Water and Life (Chapter 3)
Concept 3.1: Polar covalent bonds in water molecules result in hydrogen bonding
Water is a polar molecule due to oxygen's higher electronegativity, creating partial negative and positive charges.
This polarity enables water molecules to form hydrogen bonds with each other.
Hydrogen bonding is fundamental to water's emergent properties that support life.
Concept 3.2: Four emergent properties of water contribute to Earth’s suitability for life
Cohesive behavior: Water sticks to itself (cohesion) and other molecules (adhesion) due to hydrogen bonding, essential for water transport in plants.
Ability to moderate temperature: Water has a high specific heat () and high heat of vaporization. Hydrogen bonds absorb heat when they break and release heat when they form, allowing water to resist temperature changes and stabilize environments and organisms.
Expansion upon freezing: Ice is less dense than liquid water because hydrogen bonds form a stable, open hexagonal lattice, causing ice to float. This insulates aquatic environments, allowing life to survive below.
Versatility as a solvent: Water's polarity allows it to dissolve many ionic and polar substances (hydrophilic materials) through hydrogen bonding, making it the solvent of life. Non-polar substances (hydrophobic materials) do not dissolve.
Solution concentration is often measured in molarity ().
Concept 3.3: Acidic and basic conditions affect living organisms
Water molecules can dissociate into hydrogen ions (H+ or hydronium, H3O+) and hydroxide ions (OH−).
In pure water, at dynamic equilibrium.
Acids increase H+ concentration, while bases decrease it (often by increasing OH−).
The pH scale measures H+ concentration: .
For any aqueous solution, . pH values less than 7 are acidic, greater than 7 are basic, and 7 is neutral. Each pH unit represents a tenfold change in H+ concentration.
Buffers are substances that resist pH shifts, maintaining stability crucial for biological systems.
Ocean acidification is caused by human-generated CO2 dissolving in seawater to form carbonic acid (CO2 + H2O ⇌ H2CO3 ⇌ H+ + HCO3−), increasing H+ and reducing carbonate ions (CO3^2−) needed by marine calcifiers like corals.