹. t½=0.693/0.05=13.86 hours. This is identical regardless of whether [A]₀ is 0.001M or 1000M. After 10 half-lives: (1/2)^10=0.00098=0.098% remains. Time=10×13.86=138.6 hours=5.77 days.
k=0.693 hour⁻¹, [A]₀=2.0M, t=2 hours. [A]=2.0×e^(−0.693×2)=2.0×e^(−1.386)=2.0×0.250=0.500M. Check: t½=0.693/0.693=1.0 hour. After 2 hours=2 half-lives: 2.0×(0.5)²=2.0×0.25=0.500M ✓
Target: reach 5% of initial. n=ln(0.05)/ln(0.5)=−2.996/−0.693=4.32 half-lives. For k=0.1 s⁻¹: t½=6.93s, time=4.32×6.93=29.9 seconds. Formula: n=ln(fraction remaining)/ln(0.5)=log₂(1/fraction).
First order: t½=5,730 years (Carbon-14). k=0.693/t½=0.693/5730=1.209×10⁻⁴ year⁻¹. In seconds: k=1.209×10⁻⁴/(3.156×10⁷)=3.83×10⁻¹² s⁻¹. This allows calculation of C-14 remaining in any archaeological sample.