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NZC — Science Phase 2 (Years 4–6)

This page provides the draft progress outcome and teaching sequence for Phase 2 (Years 4–6) of the Science Learning Area. This is now available for wider feedback and familiarisation. The current Science curriculum remains in effect until 1 January 2027.

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About this resource

This page provides the draft year 4–6 Science Learning Area. This is now available for wider feedback and familiarisation. The current Science curriculum remains in effect until 1 January 2027 and can be found here The New Zealand Curriculum – Science.

Teaching Sequence

The following table presents a list of examples to illustrate the materials, tools and equipment that can support safe, purposeful, and increasingly complex teaching in Years 4 to 6. Appropriate use of a range of materials, tools, and equipment will ensure students can access all relevant knowledge and practices within the teaching sequence.

Indicative Materials, Tools, and Equipment

Materials
Solids and liquids: ice cubes, salt, sugar, sand, cooking oil, water, vinegar
Mixtures: soil samples, saltwater, baking soda and vinegar, flour and water paste
Magnetic: iron filings, paper clips, magnets
Conductive and insulated: copper wire, aluminium foil, plastic, rubber
Transparent and opaque: glass, plastic sheets, cardboard, fabric

Tool
Measuring: thermometers, rulers, measuring jugs, scales, timers
Testing: magnets, sieves, filters, conductivity testers
Recording: notebooks, pencils, observation charts, digital cameras
Manipulating: tweezers, droppers, stirring rods, funnels

Equipment
Containers: trays, jars, bowls, buckets, tin cans, various plastic bottles
Energy and circuits: batteries, wires, bulbs, switches, buzzers
Light and sound: torches, mirrors, prisms, tuning forks, water bowls
Simple machines: pulleys, ramps, levers (e.g. ruler and eraser setups)

Physical Science

Knowledge

The facts, concepts, principles, and theories to teach.

Practices

The skills, strategies, and applications to teach.

During Year 4

During Year 5

During Year 6

During Year 4

During Year 5

During Year 6

Materials

Heat and states of matter

  • Matter is anything that has mass and takes up space.
  • Matter exists in different states — solid, liquid, and gas:
    • a solid is a state of matter that has a definite shape and volume (e.g. ice)
    • a liquid is a state of matter that has a definite volume but no definite shape (e.g. water, milk)
    • a liquid flows and takes the shape of the container it is in
    • a gas is a state of matter that has neither definite shape nor definite volume
    • a gas flows easily and expands to the size of the container it is in (e.g. air in a balloon)
    • volume is the amount of space a solid, liquid, or gas takes up
    • powders are granular solids and can flow and be poured, like liquids. 
  • Matter can change state if heated or cooled (melting, boiling/evaporation, freezing, condensation).
  • At sea level, freshwater boils at 100°C and freezes at 0°C.
  • Robert Boyle (1627–1691) established the relationship between temperature and pressure in gases, known as Boyle’s Law. He is considered one of the founders of modern chemistry.

Mass, volume, and density

  • Mass is the amount of matter in an object, measured in kilograms (kg) or grams (g).
  • Volume is measured in cubic metres (m³) or litres (L).
  • Objects may have the same volume but different masses and vice versa.
  • The relationship between mass and volume is known as density.
  • The density of an object determines whether it will float or sink in another material:
    • less dense materials will float on more dense materials (e.g. foam on water, oil on water, helium balloons in air, air in water)
    • more dense materials will sink in less dense materials (e.g. coins in water, vinegar in oil, dishwashing liquid in water). 
  • The French Academy of Sciences (1790s) developed the metric system for weight, length, and volume, standardising measurements across science, industry, and education.
  • Note: Floating and sinking only occurs in liquids and gases.

Heat and states of matter

  • Investigating and recording changes of state in common materials, including water, by observing, measuring, and interpreting data
  • Making and testing predictions about how heating affects the physical properties of matter (e.g. chocolate melting, metal getting hot, water boiling)

Mass, volume, and density

  • Comparing densities of objects based on measurements of the mass (in grams) and volume (in mL)
  • Describing the density of solids and liquids using comparative language
  • Making and testing predictions of whether materials float or sink in water

Matter Interactions and Energy

Heat

  • Thermal energy comes from many sources (e.g. the Sun, fire, friction, electricity).
  • Thermal energy moves from warmer materials to cooler materials, not the other way around.
  • Thermal energy continues to transfer between materials until they both reach the same temperature.
  • Light can warm objects when it shines on them because some of the light is absorbed and is transformed into thermal energy. 
  • Temperature is a measure of how hot a substance is. Temperature can be measured using thermometers, usually in degrees Celsius (°C).
  • Anders Celsius (1701–1744) created the Celsius temperature scale, which is widely used to measure temperature changes in physical and chemical processes.
  • Note: Students at this level are not expected to know that temperature is a measure of the average kinetic energy of a substance.
     

Behaviour of Light
(See Year 3, Light and Sound)

  • Everything we see is either a light source or reflected light. For an object to be visible, light must travel from a light source to the object to the eyes. This occurs when light travels from a source directly to the eyes or when it reflects off objects and then reaches the eyes.
  • When an object appears to be reflected (e.g. in a mirror or water), light has travelled from a light source to the object, then to the reflective surface, then to the eyes.
  • Refraction of light occurs when light changes direction as it passes from one medium to another (e.g. from air into water).

Simple circuits

  • Simple circuits involve a closed loop connecting a source of electricity, wires, and a load (e.g. lightbulb, buzzer).
  • Switches can open and close a circuit to control the flow of electricity.
  • Electricity is conducted in a circuit through metal wires.
  • Circuit diagrams represent the components of circuits using standard symbols for the battery, wires, switch, and load.
  • Thomas Edison (1847–1931) developed practical electric circuits for lighting and invented the incandescent light bulb. He held over 1,000 patents and revolutionised modern technology.
     

Heat

  • Measuring temperature using a thermometer and describing how warm or cool something is in degrees Celsius (°C)
  • Applying the movement of thermal energy from warmer objects to cooler objects to everyday examples and using evidence to demonstrate how this transfer happens (e.g. ice blocks in water, food in a hot frying pan)
  • Exploring how light-emitting objects also release thermal energy (e.g. LED and incandescent bulbs)
  • Exploring how light is absorbed by objects made of different materials and shades, causing the objects to warm differently

Behaviour of light

  • Using diagrams to demonstrate how objects are visible to the eye
  • Investigating how light travels and changes direction by reflecting (e.g. from a mirror) and refracting (e.g. water to air) by predicting, observing, recording, and interpreting data

Simple circuits

  • Building a basic circuit with an on/off switch
  • Drawing a circuit diagram using standard symbols for the battery, switch, wires, and load
  • Explaining how circuits work by transferring energy electrically and transforming it into other forms of energy 

Motion and Forces

Contact forces and movement 

  • A force is a push or pull that can cause an object to move, stop, change direction, or change shape.
  • Forces have direction and size, and this can be represented by simple force-arrow diagrams.
  • Friction is a force that opposes the relative movement of objects in contact. The type of surface changes how much friction there is between two objects.
  • Speed is the distance an object travels in a given time and can be measured in kilometres per hour (km/h) or metres per second (m/s). 
  • Speed can be described as fast, slow, changing (increasing or decreasing), or constant.
  • Leonardo da Vinci (1452–1519) studied the laws of friction and motion through mechanical designs and observations. His notebooks contain early insights into physics and engineering. See Technology Learning Area for further reference.
  • Note: Students at this level are not expected to calculate speed. Shorthand for units of speed is not required. Focus should be on describing, comparing, and observing movement and forces using everyday language and observable features (e.g. fast, slow, constant, changing).

Non-contact forces
(See Year 2, Materials)

  • Some forces need contact between two objects, but non-contact forces can act at a distance.
  • Magnetic force is a non-contact force that can pull or push.
  • Magnets have two poles (north and south). Opposite poles attract (north/south), and like poles repel (north/north or south/south). 
  • Magnets attract some metals (e.g. iron). Not all metals are attracted to magnets.
  • Gravity is a non-contact force that pulls objects towards the centre of the Earth.
  • Weight is the force of gravity acting on an object due to its mass.
  • Note: at this level, units for mass are expected (e.g. kilogram, tonne) but not units for weight (newton, N).
  • William Gilbert (1544–1603) studied magnetism and non-contact forces. He coined the term ‘electricity’. 

Simple machines 

  • Simple machines (e.g. levers, pulleys, ramps) make it easier to move objects by reducing the amount of force needed or increasing the force able to be applied.

Fluids, resistance, and buoyancy 
(See Year 5, Materials)

  • Fluids are either liquids or gases. 
  • Fluids exert a pushing force, called resistance, on objects that move through them.
  • Drag (air resistance) opposes the movement of objects moving through gases (e.g. parachute).
  • Drag (water resistance) opposes the movement of objects moving through water (e.g. a hoe (paddle) on a waka).
  • Buoyancy is an upwards force exerted by a liquid on an object (e.g. a ship).
  • Buoyant force depends on the density of the fluid and the object. 
    • An object floats when the upward buoyant force from the liquid is equal to or greater than the object’s weight. An object will sink if the buoyant force is less than the object’s weight.
    • Denser fluids exert a greater buoyant force. Saltwater is denser than fresh water, which is why objects float higher and more easily in salt water.
  • Buoyancy does not explain all movement in water (e.g. flowing water can move rock and soil fragments by pushing them, not by buoyancy). 
  • Archimedes (c.287–212 BCE) formulated the principle of buoyancy.
  • Note: Measurable quantities should be interpreted through relative comparison rather than absolute measurement.

Contact forces and movement

  • Illustrating forces using force-arrow diagrams
  • Comparing the time taken and distance travelled by objects, identifying which is faster or slower
  • Predicting and testing how push and pull forces of different size or direction affect the movement of objects (e.g. fish, rockets)
  • Observing and describing the movement of by referring to direction and speed
  • Investigating how different surfaces (e.g. sandpaper, tabletop, carpet) affect friction by predicting, testing, and explaining movement

Non-contact forces

  • Predicting and explaining magnetic interactions based on pole orientation, linking predictions to observed effects and using the language of attraction and repulsion
  • Comparing how non-contact forces affect the movement of objects, focusing on qualitative observations (e.g. direction, speed)
  • Describing non-contact forces using force-arrow diagrams

Simple machines

  • Conducting practical investigations using simple machines (e.g. levers, inclined planes, pulleys), identifying patterns in how they change force or motion, and interpreting these patterns to explain their function and everyday applications
  • Using models and demonstrations to explain how some mechanisms, including levers, pulleys, and gears, can change the direction of a force, reduce the effort needed, and/or increase the effect of a force
  • Designing and constructing simple machines (e.g. levers, pulleys, ramps)

Fluids, resistance, and buoyancy 

  • Testing how air and water resistance affect falling objects by:
    • designing basic fair tests that control for at least one variable
    • measuring the dependent variable (e.g. distance travelled, time taken)
    • explaining observed effects
  • Making and testing predictions about whether objects will float or sink in water, based on their properties

Earth Systems

States of matter in the atmosphere 

(See Year 4, Materials, and Matter Interactions and Energy)

  • The Sun transfers thermal energy to the Earth’s surface, warming the air, water, and land during the day.
  • Thermal energy from the Sun causes water to evaporate from rivers, lakes, oceans, soil, and plants.
  • Water is present in the air as an invisible gas called water vapour. 
  • When water vapour in the air cools, it condenses into liquid droplets and forms visible clouds. 
  • Changes of state (evaporation, condensation, and freezing) influence the weather (e.g. rain, fog, frost, snow, types of cloud cover).
  • Rain, snow, and hail occur when water in clouds changes state and falls to Earth. 
  • Rain, snow, and hail are called precipitation.
  • The movement of water through different states and between the Earth’s surface and the atmosphere is called the water cycle. 
  • John Dalton (1766–1844) proposed the hydrological cycle and atomic theory. His work in meteorology and chemistry advanced the understanding of weather and matter.
  • Note: See Social Science Learning Area — Geography strand.
     

Rocks and minerals

  • Soils are composed of decaying organisms, living organisms (including fungi, plants, and animals), rock particles, air, and water. 
  • Rocks are composed of minerals, which can be characterised by the size, shape, and colour of crystals.
  • Fossils are formed when organisms are buried in sediment and, over time, minerals replace the organic material.
  • James Hutton (1726–1797) formulated the Theory of the Earth, proposing that geological processes occur over vast timescales. 
     

States of matter in the atmosphere

  • Using diagrams to illustrate how water cycles between states as it moves from the surface of the Earth to the atmosphere and back again
     

Rocks and minerals

  • Classifying and comparing different types of soils (e.g. clay) and rocks based on observable features (e.g. fossils, crystals) and simple physical properties
     

Earth and Space

Matariki

  • Matariki is a star cluster that becomes visible in the eastern morning sky during mid-winter in New Zealand.
  • The visibility of Matariki in the morning sky is used as an indicator of seasonal change for many iwi.
  • Puanga (Rigel) is a star that rises shortly before Matariki and is more visible in some regions. It also serves as a seasonal indicator for many iwi.
  • The Matariki star cluster is known by many cultures, including as Makali‘i in Hawai‘i, Matarii in Tahiti, Subaru in Japan, and Pleiades in Greece.
  • Dr Pauline Harris (1970–) revitalised Māori astronomical star lore and contributed to Indigenous science education and astrophysics.

Earth, Moon, and Sun

  • The Earth, Moon, and Sun are roughly spherical.
  • Earth is tilted on its axis. As the Earth orbits the Sun, this causes different parts of the Earth to be angled towards or away from the sun, receiving more or less direct sunlight. This causes seasonal change. 
  • Seasons are associated with changing temperatures and length of daylight through the year.
  • The Moon orbits the Earth and reflects light emitted from the Sun (see Year 3, Matter Interactions and Energy).
  • The Moon appears to change shape (full, crescent, quarter, gibbous) in a regular waxing and waning pattern called the lunar cycle.
  • The lunar cycle occurs because the Moon orbits Earth, changing the portion of its sunlit surface that is visible from Earth depending on the relative positions of the Moon, Earth, and Sun.
  • The Moon rises and sets at slightly different times and places in the sky each day, following a regular 29.5-day cycle. 
  • The Maramataka is the traditional Māori lunar calendar based on cycles of the moon and stars. 

The Solar System 

  • The Earth is one of eight planets orbiting the Sun in the Solar System.
  • The order of the planets from the Sun is Mercury, Venus, Earth, Mars (the rocky planets) and Jupiter, Saturn, Uranus, Neptune (the gaseous planets).
  • The Solar System includes the Sun, planets, moons, asteroids, and comets.
  • The Solar System is located within the Milky Way galaxy. 
  • Celestial bodies are natural objects in space and include planets, moons, stars, comets, asteroids, nebula, and galaxies.
  • The Sun is a star that appears larger and brighter than others because it is closer to Earth. 
  • The Sun, Moon, and stars follow observable and predictable patterns that vary by location.
  • Understanding of the Solar System has evolved from a geocentric to a heliocentric model.
  • Accurate and detailed star charts have been created through direct human observations and instruments such as telescopes.
  • Many civilisations developed sophisticated astronomical knowledge (e.g. Babylonian, Chinese, Indian, Celtic, Polynesian).
  • Galileo Galilei (1564–1642) supported the heliocentric model with telescopic observations. He discovered moons of Jupiter and phases of Venus. Also demonstrated that density is a measurable property of matter and conducted experiments on falling bodies and motion. 

Matariki

  • Identifying annual changes in the position of Matariki and when they occur
  • Recognising and predicting the positioning of major constellations in the night sky
  • Relating the positioning of Matariki to seasonal and environmental patterns

Earth, Moon, and Sun

  • Observing and describing seasonal changes in nature and explaining how they connect to patterns in variations of sunlight and temperature (e.g. warm summers, cool winters)
  • Interpreting data on sunrise, sunset, and daylight length to identify seasonal patterns and predict changes across the year (e.g. longer summer days, shorter winter days)
  • Using diagrams to show the journey light takes from the Sun to the Earth directly and via reflection from the Moon
  • Using models to explain the movement of the Moon around the Earth and the Earth around the Sun

The Solar System 

  • Using models and simulations to investigate the relative size, spacing, and movement of celestial bodies in the Solar System
  • Observing and interpreting patterns in the apparent movement of the Sun, Moon, and stars from different locations on Earth
  • Communicating why changes in scientific models and improvements in technology are important for understanding the Solar System

Biological Science

Knowledge

The facts, concepts, principles, and theories to teach.

Practices

The skills, strategies, and applications to teach.

During Year 4

During Year 5

During Year 6

During Year 4

During Year 5

During Year 6

Organism Diversity

Taxonomy

  • The scientific classification system (or taxonomy) uses accepted criteria, including observable features, to divide organisms into categories and sub-categories.
  • Categories of organisms include animals, plants, fungi, and bacteria.
  • Animals can be vertebrate or invertebrate:
    • vertebrates include fish, amphibians, reptiles, birds, and mammals
    • invertebrates include molluscs (snails and slugs), worms, spiders, and insects.
  • Plants include flowering plants (including grasses) and non-flowering plants (ferns and mosses).
  • A species is a group of organisms that are the same kind and can have offspring together. These offspring can also grow up and have their own offspring.
  • Organisms have a scientific name, based on their species (e.g. humans’ scientific name is Homo sapiens).
  • Some organisms can only be observed through a microscope, not with the naked eye. These are called microorganisms.  
  • Fungi are a diverse group of organisms that include mushrooms, moulds, and yeasts, each with unique structures. 
  • Bacteria are microorganisms that are found everywhere on Earth and can be beneficial (e.g. in the human digestive system), neutral, or harmful (e.g. germs) to humans.
  • There are many plants and animals that are now extinct.
  • Organisms that have very different observable features (that look different) are less likely to be closely related. 
  • Organisms that have very similar observable features (that look alike) are often closely related.
  • Carl Linnaeus (1707–1778) developed a system for classifying organisms by type and habitat. His binomial nomenclature system is still used in taxonomy today.

Reproductive strategies

  • Organisms have different strategies to enable them to successfully reproduce.
  • Fruits develop from flowers.
  • Seeds have specialised parts that aid in dispersal (e.g. wings, hooks, fleshy coatings).
  • Animals, plants, and fungi reproduce in different ways, including laying eggs, giving birth to live young, and producing seeds or spores.
  • Some types of organisms produce many offspring (e.g. wētāpunga, mice), while others produce few (e.g. humans, kiwi).
  • Some organisms can reproduce from parts of themselves (e.g. potato offcuts, stem cuttings).
  • Note: Students at this level are not expected to understand the r/K model.

Evolution and inheritance

  • Offspring inherit characteristics from their parents, but there is variation among offspring (they are not identical to their parents).
  • Organisms that are better adapted to their environment are more likely to survive to reproduce. This is called natural selection.
  • Natural selection means that over generations, certain inherited characteristics become more or less common in a population.
  • Over a very long period of time, the process of natural selection can lead to the evolution of new species (e.g. kākā, kea, and kākāpō evolved from a shared ancestor into forest, alpine, and nocturnal parrot species).
  • Fossils provide evidence that organisms have changed over millions of years.
  • All organisms share common ancestors. Over long periods of time, those ancestors have gradually evolved into different species.
  • Scientists try to understand what the family tree of all organisms (the ‘tree of life’) looks like by studying fossils and the physical features of species.
  • Joan Wiffen (1922–2009) discovered the first dinosaur fossils in New Zealand. Her work changed the understanding of prehistoric life in the region.
  • Note: At this stage, students are not expected to understand how genes and chromosomes work.

Taxonomy

  • Classifying animals as vertebrates or invertebrates
  • Classifying plants as flowering or non-flowering
  • Identifying and grouping common types of fungi based on observable characteristics

Reproductive strategies

  • Investigating how fruits develop from flowers as part of a plant’s reproductive process
  • Identifying and explaining how different seed structures support dispersal by wind, water, or animals
  • Classifying organisms based on how they reproduce (e.g. egg-laying, live birth, seed production)
  • Comparing different reproductive strategies in animals, plants, and fungi

Evolution and inheritance

  • Using cause-and-effect language to explain how natural selection could lead to particular characteristics becoming more common in a population over time (e.g. long necks in giraffes, sweet berries on a kawakawa)
  • Using fossil evidence to infer how organisms have changed over time
  • Communicating using diagrams (e.g. tree of life) how different species are related through common ancestors (e.g. kākā, kea, kākāpō)

Body Systems

Digestion

  • Animals’ digestive systems break down food and absorb nutrients for fuel and growth.
  • The human digestive system has parts, and the structure of each part relates to its function, including:
    • mouth
    • teeth (incisors, canines, premolars, and molars, which all have different functions)
    • tongue 
    • oesophagus 
    • stomach 
    • liver 
    • small intestine
    • large intestine
    • rectum.
  • Bacteria can aid digestion by breaking down and helping absorb food.

Reproduction
(See Year 2, Organism Diversity)

  • All living organisms reproduce. 
  • Sexual reproduction involves two parents (e.g. humans, birds, flowering plants) and produces offspring that exhibit a mix of both parents’ characteristics.
  • Asexually produced offspring are copies of their parent (potato tubers, yeast budding, strawberry plants through runners).
  • Animals reproduce sexually through:
    • sperm and egg formation
    • fertilisation.
  • Flowering plants reproduce sexually through:
    • pollination
    • fertilisation (seed formation)
    • seed dispersal
    • germination.
  • Most fungi reproduce sexually, involving:
    • fertilisation
    • fruiting bodies (e.g. mushrooms)
    • spore formation 
    • dispersal 
    • germination.

Interconnected systems (digestive, respiratory, circulatory)

  • The respiratory system allows animals to take in oxygen, which they need to live, and exchange it for carbon dioxide. This is called breathing.
  • Air is a mixture of gases such as nitrogen, carbon dioxide, oxygen, and water vapour.
  • The human respiratory system includes the trachea, lungs, diaphragm, ribs, and intercostal muscles. The structure of each part supports its role in breathing (e.g. the ribs form a protective cage, while the diaphragm and intercostal muscles draw air into the chest cavity).
  • Some animals, like fish, respire using gills, which take oxygen out of water.
  • The circulatory system transports nutrients and gases throughout the body.
  • The human circulatory system moves blood around the body and includes the heart, blood, and blood vessels. The structure of these parts relates to their function.
  • The digestive, respiratory, and circulatory systems work together to supply oxygen, water, and nutrients to the human body.
  • William Harvey (1578–1657) discovered the modern pulmonary system and circulation of blood. His experiments laid the foundation for cardiovascular physiology.
  • Note: Detailed anatomical knowledge such as the names of heart chambers, valves, and specific blood vessels (arteries, veins, capillaries) and formal classification of cell types are not required.

Digestion

  • Identifying parts of the human digestive system and explaining their functions
  • Comparing the structure and function of different types of human teeth
  • Tracking the pathway of food through the digestive system using diagrams or physical representations and explaining how the structure and function of each part aids digestion

Reproduction

  • Investigating the advantages and disadvantages of sexual and asexual reproduction (e.g. strawberry runners vs strawberry fruit)
  • Sequencing and comparing the stages of reproduction in animals, flowering plants, and fungi to identify similarities and differences

Interconnected systems (digestive, respiratory, circulatory)

  • Using diagrams to explain how the respiratory and circulatory systems interact to transport gases and nutrients throughout the body
  • Investigating how the respiratory and circulatory systems respond to the body’s needs (e.g. measuring how heart and breathing rate changes in response to exercise and recording and presenting relevant data)

Ecosystems

Relationships in an ecosystem

  • An ecosystem is a community of organisms interacting with each other and with their habitat (e.g. water, land, air).
  • Organisms in an ecosystem are interdependent and have roles that cycle matter through the system, for example:
    • a producer makes sugars through photosynthesis
    • a consumer eats plants or other animals for sugars and other nutrients
    • a decomposer breaks down dead organisms, returning nutrients to the soil.
  • There is a range of ways to describe relationships between organisms in an ecosystem, for example:
    • a predator is an organism that hunts and eats other organisms
    • prey are organisms that are hunted and eaten by predators
    • in mutualism, two organisms benefit from helping each other (e.g. bees and flowers)
    • in parasitism, one organism benefits while the other is harmed (e.g. fleas on a dog).
  • Soils are composed of decaying organisms, living organisms (including fungi, plants, and animals), rock particles, air, and water.
  • Arthur Tansley (1871–1955) introduced the concept of the ecosystem, integrating organisms and their environment into ecological studies.
     

Relationships in an ecosystem

  • Applying ecosystems concepts to known and unknown examples to identify interdependence of species within the ecosystem (e.g. food webs, plants need pollinators, animals need food and shelter) 
  • Categorising organisms in food webs as producers, consumers, or decomposers
  • Representing relationships in ecosystems using food webs

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