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THE PHYSICAL EDITION

Warmth and Ice

Vince packs ice for a picnic, discovers a wet hand and tries a towel to help the ice last. Follow the same water as it melts, pours into round wells and becomes ice again the next morning.

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Explore the science

Solid water keeps a shapePages 1–2

Vince packs two matching closed tubs, with two ice cubes in each. A spare cube sits separately in the ice tray. Ice is solid water. The pieces keep their own block shapes while frozen, unlike the liquid water Vince will pour later.

Ask together: What shapes can you see in the tubs?

Warm contact and meltingPages 3–4

Vince holds the spare cube over a dish. A closer view shows meltwater on his palm and a drop falling below it. Energy transfers from his warmer hand to the colder ice, helping it melt while his hand cools. Warmer air and surfaces can melt ice too.

Ask together: Where is the water on Vince’s hand coming from?

A question to tryPages 5–6

Vince brings both tubs together to the garden table. A folded towel lies beside them. His wet-hand discovery gives him a reason to wonder whether the picnic ice will last. He is about to try wrapping one tub; this scene does not yet show a result.

Ask together: What do you think Vince could try with the towel?

Comparing wrapped and barePages 7–8

Vince folds a thick towel beneath, around and over one closed tub. The matching tub beside it stays bare. A thick, dry wrap can slow energy transfer from warmer surroundings to colder ice. Keeping the starting ice, tubs, place and waiting time alike makes the wrap the important difference to compare.

Ask together: What is the same about the two tubs, and what has Vince changed?

Insulation slows meltingPages 9–10

After setting out the picnic, Vince opens both tubs. Some ice has melted in each, but larger pieces remain in the tub he wrapped. The wrap has slowed melting; it has not made new ice or stopped all change. These pictured amounts illustrate the difference rather than report a measured trial.

Ask together: What differences can you see inside the two tubs?

Liquid flow and a new shapePages 11–12

Later, the ice in both tubs has melted. Vince pours water from the formerly wrapped tub into the round wells of a mould. The wrap did not keep the ice forever. It is still the same water, now a liquid that flows into the lower part of each well.

Ask together: What can this water do that the hard blocks could not?

Trying to make ice againPages 13–14

Vince slides the mould into the lower freezer drawer. Its four round wells contain shallow water with space below the rims. A working freezer removes energy from the water. If the water cools enough, it can freeze; the change needs time. The space above it leaves room for expansion.

Ask together: What do you think Vince will find when he comes back?

Freezing into a new shapePages 15–16

The next morning, three round pieces of ice remain in the mould and one rests on a saucer beside it. One well is empty. The meltwater has become solid again. The new pieces have the round outlines of the wells, and the piece on the saucer keeps that shape. It is still water, even though its form and shape have changed.

Ask together: How is this ice like the ice at the start, and how is it different?

Sources and evidence
  1. Solid ice keeps a shape of its own; when it melts, the same material is liquid water that can flow and take the shape of the lower part of its container.

    Lesson 2.5: Changing State—Melting
    Key Concepts; Engage, Step 2: Where do you think the energy came from to melt the ice?; Explore, Step 3: How could you set up an experiment to test your method?: Melting changes a solid into liquid. Air and a supporting surface can supply energy to colder ice. The lesson suggests hand contact as a way to warm ice, and recommends similar starting pieces when comparing treatments.

    Taking the Shape of the Container
    Answer by Tamara, paragraphs on ice and liquids, published 22 October 2007: The explanation contrasts stiff solid ice with flowing liquid water. Gravity draws the water downward while the vessel confines it. This supports pouring meltwater into new wells and later observing solid pieces whose outer shapes come from those wells.

    Liquid water flows into the lower part of a container; it does not fill all the available space as a gas would.

    Ice keeps its own shape while frozen, but that shape gradually changes as it melts. The material is still water.

  2. Energy transfers from Vince's warmer hand and warmer surroundings toward colder ice, helping it melt. His hand loses energy during contact, so the ice can feel cold while his palm becomes wet.

    Lesson 2.5: Changing State—Melting
    Key Concepts; Engage, Step 2: Where do you think the energy came from to melt the ice?; Explore, Step 3: How could you set up an experiment to test your method?: Melting changes a solid into liquid. Air and a supporting surface can supply energy to colder ice. The lesson suggests hand contact as a way to warm ice, and recommends similar starting pieces when comparing treatments.

    This scene shows brief contact and meltwater, not a timed test of how quickly a hand melts ice.

    Warmer air and surfaces can also transfer energy to ice. Touching it is not necessary for melting.

    Heat is a transfer of energy, not a visible substance. The visible drops are melted ice.

    The handled cube stays separate from the ice used for the wrapped-versus-bare comparison.

  3. A sufficiently thick dry insulating wrap around a closed ice container can slow transfer from warmer surroundings, leaving more ice after the same interval than an otherwise matching bare container.

    Activity – Be Cool... with Insulation!
    Materials; Procedure, steps 1–3; How does it work?; Safety Suggestions: The activity compares ice inside covered containers with and without insulating material; socks are an example. It calls for approximately equal starting ice. Warmer surroundings supply energy to the ice. Materials from the activity should not be consumed.

    The pictured amounts are illustrative, not measured results.

    A thick, dry wrap can slow heat transfer to colder ice. It does not make cold or prevent melting forever.

    The towel stays outside the closed tub, separate from the meltwater.

  4. After the meltwater is cooled sufficiently in a working freezer, it can become solid ice again; round mould wells give the new solid pieces round outer shapes.

    Lesson 2.4: Changing State—Freezing
    Key Concepts; Engage, Step 1: Teacher Preparation; Explain, steps 4–5: Water becomes solid ice when cooled sufficiently. A teacher demonstration places a small quantity of water in a freezer overnight and observes it the next day. Freezing expands the water, so an open flexible tray with headroom is appropriate. The source does not promise a universal freezing time.

    Taking the Shape of the Container
    Answer by Tamara, paragraphs on ice and liquids, published 22 October 2007: The explanation contrasts stiff solid ice with flowing liquid water. Gravity draws the water downward while the vessel confines it. This supports pouring meltwater into new wells and later observing solid pieces whose outer shapes come from those wells.

    Pump Up Your Savings with Heat Pumps
    How They Work, opening paragraph: Refrigeration uses electrical work to move thermal energy out of the cooled space. Combined with the freezing source, this supports explaining that the freezer removes energy from the water; it does not add a substance called cold.

    A freezer removes energy from water; it does not add a substance called cold.

    Freezing depends on the water amount, starting temperature and freezer conditions. The next-morning scene does not promise a universal freezing time.

    Water expands as it freezes, so the partly filled, freezer-safe mould leaves room below its rims.

    The open round wells produce shallow round pieces, not spheres. Freezing changes the water’s form; it does not restore the original square cubes.

    This exploratory meltwater and refrozen ice are kept separate from food and drinks.

  5. A useful wrapped-versus-bare comparison changes the wrap while keeping the other important starting conditions alike.

    Lesson 2.5: Changing State—Melting
    Key Concepts; Engage, Step 2: Where do you think the energy came from to melt the ice?; Explore, Step 3: How could you set up an experiment to test your method?: Melting changes a solid into liquid. Air and a supporting surface can supply energy to colder ice. The lesson suggests hand contact as a way to warm ice, and recommends similar starting pieces when comparing treatments.

    Activity – Be Cool... with Insulation!
    Materials; Procedure, steps 1–3; How does it work?; Safety Suggestions: The activity compares ice inside covered containers with and without insulating material; socks are an example. It calls for approximately equal starting ice. Warmer surroundings supply energy to the ice. Materials from the activity should not be consumed.

    A useful comparison begins with similar ice pieces at the same temperature in matching closed tubs, kept together for the same interval. Only one tub is wrapped.

    The illustrations show a qualitative comparison, not a measured experiment or a guarantee that every wrap will perform the same way.

Water and Wind

Water and Wind, pages 1–2: Wind moves the pinwheel.

Spread 1 / 12

Wind tickles my cheek. Round goes my pinwheel.

Explore the science

Wind & forcesPages 1–2

Wind moves the pinwheel. Wind is moving air. Vince feels it on his cheek and sees it push the pinwheel's angled blades.

Ask together: What tells you that the air is moving?

Currents & eddiesPages 3–4

Water passes the rock. A leaf circles behind it. Most water passes the rock; some circles back in an eddy. Laminar flow is orderly; turbulence is irregular, mixing motion. A swirl alone cannot distinguish them.

Ask together: How does the leaf move compared with the water passing the rock?

Waves & energyPages 5–6

Waves spread from the stream. The duck bobs. The falling stream makes waves that carry energy outward and make the toys bob. The stream's current also carries toys along. Bobbing and drifting are different motions.

Ask together: What moves up and down? What moves along the pond?

BuoyancyPages 7–8

A duck floats. A pebble sinks. Water pushes upward on both objects. This buoyancy balances the duck's weight, but not the pebble's. The pebble's splash makes the rings on the next spread.

Ask together: Where is each object compared with the surface?

When waves meetPages 9–10

Two wave patterns approach one another. When gentle waves overlap, their heights add, briefly raising or lowering the surface. This interference does not erase the waves; they continue through one another.

Ask together: What might happen where the two patterns meet?

Surface tensionPages 11–12

Tiny dents appear beneath the strider’s legs. Surface tension helps support the strider where its water-repellent legs dent the water. The duck floats mainly by displacing water.

Ask together: What do you notice where its legs meet the water?

Suction & pressurePages 13–14

The duck bubbles, fills and squirts. Squeeze underwater: air bubbles out. Release with the opening submerged: the elastic duck springs back, lowering pressure inside. The surrounding water pressure pushes water in. Squeeze above water: water exits through that same opening.

Ask together: What changes when Vince squeezes and then lets go?

Lift & gravityPages 15–16

A paper plane glides forward and down. The throw starts the plane moving. Airflow around its wings produces lift and turns air downward. Gravity pulls down; drag resists motion. In still air, the plane glides forward and gradually descends.

Ask together: Where might the plane go next?

ViscosityPages 17–18

Milk runs. Honey stretches into a thread. Honey's greater viscosity means greater resistance to flow. It makes a slow thread while milk runs readily. Temperature and pouring method also matter; this snack is an observation, not a controlled test.

Ask together: How do the milk and honey move differently?

Draining & swirlingPages 19–20

Foam curves inward toward the drain. Gravity drives water through the drain. Existing turning motion can become a curved inward flow, traced by foam. Here water travels to the outlet, unlike waves crossing the pond. Not every drain swirls.

Ask together: Can you follow the foam toward the drain?

Scientific observationPages 21–22

Vince sketches what he noticed. Vince records something he noticed. Drawings, marks or words let him return to an observation. He does not need all the answers.

Ask together: Which earlier picture matches one of his drawings?

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