Unit 1: Fundamentals of environmental physics

Table of Contents

Basic concepts of light and matter

In environmental science, we study the interaction between energy and matter. The environment is composed of matter (atoms, molecules, soil, water, air) and is driven by energy, primarily from light (solar radiation).

The entire range of EMR is called the Electromagnetic Spectrum. This includes (from high energy/short wavelength to low energy/long wavelength): gamma rays, X-rays, ultraviolet (UV), visible light, infrared (IR), microwaves, and radio waves.

Real-world Application: The interaction of light and matter drives everything:

Quantum mechanics

Relation between energy, wavelength and frequency

Quantum mechanics explains that energy is not continuous but comes in discrete packets called quanta (for light, these are photons). The energy of a single photon is directly related to its frequency and inversely related to its wavelength.

Formula 1: Planck's Equation

E = hν

The frequency and wavelength of light are related by the speed of light (c).

Formula 2: Wave Equation

c = λν

By combining these two equations (rearranging Formula 2 as ν = c / λ and substituting into Formula 1), we get the most common form used in environmental science:

Formula 3: Energy-Wavelength Relation

E = hc / λ

Key Concept: This formula explains why UV radiation is dangerous while visible light is not.

Black body radiation

A black body is a theoretical, ideal object that absorbs 100% of the radiation that hits it (it doesn't reflect any) and emits radiation perfectly based on its temperature.

While no real object is a perfect black body, the Sun and the Earth are often approximated as black bodies to model the planet's energy budget.

There are two key laws governing black body radiation:

  1. Stefan-Boltzmann Law: Describes the total amount of energy an object radiates. It states that the total energy (E) radiated per unit surface area is proportional to the fourth power of its absolute temperature (T, in Kelvin).
    Formula: E = σT⁴ (where σ is the Stefan-Boltzmann constant)

    Implication: A small increase in temperature leads to a large increase in radiated energy. This is a key factor in global warming.

  2. Wien's Displacement Law: Describes the peak wavelength (λ_max) of the emitted radiation. It states that the peak wavelength is inversely proportional to the absolute temperature (T).
    Formula: λ_max = b / T (where b is Wien's displacement constant)
Application (Sun vs. Earth): This difference is the entire basis for the greenhouse effect. The atmosphere is transparent to the Sun's incoming short-wave radiation but opaque (absorbent) to the Earth's outgoing long-wave (infrared) radiation.

Spectroscopic concepts

Introduction to the concept of absorption and transmission of light

When light (a photon) hits a molecule, one of three things can happen:

Spectroscopy is the study of how EMR interacts with matter. In environmental chemistry, we use it to identify and quantify substances.

Beer-Lambert Law

The Beer-Lambert Law (or Beer's Law) is a fundamental principle for measuring the concentration of a substance in a solution. It states that the amount of light absorbed by a solution is directly proportional to the concentration of the absorbing substance and the path length of the light through the solution.

Formula: Beer-Lambert Law

A = εcl

Practical Application: This is the basis of colorimetry.
  1. You want to measure the amount of phosphate (a pollutant) in a water sample.
  2. Phosphate itself is colorless, so you add a reagent that reacts with phosphate to produce a blue color.
  3. The intensity of the blue color is proportional to the concentration of phosphate.
  4. You place the blue sample in a spectrophotometer, shine a light through it (at the wavelength the blue color absorbs most), and measure the Absorbance (A).
  5. Since you know 'ε' and 'l', you can rearrange the formula (c = A / εl) to find the concentration (c) of the phosphate.

Basic concepts of pressure, force, work and energy

Laws of thermodynamics

Thermodynamics is the study of energy, its transformations, and its relationship to matter. These laws are fundamental to understanding energy flow in ecosystems.

First Law of Thermodynamics (Law of Conservation of Energy)

"Energy cannot be created or destroyed, only changed from one form to another."

Ecological Implication: All energy in an ecosystem must be accounted for. The total energy from the sun that is captured by plants (producers) is either:

This law explains the flow of energy through a food web.

Second Law of Thermodynamics (Law of Entropy)

"In any energy conversion, some energy is converted to a less useful form (usually heat), and the total disorder (entropy) of the system increases."

This means no energy transfer is 100% efficient.
Ecological Implication: This is the most important law in ecology. It explains:

Be able to explain the 10% rule and ecological pyramids using the First and Second Laws of Thermodynamics.