Env. Science
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AP Environmental Science — Quantitative Relationships

6 sections · 35 entries · print it and keep it beside your practice sets

AP Environmental Science does not publish an equation sheet, and a calculator is allowed on both sections — so about a quarter of the points come from arithmetic you set up yourself. These are the relationships the exam reuses year after year. Show every unit conversion: setup earns credit even when the final number is wrong.

Practise with the sheet, not from memory. The College Board hands out its own version of this page on exam day, so nothing here is worth memorising for its own sake. What earns points is speed: knowing which section a quantity lives in, and reading off the right line without breaking your train of thought. Keep this open (or printed) for every practice set you do.

Human population

Rule of 70
doubling time (years) = 70 / growth rate (% per year)

Doubling time from a percentage growth rate

A country growing at 2%/yr doubles in about 35 years. Works for any exponentially growing quantity, including energy demand.

NIR
NIR (%) = (CBR − CDR) / 10

Natural increase rate from crude birth and death rates (per 1,000 people)

Growth rate
growth rate (%) = ((CBR + immigration) − (CDR + emigration)) / 10

Including migration

TFR

Total fertility rate — average children per woman

Replacement-level fertility is about 2.1 in developed countries; higher where child mortality is high.

Population density
density = population / land area

People per unit area

IPAT
I = P × A × T

Environmental impact model

Impact = Population × Affluence × Technology.

Percent change, rates & efficiency

% change
% change = ((new − original) / original) × 100

Change relative to the starting value

Always divide by the ORIGINAL value. Note the difference between a change of 5 percentage points and a 5% change.

Rate
rate = amount / time

Any per-unit-time quantity

Efficiency
efficiency (%) = (useful energy out / total energy in) × 100

Useful output over total input

Trophic efficiency
energy at next level ≈ 0.10 × energy at current level

The 10% rule for energy transfer between trophic levels

Residence time
residence time = size of reservoir / flux in (or out)

Average time a molecule spends in a reservoir

Energy & power

Energy
energy = power × time

Energy from power and time

1 kW running for 1 hour = 1 kWh. This single line is behind most APES energy math.

kWh
1 kWh = 3.6 × 10⁶ J = 3.6 MJ

Kilowatt-hour in joules

EROEI
EROEI = energy returned / energy invested

Energy returned on energy invested

Dimensionless. Greater than 1 means net energy gain; conventional oil is high, tar sands and corn ethanol are low.

Capacity factor
capacity factor = actual output / (rated power × time)

How much of nameplate capacity a plant actually delivers

Fuel math
mass of fuel × energy per unit mass × efficiency = useful energy

Typical setup

Pollution, decay & toxicity

Half-life
remaining = initial × (1/2)^(t / t½)

Amount remaining after time t

After n half-lives, the fraction left is 1/2ⁿ: 3 half-lives leaves 12.5%.

ppm / ppb
1 ppm = 1 mg/L; 1 ppb = 1 μg/L = 0.001 mg/L

Concentration in water

Loading
loading = concentration × volume (or discharge)

Mass of pollutant delivered by a flow

LD50

Dose lethal to 50% of a test population

A LOWER LD50 means a MORE toxic substance.

BOD

Biochemical oxygen demand — oxygen consumed by decomposers

High BOD drives dissolved oxygen down, which is what kills fish in a eutrophic lake.

GWP
CO₂-equivalent = mass × GWP

Global warming potential, relative to CO₂ over 100 years

CO₂ = 1 by definition; methane ≈ 25–30; nitrous oxide ≈ 265–300. Multiply mass by GWP to compare gases.

Water & land

Q (discharge)
Q = A × v

Stream discharge from cross-sectional area and velocity

Units: m² × m/s = m³/s. Doubling the width of a channel at the same depth and speed doubles the discharge.

Volume of water
1 m³ = 1,000 L; 1 hectare = 10,000 m²; 1 km² = 100 hectares

Useful conversions

Irrigation / yield
total = area × per-area rate

Typical setup

Soil erosion
erosion rate = mass of soil lost / (area × time)

Mass lost per area per year

Biodiversity

Simpson’s index
D = 1 − Σ (n/N)²

Diversity index; n = individuals of one species, N = total individuals

Higher D means greater diversity. D = 0 is a monoculture; the maximum approaches 1.

Species richness

Simple count of species present

Richness ignores evenness — two communities with the same richness can have very different Simpson values.

Relative abundance
relative abundance = n / N

Share of the community made up by one species

Mark–recapture
N ≈ (number marked × total in second catch) / (marked recaptured)

Lincoln index estimate of population size

# Constants & conversions

CO₂
≈ 420 ppm

Approximate current atmospheric carbon dioxide concentration

Pre-industrial was about 280 ppm.

Atmosphere
78% N₂, 21% O₂, ~0.04% CO₂

Composition of dry air by volume

Earth’s water
~97% saltwater, ~3% fresh; of the fresh, ~69% is in ice caps and glaciers

Distribution of water

Solar constant
≈ 1,370 W/m²

Incoming solar radiation at the top of the atmosphere

Albedo
fresh snow ≈ 0.8–0.9; forest ≈ 0.1–0.2; Earth average ≈ 0.3

Fraction of sunlight reflected

Practise with the sheet openExam-skill drillsCheatsheet