Water.  Water is the biological medium on Earth  All living organisms require water more than any other substance  Most cells are surrounded by water,

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Presentation transcript:

Water

 Water is the biological medium on Earth  All living organisms require water more than any other substance  Most cells are surrounded by water, and cells themselves are about 70–95% water  The abundance of water is the main reason the Earth is habitable

 The water molecule is a polar molecule: The opposite ends have opposite charges  Polarity allows water molecules to form hydrogen bonds with each other Oxygen is so electronegative that shared electrons spend more time around the O causing weak positive charges near the H’s

Hydrogen bond  – – H  + + H O — —  + +  + +  + +  – –  – –  – –

Cohesive behavior Ability to moderate temperature Expansion upon freezing Versatility as a solvent

 Cohesion = property of being held together by hydrogen bonds. The transport of water in plants relies upon cohesion of water molecules

Surface tension = measure of how difficult it is to stretch or break the surface of a liquid. (This phenomenon is related to cohesion)

 Water absorbs heat from warmer air and releases stored heat to cooler air  Water can absorb or release a large amount of heat with only a slight change in its own temperature

 A large body of water can have a moderating effect on climate. Lowering day time temperatures by absorbing heat and raising nighttime temps by releasing that stored heat.

 A calorie (cal) is the amount of heat required to raise the temperature of 1 g of water by 1°C  The specific heat of a substance is the amount of heat that must be absorbed or lost for 1 g of that substance to change its temperature by 1ºC  Water resists changing its temperature because of its high specific heat

 Evaporation is transformation of a substance from liquid to gas  Heat of vaporization is the heat a liquid must absorb for 1 g to be converted to gas  As a liquid evaporates, its remaining surface cools, a process called evaporative cooling  Evaporative cooling of water helps stabilize temperatures in organisms and bodies of water

 Ice floats in liquid water because hydrogen bonds in ice are more “ordered,” making ice less dense  If ice sank, all bodies of water would eventually freeze solid, making life impossible on Earth

 A solution is a liquid that is a homogeneous mixture of substances  A solvent is the dissolving agent of a solution  The solute is the substance that is dissolved  An aqueous solution is one in which water is the solvent  A hydrophilic substance is one that has an affinity for water  A hydrophobic substance is one that does not have an affinity for water  Oil molecules are hydrophobic because they have relatively nonpolar bonds

Water is a versatile solvent due to its polarity, which allows it to form hydrogen bonds easily When an ionic compound is dissolved in water, each ion is surrounded by a sphere of water molecules called a hydration shell

A hydrogen atom in a hydrogen bond between two water molecules can shift from one to the other: The hydrogen atom leaves its electron behind and is transferred as a proton, or hydrogen ion (H + ) The molecule with the extra proton is now a hydronium ion (H 3 O + ), though it is often represented as H + The molecule that lost the proton is now a hydroxide ion (OH – ) Water is in a state of dynamic equilibrium in which water molecules dissociate at the same rate at which they are being reformed

 An acid is any substance that increases the H + concentration of a solution  A base is any substance that reduces the H + concentration of a solution  pH scale

 Buffers are substances that minimize changes in concentrations of H + and OH – in a solution

 Acid precipitation refers to rain, snow, or fog with a pH lower than 5.6  Acid precipitation is caused mainly by the mixing of different pollutants with water in the air and can fall at some distance from the source of pollutants  Acid precipitation can damage life in lakes and streams  Effects of acid precipitation on soil chemistry are contributing to the decline of some forests

Fig More acidic 0 Acid rain Acid rain Normal rain More basic