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Chapter 3: Water and the Fitness of the Environment
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Water
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Water A common but exceptional substance
Makes life as we know it possible on Earth Organisms composed mainly of water (70-95%) and live in an environment dominated by water (75% of surface) Life on Earth began in water and evolved there for 3 billion years before spreading onto land Water is the only common substance to exist in all 3 physical states (solid, liquid, gas)
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Figure 3.5x1 Ice, water, and steam
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Hydrogen Bonding/Polarity
Polar covalent bonds between oxygen and hydrogen due to oxygen’s high electronegativity Note the bent shape of a water molecule Anomalous properties of water arise from attractions between polar molecules CD-ROM Activity 3A
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Figure 3.1 Hydrogen bonds between water molecules
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Important Properties of Water
Cohesive behavior Ability to stabilize temperature Expansion upon freezing Versatility as a solvent
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Cohesion Cohesion Adhesion Surface Tension
Due to hydrogen bonding holding individual molecules together Hydrogen bonds are made and broken with great frequency Contributes to the transport of water against gravity in a plant stem Adhesion Clinging of one substance to another Surface Tension A measure of how difficult it is to stretch or break the surface of a liquid
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Figure 3.3 Walking on water
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Stabilization of Temperature
Kinetic Energy - the energy of motion Heat - the total kinetic energy of a sample Temperature - the average kinetic energy of a sample Heat passes from warmer to cooler bodies until temperatures are equal Note an ice cube works by absorbing heat, not by adding coldness!
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Stabilization of Temperature
calorie – the amount of energy needed to increase the temperature of 1 gram of water 1 degree centigrade 1000 calories = 1 kilocalorie = 1 Calorie Specific Heat - the amount of energy needed to increase the temperature of 1 gram of a substance 1 degree centigrade
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Stabilization of Temperature
Water has a very high specific heat compared to most other substances Reason = hydrogen bonding Relevance to life on Earth – a large body of water can absorb and store a huge amount of heat from the sun during the daytime while only warming a few degrees; at night, the gradually cooling water can warm the air.
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Evaporative cooling
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Evaporative Cooling Heat of vaporization – the quantity of heat 1 gram of a liquid must absorb to be converted from a liquid to a gas Evaporative cooling – you are decreasing the average temperature because the hottest molecules are leaving
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Ice floats and frozen benzene sinks
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Expansion Upon Freezing
Ice is less dense than water due to packing caused by hydrogen bonding This keeps ice from sinking and bodies of water from freezing completely
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Figure 3.5 The structure of ice (Layer 2)
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Figure 3.6 Floating ice and the fitness of the environment
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Versatility as a Solvent
Solution A liquid that is a completely homogeneous mixture of two or more substances Solute The substance that is dissolved in a solution Solvent The dissolving agent of the solution Aqueous solution A solution in which water is the solvent
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Versatility as a Solvent
Sphere of hydration formed around dissolved particles Water is a versatile solvent, but not a universal solvent! Hydrophilic = water-loving Hydrophobic = lipid-loving Note: A compound does not have to be ionic to dissolve in water, it must be polar Molarity = moles of solute/liter of solution
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A crystal of table salt dissolving in water
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Dissociation of Water Molecules
2 H2O ↔ H3O OH- hydronium hydroxide ion ion Although the dissociation of water is reversible and statistically rare (1 in 554 million), it is exceedingly important in the chemistry of life.
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Ionization of water
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Dissociation of Water Molecules
H2O ↔ H OH- hydrogen hydroxide ion ion Water can be considered a very weak acid [H+] = 1 x 10-7M [OH-] = 1 x 10-7M
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Acids HCl → H+ + Cl- H2CO3 ↔ H+ + HCO3-
Acid = a substance that increases the hydrogen ion concentration of a solution HCl → H Cl- HCl is an example of a strong acid. It dissociates completely H2CO3 ↔ H HCO3- Carbonic acid is a weak acid that reversibly releases and reaccepts hydrogen ions
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Bases Base = a substance that reduces the hydrogen ion concentration of a solution Some bases do this by accepting a hydrogen atom NH3 + H+ ↔ NH4+ Some bases do this by dissociating to form hydroxide ions NaOH → Na+ + OH-
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pH For any solution: [H+] x [OH-] = 10-14
pH = -log [H+] Each pH unit represents a 10-fold difference in [H+] and [OH-] !!!!!!!! [H+] > [OH-] solution is acidic pH < 7 [H+] = [OH-] solution is neutral pH = 7 [H+] < [OH-] solution is basic pH > 7
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Figure 3.9 The pH of some aqueous solutions
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pH of Biological Systems
Most biological fluids are within the range of pH 6 to 8. An exception is the digestive juices of the stomach at pH 2. In biological systems, slight changes in pH can be harmful. Chemical processes within the body are very sensitive to the concentrations of H+ and OH– Ex: Blood pH is normally pH A person can survive only minutes if pH drops to 7 or is raised to 7.8 Therefore, biological systems rely on buffers to resist changes in pH.
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Buffers Buffers are substances that minimize the changes in concentrations of H+ and OH– Buffers work by accepting H+ from the solution when they are in excess and donating H+ to the solution when they have been depleted. Most buffers are composed of a weak acid and its corresponding base. H2CO3 ↔ H HCO3- (H+ donor) (H+ acceptor) acid base Le Chatelier’s Principle
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Acid Precipitation Rain, snow or fog with a pH below 5.6
Results from a reaction between water vapor and sulfur oxides or nitrogen oxides produced by the combustion of fossil fuels Destructive to aquatic systems such as ponds/May also cause serious harm to plants due to changes in soil pH
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Figure 3.10 The effects of acid precipitation on a forest
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Figure 3.10x2 Acid rain damage to statuary, 1908 & 1968
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