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Water and Life: Properties, Structure, and Biological Importance

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Water and Life

Overview: The Molecule That Supports All of Life

Water is the essential biological medium on Earth, making up 70–95% of most cells and surrounding them. Its abundance is a primary reason Earth is habitable, and it is unique in existing naturally in all three physical states: solid, liquid, and gas. All living organisms require water more than any other substance.

The Structure of Water Molecules

Polarity and Hydrogen Bonding

Water molecules are polar, meaning their opposite ends have opposite charges. This polarity enables water molecules to form hydrogen bonds with each other, which are weaker than covalent bonds but crucial for water's properties. Hydrogen bonds break and reform rapidly, giving water a higher organizational structure.

  • Polar covalent bonds within water molecules create regions of partial positive and negative charge.

  • Hydrogen bonds form between the hydrogen of one water molecule and the oxygen of another.

  • These interactions are responsible for water's unique properties.

Hydrogen Bonds Between Water Molecules

Emergent Properties of Water

Four Properties That Facilitate Life

Water's structure gives rise to four emergent properties that are critical for life:

  • Cohesion and adhesion

  • Ability to moderate temperature

  • Expansion upon freezing

  • Versatility as a solvent

Cohesion and Adhesion

Cohesion refers to the attraction between water molecules due to hydrogen bonding, which helps transport water against gravity in plants. Adhesion is the attraction between water and other substances, such as plant cell walls or the meniscus in a graduated cylinder.

  • Cohesion enables water transport in plants.

  • Adhesion assists water movement along surfaces.

Water Transport in Plants

Heat and Temperature

Kinetic energy is the energy of motion, and heat is the total kinetic energy due to molecular motion. Temperature measures the intensity of heat, reflecting the average kinetic energy of molecules. Water absorbs and releases heat with minimal temperature change, moderating Earth's climate.

  • Calorie (cal): Heat required to raise 1 g of water by 1°C.

  • Joule (J): 1 J = 0.239 cal; 1 cal = 4.184 J.

Water’s High Specific Heat

The specific heat of water is 1 cal/g/°C, much higher than many substances (e.g., stainless steel: 0.11 cal/g/°C). This property is due to hydrogen bonding: heat is absorbed to break bonds and released when bonds form. Water's high specific heat stabilizes temperature, supporting life.

Evaporative Cooling

Evaporation transforms liquid to gas, requiring energy. The heat of vaporization for water is 580 cal/g at 25°C. As water evaporates, the surface cools, stabilizing temperatures in organisms and bodies of water (e.g., sweating).

Insulation by Floating Ice

Ice floats because hydrogen bonds in ice are more ordered, making it less dense than liquid water. Water reaches its greatest density at 4°C. If ice sank, bodies of water would freeze solid, threatening life.

Ice: Crystalline Structure and Floating Barrier

Water as a Solvent

Solution, Solvent, and Solute

A solution is a homogeneous mixture of substances. The solvent is the dissolving agent, and the solute is the substance dissolved. An aqueous solution uses water as the solvent.

Versatility as a Solvent

Water's polarity allows it to dissolve ionic compounds and polar molecules. When an ionic compound dissolves, each ion is surrounded by a hydration shell of water molecules.

Table Salt Dissolving in Water

Dissolving Nonionic Polar Molecules

Water can also dissolve nonionic polar molecules, including large molecules like proteins, if they have ionic and polar regions.

A Water-soluble Protein

Hydrophilic and Hydrophobic Substances

A hydrophilic substance has an affinity for water, while a hydrophobic substance does not. Oil molecules are hydrophobic due to nonpolar bonds. A colloid is a stable suspension of fine particles in a liquid.

Solute Concentration in Aqueous Solutions

Most biochemical reactions occur in water, and their rates depend on solute concentration. Molarity (M) is the number of moles of solute per liter of solution.

  • 1 mole (mol): 6.02 × 1023 molecules (Avogadro’s number).

  • Molecular mass: Sum of all atomic masses in a molecule.

Acidic and Basic Conditions

Dissociation of Water

A hydrogen atom in a hydrogen bond can shift between water molecules, forming hydronium (H3O+) and hydroxide (OH–) ions. This dissociation, though rare, significantly affects biological systems.

pH and Its Effects

pH measures the concentration of H+ ions in solution. Changes in H+ and OH– concentrations can drastically affect cell chemistry. Acids increase H+ concentration; bases decrease it.

  • Acid: Increases H+ concentration (e.g., HCl → H+ + Cl–).

  • Base: Reduces H+ concentration (e.g., NaOH → Na+ + OH–).

The pH Scale

In aqueous solution at 25°C, the product of H+ and OH– concentrations is constant:

  • Neutral solution: , pH = 7

Acidic solutions have pH < 7; basic solutions have pH > 7. Most biological fluids have pH 6–8. Each pH unit represents a tenfold change in H+ concentration.

The pH Scale and pH Values of some Aqueous Solutions

Buffers

Buffers minimize changes in H+ and OH– concentrations, maintaining pH near 7 in living cells. Most buffers consist of an acid-base pair that reversibly combines with H+ (e.g., carbonic acid system: ).

  • Example: Tums as a pH neutralizer.

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