IB ESS SL & HL 1.2 Systems Paper 1 & 2 ~13 min read

Open, Closed and Isolated Systems

Every system in this course gets sorted by one question: what crosses its boundary? Energy, matter, both, or neither. Answer that and you have classified it — and the answer explains why the Earth recycles everything it has.

📘 What you need to know

The three types

Which category a system falls into depends entirely on how energy and matter flow across its boundary.

What crosses the boundary? The one question that sorts every system into three types OPEN system energy: in and out matter: in and out an ecosystem, your body CLOSED system energy: in and out matter: stays inside the Earth, a sealed terrarium ISOLATED system energy: none matter: none theoretical only Amber arrows are energy; green arrows are matter Notice matter circulating inside the closed system rather than leaving it
Only two arrows change between the first two panels. That difference is the entire classification.

Open systems

Both energy and matter are exchanged with the surroundings. Open systems are usually organic (living) systems that interact with their environment by taking in energy and new matter, often as biomass, and expelling energy and matter as waste products or as organisms leaving.

An ecosystem or habitat is an open system. So is your body — energy and matter are exchanged with your environment as food, water, movement and waste.

Closed systems

Energy, but not matter, is exchanged. Closed systems are usually inorganic (non-living).

The Earth and its atmosphere can be viewed as a closed system:

Why this matters beyond the definition. If the Earth is closed to matter, then every atom we have is all we will ever have. Nothing is thrown “away” — it just moves to another storage. That single consequence underpins every waste, pollution and resource topic later in the course.

Global geochemical cycles are approximated to closed systems, because elements and compounds are continuously recycled between Earth’s natural reservoirs — the atmosphere, hydrosphere, lithosphere and biosphere. Overall quantities stay relatively constant over geological timescales. Carbon, for example, moves between the atmosphere, oceans and terrestrial ecosystems through photosynthesis, respiration and oceanic absorption, maintaining a dynamic equilibrium.

Artificial closed systems

Isolated systems

Neither energy nor matter is exchanged. Isolated systems do not exist naturally — they are a theoretical concept, though the entire Universe could arguably be considered one.

Systems at different scales

Environmental systems are interconnected networks of components and processes, found at every scale from a single organism to a whole ecosystem. They include interactions between living organisms, their habitats, and physical elements such as water, air and soil.

The same tools work at every scale Storages and flows describe a leaf and a planet equally well bromeliad rainforest the planet small-scale local system organisms live in its leaves large-scale ecosystem countless species interacting one integrated system atmosphere, oceans and land Each larger system contains the smaller ones inside it
Within a bromeliad’s leaves, organisms interact to form a microcosm. Within a rainforest you get predator-prey relationships, symbiosis, competition and nutrient cycles.

Earth as a single integrated system

Rather than a collection of independent parts, Earth can be seen as a complex integrated system of interconnected components.

The six components of the Earth system All six exchange energy and matter with one another constantly biosphere all living organisms hydrosphere oceans, rivers, lakes, groundwater cryosphere glaciers, ice caps, permafrost geosphere rocks, minerals, landforms atmosphere the layers of gas around Earth anthroposphere human activity and infrastructure The anthroposphere is the newest, and now shapes all the others Learn all six by name: they are used throughout the rest of the course
The atmosphere itself has layers — troposphere, stratosphere, mesosphere, thermosphere and exosphere — which you meet properly in Topic 6.

The Gaia hypothesis

The Gaia hypothesis, proposed by James Lovelock in the 1970s, presents a holistic view of Earth as a single, self-regulating system. Lovelock argued that Earth’s biota (living organisms) and their environment are closely linked and act together as one integrated system, with feedback mechanisms maintaining stability on a global scale — rather like homeostasis in a living organism.

It was introduced to explain how the composition of the atmosphere affects global temperature, and how the two are connected through complex feedback. Greenhouse gases such as carbon dioxide and methane raise global temperatures; in response, feedback mechanisms such as increased evaporation producing more cloud cover, or enhanced plant growth absorbing more carbon dioxide, may act to moderate that increase.

Support for GaiaCriticism of Gaia
A useful framework for understanding how Earth’s systems interconnectCriticised for anthropomorphism — comparing the Earth to a living organism
Refined over time with contributions from scientists such as Lynn MargulisCriticised for a lack of testability as a scientific hypothesis
Gaia is a gift for evaluation questions because it has a genuine two-sided argument. Some scientists find it a useful model of interconnection; others object that calling the Earth alive is not testable. Give both sides and then take a position — that structure is exactly what “evaluate” wants.

Worked examples

WE 1

Classifying systems

Distinguish between open, closed and isolated systems. (3 marks)

Open Both energy and matter are exchanged between the system and its surroundings. An ecosystem is an example. Closed Energy is exchanged but matter is not. The Earth is treated this way: solar radiation in, heat out, matter recycled inside. Isolated Neither energy nor matter is exchanged. These do not occur naturally and are a theoretical concept only. Both, energy only, or neither always say “energy and matter” explicitly — that is what is being compared
WE 2

The Earth as a closed system

Explain why the Earth is usually described as a closed system. (4 marks)

Step 1: energy crosses the boundary The main input is solar radiation, and the main output is heat re-radiated from the Earth’s surface as infrared. Step 2: matter does not Matter is recycled completely within the system through global geochemical cycles, so the total quantity of each element stays roughly constant. Step 3: the exception, and why it is ignored Very small amounts of matter do cross the boundary as meteorites, spacecraft and satellites, but these quantities are negligible. Step 4: the definition applied Since energy is exchanged but matter effectively is not, the Earth fits the definition of a closed system. Energy passes through; matter goes round and round mentioning the meteorite exception, and calling it negligible, shows precision
WE 3

Evaluating the Gaia hypothesis

Outline the Gaia hypothesis and evaluate its usefulness. (4 marks)

What it proposes Proposed by James Lovelock in the 1970s, it treats Earth as a single self-regulating system in which living organisms and their environment act together as one integrated whole. How it works Feedback mechanisms maintain stability, rather like homeostasis: rising temperatures may trigger more evaporation and cloud cover, or more plant growth absorbing carbon dioxide. Strength It is a useful framework for understanding how Earth’s systems are interconnected, and has been refined by scientists such as Lynn Margulis. Limitation It has been criticised for anthropomorphism, treating the Earth as a living organism, and for lacking testability. A valuable model of interconnection, but weak as a testable scientific hypothesis the judgement in the last line is what separates evaluate from describe

💡 Exam tips

⚠ Common mistakes

Up next: Equilibrium and Feedback Loops. You know what crosses the boundary. Now for the mechanism that keeps a system steady despite all that traffic — and the one that sends it spiralling.

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