Freezing and Melting of Water

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Freezing and Melting of Water

Introduction

The water molecule (H2O) is formed by one atom of oxygen, bound to two atoms of hydrogen. The hydrogen atoms are "attached" to one side of the oxygen atom, resulting in a water molecule having a positive charge on the side where the hydrogen atoms are and a negative charge on the other side, where the oxygen atom is. Since opposite electrical charges attract, water molecules tend to attract each other. All these water molecules attracting each other mean they tend to clump together.

Earth's water (about 70 percent of the Earth's surface is water-covered) is constantly interacting, changing, and in movement.

The freezing temperature (the temperature that a substance turns from a solid to a liquid) is 0o on the Celsius scale, and 100o is water's boiling point (at sea level; 1 atmosphere pressure, 76mm Hg or 101.3 KPa.).

Another important characteristic is that water has a high specific heat index. This means that it can absorb a lot of heat before it begins to get hot. The high specific heat index of water helps regulate the rate at which air changes temperature, which is why the temperature change between seasons is gradual rather than sudden, especially near the oceans.

Aim

To investigate the cooling and warming behaviour of water. By examining graphs of the data, the freezing and melting temperature were determined and compared.
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Apparatus

* LabPro

* TI Graphing Calculator

* DataMate Program

* Temperature Probe

* Ring stand

* Utility clamp

* 400-ml beaker

* 10-ml graduated cylinder

* test tube

* salt

* ice

* water

Procedure

Part I Freezing

. A 400-ml beaker was filled 1/3 full with ice, then 100-ml of water was added

2. 5-ml of water was put into a test tube and a utility clamp was used to fasten the test tube to a ring stand. The ...

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