Lab

See the idea. Put it to the test.

956 practicals from Kindergarten to Year 12, in 9 subjects. A practical gives the idea, what you need, the steps, what you should see and a safety card. A teacher-led practical gives the idea and its hazards; its method is for tutors on the learning platform.

Review

Reviewed before publication (owner’s confirmation, 24 September 2026). That covers every practical here, and a practical’s page lists the sources its author read.

A safety card on every page

The risk, who supervises and the hazards. The 38 teacher-led practicals show their idea and hazards here; their materials, steps and sources, and any result, control or note that states a number or an amount, are for tutors and administrators on the learning platform.

School laboratory, not for home

207 practicals are medium or high risk. Each says so on its page: In a school laboratory, with a teacher supervising, under the school's risk assessment. Not for home.

Curriculum references

Each practical lists the NSW syllabus outcomes and Australian Curriculum v9 codes it supports. They are references, not a verified or complete curriculum alignment.

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A practical is carried out at the bench, in the classroom or outdoors. A practical with its model not built stands on its own; the page says where a step mentions the model. A calculation and data practical works from published figures by hand, with a calculator or in a spreadsheet. No Lab page includes an interactive model; the Concept Studio holds the demonstrations.

13 practicals

Earth and Environmental Science 11–12 · Environment and sustainability · Weather and climate

  1. Earth and Environmental Science 11–12 · Year 11

    Albedo: how surface colour changes the energy absorbed and the temperature reached

    A surface reflects a fraction of the sunlight it receives (its albedo) and absorbs the rest, so ice, forest, ocean and city roofs warm at different rates under the same Sun.

    PracticalLow risk
  2. Earth and Environmental Science 11–12 · Year 11

    Angle of sunlight and energy received: the cosine law with a lamp and a light meter

    The energy a surface receives per square metre falls with the cosine of the angle from the perpendicular, which is why latitude, season and axial tilt control climate.

    Practical, model not builtLow risk
  3. Earth and Environmental Science 11–12 · Year 11

    Convection currents in a beaker (syllabus practical)

    Heated fluid expands, becomes less dense and rises while cooler fluid sinks, the circulation that carries heat through the mantle, oceans and atmosphere.

    PracticalMedium risk
  4. Earth and Environmental Science 11–12 · Year 11

    Density-driven ocean currents: cold, salty water sinking under warm, fresh water

    Temperature and salinity set seawater density, and density differences drive the deep circulation that moves heat between the poles and the tropics.

    PracticalLow risk
  5. Earth and Environmental Science 11–12 · Year 11

    Properties of water that shape the Earth: heat capacity, density of ice, surface tension and solvent action

    Water’s high heat capacity, expansion on freezing, surface tension and solvent power each follow from hydrogen bonding and each governs a large-scale Earth process.

    PracticalMedium risk
  6. Earth and Environmental Science 11–12 · Year 11

    Stick-slip on a brick: elastic energy storage and sudden release as an earthquake model

    Rock across a locked fault stores elastic potential energy until friction fails, and the sudden slip releases that energy as seismic waves.

    Practical, model not builtLow risk
  7. Earth and Environmental Science 11–12 · Year 11

    What drives the plates: a pupil model of slab pull, ridge push and mantle drag

    A cold, dense slab sinking at a subduction zone pulls the rest of the plate after it, and plate speeds show that this pull matters more than ridge push or mantle drag.

    PracticalLow risk
  8. Earth and Environmental Science 11–12 · Year 12

    Floating ice against land ice: which raises sea level when it melts

    Floating ice already displaces its own mass of water, so in fresh water its melting does not change the level, whereas ice resting on land adds new water to the ocean.

    PracticalLow risk
  9. Earth and Environmental Science 11–12 · Year 12

    Milankovitch cycles by hand: modelling eccentricity, tilt and precession

    Slow changes in the Earth’s orbit and axis redistribute sunlight between seasons and hemispheres over tens of thousands of years, pacing the ice ages.

    PracticalLow risk
  10. Earth and Environmental Science 11–12 · Year 12

    Ocean acidification: carbon dioxide lowering the pH of water and attacking carbonate shells

    Carbon dioxide dissolving in water forms carbonic acid, which lowers pH and dissolves calcium carbonate, the chemistry that threatens shell-building marine life.

    Practical, model not builtLow risk
  11. Earth and Environmental Science 11–12 · Year 12

    The greenhouse effect in a bottle, and why the bottle model needs care

    Carbon dioxide absorbs infrared radiation and warms the air, but a bottle mostly measures trapped convection, so the practical teaches both the effect and the limits of a physical model.

    PracticalLow risk
  12. Earth and Environmental Science 11–12 · Year 12

    Thermal expansion of water: measuring the rise in a flask and scaling to sea level

    Warmer water occupies more volume, so a warming ocean rises even before any ice melts, and the effect is measurable in a flask with a narrow tube.

    Practical, model not builtLow risk
  13. Earth and Environmental Science 11–12 · Year 12

    Tree rings as climate records: counting, measuring and cross-dating

    A tree adds one ring a year whose width follows the growing conditions, so ring sequences from overlapping trees give a dated record of past climate.

    PracticalLow risk

For tutors and administrators

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