Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby...

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Transcript of Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby...

Page 1: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.
Page 2: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock. The properties of liquids are related to intermolecular interactions. You will learn about some of the properties of liquids.

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Page 3: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.
Page 4: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

A Model for Liquids

What factors determine the physical properties of a liquid?

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Page 5: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Substances that can flow are referred to as fluids. Both liquids and gases are fluids.

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Page 6: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

The interplay between the disruptive motions of particles in a liquid and the attractions among the particles determines the physical properties of liquids.

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Page 7: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Evaporation

What is the relationship between evaporation and kinetic energy?

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Page 8: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

The conversion of a liquid to a gas or vapor is called vaporization.

When such a conversion occurs at the surface of a liquid that is not boiling, the process is called evaporation.

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Page 9: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

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In an open container, molecules that evaporate can escape from the container.

Page 10: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

In a closed container, the molecules cannot escape. They collect as a vapor above the liquid. Some molecules condense back into a liquid.

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Page 11: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

During evaporation, only those molecules with a certain minimum kinetic energy can escape from the surface of the liquid.

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Page 12: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Animation 15 Observe the phenomenon of evaporation

from a molecular perspective.

Page 13: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Vapor Pressure

When can a dynamic equilibrium exist between a liquid and its vapor?

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Page 14: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Vapor pressure is a measure of the force exerted by a gas above a liquid.

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Page 15: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

In a system at constant vapor pressure, a dynamic equilibrium exists between the vapor and the liquid. The system is in equilibrium because the rate of evaporation of liquid equals the rate of condensation of vapor.

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Page 16: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Vapor Pressure and Temperature Change

An increase in the temperature of a contained liquid increases the vapor pressure.

The particles in the warmed liquid have increased kinetic energy. As a result, more of the particles will have the minimum kinetic energy necessary to escape the surface of the liquid.

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Page 17: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

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Page 18: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Vapor Pressure Measurements

The vapor pressure of a liquid can be determined with a device called a manometer.

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Page 19: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Manometer

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Page 20: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Boiling Point

Under what conditions does boiling occur?

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Page 21: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

When a liquid is heated to a temperature at which particles throughout the liquid have enough kinetic energy to vaporize, the liquid begins to boil.

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Page 22: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

The temperature at which the vapor pressure of the liquid is just equal to the external pressure on the liquid is the boiling point (bp).

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Page 23: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Boiling Point and Pressure Changes

Because a liquid boils when its vapor pressure is equal to the external pressure, liquids don’t always boil at the same temperature.

At a lower external pressure, the boiling point decreases.

At a higher external pressure, the boiling point increases.

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Page 24: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Altitude and Boiling Point

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Page 25: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

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Page 26: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Animation 16 Relate vapor pressure and boiling point to

intermolecular attractive forces.

Page 27: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

Normal Boiling Point

Because a liquid can have various boiling points depending on pressure, the normal boiling point is defined as the boiling point of a liquid at a pressure of 101.3 kPa.

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Page 28: Hot lava oozes and flows, scorching everything in its path, and occasionally overrunning nearby houses. When the lava cools, it solidifies into rock.

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